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Skeleton of an unusual, cat-sized marsupial relative (Metatheria: Marsupialiformes) from the middle Eocene (Lutetian: 44-43 million years ago) of Turkey

  • A. Murat Maga,

    Affiliations Division of Craniofacial Medicine, Department of Pediatrics, University of Washington, Seattle, Washington, United States of America, Department of Anthropology, University of Washington, Seattle, Washington, United States of America, Center for Developmental Biology and Regenerative Medicine, Seattle Children’s Research Institute, Seattle, Washington, United States of America

  • Robin M. D. Beck

    Affiliations School of Environmental and Life Sciences, University of Salford, Manchester, Salford, United Kingdom, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales, Australia

Skeleton of an unusual, cat-sized marsupial relative (Metatheria: Marsupialiformes) from the middle Eocene (Lutetian: 44-43 million years ago) of Turkey

  • A. Murat Maga, 
  • Robin M. D. Beck


9 Nov 2017: Maga AM, Beck RMD (2017) Correction: Skeleton of an unusual, cat-sized marsupial relative (Metatheria: Marsupialiformes) from the middle Eocene (Lutetian: 44-43 million years ago) of Turkey. PLOS ONE 12(11): e0188132. View correction


We describe a near-complete, three-dimensionally preserved skeleton of a metatherian (relative of modern marsupials) from the middle Eocene (Lutetian: 44–43 million years ago) Lülük member of the Uzunçarşıdere Formation, central Turkey. With an estimated body mass of 3–4 kg, about the size of a domestic cat (Felis catus) or spotted quoll (Dasyurus maculatus), it is an order of magnitude larger than the largest fossil metatherians previously known from the Cenozoic of the northern hemisphere. This new taxon is characterised by large, broad third premolars that probably represent adaptations for hard object feeding (durophagy), and its craniodental morphology suggests the capacity to generate high bite forces. Qualitative and quantitative functional analyses of its postcranial skeleton indicate that it was probably scansorial and relatively agile, perhaps broadly similar in locomotor mode to the spotted quoll, but with a greater capacity for climbing and grasping. Bayesian phylogenetic analysis of a total evidence dataset comprising 259 morphological characters and 9kb of DNA sequence data from five nuclear protein-coding genes, using both undated and “tip-and-node dating” approaches, place the new taxon outside the marsupial crown-clade, but within the clade Marsupialiformes. It demonstrates that at least one metatherian lineage evolved to occupy the small-medium, meso- or hypo-carnivore niche in the northern hemisphere during the early Cenozoic, at a time when there were numerous eutherians (placentals and their fossil relatives) filling similar niches. However, the known mammal fauna from Uzunçarşıdere Formation appears highly endemic, and geological evidence suggests that this region of Turkey was an island for at least part of the early Cenozoic, and so the new taxon may have evolved in isolation from potential eutherian competitors. Nevertheless, the new taxon reveals previously unsuspected ecomorphological disparity among northern hemisphere metatherians during the first half of the Cenozoic.


Current fossil evidence indicates that the mammalian clades Metatheria (= Marsupialia plus all fossil taxa more closely related to marsupials than to placentals) and Eutheria (= Placentalia plus all fossil taxa more closely related to placentals than to marsupials) probably diverged at least 160 million years ago (MYA) [1]. This date is broadly congruent with recent molecular clock estimates for the timing of the split between marsupials and placentals [25]. During the Mesozoic, metatherians and eutherians were moderately diverse taxonomically [6], but they were restricted to relatively small body sizes (<7 kg) and exhibited limited ecomorphological disparity [68]. Metatherians seem to have been affected much more severely than eutherians by the K-Pg mass extinction event [79].

From the Palaeocene onwards, eutherians (including placentals) radiated massively, going on to dominate mammalian faunas in most of the world, in terms of both number of species and ecomorphological disparity [10, 11]. Metatherians dispersed to South America in the latest Cretaceous or early Palaeocene [1214], and they diversified widely in South America, Antarctica and Australia during the Cenozoic [12, 1419]. In the northern hemisphere, by contrast, the Cenozoic fossil record of Metatheria is characterised by low species diversity and very limited ecomorphological disparity, with northern hemisphere metatherians eventually going extinct during the middle Miocene [10, 20, 21]. A single didelphid marsupial, the Virginia opossum (Didelphis virginiana), is currently widespread in North America, the result of dispersal from South America within the last one million years [22]. However, besides the Virginia opossum and a few other didelphid species that occur in Central America, marsupials are now entirely absent from the northern hemisphere (except for a handful of human introductions). The comparative lack of evolutionary success of metatherians in the northern hemisphere during the Cenozoic has often been argued to be because they are competitively inferior to eutherians [23, 24].

Here, we describe a three-dimensionally preserved partial skull and near complete postcranial skeleton of a new metatherian from the middle Eocene (Lutetian) Uzunçarşıdere Formation in central Turkey. Not only is it remarkably well-preserved, it also reveals previously unsuspected ecomorphological disparity among northern hemisphere metatherians during the Cenozoic. We present qualitative and quantitative functional analyses of its craniodental and postcranial morphology, and we test its evolutionary relationships via Bayesian undated and “tip-and-node dating” phylogenetic analyses of a total evidence dataset comprising 259 morphological characters and 9kb of DNA sequence data from five nuclear protein-coding genes. Finally, we discuss the significance of this taxon for understanding the relative success of eutherians and metatherians in the northern hemisphere during the Cenozoic.

Materials and methods


The specimen described here was discovered and collected by one of us (AMM) from the Uzunçarşıdere Formation in the summer of 2002, during fieldwork with Nizamettin Kazanc1 (Ankara Üniversitesi) and Mary Maas (University of Texas at Austin). No permits were required for the described study, which complied with all relevant regulations. The specimen has been deposited as specimen number AÜJM 2002–25 in a permanent repository, namely Ankara Üniversitesi Jeoloji Müzesi (AÜJM) in Ankara, Turkey; the specimen is publically accessible.

Nomenclatural acts

The electronic edition of this article conforms to the requirements of the amended International Code of Zoological Nomenclature, and hence the new names contained herein are available under that Code from the electronic edition of this article. This published work and the nomenclatural acts it contains have been registered in ZooBank, the online registration system for the ICZN. The ZooBank LSIDs (Life Science Identifiers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefix “”. The LSID for this publication is: The electronic edition of this work was published in a journal with an ISSN, and has been archived and is available from the following digital repositories: PubMed Central, LOCKSS.

CT scanning

Selected elements of AÜJM 2002–25 were scanned at the Small Animal Tomographic Analysis Facility of Seattle Children’s Research Institute using a Skyscan 1076C desktop micro-CT scanner (Bruker, Belgium). Acquisition parameters were as follows: 1.0mm Al filter, 100kV, 100μA, 360° scan with 1.0° rotational steps. At each rotation, two frames were acquired and averaged. Shadow images from the scan were reconstructed as PNG stacks with 0.036mm isotropic voxels using the scanner vendor’s reconstruction software, NRecon. 3D volume rendering of the PNG stacks was carried out using 3D Slicer 4.6.2 [25], with the exception of Fig 16A, which was produced using Drishti 2.6.3 [26].

Comparative material

As part of this study, comparative material of modern and fossil metatherians was examined in the following collections: Australian Museum, Sydney, Australia (prefix AM); American Museum of Natural History, New York, USA (prefix AMNH); Vertebrate Paleontology Laboratory, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas (prefix TMM), Smithsonian National Museum of Natural History, Washington DC, USA (prefix USNM). A full list of the specimens examined is given in S1 Text.


Description of the dentition of AÜJM 2002–25 follows standard terminology for tribosphenic metatherians [6, 2730]. Description of the cranium draws on a range of studies of metatherian cranial anatomy [27, 3139]. Description of the postcranium follows studies of metatherians [32, 3956] and of other therian mammals [5762].

Body mass estimate

The dentition of AÜJM 2002–25, with its steep molar size gradient in which m4 is much larger than m1, is unlike that of any living marsupial; thus, we have chosen not to estimate body mass using tooth size [6365]. Instead, we estimated body mass based on total jaw length using the “dasyuromorphian” dataset of Myers [65], because dasyuromorphians (e.g. Dasyurus spp., Sarcophilus harrisii) appear to represent reasonable ecomorphological analogues for AÜJM 2002–25. The regression equation calculated by Myers [65] is log10(body mass) = –2.722 + (3.207* log10[total jaw length]), with a “smearing estimate” of 2.3% and a percentage error of 18%. Both mandibles are slightly damaged anteriorly in AÜJM 2002–25 (the left mandible is slightly more complete, and so was used to measure total jaw length), and so the body mass estimate using this equation is likely to be a slight underestimate.

Qualitative morphofunctional analyses

Qualitative functional analysis of the dentition follows Muizon and Lange-Badré [66], whilst that of the skeleton follows multiple studies [32, 39, 41, 4345, 4749, 5155, 5762].

Quantitative morphofunctional analyses

Zimicz [67, 68] presented five dental indices, modified from previous work by Van Valkenburgh [69], that can be used to quantitatively compare tooth shape in carnivorous metatherians, namely: Relative Grinding Area (RGA) = square root of the area of the talonid of m4/length of m4; Relative Premolar Size (RPS) = width of the largest lower premolar/cube root of body mass in kg; Premolar Shape (PS) = width of the largest lower premolar/length of largest lower premolar; Relative Premolar Length (RPL) = length of largest lower premolar/length of m4; Relative Blade Length (RBL) or Trigonid Length of the Carnassial Molar (TLC) = length of the trigonid of m4/total length of m4. These indices were calculated for AÜJM 2002–25 and compared with 31 other similarly-sized (<10 kg), carnivorously-adapted metatherians (both modern and fossil), based on either published data or our own measurements of specimens. Body mass estimates for modern taxa are from the PanTHERIA database [70]. Body mass estimates for fossil taxa were taken from the literature, or were calculated using published predictive regression equations based on dental measurements.

Values for individual indices calculated for AÜJM 2002–25 were compared to the critical values presented by Zimicz [67, 68], which are as follows: for RGA, <0.5 = hypercarnivore, 0.5–0.8 = mesocarnivore, >0.8 = hypocarnivore; for PS, >0.58 = bone-cracker (or other durophage), <0.58 = non-bone-cracker; for RPS, >2.6 = bone-cracker (or other durophage), <2.6 = non-bone-cracker; for RPL, >0.7 = hypercarnivore, <0.7 = mesocarnivore or hypocarnivore; for RBL/TLC, >0.9 = hypercarnivore, 0.8–0.9 = bone-cracker (or other durophage), 0.7–0.8 = mesocarnivore, <0.7 = hypocarnivore. These values of RGA, RPS, PS, RPL and RBL were also subjected to principal component analysis (PCA) in PAST 3.07 [71] to determine where AÜJM 2002–25 and other carnivorously-adapted metatherians fall in dental morphospace. Because the indices are all dimensionless ratios, the analysis used the variance-covariance matrix, rather than the correlation matrix.

The cranium of AÜJM 2002–25 is too incomplete to allow calculation of bite force using the “dry skull” method [72, 73]. Instead, we used the method of Therrien [74], as modified for metatherians by Wilson et al. [75], to calculate relative bite force based on measurements of the mandible. We measured the dorsoventral radius of the mandible in medial view rather than lateral view (as was done by Therrien [74]), because the molar crowns extend much further ventrally (and the roots are partially exposed) in lateral view than in medial view.

Chen and Wilson [76] identified 30 postcranial indices that collectively perform well at correctly identifying locomotor mode of extant small-bodied mammals. Of these, 24 can be calculated for AÜJM 2002–25. We added AÜJM 2002–25 to the “five-locomotor-mode” dataset of Chen and Wilson [76], which comprises 87 modern mammals of known locomotor mode, namely either “Arboreal”, “Scansorial”, “Semiaquatic”, “Semifossorial” and “Terrestrial”. The 24 indices for this combined taxon set were then subjected to phylogenetically flexible discriminant analysis [77, 78] using a modified version of an R script written by L. Schmitz (available here:, using the phylogeny and divergence times of Bininda-Emonds et al. [79] for relationships among the modern taxa, and assuming equal prior probabilities for the five locomotor modes.

Phylogenetic analysis

To assess the evolutionary relationships of the new taxon, we added it to a modified version of the total evidence dataset of Beck et al. [80]; this includes 33 metatherian terminals, including representatives of all modern marsupial orders, plus key fossil metatherian taxa known from well-preserved craniodental and/or postcranial material, namely Asiatherium, Deltatheridium, Pucadelphys, Mayulestes, Andinodelphys, Herpetotherium, Djarthia and a composite Peradectidae terminal that combines character scores from Peradectes and Mimoperadectes. This dataset comprises 259 morphological characters (of which 27 [= 10.4%] are dental, 78 [= 30.1%] are cranial, 146 [= 56.4%] are postcranial and 8 [= 3.1%] are soft tissue) and 9012 base pairs of sequence data from five nuclear protein-coding genes (APOB, BRCA1, IRBP, RAG1 and VWF; see Beck et al. [37, 80] for full details). We also added the Late Cretaceous stagodontid Didelphodon vorax, which shows some dental similarities to taxon described here, with character scores based on the description of Wilson et al. [75] and on isolated tarsals from Dinosaur Park in Canada that were tentatively referred to Didelphodon by Szalay [56]. The new taxon could be scored for 98 morphological characters (= 37.8%), of which 19 are dental, 13 are cranial, and 66 are postcranial, whilst Didelphodon could be scored for 73 (= 28.2%), of which 24 are dental, 35 are cranial, and 14 are postcranial; character scores for Anatoliadelphys and Didelphodon are given in S2 Text. As in Beck et al. [37, 80], 49 characters representing plausible morphoclines were specified as ordered (see S2 Text). The enigmatic fossil Australian marsupial Yalkaparidon [37] was deleted, as preliminary analyses indicated that its phylogenetic position was highly unstable. The final taxon set comprised 34 fossil and modern metatherian terminals, plus five non-metatherian outgroup terminals (the extant monotremes Ornithorhynchus and Tachyglossus, the fossil stem-therian Vincelestes, and the fossil eutherians Asioryctes and Ukhaatherium).

The resultant total evidence matrix (available for download as S1 File) was analysed using Bayesian undated and “tip-and-node dating” analysis in MrBayes 3.2.6 [81], following the general approach of Beck et al. [37, 80]. In brief, an appropriate partitioning scheme and set of models was determined for the sequence data using PartitionFinder v1.0.1 [82], using the Bayesian Information Criterion, linked branch lengths and the “greedy” search algorithm, whilst the morphological data was assigned a single Mk model [83], assuming that only parsimony-informative characters had been scored and with a gamma distribution to model rate heterogeneity between sites. For the “tip-and-node dating” analysis, temporal information was incorporated via ages for the terminals (taken from the literature; assumed age ranges for terminals are listed in S3 Text) and offset-exponential age priors on selected nodes [8487]. A single Independent Gamma Rates (IGR) clock model [84] and a Fossilised Birth-Death (FBD) tree prior that assumed “diversity” sampling [86] were implemented. Because our taxon set was at the level of genera, we assumed that the sampling probability of our modern taxa was 0.25 (= 23 out of a total of 93 currently recognised genera). Both the undated and dated analyses were run 20x106 generations, sampling every 5x103 generations, with each analysis comprising four independent runs of four chains (three “heated,” one “cold”). An appropriate burn-in period was determined using Tracer v1.6 [88]. The post-burn-in trees from the undated analysis were summarised using 50% majority rule consensus in MrBayes, whereas those from the dated analysis were summarised as a maximum clade credibility (MCC) tree using TreeAnnotator v1.8.3, after first converting branch lengths from substitutions per site to millions of years using the perl script (available here: Support was assessed using Bayesian posterior probabilities for both analyses, and divergence times from the dated analysis were calculated as median heights (with 95% highest posterior densities used as confidence intervals).

The morphological characters were then mapped onto the undated and dated phylogenies to identify unambiguous synapomorphies (i.e. character state changes that are synapomorphies under both Accelerated Transformation [ACCTRAN] and Delayed Transformation [DELTRAN]) using PAUP* 4.0a152, assuming the maximum parsimony criterion.


Systematic palaeontology





Anatoliadelphys gen. nov.

Anatoliadelphys maasae sp. nov.


Anatolia (Greek): the geographic name for the Asian part of Turkey; delphys (Greek): uterus, a common suffix for marsupials and their fossil relatives; maasae: in honour of Dr. Mary Maas and her contributions to Paleogene mammalian palaeontology, particularly in Turkey.


Ankara Üniversitesi Jeoloji Müzesi (AÜJM) specimen 2002–25, which comprises a fragmented partial cranium, both dentaries, and associated postcranial elements, including most of the vertebral column, partial pectoral and pelvic girdles, all of the long limb bones, both calcanei, two metapodials, and a few phalanges.

Locality and age.

AÜJM 2002–25 was collected from the Lülük member of the Uzunçarşıdere Formation (UCF), which is part of the small Orhaniye-Güvenç sedimentary basin located at the northwestern edge of the city of Ankara, approximately 5 km southwest of the town of Kazan, in central Turkey [89]. The Lülük member is the lowest of the three members currently recognised within the UCF (together with the Gökdere [middle], and Sarıbeyler [upper] members), and is the source of all fossil mammals known from the UCF to date [8994]. AÜJM 2002–25 is from locality AK33, which is approximately 90m above the base of the UCF, at Memlik village (N40° 5.5914’, E32° 44.3924’). Until recently, the age of the UCF was poorly constrained, but a combination of U-Pb dating of zircons and magnetostratigraphy now support a date of 44–42 MYA (= Lutetian) for the formation as a whole, and 44–43 MYA for the Lülük member [89, 94].


Anatoliadelphys maasae differs from all other metatherians in the following combination of features: comparatively large size (estimated body mass 3–4 kg); premolars increase markedly in size posteriorly (occlusal area of p1 less than one sixth that of p3); P3 and p3 very large (similar in occlusal area to M2 and m2 respectively) and also broad (labiolingual width:mesiodistal length ratio is 0.89 for P3 and 0.7 for p3); modified tribosphenic molar dentition, in which M1-3 and m1-4 increase markedly in size posteriorly (occlusal area of M1 approximately one third that of M3; occlusal area of m1 approximately one seventh that of m4); upper molars with cingula extending along the anterior and posterior margins; protocone large but conules indistinct or absent; metacone taller than the paracone on M3 but smaller than the paracone on M4; centrocrista v-shaped on M3, with the premetacrista extending labially to stylar cusp D; centrocrista straight on M4; parastylar lobe very large on M4; anterior cingulid weakly developed on m3-4; m4 trigonid dominated by enormous protoconid, with paraconid and metaconid both greatly reduced; preentocristid and cristid obliqua of m3-4 both with carnassial notch; posterior cingulid present but very faint on m3-4; strongly curved radius and tibia; femur with prominent third trochanter, well-marked trochlea and distal condyles of approximately equal width; calcaneus with medially-inflected tuber, large peroneal process with prominent groove for peroneus longus tendon, concave calcaneocuboid facet, and prominent pit (probably for plantar calcaneocuboid ligament) on ventral surface.



Relative to other fossil metatherian specimens known from the Cenozoic of Laurasia, AÜJM 2002–25 is remarkably well-preserved (Fig 1). It is more complete than skeletal remains of the herpetotheriiid Herpetotherium cf. fugax that have been described from the early Oligocene (Orellan) of North America [49, 50]. Several fossil metatherian specimens from Eocene deposits at Messel and Geiseltal in Germany are more complete than AÜJM 2002–25, and include some soft tissue preservation, but they are badly crushed [95, 96]; as a result, comparatively little information can be extracted from them. By virtue of its combination of completeness and three-dimensional preservation, AÜJM 2002–25 is a particularly significant specimen.

Fig 1. Holotype skeleton of Anatoliadelphys maasae (AÜJM 2002–25).

Scale bar = 5 cm.

The following elements are preserved: a partial cranium, broken into multiple fragments but preserving left and right C1 P1-3 M1-4; left and right dentaries, damaged anteriorly but preserving c1 p1-3 m1-4; most of the vertebral column, although many vertebrae are represented by the centrum only; the manubrium sterni and sternebrae; left and right partial scapulae; left and right humeri; left and right ulnae; left and right radii; left and right ossa coxae; left and right femorae; left and right tibiae; left and right fibulae; left and right calcanea; two metapodials; four proximal and two intermediate phalanges. A detailed description of each these elements follows.

Dentition as a whole.

The upper and lower dentition anterior to the canines is not preserved in AÜJM 2002–25. The specimen does not preserve any direct evidence of the pattern of dental replacement, but the postcanine dentition comprises three premolariform teeth and four molariform teeth in the upper and lower jaws, suggesting the presence of a typical metatherian dental formula of three premolars and four molars [6, 97, 98]. With the exceptions of M3-4 and m3-4, the postcanine teeth are heavily worn, and so aspects of their occlusal morphology are unclear.

Upper dentition.

A large, robust, caniniform, single-rooted C1 is present (Figs 2 and 3). The anteroventral tip of C1 bears a sulcus or wear facet, resulting from contact with c1.

Fig 2. Volume-rendered CT image of right maxilla of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

C1 P2-3 M1-4 are preserved. Note that the maxillary fragment housing M4 is slightly displaced relative to the intact morphology (the correct position for M4 can be seen in Figs 4 and 5). A, anterior view; B, medial view; C, lateral view; D, ventral (occlusal) view. Abbreviations: iof, infraorbital foramen;? pv,? palatal vacuity. Scale bar = 1 cm.

Fig 3. Stereo-photograph of right maxilla of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in ventral (occlusal) view.

C1 P2-3 M1-3 are preserved. Scale bar = 1 cm.

The right maxilla (Figs 2 and 3) retains P2 and P3 in situ, and also has a tiny alveolus for P1. P2 is very heavily worn, and little can be inferred regarding its occlusal morphology. P3 is fully erupted but considerably less worn than is P2, suggesting that it erupted much later; M4 is also fully erupted and lightly worn, indicating that AÜJM 2002–25 represents an adult individual. A similar wear pattern is seen in the lower dentition. Collectively, this is consistent with a marsupial-type pattern of dental replacement (in which replacement occurs only at the third premolar locus [6, 99, 100]), and suggests that the third premolars erupted about the same time as the fourth molars; however, other interpretations are possible [6, 101]. P3 is nearly as wide as it is long (labiolingual width:mesiodistal length ratio is 0.87), and is similar in size in terms of occlusal area to M2.

The left upper molars are somewhat better preserved than those on the right side (Figs 4 and 5). From anterior to posterior, molar size increases markedly (Table 1). M1-M3 are triangular in occlusal outline, whilst M4 has an enlarged parastylar region and greatly reduced metastylar region.

Fig 4. Right upper molars (M1-4) of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in ventral (occlusal) view.

A, Volume-rendered CT image; B, interpretative drawing (damaged areas are indicated in grey). Abbreviations: cc, centrocrista; ec, ectoflexus; poc, postcingulum; pome, postmetacrista; popa, postparacrista; popr, postprotocrista; pr, protocone; prc, precingulum; prme, premetacrista; prpa, preparacrista; prpr, preprotocrista; StB, stylar cusp B; StC, stylar cusp C; StD, stylar cusp D; tnb, trigon basin. Scale bar = 0.5 cm.

Fig 5. Stereo-photograph of left maxilla of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in ventral (occlusal) view.

M1-4 are preserved. Scale bar = 1 cm.

Table 1. Dimensions of upper teeth (in mm) of AÜJM 2002–25, holotype of Anatoliadelphys maasae.

M1 is the smallest molar, and is so heavily worn that no morphological interpretation can be made beyond that it is broadly triangular in outline, probably with an ectoflexus present.

M2 is less worn than M1, but its cusps are nevertheless barely identifiable due to the degree of wear. It appears broadly similar in occlusal outline to M1 but is ~30% larger in linear dimensions. A distinct ectoflexus is present. Two large stylar cusps appear to be present, one either side of the ectoflexus, with a possible third present at the posterolabial corner of the tooth; based on their positions and on comparison with other metatherians, we identify them (from anterior to posterior) as StB, StD and? StE, of which StD is the tallest, followed by StB. What remains of the metacone is taller than the paracone. The centrocrista is heavily worn, but appears to have been v-shaped. The preparacrista is much shorter than the postmetacrista. The protocone is anteroposteriorly broad, and is anterior to the midline of the tooth, in line with the paracone. A narrow cingulum extends along the anterior margin of the tooth, low down on the tooth crown, from level with the protocone to the anterolabial corner of the tooth; it may represent a conjoined precingulum and anterolabial cingulum. A similar, but somewhat narrower postcingulum extends along the posterior margin of the tooth, behind the postmetacrista, to the posterolabial corner of the tooth.

M3 is ~20% larger in linear dimensions than M2 and is the largest upper molar in terms of occlusal area. The ectoflexus is deeper than on M2. Anterior to the ectoflexus, there is a relatively well-developed StB. Posterior to the ectoflexus, the stylar shelf forms a labiolingually compressed crest that extends along the labial margin of the tooth; anteriorly, this crest rises to a distinct stylar cusp, which we identify as StD. This cusp is the tallest on the tooth crown, and is connected to the metacone via the premetacrista. The metacone is distinctly taller than the paracone.

The molar crests are better preserved on the right M3 than on the left. The preparacrista runs toward the anterolabial corner of the tooth, but terminates just before it. The preparacrista is slightly notched in anterior view. The centrocrista is unusual in that the postparacrista and premetacrista do not contact each other directly; instead, the premetacrista extends labially to terminate at StD, whilst the postparacrista extends posterolabially from the paracone and appears to terminate at the base of the premetacrista. A superficially similar centrocrista morphology is seen in Hatcheritherium alpha from the Late Cretaceous of North America [13], but in this taxon the premetacrista terminates at StC (which is absent in Anatoliadelphys), anterior to a very tall StD. The premetacrista is distinctly notched.

The postmetacrista is significantly longer than the premetacrista, and it rapidly reduces in height as it extends from the metacone towards the posterolabial corner of the tooth. The trigon basin is almost flat. The protocone is anterior to the midline of the tooth, and slightly anterior to the ectoflexus. The protocone is anteroposteriorly broad, and the pre- and postprotocrista meet at almost a right angle. Distinct conules are not present. Similarly to M2, a narrow cingulum extends along the anterior margin of the tooth, low down on the tooth crown, from level with the protocone to the anterolabial corner of the tooth; it broadens at the level of the paracone and remains the same width as it continues labially, where it may represent the homologue of the anterolabial cingulum. A narrow cingulum also extends along part of the posterior margin of the tooth, from level with the metacone to the posterolabial corner of the tooth.

The M4 is proportionately longer anteroposteriorly (relative to M1-3) than those of most other tribosphenic metatherians, due in part to its large parastylar region; however, it still appears somewhat anteroposteriorly compressed relative to the more anterior molars, due to reduction of the metastylar region. The most prominent cusp is the massive, spire-like paracone, which is connected to the metacone via a well-developed, linear centrocrista. As in the more anterior molars, a preparacrista extends towards the anterolabial corner of the tooth, but terminates just before reaching it. The postmetacrista is high, short and terminates at a small swelling that is probably StE. Anterior to this, a tiny bump on the labial margin of the tooth may be StD. Much larger stylar cusps are present in the B and C positions. In occlusal view, StB is anteroposteriorly broad and crestlike, dominating the parastylar region, but it is similar in height to StC when viewed labially. A crest extends lingually from the metacone towards the postprotocrista; a tiny swelling at its midpoint might represent the metaconule. The preprotocrista and postprotocrista meet at right angles. As in M2 and M3, the protocone is anteroposterorly broad and positioned anteriorly relative to the midline of the tooth, and a weakly developed cingulum extends along the entire anterior margin of the tooth, low down on the crown. A postcingulum also extends along the posterior margin; this cingulum is slightly wider than on M3, and extends labially from a point below the swelling that might represent the metaconule to stylar cusp E.


Fragments of both the left and right maxillae are present (Figs 2, 3 and 5). The largest and best preserved of these is a fragment of the right maxilla that retains the C1, P1-3 and M1-3 (Figs 2 and 3; these teeth are described above). When this fragment is viewed laterally, the infraorbital foramen can be identified as an opening in a relatively posterior position, above the anterior root of M2. The infraorbital foramen appears relatively well-developed, but the incompleteness of the cranium means that its relative size cannot be easily compared to the infraorbital foramina of other metatherians [75, 102].

The medial side of this maxillary fragment is concealed by matrix, but CT scans reveal the presence of a piece of the right nasal within the matrix. The CT scans also suggest that some of the maxillary turbinals and the maxillary foramen (the posterior opening of the infraorbital canal) are also preserved. In ventral view, only the alveolar process and a small portion of the palatal process are preserved; the lateral edge of a palatal vacuity may be present medial to P3-M1, but the specimen is too damaged to be certain of this. Palatal vacuities are found in most metatherians, but are absent in deltatheroidans, sparassodonts, Pucadelphys and Mayulestes, all of which fall outside Marsupialia [103].

Other cranial fragments include one comprising a part of the palatal process of the maxilla with the right M4 in situ, together with part of the palatine (this fragment has been glued to the larger right maxillary fragment described above–see Fig 2), and another comprising a partial left maxilla with M1-4 in situ (Fig 5). A notable feature of these fragments is the presence of a deep pit in the palatal process of the maxilla, between M3 and M4, which would have housed the very large protoconid of m4 during occlusion. Similar pits have been reported in sparassocynids [104], sparassodonts (character 21 of [32]) and Thylacinus species [105].

Basicranial fragment.

A long, badly damaged fragment can be identified as part of the left side of the basicranium, preserving parts of the palatine, basisphenoid and alisphenoid, and possibly also parts of the pterygoid and presphenoid (Fig 6). In ventral view, the most easily identifiable feature is the transverse canal foramen, which is found in most (but not all) metatherians [106], but which is less common in eutherians. Posteriorly, there is an opening that extends anterodorsally, which we tentatively identify as the carotid foramen; if so, this foramen may be located entirely within the basisphenoid, but this cannot be confirmed because of poor preservation. Nevertheless, it is clear that the transverse canal foramen is positioned anterior to the carotid foramen, as in most metatherians [37, 106]. The crest medial to the transverse canal foramen is probably the posterior part of the entopterygoid crest, which gradually enlarges anteriorly and joins the lateral wall of nasopharyngeal passage.

Fig 6. Volume-rendered CT images of nasopharyngeal-sphenoid region of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in ventral view.

A, cranial fragment from left side; B, mirrored version of A, showing approximate morphology of intact nasopharyngeal-sphenoid region. Abbreviations: cf, carotid foramen; enpc, entopterygoid crest;? pt,? pterygoid; tcf, transverse canal foramen. Scale bar = 1 cm.

In dorsal view, the crests forming the border of the sulcus for the internal opening of the foramen rotundum can be identified. The hypophyseal fossa is badly damaged. A small portion of the lateral wall of alisphenoid is preserved above the sulcus for the foramen rotundum. The crest anteromedial to the internal opening of the foramen rotundum is possibly the lateral border of the sphenorbital fissure. On the left side of the anteriormost edge of this basicranial fragment, a sulcus that may be for the sphenopalatine emissary vein is preserved, as is the posterior border of the sphenopalatine foramen.


Parts of both the left and right jugals are preserved (Figs 7 and 8). The left fragment is almost complete, missing only a small portion of its posterodorsal margin (Fig 7); it articulates perfectly with the preserved zygomatic process of the left maxilla. The right fragment is more damaged, and only the middle third is preserved (Fig 8).

Fig 7. Volume-rendered CT images of left jugal of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, medial view; B, lateral view; C, dorsal view; D, ventral view. Abbreviations: frp, frontal process of the jugal; fsq, facet for squamosal; gpju, glenoid process of the jugal; sma, sulcus for the masseter muscle. Scale bar = 1 cm.

Fig 8. Volume-rendered CT images of right jugal of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, medial view; B, lateral view. Abbreviations: frp, frontal process of the jugal; sma, sulcus for masseter muscle. Scale bar = 1 cm.

Anteriorly, there does not appear to be a distinct depression on the lateral wall of the zygomatic process of the jugal for the zygomaticus and levator labii muscles, whereas such a depression is seen in at least some didelphids [36, 107]; however, this region is slightly damaged in AÜJM 2002–25. A distinct frontal process (representing the ventral point of attachment of the postorbital ligament) is identifiable on the dorsal margin of the left jugal fragment, but it is damaged. In ventral view, the jugal widens posteriorly, and forms a distinct, faceted preglenoid process, which would have formed the anterolateral margin of the glenoid fossa [36]. The medial surface of the jugal is concave, and it houses a large nutrient foramen anterior to the frontal process.


Parts of both the right and left squamosals are preserved (Figs 9 and 10). Only the glenoid fossa and the postglenoid process of the right squamosal are preserved (Fig 9), but the left squamosal is nearly complete, lacking only the zygomatic process (Fig 10).

Fig 9. Volume-rendered CT images of partial right squamosal of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, dorsal view; D, ventral view; E, medial view; F, lateral view. Abbreviations: fju, facet for jugal; gf, glenoid fossa; pgp, postglenoid process; pzc, postzygomatic crest; sgf, supraglenoid foramen; spgv, sulcus for postglenoid vein;? sps,? sulcus for prootic sinus. Scale bar = 1 cm.

Fig 10. Volume-rendered CT images of partial left squamosal of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, posterodorsal view; D, ventral view; E, medial view; F, lateral view. Abbreviations: gf, glenoid fossa; pgp, postglenoid process;? pts,? posttemporal sulcus; sgf, supraglenoid foramen; smb, suprameatal bridge;? smf,? suprameatal foramen (= “subsquamosal foramen” of Wible [36]); spgv, sulcus for postglenoid vein;? sps,? sulcus for prootic sinus; ssqf, subsquamosal foramen (= “suprameatal foramen” of Wible [36]). Scale bar = 1 cm.

In lateral view, the squamosal appears roughly rectangular in shape. The suprameatal bridge is short but robust. The subsquamosal foramen [27, 31, 108110] (= the “suprameatal foramen” of Wible [36]), which transmits a temporal branch of the postglenoid artery and vein, is paired, with the anterior opening much larger than the posterior. Dorsal to the suprameatal bridge, there is at least one vascular opening that probably represents a subsquamosal foramen (= “suprameatal foramen” sensu Wible [36]). There is also a distinct supraglenoid foramen opening in the lateral side of the zygomatic process of the squamosal, dorsal to the postglenoid process. In ventral view, the glenoid fossa is mediolaterally elongate and roughly oval in shape. The anterolateral margin of the glenoid fossa would have been bordered by a prominent glenoid process of the jugal in life (see above). The postglenoid process appears robust and unpneumatised. The medial edge of the postglenoid process is grooved by a prominent sulcus that presumably transmitted the postglenoid vein from the postglenoid foramen, but the postglenoid foramen itself is not preserved intact; it may have been completed medially by the petrosal, as is seen in some marsupials (e.g. some peramelemorphians [111]). In medial view, the vertical sulcus for the prootic sinus may be faintly visible on the squamosal, and on the left squamosal a horizontal sulcus may represent the posttemporal sulcus housing the arteria and vena diploetica magna [35].

Posterior cranial roof.

A fragment representing the posterior part of the dorsal cranial roof is preserved (Fig 11); it appears to comprise the interparietal (posterodorsally), the paired parietals (dorsolaterally), and supraoccipital (posteriorly). In dorsal view, a thick, well-developed sagittal crest is clearly identifiable, extending anteriorly from the nuchal (lambdoid) crest, along the interparietal and onto the parietals; the crest is damaged anteriorly. Multiple pairs of foramina are present on the dorsal surface of this fragment, of which two bilateral pairs are particularly prominent. One pair of these is located approximately halfway along the preserved length of the fragment, either side of the base of the sagittal crest, at the anterior end of the interparietal; these foramina penetrate anteroventrally into the cranium. The second pair is positioned more posterolaterally, opening adjacent to or within the interparietal-parietal suture; a posteriorly-directed sulcus extends from each of these foramina. These foramina may be for emissary veins draining venous blood. Further laterally, a raised ridge marks the suture with the squamosal.

Fig 11. Volume-rendered CT image of cranial roof of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in dorsal view.

Only the posterior part of the dorsal cranial roof is preserved. Abbreviations: for, foramina; ip, interparietal; ip-pa, interparietal-parietal suture; nc, nuchal (lambdoid) crest; pa, parietal; pa-sq, path of parietal-squamosal suture; sc, sagittal crest. Scale bar = 1 cm.

Didelphids are unusual among mammals in that the supraoccipital and interparietal are entirely fused without any trace of a suture in postweaning juveniles or older individuals [27, 36]; in other marsupials, by contrast, the suture between supraoccipital and interparietal can usually be identified, roughly corresponding to the path of the nuchal crest (if present), except in very old or heavily ossified individuals [27]. Based on its known morphology and the results of our phylogenetic analysis (see below), Anataoliadelphys maasae is clearly not a didelphid; nevertheless, a suture delimiting the boundary between interparietal and supraoccipital cannot be clearly identified in AÜJM 2002–25. We are confident that an interparietal was present as a distinct bone, as it appears to be consistently present in mammals [112]. However, the interparietal-supraoccipital suture may be concealed by the prominent nuchal crest of this specimen. Similarly, the midline suture is not apparent in AÜJM 2002–25, but might be concealed by the very prominent sagittal crest; the midline parietal suture is fused in some marsupials [27].

In posterior view, the nuchal crest appears well-developed, with a concave posterior surface; however, the ventral half of the posterior surface is somewhat crushed and displaced anteriorly, exaggerating the concavity of the surface. Multiple bilaterally symmetric foramina are present on the posterior surface. Posteroventral to the point of contact between the nuchal and sagittal crests, there is a median foramen. In anterior view, the vermis impression appears round and deep.

Other cranial fragments.

As discussed above, CT scanning of the large right maxillary fragment reveals that part of the right nasal is preserved within the matrix that covers the medial side. However, this nasal fragment does not preserve any remarkable features.

A large fragment of bone was found attached to the angular process of the left mandible, which had broken off the main body of the mandible. Due to their fragile nature, it was not possible to separate these fragments and reattach the mandibular parts to the rest of the mandible. The non-mandibular fragment has a slightly convex outer surface, and so could represent either part of the iliac blade or a part of the sidewall of the cranium. However, both ilia are almost complete, and the weathering pattern and pigmentation of this fragment closely resembles the right squamosal. We therefore interpret it as a fragment of the right cranial wall. The lateral side is mostly convex, with a flaring posterodorsal margin. The anterodorsal margin bears a small nutrient foramen with a posterodorsal opening. Most of the medial view is obscured by the overlying angular process of the left mandible.

Two petrosal fragments are preserved, but both are heavily damaged. Only an elongate mastoid exposure and a conical and relatively shallow subarcuate fossa can be recognised on a fragment of the pars canalicularis of the right petrosal. The subarcuate fossa is relatively deep in most metatherians, but it is shallow in Sarcophilus and some sparassodonts (e.g. Pharsophorus), and it is reportedly entirely absent in the vombatids Vombatus and Lasiorhinus and some sparassodonts (e.g. Lycopsis, Prothylacinus, Arctodictis) [31, 32, 113].

Lower dentition.

The left and right dentaries of AÜJM 2002–25 both preserve c1 and the entire postcanine dentition (p1-3 m1-m4), but these teeth are better preserved on the left side (Figs 1219).

Fig 12. Volume-rendered CT image of left dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, medial view; B, lateral view; C, dorsal (occlusal) view. Abbreviations: ang, angular process; coc, coronoid crest; con, dentary condyle; mas, mandibular symphysis; mf, mental foramen; psmf, posterior shelf of the masseteric fossa; vmr, ventromedial ridge. Scale bar = 2.5 cm.

Fig 13. Stereo-photograph of left dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in medial view.

Scale bar = 1 cm.

Fig 14. Stereo-photograph of left dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in lateral view.

Scale bar = 1 cm.

Fig 15. Stereo-photograph of left dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in dorsal (occlusal) view.

Scale bar = 1 cm.

Fig 16. Left lower molars (m1-4) of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in dorsal (occlusal) view.

A, Volume-rendered CT image; B, interpretative drawing (damaged areas are indicated in grey). Abbreviations: ancd, anterior cingulid; co, cristid obliqua; end, entoconid; hld, hypoconulid; hyd, hypoconid; mcd, metacristid; med, metaconid; pacd, paracristid; pad, paraconid; pecd, preentocristid; phcd, posthypocristid; prd, protoconid; tab, talonid basin;. Scale bar = 0.5 cm.

Fig 17. Stereo-photograph of right dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in medial view.

Scale bar = 1 cm.

Fig 18. Stereo-photograph of right dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in lateral view.

Scale bar = 1 cm.

Fig 19. Stereo-photograph of right dentary of holotype of Anatoliadelphys maasae (AÜJM 2002–25) in dorsal (occlusal) view.

Scale bar = 1 cm.

The c1 is a single rooted, caniniform tooth that is not as tall as C1.

Three premolars are present, namely p1-3. Of these, p1 is tiny but double-rooted, and is oriented posterolingually-anterolabially relative to the major axis of the dentary; it is heavily worn. The p2 is also double-rooted, markedly larger than p1 but also heavily worn. The double-rooted p3 is by far the largest of the three premolars; it is somewhat less worn than p1 and p2 (see our earlier comments about how this pattern of wear may indicate marsupial-type dental replacement), but most of the occlusal surface has nevertheless been lost through wear. It is broad labiolingually (width:length ratio = 0.70), and it is about as large as m2 in terms of occlusal area.

The lower molars increase markedly in size from anterior to posterior, with m4 being the largest tooth, with an occlusal area about seven times larger than that of m1 (Table 2). The lower molars are distinctly “exodaenodont” sensu Sigé et al. [114]: the labial side of the molar crown extends much further ventrally than does the lingual side of the crown, with the degree of ventral extension greater in m3-4 than in m1-2. The molar roots are also partially exposed in labial (but not lingual) view.

Table 2. Dimensions of lower teeth (in mm) of AÜJM 2002–25, holotype of Anatoliadelphys maasae.

In labial and lingual views, an unusual, more-or-less continuous wear surface can be seen on the left lower dentition, formed by the occlusal surfaces of m1, m2 and the trigonid of m3; this wear surface is not as obvious on the right lower dentition because of damage to the labial side of m3.

The m1 and m2 are both heavily worn, and so their occlusal morphology cannot be identified. On m3, the paraconid and metaconid are both low. The protoconid is worn to its base, and so it is not possible to confidently determine its original height; however, based on its large base, it was probably a tall, prominent cuspid. A very weak anterior cingulid (= precingulid) is present. Overall, the lingual margin of the talonid is somewhat higher than the labial margin. The talonid basin is relatively shallow. Of the talonid cuspids, the cuspid occupying the position of the hypoconulid (at the distolingual corner of the tooth) is the tallest. However, the hypoconid and entoconid are both worn. Despite this wear, a preentocristid with a distinct carnassial notch appears to be identifiable. The cristid obliqua terminates at approximately the midpoint of the protocristid, and also exhibits a distinct carnassial notch. An extremely faint, vestigial posterior cingulid (= postcingulid) appears to be present, below the crest connecting the hypoconid and hypoconulid (the posthypocristid). On m4, the massive protoconid dominates the trigonid. The paraconid and metaconid are reduced to small swellings at the lingual ends of the paracristid and protocristid, respectively. As on m3, a vestigial anterior cingulid is present. The talonid is similar to m3 in that the lingual margin is higher than labial margin, the talonid basin is shallow, and the talonid cuspids are weakly developed. As on m3, there appears to be a carnassial notch in both the preentocristid and the cristid obliqua, and an extremely faint posterior cingulid appears to be present.


Both left and right mandibles are preserved (Figs 1215 and 1719). Both are largely complete except for damage anteriorly, at the anterior end of the mandibular symphysis. As a result of this, no incisors are preserved (except for one questionable tooth fragment), but there is evidence of at least two incisor alveoli. Both dentaries preserve c1 p1-3 m1-4 (described above). There is no diastema between c1 and p1, nor between p1 and p2. The retromolar space between m4 and the coronoid process is relatively long, being slightly shorter than the length of m4. The anterior margin of the coronoid process is mediolaterally thick and forms a distinct coronoid crest, whilst the dorsal margin is broken on both mandibles. The posterior margin of the coronoid process is mediolaterally thin, and slightly concave posteriorly.

There are two mental foramina on the lateral side of the dentary: the anterior one is positioned below the anterior root of the p2, whilst the posterior one is below the anterior root of m2. A short sulcus extends anteriorly from the posterior mental foramen. Overall, the mandibular body is robust and deep. The lateral surface of the body is not flat, but rather is somewhat concave. The masseteric fossa is well-excavated, and its ventral border forms a distinct shelf posteriorly (the posterior shelf of the masseteric fossa [38]). The condylar process is transversely wide. The mandibular condyle itself is oriented posterodorsally; in mediolateral view, it is slightly lower than the occlusal surface of m4.

The medial surface of the mandibular body is convex. The mandibular symphysis is unfused, and extends posteriorly to a point approximately below the midpoint of p3. Immediately posterior to the symphysis, the ventral margin of the body forms a distinct, medially-directed ridge or thickening; this ridge is much better developed than in Didelphis. The ridge has two distinct parts: an anterior part that begins immediately posterior to the symphysis and extends posteriorly to below the anterior root of m4, and a posterior crest that starts from level with the posterior margin of m4 and expands into a medially inflected lamina, namely the medially inflected angular process characteristic of metatherians [6, 115]. Based on evidence from the jaw musculature of Didelphis [116], the anterior part of this ridge may represent the attachments of the genioglossus, geniohyoideus and anterior belly of the digastric (and perhaps the mylohyoideus posteriorly), whilst the posterior part may reflect the attachment of the superficial masseter (and perhaps the mylohyoideus anteriorly), where it wraps around the ventral margin of the mandibular body.


The atlas is only partially preserved (Fig 20).

Fig 20. Volume-rendered CT images of atlas vertebra (C1) of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view. Abbreviations: caf, caudal articular facet (= postzygapophysis); crf, cranial (exoccipital) articular facet (= prezygapophysis); da, dorsal arch; tp, transverse process. Scale bar = 1 cm.

The right half is relatively complete, and preserves the cranial (exoccipital) articular facet or prezygapophysis (for articulation with the occipital condyles) and caudal articular facet or postzygapophysis (for articulation with the axis), transverse process, and right half of the dorsal (neural) arch. The left fragment comprises the caudal articular facet and transverse process only. The cranial articular facet is concave. The preserved portion of the dorsal arch shows no evidence for an atlantal foramen. An enclosed transverse foramen also appears to be absent, but there is a well-developed groove between the ventrolateral margin of the cranial articular facet and the base of the transverse process on the right side, resembling the morphology observed in Didelphis [46] and also the alar notch of the dog [57]. A similar, well-developed groove is present posteriorly, between the caudal articular facet and the transverse process. The right transverse process is complete; compared to that of Didelphis, it is more slender in AÜJM 2002–25, and it does not extend posteriorly as far as the level of the caudal articular facet; however, the transverse processes of the atlas of Didelphis are particularly well-developed.


The axis is only partially preserved, with the dorsal arch and transverse processes broken away (Fig 21).

Fig 21. Volume-rendered CT images of axis vertebra (C2) of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, dorsal view; D, ventral view. Abbreviations: atlf, atlantal facet (= prezygapophysis); caf, caudal articular facet (= postzygapophysis); da, dorsal arch; de, dens; flc, fossa for longus colli muscles; vmc, ventral median crest. Scale bar = 1 cm.

The atlantal (cranial) articular facet (= prezygapophysis) and dens are not connected, but are instead separated by a short and shallow sulcus. Due to the breakage to the left and right transverse processes, it is not possible to determine whether the transverse foramen was fully enclosed by bone or incomplete. In ventral view, a prominent fossa for the longus colli muscle (an important depressor of the head) is present bilaterally, either side of a prominent ventral median crest that extends from the posterior (caudal) margin of the axis to the dens. A similar morphology has been reported in the early Palaeogene marsupialiforms Pucadelphys and Mayulestes [39, 45].

Other cervical vertebrae.

An articulated series of five cervical vertebrae (C3-7) are preserved in AÜJM 2002–25 (Fig 1). However, most comprise the vertebral centra and partial neural arches only; C3 is one of the better preserved (Fig 22).

Fig 22. Volume-rendered CT images of cranial vertebra C3 of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, ventral view. Abbreviations: flc, fossa for longus colli muscles; tp, transverse process; vmc, ventral median crest. Scale bar = 1 cm.

Similar to the axis vertebra (C2), there is a prominent fossa for the longus colli muscle present bilaterally on the ventral surface of vertebra C3, as also seen in Mayulestes [39]. The articulations between the vertebrae occur both on the vertebral centra and on the zygapophyses. In all five cervical vertebrae, the articular surfaces on the centra are flat. C7 bears a pair of transverse foramina.

Thoracic vertebrae.

Nine vertebral centra preserved in AÜJM 2002–25 can be identified as coming from the thoracic region (Fig 1). The centra are mostly damaged, and they do not preserve any diagnostic morphology that would definitively identify them as coming from the thoracic series, such as long neural processes, or articular facets for ribs. However, given that the complete series of cervical and lumbar vertebrae are known for this specimen, by elimination they must represent thoracic vertebrae. Marsupials consistently have 19 thoracolumbar vertebrae, and this is likely also plesiomorphic for Metatheria as a whole [117]; given the presence of six lumbar vertebrae (see below), this implies that Anatoliadelphys would originally have had a total 13 thoracic vertebrae.c

Lumbar vertebrae.

A complete set of six articulated lumbar vertebrae (L1-6) are preserved (Fig 1), with L1, L2, L3 and L4 represented by the vertebral centrum alone. L5 is one of the best preserved of these (Fig 23): the tips of the transverse processes are broken, and the dorsal (neural) arch is partially preserved.

Fig 23. Volume-rendered CT images of lumbar vertebra L5 of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, dorsal view; D, ventral view; E, right lateral view. Scale bar = 1 cm.

On L6, the transverse process is complete on one side but broken on the other, the (dorsal) neural arch is present (although the neural process is missing), and the pre- and post-zygapophyses are broken.


AÜJM 2002–25 preserves the sacrum, which comprises three partially fused sacral vertebrae (Fig 24). The sacrum is robust, but damage to the sacral vertebrae means that relatively little else can be inferred about its morphology, including how many of the vertebrae articulated with the ossa coxae (innominate bones).

Fig 24. Photographs of sacrum of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, dorsal view; B, ventral view. Abbreviations: S1, first sacral vertebra; S2, second sacral vertebra; S3, third sacral vertebra. Scale bar = 1 cm.

Caudal vertebrae.

Five vertebrae can be identified as proximal caudal vertebrae, based on the size of their transverse processes (Fig 1); of these, Ca3 is one of the best preserved (Fig 25).

Fig 25. Volume-rendered CT images of caudal vertebra Ca3 of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, anterior view; B, posterior view; C, dorsal view; D, left lateral view. Abbreviations: prz, prezygapophysis; poz, postzygapophysis; tp, transverse process. Scale bar = 1 cm.

A single vertebra can be identified as a caudal vertebra belonging to the middle part of the series, based on its long vertebral body and lack of transverse processes. A group of vertebrae is here identified as representing distal caudal vertebrae because of their diminishing vertebral length. The total number of elements identified as caudal vertebrae is nine, but we identify multiple gaps in the size rank of the vertebral bodies, and so the total caudal vertebral count is clearly much greater than nine, probably at least 12. The preserved caudal vertebrae are quite broad mediolaterally, suggesting a relatively thick tail. However, it is impossible to accurately estimate the total length of the tail relative to body size.


The manubrium and four sternebrae are preserved (Fig 1). The morphology of these elements closely resembles those of marsupials, with the manubrium (Fig 26) having prominent lateral processes anteriorly for articulation with the first pair of ribs, and a distinct ventral keel that is particularly prominent towards the anterior end, suggesting the presence of a well-developed M. pectoralis [40, 45, 118].

Fig 26. Volume-rendered CT images of manubrium of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, dorsal view; B, ventral view. Scale bar = 1 cm.


Partial left and right scapulae are present, but the glenoid is the only region intact on both sides (Fig 1). The right scapular fragment also preserves parts of the cranial and caudal borders (Fig 27).

Fig 27. Volume-rendered CT images of right scapula of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, lateral view; B, medial view; C, distal view. Abbreviations: cp, coracoid process; gf, glenoid fossa; if, infraspinous fossa; sf, supraspinous fossa; sgt, supraglenoid tubercle; ssp, scapular spine. Scale bar = 1 cm.

The glenoid is a cranially-elongated oval shape. Unlike the condition in Didelphis, the coracoid process is distinctly separated from the supraglenoid tubercle by a deep, narrow sulcus, which is visible on both medial and lateral surfaces. The tip of the coracoid process is broken in almost identical locations on both the left and right scapular fragments, and so it is difficult to determine exactly how far it projected medially. The origin of the coracoid process is positioned relatively laterally (towards the midline of the glenoid cavity), and overall the base is broader than in Didelphis. Most of the scapular spine is missing, as is the entire acromion, and so it is not possible to infer the morphology of the hamatus process. Similarly, very little of the caudal border and none of vertebral border is preserved, and so the overall shape of the scapula (more rectangular versus more triangular) is uncertain. The posterior region of the neck lacks well-developed fossae for the M. teres minor and the caput longum of the M. triceps brachii [43, 57, 58]; Muizon (39) reported a similar morphology in Mayulestes and sparassodonts.


Both humeri are preserved in AÜJM 2002–25, but they differ in preservation. The right humerus is largely intact (Fig 28), but the left appears to have undergone plastic deformation of the distal part during fossilisation.

Fig 28. Photographs of right humerus of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, cranial (anterior) view; B, caudal (posterior) view; C, medial view; D, lateral view. Abbreviations: bg, bicipital groove; cap, capitulum; dpc, deltopectoral crest; dt, deltoid tuberosity; gtu, greater tuberosity; hh, humeral head; lec, lateral epicondylar crest; ltu, lesser tuberosity; mep, medial epicondyle; olf, olecranon fossa; raf, radial fossa; tl, tricipital line; tro, trochlea. Scale bar = 1 cm.

The intertubercular sulcus between the greater and lesser tubercles is deep. The head (= condyle) is separated from both tubercles by a shallow sulcus extending around its anterior perimeter. The separation between the head and the lesser tubercle appears to be more pronounced than that of Didelphis. In addition, the proximal portion of the head is more convex (almost spherical) when compared to that of Didelphis. The humeral head and greater tubercle are similar in height, as is usual for metatherians [119]. The head is positioned further posteriorly relative to the humeral shaft (i.e. it is distinctly “beaked” [47]) than that of Caluromys, but is similar in this regard to Didelphis.

In proximal view, the greater tubercle appears elongated and has an oblique anteromedial-posterolateral orientation, similar to that seen in Didelphis. The lesser tubercle is separated from the humeral head by a shallow groove, which opens anterolaterally into the intertubercular sulcus. The lesser tubercle is almost half the size of the greater tubercle; the lesser tubercle is also more rounded, and it is oriented nearly perpendicularly relative to the major axis of the greater tubercle. The lesser tubercle is lower than greater tubercle.

In mediolateral view, the shaft of the humerus appears weakly sigmoidal in shape, as in Didelphis, whereas that of Caluromys appears almost straight [43]. In medial view, the intertubercular sulcus (= bicipital groove) is pronounced. The sulcus is located on the anteromedial margin of the humerus. It is deepest proximally, and gradually becomes shallower distally. It extends as a distinct groove from the tubercles to almost the midpoint of the humerus. The medial wall of the groove is formed by the lesser tubercle crest, referred to as the crista tuberculi minoris in the dog [57]. At the distal end of the groove, the lesser tubercle crest first makes a very sharp medial projection as the teres tuberosity and then gradually tapers into the shaft. Interestingly, there appears to be no distinct lesser tubercle crest in Didelphis, and yet the teres tuberosity is prominent. The well-developed lesser tubercle crest in AÜJM 2002–25 indicates that the medial head of the M. triceps brachii was very well-developed, allowing powerful forearm extensions.

Laterally, the other wall of the intertubercular groove is formed by the deltopectoral crest, which extends slightly more distally than does the lesser tubercle crest. The deltopectoral surface is the area bound by the deltopectoral crest (medially) and the tricipital line (posterolaterally). In AÜJM 2002–25, the deltopectoral surface is triangular in shape, slightly concave, and faces anterolaterally. Compared to Didelphis, this surface is shorter, and relatively wider, and the tricipital line is more obvious. In Didelphis, the course of the tricipital line from its origin at the posterolateral edge of the greater tubercle to its fusion with deltopectoral crest is hard to identify in parts, and at times is only visible as weak muscle scars. In AÜJM 2002–25, the proximal half of the tricipital line (to which the M. triceps brachii caput lateralis attaches) runs straight distally, whereas the distal half bends medially and runs towards the deltopectoral crest, where together they form a ‘V’ shape. Throughout its course, there is no interruption in the definition of the tricipital line. Posteriorly, the fossa on the humeral shaft posterodistal to the lesser tubercle is shallow and runs two-thirds of the length of the lesser tubercle crest.

Distally, the most notable feature on the humerus is the mediolateral expansion of the distal end. This can be quantified as the Humeral Epicondylar Index (HEI = maximum distal width of the humerus/maximum length of the humerus [76]), which is 0.36 for AÜJM 2002–25. This HEI value is greater than in dasyurids and most didelphids (including Didelphis and Caluromys), but is similar to those of the didelphids Marmosa and Micoureus [76]. Parts of the lateral epicondylar crest (or supinator ridge) are broken in both the left and right humeri, but this crest was clearly well-developed. On the right humerus, only a small portion of the proximal aspect of the lateral epicondylar crest is broken, and so it can be seen that the crest spans approximately one-third of the total humeral length. However, the breakage on both left and right sides render the exact shape of the crest unclear.

In cranial view, the lateral epicondylar surface is concave. Distally, the capitulum is damaged on the right humerus, but intact on the left, which indicates a relatively spherical articular surface. There is a slight asymmetry between left and right humeri in terms of the depth of the radial fossa, with this fossa shallower on the right than on the left. The left radial fossa seems deeper than that of Didelphis, but this may be the result of post-mortem deformation. There is no continuous lateral extension (or “tail”) of the capitulum in AÜJM 2002–25; instead there is a distinct groove between the capitulum and the keel that forms the distolateral corner of the humerus. A capitular tail is found in Didelphis and other large didelphids (see character 56 of Horovitz and Sánchez-Villagra [119] and character 64 of Flores [40]), and also many fossil metatherians [28, 59], and it was found to be a synapomorphy of Metatheria by O’Leary et al. [98]; its absence in AÜJM 2002–25 is presumably a secondary loss. An oval-shaped entepicondylar foramen is present, but it is smaller than that seen in Didelphis. The trochlea has moderately well-defined crests, but is not as medially deflected as it is in Didelphis. In caudal view, the olecranon fossa is deeper than in Didelphis, but shallower than in Dasyurus.


Both left and right ulnae are preserved. The right ulna is practically complete, except that the proximal end is slightly damaged, and the styloid process is missing from the distal end (Fig 29). The bone is broken into several pieces, but the pieces fit together almost perfectly. The left ulna, however, is represented by the proximal half only.

Fig 29. Photographs of right ulna of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, cranial (anterior) view; B, caudal (posterior) view; C, medial view; D, lateral view. Abbreviations: an, anconeal process; cop, coronoid process; ol, olecranon process; rn, radial notch; trn, trochlear notch. Scale bar = 1 cm.

The ulna is the longest bone of the forelimb in AÜJM 2002–25. In cranial view, the shaft is distinctly bowed, such that the medial border is concave and the lateral border is convex. The ulna of Didelphis also appears bowed, but the overall degree of curvature is much less than that in AÜJM 2002–25. The curvature observed in AÜJM 2002–25 does not appear to be caused by skeletal pathology or the fossilisation process. In mediolateral view, the ulna as a whole shows a sigmoidal curvature, similar to that seen in Didelphis.

The Olecranon Process Length Index (OPLI = olecranon process length/total ulnar length [76]) in AÜJM 2002–25 is 0.18, but this is only approximate as the proximal end of the olecranon process is damaged and the styloid process is missing from the distal end. Nevertheless, this OPLI value is similar to that of Didelphis and much greater than that of Caluromys [76].

In cranial view, the olecranon process does not appear strongly medially inflected, nor does it appear medially twisted as it is in Asiatherium [120]. The curve of the posterior border of the olecranon process is less than in Caluromys, but similar to that seen in Didelphis (see character 71 of Flores [40]). The depression on the medial side of the proximal ulna is the fossa for the M. flexor carpi ulnaris [39]; this fossa is quite deep in Caluromys and Mayulestes, but varies in depth in Didelphis, although it is never as deep as it is in Caluromys. In AÜJM 2002–25, the fossa for the M. flexor carpi ulnaris is neither long nor deep (as it is in Caluromys), but it falls within the range of morphologies seen in Didelphis.

In medial view, the distal half of the trochlear notch is deeper and more concave (similar to Didelphis) than the proximal half, which is shallower and low (as in Caluromys). The anconeal process (the beak of the olecranon) is moderately salient, but not as high as in Didelphis. The width of the trochlear notch is similar to that seen in Didelphis. The orientation and the prominence of the coronoid process are also very similar to the morphology observed in Didelphis.

The radial notch is distolateral to the trochlear notch. In Didelphis, the boundary between the radial notch and the lateral humeral articular surface within the trochlear notch are clearly demarcated by a salient ridge. In AÜJM 2002–25, however, these surfaces are almost continuous on the right ulna; the left shows a line of separation between the two surfaces, but it does not approach the morphology seen in Didelphis. The articular surface of the radial notch is more laterally facing than in Didelphis, in which it faces more anteriorly. The radial notch does not appear to extend onto the lateral border of the coronoid process, whereas it does so in Didelphis and Caluromys.

In cranial view, the fossa for the M. brachialis and M. biceps is quite deep and medially positioned, and it is just distal to the coronoid process. The fossa is proximodistally-elongated and surrounded by two ridges running from the medial and lateral borders of coronoid process. The lateral ridge separates the brachialis fossa from another slight depression, which Muizon [39] referred to as the ‘supinator fossa’ in Mayulestes. The lateral border of the supinator fossa is formed by a salient supinator crest in Mayulestes [39]. In AÜJM 2002–25, the lateral border of the supinator fossa is not raised into a crest or a ridge, but at the distolateral corner of the supinator fossa this lateral border rises to form the interosseous crest. The interosseous crest is salient and extends distally along the entire length of the ulnar shaft, forming the craniolateral border of the shaft. This crest is not as sharp in cross section as it is in Caluromys or Didelphis, but it is still sharper and more salient than the equivalent crest in Sarcophilus. Viewing the ulnar shaft laterally, there is a fossa for the M. abductor pollicis longus, caudal to the interosseous crest: this fossa is well-marked proximally, but distally it gradually becomes shallower and eventually disappears. The morphology of this fossa is more similar to the condition seen in Didelphis than in Caluromys, in which this fossa extends for practically the entire length of the ulnar shaft.

Medially, the pronator crest (the origin of the M. pronator quadratus) at the distal end of the diaphysis is shorter but more prominent than in Didelphis, but less salient than in Caluromys. As already discussed, the styloid process is not preserved.


Both radii are preserved. The right radius is almost complete; there is a major crack in the midshaft and the two sides do not match up either side of the crack, but evidently no more than a few millimetres of the shaft are missing (Fig 30). The left radius preserves the distal three-quarters of the bone; the portion from the distal portion of the bicipital tuber to the radial head is missing. Proximally, the radial head appears rounded in proximal view, similar in shape to those of Didelphis and Caluromys, whereas it is transversely wider and more oval-shaped in some other metatherians (e.g. Asiatherium, Mayulestes, Pucadelphys, some sparassodonts, Thylacinus [28, 39, 120]). However, the facet for the humeral capitulum is deeper than that of Didelphis, possibly reflecting the fact that the capitulum is more spherical in AÜJM 2002–25 than in Didelphis. The size and the shape of the ulnar articular facet on the caudal side of the radial head are similar to the morphology seen in Didelphis.

Fig 30. Photographs of right radius of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, cranial (anterior) view; B, caudal (posterior) view; C, medial view; D, lateral view. Abbreviations: bt, bicipital tuberosity; sp, styloid process. Scale bar = 1 cm.

Along the shaft, the bicipital tuberosity is caudally very prominent, and is proportionately more salient than even the largest Didelphis specimens examined; this tuberosity is very weak in the fossil metatherian Mayulestes [39]. The bicipital tuberosity is proximodistally more distant from the radial head than in Dasyurus, but is similarly positioned to that of Didelphis. In medial view, there is a small but noticeable depression just anterior to the bicipital tuberosity. Didelphis lacks a similar depression, but Caluromys resembles AÜJM 2002–25 in this regard.

In caudal view, a ridge on the lateral side can be identified extending from approximately midpoint of the shaft to the proximal third. This ridge is the radial counterpart of the interosseous crest of ulna. A similar ridge can be identified in Didelphis, but the degree of cresting is much less than in AÜJM 2002–25. Caluromys, meanwhile, differs from AÜJM 2002–25 in that this interosseous crest extends along the entire radial shaft. Instead, the condition in AÜJM 2002–25 appears more similar to Dasyurus in this regard. Further distally, the ridge becomes identifiable again, forming the pronator crest. None of the Didelphis specimens examined for this study have a pronator crest as prominent as that in AÜJM 2002–25.

The cranial surface of the radial shaft is relatively flat, and is rectangular proximally. Both the medial and lateral borders of the anterior side merge around the midshaft, and then continue distally as a single well-defined lateral border. The lateral border terminates distally as the dorsal tubercle, which separates the sulcus for the tendons of the M. extensor digitorum communis (laterally) from the sulcus for the M. extensor carpi radialis (medially). Lateral to the M. extensor digitorum communis sulcus, there is no ridge marking the probable insertion of the M. abductor pollicus longus, and hence this muscle/tendon was probably not particularly strongly developed. Didelphis also lacks a prominent ridge for the M. abductor pollicus longus, but this ridge is very well-developed in Caluromys [39, 43]. Curvature of the radial shaft means that it is strongly convex cranially and concave caudally, to a greater extent than seen in Didelphis, but similar to that seen in the didelphid Monodelphis and the stem-marsupial Pucadelphys [43]. The cross section of the shaft is triangular throughout the length of the radius; however the apex of the triangle projects caudally in the proximal half, whereas it projects cranially in the distal half.

In distal view, the scapholunar articulation is oval and more concave than in Didelphis, and is also larger. The styloid process projects more vertically from the articular surface compared to the more gradual inclination seen in Didelphis. Viewed medially, the styloid process is almost hook-shaped, with a notch on its posterior margin; by contrast, in Didelphis it is straight, whereas in Sarcophilus it has a trochlear shape. The distal ulnar facet is restricted to the lateral margin of the distal radius, and is smaller than in Didelphis.

Os coxae.

Both ossa coxae (innominate bones) are preserved; they are both mostly complete, missing only the ischiopubic ramus and parts of the iliac crest (Fig 31). Damage to these elements and to the sacrum (Fig 24) means that it is unclear how many sacral vertebrae made contact with the ilium. The ilium is long, forming 61% of the total length of the os coxae; it is relatively flat and bladelike and flares laterally in dorsal view, as in dasyurids but unlike the condition in didelphids except Metachirus [39, 44, 48]. However, the iliac fossa does not appear as small in AÜJM 2002–25 as it is in dasyurids and Metachirus [44]. The iliopubic process (or eminence) is well-developed. The acetabulum is relatively spherical but somewhat elongated dorsoventrally. In dorsal view, there is a slight emargination of the dorsal acetabular rim, but the acetabulum is nevertheless fully enclosed dorsally. The acetabular notch is deep, and located on the caudoventral margin of the acetabulum. There is a distinct tuberosity for the M. rectus femoris anterior to the acetabulum, as in the fossil metatherians Herpetotherium, Mayulestes and Pucadelphys, whereas this is uncommon in extant marsupials, although it is seen in dasyurids [49, 119]. Damage means that the likely area of contact between the pubis and the epipubic bones cannot be identified.

Fig 31. Photographs of left os coxae (innominate) of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, dorsal view. B, medial view. C, lateral view. Abbreviations: ac, acetabular crest; acf, acetabular foramen; gf, gluteal fossa; if, iliacus fossa; ipe, iliopubic eminence; isp, ischatic spine; of, obturator foramen; trf, tuberosity for M. rectus femoris. Scale bar = 1 cm.

Epipubic bones.

Both epipubic (marsupial) bones are preserved intact (Fig 1); they appear relatively robust but are otherwise unremarkable and lack distinctive morphological features.


Both femora are preserved. The left femur was in contact with the pelvis when AÜJM 2002–25 was excavated. However, in the process of preparing the specimen, it became clear that the femur had been displaced superiorly with respect to the os coxae during fossilisation, and the head was no longer in articulation with the acetabulum; thus, the left femur was also removed from the matrix. The only major structure missing from the right femur is the intertrochanteric crest. However, the left femur is better preserved overall (Fig 32).

Fig 32. Photographs of left femur of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, cranial (anterior) view; B, caudal (posterior) view; C, medial view; D, lateral view. Abbreviations: fh, femoral head; icg, intercondylar groove; lc, lateral condyle; le, lateral epicondyle; ltr, lesser trochanter; mc, medial condyle; me, medial epicondyle; tro, trochlea; trf, trochanteric fossa; ttr, third trochanter. Scale bar = 1 cm.

The overall shape of the femur is broadly similar to that of Didelphis, although proportionately it is slightly more robust. Unlike the straight femur of Didelphis, the bone appears curved in cranial view, with the medial margin convex and the lateral margin concave, especially in the distal two thirds. In lateral view, the proximal epiphysis seems to be positioned slightly more cranially than that of Didelphis, and is more similar in this regard to Caluromys. When viewed medially, laterally, or proximally, the femoral head is also positioned more cranially relative to the greater trochanter in AÜJM 2002–25 than in Didelphis, but is similarly positioned to that of Caluromys. The femoral head is more spherical and rounded than that of Didelphis, but the anteroposterior dimension of the femoral head is slightly larger than the mediolateral dimension.

On the right specimen, the epiphysial surface surrounding the cranial half of the femoral head is damaged, and this damage extends laterally as far as the contact between the head and the neck. The preservation of the head on the right femur is better, but there is a crack running around the entire perimeter of the contact between the head and the neck, which makes it difficult to interpret. As a result, it is difficult to determine whether or not the proximolateral part of the articular surface extends onto the femoral neck. However, as far as can be judged, the condition in AÜJM 2002–25 seems to be more similar to that of Dasyurus and Sarcophilus, both of which show little expansion of the articular surface onto the neck compared to Didelphis and Caluromys. A shallow depression can be seen on the caudomedial quadrant of the head of the right femur, positioned towards the centre. If this is the fovea capitis (for attachment of the ligament of the femoral head), than it is in the practically same spot as it is in Didelphis. The head of the left femur is too weathered to provide any unequivocal information regarding the position of the fovea capitis.

In craniocaudal view, the greater trochanter appears roughly the same height as the femoral head, as in most metatherians [49, 119]. On the lateral edge of the greater trochanter, the site of attachment for the M. gluteus medius and M. gluteus profundus is salient and crestlike. In proximal view, the highest point on the greater trochanter is a medially-positioned, salient tubercle, which is probably the origin for the M. piriformis [44]. There is no prominent fossa on the anterior face of the greater trochanter, which houses the M. vastus lateralis [39, 44]. However, there is a wide and shallow depression distomedial to the greater trochanter, which continues a short distance distally.

The lesser trochanter is better developed in AÜJM 2002–25 than in Didelphis, and more like the condition in the dasyurids Dasyurus and Sarcophilus, in which the lesser trochanter extends further proximally towards the femoral head; however, the lesser trochanter extends further medially in Dasyurus, to a point close to or level with the medial edge of the femoral head [44]. The lesser trochanter of AÜJM 2002–25 also resembles that of Sarcophilus in its degree of distal extension (to approximately 25% of the total length of the bone). AÜJM 2002–25 differs from Caluromys in that the lesser trochanter is twice as long proximodistally as it is wide mediolaterally; in Caluromys these two dimensions are almost equal [44]. In didelphids, the third trochanter is either missing (e.g. Didelphis), or only visible as a faint scar line (e.g. Caluromys, Metachirus), and it is also uncommon in other marsupials, whereas it is found in several stem-marsupials, including Herpetotherium and Mayulestes [39, 47, 49, 51, 80]. The third trochanter is a prominent, flaring tubercle in AÜJM 2002–25; it differs from that of Mayulestes, which is more obviously continuous with the crestlike lateral border of the greater trochanter [39].

On the caudal side of the proximal femur, the intertrochanteric fossa is shallower than in Didelphis and Caluromys. However, the proximodistal extension of this fossa is longer than in Didelphis, and it extends mediodistally into the concave surface of the flaring lesser trochanter. Just proximal to this opening, there is a salient tubercle, which lies on the elevated surface that forms the medial border of the intertrochanteric fossa.

In medial and lateral views, the femoral shaft appears smooth and straight. However in cranial view, a concavity is noticeable on the lateral side, starting from the level of third trochanter and extending to the lateral condyle. Similarly, the medial margin has a sigmoid shape. The degree of distal curvature somewhat resembles the condition in the dasyurids Sarcophilus and Dasyurus; however, because dasyurids lack a third trochanter, the degree of curvature does not appear as exaggerated as in AÜJM 2002–25.

Distally, the anterior surface of the bone bears a well-developed trochlea, as in Herpetotherium [49], although it is unclear whether a patella was present or not; the patella is absent in most marsupials, but it is present in the stem-marsupial sparassodonts [121]. The medial and lateral crests of the trochlea are similar in height, and the trochlear surface is relatively symmetrical. Neither the medial nor the lateral sides of the trochlea seem to extend proximally onto the diaphysis. The distal portion of the femoral shaft, just proximal to the trochlea, bears a sulcus for the M. vasti and M. rectus femoris tendons [39]. The medial epicondyle is slightly wider than the lateral one, but the lateral epicondyle projects further beyond the edge of the femoral shaft, possibly reflecting contact with the fibula. The medial epicondyle and condyle are deeper proximodistally because they extend slightly more distally than the lateral epicondyle and condyle, as can be seen visible in both cranial and caudal views. In caudal view, the medial and lateral condyles appear similar in width, but the medial condyle is deeper proximodistally, extending further both proximally and distally.


Both tibiae are preserved. Both are complete, but there are some preservational differences between the two. The distal epiphysis of the right specimen was disarticulated when excavated; it was found later in the matrix, but the proximal surface on the epiphysis and the distal surface on the diaphysis were damaged to such an extent that the fit between two fragments is not a good one. The left tibia is broken, but the fits between all the breaks seem to be close, suggesting that relatively little bone has been lost (Fig 33).

Fig 33. Photographs of left tibia of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, cranial (anterior) view; B, caudal (posterior) view; C, medial view; D, lateral view. Abbreviations: ice, intercondylar eminence; lc, lateral condyle; mc, medial condyle; mm, medial malleolus; ttu, tibial tuberosity. Scale bar = 1 cm.

Similar to the femur, the tibia of AÜJM 2002–25 is proportionately more robust than that of Didelphis. In cranial and caudal views, the tibial shaft is sigmoidal in shape: the medial border of the shaft is initially concave, but this changes further distally, towards the midpoint of the shaft. In medial and lateral views, the tibia is strongly curved craniocaudally, with a concave caudal border and convex cranial border. The right tibia is more curved than the left, especially distally, but no significant deformation or pathology is identifiable on either bone. The left tibia is more broken, and the degree of craniocaudal curvature may have been artefactually reduced when the pieces were reassembled. However, the fit between the preserved pieces appears very close, and so we assume that the left specimen preserves the “true” degree of curvature. However, even when compared to the straighter left tibia of AÜJM 2002–25, most didelphids (with some exceptions, e.g. Chironectes–see character 99 of Flores [40]) show a lesser degree of craniocaudal curvature of the tibial shaft; in this regard, AÜJM 2002–25 more closely resembles the stem-marsupials Mayulestes and Pucadelphys [39, 44].

In proximal view, the craniocaudal length of the proximal epiphysis is relatively short. However, the overall morphology of the proximal epiphysis is broadly similar to that of Didelphis. The tibial tuberosity is prominent, and is almost as large as that of Didelphis. The lateral condyle has a slightly convex articular surface, which is roughly triangular in shape. The proximal fibular facet occupies the entire caudal border of the lateral condyle. The medial condyle is approximately “reniform” or bean-shaped, and is slightly lower than the lateral condyle. The lateral half of the medial condyle is excavated and deeper than the medial half. The intercondylar eminence is wider than in Didelphis.

In cranial view, there is no obvious tibial crest proximally (unlike the stem-metatherian Herpetotherium [49]), but ~30–50% of the way from the proximal end, the tibial shaft becomes mediolaterally narrower, and a smooth, rounded ridge is formed that continues distally. The lateral tibial fossa, positioned on the proximal shaft just distal to the epiphysis, is shorter but deeper than that of Didelphis, and in this regard is more similar to that of Dasyurus. The medial tibial fossa is only identifiable on the right specimen; it differs from the condition in Didelphis, in which it is flat. However, this fossa is shallower in AÜJM 2002–25 than in Caluromys.

On the posterior side of the proximal tibia, the fossa just distal to the popliteal notch is deeper than in Didelphis, resembling Mayulestes in this regard. The distal two-thirds of the shaft is mediolaterally compressed. The degree of compression of the distal shaft is broadly comparable to that of Didelphis and Dasyurus, but in those taxa the cresting forms at the distal third of the bone and becomes increasing well-developed distally.

The facet for the fibular articulation is on the lateral side of the distal epiphysis, and occupies the whole of the lateral margin. With the exception of the distal epiphysis on the right tibia, all of the epiphyses appear fused with the diaphyses. However, as is common in living marsupials [122], the suture lines are usually visible. The distal epiphysis bears the medial malleolus, which is higher and more prominent than in Didelphis. The lateral facet for the astragalus is reniform in shape, smooth and has a caudoproximal-to-craniodistal slope. The slope seems to be shallower than that seen in Didelphis; however the degree of slope is difficult to judge because the bone itself also bends caudally. In lateral view, the medial astragalotibial facet on the lateral side of the malleolus makes a sharp, almost vertical contact with the lateral astragalar astragalotibial facet. This differs from the condition in Didelphis, in which the contact is more gradual, and the angle between the two surfaces is wider. In therians, the distal articular surface of the tibia for the astragalus bears two distinct facets for contact with the astragalus: the medial and the lateral astragalotibial facets. In some metatherians, there is a caudal extension of the lateral astragalotibial facet, referred to as the “posterior astragalotibial facet” [56], which is typically separated from the medial astragalotibial facet by a distinct notch. The lateral astragalotibial facet appears to be slightly extended caudally in AÜJM 2002–25, but much less so than in the posterior astragalotibial facet of some marsupials, and there is no distinct notch between this extension and the medial astragalotibial facet.


Both left and right fibulae are preserved, but neither is complete (Fig 1). The proximal and distal ends are intact in both fibulae. In the right specimen, the entire shaft is also preserved, but a major break is present approximately one-third the distance from the end of the shaft, and the matching contacts between the proximal and distal parts are minimal (Fig 34). As a result, the full intact morphology of the fibula cannot be ascertained, although the shaft appears relatively straight, as in other metatherians [44].

Fig 34. Volume-rendered CT images of right fibula of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, medial view of proximal end; B, lateral view of proximal end; C, medial view of distal end; D, lateral view of distal end; E, proximal (dorsal) view of proximal end; F, distal (ventral) view of distal end. Abbreviations: AFi, astragalofibular facet; CaFi, calcaneofibular facet;? fef,? femoral facet; gr, groove for M. peroneus brevis, M. peroneus longus and M. extensor digitorum lateralis; pff, parafibular (fabellar) facet; tf, tibial facet. Scale bar = 1 cm.

Overall the fibula is more robust than that of Didelphis. In proximal view, the proximal epiphysis is large and laterally flaring as in Didelphis, but less than in Caluromys [44]. The craniomedial part of this epiphysis bears the proximal tibial facet. In Didelphis, this facet is deep, concave, and almost saddle-shaped, and it is even deeper in Caluromys. In AÜJM 2002–25, the proximal tibial facet is still concave, but it is shallower than in Didelphis. There is a tubercle on the anteromedial side of the flare, just distal to the proximal tibial facet, but this tubercle is smaller than in Didelphis. In Caluromys, this tubercle is the site of origin of the M. extensor digitorum longus and M. peroneus brevis [44].

When the proximal epiphysis is viewed mediolaterally, the proximalmost point of the parafibular (fabellar) facet is identifiable as a distinct apex. The facet is flat and steep, with its long axis oriented from medioproximal to laterodistal. There is a small groove anteromedial to the apex that separates it from what is probably a facet for contact with the femur (unless it is for the tendon of the M. gastrocnemius externus).

Proximally, the cross-section of the shaft appears mediolaterally compressed, but distally it gradually becomes wider: at a distance of approximately one third of the total shaft length from the proximal end, it is nearly as wide mediolaterally as deep craniocaudally. However, the fibula is deeper craniocaudally than it is wide mediolaterally throughout its entire length. A craniomedial crest originates from the tubercle for the M. peroneus brevis and extends distally as far as the distal 25% of the length of the bone, at which point it becomes smoother and bifurcates. The lateral bifurcation extends as far as the malleolus, whilst the medial bifurcation ends at the distal tibial facet. In life, this crest probably served as an attachment for the interosseus membrane, which was also attached to the crest on the anterolateral side of the tibia.

The shape of the shaft appears to differ somewhat between the left and right fibulae. Distally, the shaft seems to curve slightly caudally on the left side, whereas the shaft of the right fibula appears straight in all views. However, it is not clear which is the real condition, because both bones are fragmented. Some Didelphis specimens exhibit a caudal curvature of the distal shaft, but to a lesser extent than in AÜJM 2002–25.

The distal epiphysis bears a groove visible in lateral view, which is probably for the tendons of the M. peroneus brevis, M. peroneus longus and M. extensor digitorum lateralis. This groove is weaker than that seen in Didelphis, which is in turn weaker than that in Caluromys. Compared to Didelphis, the malleolus is smaller in lateral view and it does not seem to extend as far laterally when viewed cranially. The medial side of the distal epiphysis is rounded and articulates with the tibia. In distal view, the astragalofibular facet is roughly triangular in shape. In the same view, there is a deep depression separating the malleolus from the astragalofibular facet. It seems likely that malleolus contacted the calcaneus, and there is also evidence for a calcaneofibular facet on the calcaneus, lateral to (and continuous with) the ectal facet (see below).


Both calcanei are complete and well-preserved (Fig 35). Overall, the calcaneus is relatively robust, especially the calcaneal tuber, which is dorsoventrally very deep. In dorsal view, the tuber is distinctly inflected medially. The ectal (posterior calcaneoastragalar) facet is almost round: its longest axis is anteroposterior, but it is nearly as large mediolaterally and anterolaterally-to-posteromedially. A faint ridge extending anterolaterally from the midpoint of the posterior border of the ectal facet, coinciding with a slight change in facet curvature, probably represents the border between the “true” ectal facet (medially) and a facet for articulation with the fibula (laterally); the morphology of the distal fibula also suggests fibula-calcaneus contact (see above).

Fig 35. Volume-rendered CT images of left calcaneus of holotype of Anatoliadelphys maasae (AÜJM 2002–25).

A, dorsal view. B, ventral (plantar) view. C, distal view. D, medial view. E, lateral view. Abbreviations: at, anterior plantar tubercle; ccf, calcaneocuboid facet; CaFi, calcaneofibular facet; ecf, ectal facet; gtpl, groove for the tendon of M. peroneus longus;? pccl,? pit for plantar calcaneocuboid ligament; pp, peroneal process; sc, sulcus calcanei; suf, sustentacular facet. Scale bar = 1 cm.

The sustentaculum is roughly rectangular in outline. The sustentacular facet extends the entire length of the dorsal surface of the sustentaculum, terminating anteriorly at the medial margin of the calcaneocuboid facet. A wide calcaneal sulcus separates the sustentacular facet from the ectal facet. The sustentacular facet faces somewhat medially at its anterior end, but more dorsally further posteriorly; nevertheless, it seems likely that the degree of superposition of the astragalus on the calcaneus was greater than in the stem-marsupials Herpetotherium [49], Mayulestes [44] and Pucadelphys [47].

There is a distinct raised area at the anterodorsal margin of calcaneus, anterior to the ectal facet and anteromedial to the sustentacular facet. This is unlikely to be a facet for contact with the astragalus, as is (for example) the distal calcaneoastragalar facet seen in dasyuromorphians [56]; this is because the sustentacular facet of AÜJM 2002–25 is large and extends the entire length of the sustentaculum, and the raised area is distinctly medial to the sustentacular facet, whereas the distal calcaneoastragalar facet of dasyuromorphians is immediately anterior to the sustentacular facet. Instead, this raised area is probably for attachment of the anterior (or dorsal) astragalocalcaneal ligament and/or the M. extensor digitorum brevis.

The peroneal process is prominent, but it does not extend anteriorly beyond the level of the calcaneocuboid facet. There is a well-developed groove for the tendon of the M. peroneus longus on the dorsolateral surface of the peroneal process; the medial wall of this groove is particularly prominent and dorsally extensive.

In ventral view, the sustentaculum is triangular in outline. A well-marked groove on the ventral surface of the sustentaculum, towards its medial edge, probably housed the tendons of the M. flexor digitorum fibularis (= M. flexor hallucis longus) and the M. flexor digitorum brevis. Lateral to the anterior part of the sustentaculum, in line with the medial edge of the calcaneal tuber, a raised area represents the anterior plantar tubercle, to which would have attached the plantar calcaneocuboid ligament. Immediately lateral to this, and extending further anteriorly, is a very well-marked pit; this pit clearly did not house a proximal extension of the cuboid like that seen in didelphids [56] because it is not continuous with the calcaneocuboid facet, but rather is enclosed anteromedially by a sharply-defined wall. Instead, it probably represents an additional area of attachment of the calcaneocuboid ligament; a similar fossa or groove has been reported in the sparassodont Lycopsis [54] and a few other mammals [123, 124].

In distal view the calcaneocuboid facet is roughly trapezoidal in shape, and is concave. It is not subdivided into distinct facets with different orientations (as seen in some metatherians [49, 51, 56, 125]), but rather forms a single, relatively continuous surface. A distinct groove or fossa immediately lateral to the lateral margin of the calcaneocuboid facet is presumably for the lateral calcaneocuboid ligament.

Compared to other fossil metatherian calcanei known from the early Palaeogene, that of AÜJM 2002–25 shows the greatest overall (phenetic) resemblance to the “Itaborai Metatherian Group” (IMG) III morphotype from the? early Eocene Itaborai fauna of Brazil, and the “Bridger Metatherian Group” (BMG) I morphotype from the middle Eocene Bridger formation of North America, both of which were described by Szalay (56).


AÜJM 2002–25 preserves two metapodials (Fig 1). One of these is complete and bears a distinct lateral hook-like projection, allowing it to be confidently identified as the fifth metatarsal. The proximal surface, which is the only feature that allows a metapodial to be identified as either metacarpal or metatarsal, is broken in the second specimen. This specimen is neither the first nor the fifth metatarsal, but no more precise identification can be made.


AÜJM 2002–25 preserves four proximal and two intermediate phalanges (Fig 1). Only two of the proximal phalanges are complete: of these, one has a longer and more slender shaft and a sharp distal articular surface, whereas the other shows a more robust and shorter shaft, with a wide distal articular head. The morphology of the former is more consistent with identification as a pedal proximal phalanx, whereas the latter agrees more with the typical morphology of manual phalanges. The remaining two proximal phalanges preserve no diagnostic feature that would allow them to be identified as either manual or pedal. The two intermediate phalanges are also broken, and hence they also cannot be identified as belonging to either the manus or the pes.

Body mass estimate

Total length of the intact part of the left mandible of AÜJM 2002–25 is 88.2 mm. Using the total jaw length regression equation of Myers [65] for his “dasyuromorphian” dataset and taking into account the “smearing estimate” gives a body mass estimate of 3.37 kg for AÜJM 2002–25, with a range of 2.76–3.97 kg when the percentage error is taken into account. Given that the left mandible is slightly damaged anteriorly, this is undoubtedly a slight underestimate, and so a body mass of 3–4 kg (similar to a typical domestic cat, or a male spotted quoll [Dasyurus maculatus]) seems probable.

Morphofunctional analysis

Dentition and cranium.

The preserved dentition of AÜJM 2002–25 comprises robust canines, three premolars that increase markedly in size posteriorly (with P3 and p3 large and very broad) and four molars that also increase markedly in size posteriorly. The large, labiolingually broad P3/p3 and the extreme wear of the postcanine dentition are suggestive of durophagy. The exact functional significance of the peculiar, more-or-less continuous wear surface formed by m1, m2 and the trigonid of m3 (more clearly seen on the left mandible) is unclear, but presumably reflects the consumption of particularly abrasive food items.

In general, hypercarnivorous mammals are characterised by a suite of characteristic molar features [66]. On the upper molars, the postmetacrista is elongate and often has a carnassial notch, and the paracone is reduced, while on the lower molars the paraconid is tall, the paracristid is tall and blade-like and often has a carnassial notch, and the metaconid is reduced; collectively, the morphology of the upper and lower molars reflects an increased emphasis on postvallum-prevallid shear. In addition, the protocone of the upper molars and talonid of the lower molars are also usually reduced, reflecting reduced emphasis on crushing. Anatoliadelphys exhibits only some of these features (Figs 25 and 1219): the postmetacrista and paracristid are relatively elongate (particularly on M3 and m4 respectively), but neither crest has a distinct carnassial notch, and the paraconid is very low (rather than tall) on the lower molars. The protocone is also prominent and anteroposteriorly broad, and the talonid with which it occludes is similarly well-developed, reflecting a well-developed capacity for crushing. The latter may reflect durophagy or, alternatively, a meso- or hypo-carnivorous (rather than hypercarnivorous) diet.

The cingula that extend along the anterior and posterior margins of the upper molars are distinctive features of Anatoliadelphys. It has often been suggested that the function of dental cingula is to prevent damage to the gingiva from impacted food items and/or the cusps of occluding teeth [126129]. However, a recent study using finite element analysis of simplified “virtual” tooth models concluded that dental cingula may function to reduce tensile strains in the enamel caused by forces generated when consuming soft foods, with partial cingula particularly effective at reducing strains generated by asymmetrical loads [130]. Regardless, the functional significance of the dental cingula of Anatoliadelphys is not obvious, for several reasons. Firstly, whilst the upper molar cingula are relatively well-developed in Anatoliadelphys, the anterior cingulid (precingulid) and posterior cingulid (postcingulid) on the lower molars are extremely weakly developed or absent. Secondly, the presence of such upper molar cingula is rare within metatherians (see character 50 of Williamson et al. [28, 131]). Thirdly, although the study of Anderson et al. [130] found that a dental cingulum is of greater functional importance under “soft-food” forces than under “hard-food” forces, the craniodental morphology of Anatoliadelphys strongly suggests some degree of durophagy.

The five dental indices of Zimicz [67] for Anatoliadelphys and a range of other faunivorous metatherians are shown in Table 3. When considered individually, these indices support different interpretations for the diet of Anatoliadelphys. Following the critical values proposed by Zimicz [67], a Relative Grinding Area index (RGA) of 0.65 suggests mesocarnivory, whilst Premolar Shape (PS) and Relative Premolar Size (RPS) indices of 0.70 and 2.89 respectively are congruent with its being a bonecracker or other durophage. A Relative Premolar Length index of 0.75 suggests hypercarnivory, whilst a Relative Blade Length (RBL) index of 0.61 indicates hypocarnivory.

Table 3. Body masses and morphofunctional dental indices (from Zimicz [67]) for Anatoliadelphys and other carnivorous metatherians weighing <10 kg.

RGA (Relative Grinding Area) = square root of the area of the talonid of m4/length of m4; RPS (Relative Premolar Size) = width of the largest lower premolar/cube root of body mass in kg; PS (Premolar Shape) = width of the largest lower premolar/length of largest lower premolar; RPL (Relative Premolar Length) = length of largest lower premolar/length of m4; RBL (Relative Blade Length) = length of the trigonid of m4/total length of m4. The dagger symbol (†) indicates fossil taxa.

A principal component analysis of all five dental indices for Anatoliadelphys and a wide range of fossil and modern metatherians (Fig 36) places Anatoliadelphys closest to the fossil stagodontids Eodelphis and Didelphodon, with which it shares high values for Principal Component (PC) 1. Higher values of PC1 indicate a larger Relative Premolar Size (RPS) index, and so plausibly represent increasing durophagy. Numerous papers have proposed that stagodontids were specialised durophages [29, 75, 101, 145147], and it is striking that Anatoliadelphys, Eodelphis and Didelphodon all show greater PC1 and RPS values than the living bone-cracker Sarcophilus; however, it should be noted that they considerably smaller in terms of body mass than Sarcophilus, and it seems plausible that RPS does not need to be as large for effective processing of hard food items in larger-bodied taxa. A possible example of this is the late Oligocene sparassodont Australohyaena antiqua, which has an estimated body mass of approximately 70 kg (i.e. nearly ten times larger than that of Sarcophilus), and has an RPS of 2.32, which is less than the critical value proposed by Zimicz [67, 68] as indicating durophagy (RPS ≥ 2.6), even though its skull shows numerous probable bone-cracking specialisations [148].

Fig 36. Principal component analysis of five morphofunctional dental indices for Anatoliadelphys maasae and other carnivorously-adapted metatherians.

The morphofunctional dental indices used were Relative Grinding Area (RGA), Relative Premolar Size (RPS), Premolar Size (PS), Relative Premolar Length (RPL) and Relative Blade Length (RBL). The plot shows the first two principal components (PCs) only.

Using the method of Therrien [76], as modified for metatherians by Wilson et al. [77], estimated dorsoventral bending force (Zx/L) at c1 for the ~3-4kg Anatoliadelphys maasae (Zx/L = 0.013) is similar to that for the extant didelphid Didelphis virginiana (Zx/L = 0.015), which has an average mass of ~2.5 kg [70]. However, this is considerably less than in the Late Cretaceous stagodontid Didelphodon vorax (Zx/L = 0.023), which weighed up to 5.2 kg [75], or the much larger (~8.2 kg [70]) extant dasyurid Sarcophilus harrisii (Zx/L = 0.074; Table 4). The mandible of A. maasae is predicted as being capable of being able to resist high forces more posteriorly, largely due to the dorsoventrally deep mandibular body, particularly in the region of m3 and m4; estimated dorsoventral bending force immediately posterior to m4 is ~40% greater in A. maasae (Zx/L = 0.062) than in D. vorax (Zx/L = 0.044), and nearly twice that of D. virginiana (Zx/L = 0.035). Estimates of bite force in A. maasae will require further testing, for example via finite element analysis of the mandible [149], or by discovery of more complete cranial remains that might allow calculation of bite force using the “dry skull method” [72, 73]; nevertheless, its mandibular morphology clearly indicates that it was capable of generating high bite forces relative to body size, particularly towards the back of the jaw.

Table 4. Measurements and calculations of mandibular bending strength for Anatoliadelphys maasae, Didelphodon vorax, Sarcophilus harrisii and Didelphis virginiana, based on the methods of Therrien [74], as modified for metatherians by Wilson et al. [75].

Values for Anatoliadelphys maasae are from this study; values for the other taxa are taken from Wilson et al. [75]. Ix = second moment of area about the labiolingual axis; Zx = bending strength in the dorsoventral plane; Iy = second moment of area about the dorsoventral axis; Zy = bending strength in the labiolingual plane.

Sarcophilus harrisii is the smallest bone-cracking mammal alive today, weighing ~8kg, ~2-3x larger than Anatoliadelphys. It is unclear whether there is a lower limit on body size for bone-cracking to be a feasible dietary strategy. Nevertheless, the comparatively small size of Anatoliadelphys relative to known bone-cracking mammals may be an indication that it was not a bone-cracker, but instead consumed other hard food items such as hard-shelled invertebrates (as has been proposed for the enigmatic fossil marsupial Malleodectes) [150, 151].

The prominent sagittal crest of Anatoliadelphys, probably approximately similar in size to that of Didelphis, indicates that the temporal musculature was well-developed. The area of origin of the deep masseter on the ventrolateral surface of the zygomatic process and the posterior shelf of the masseteric fossa are also prominent, suggesting that the masseter muscles were also well-developed. Collectively, the powerfully-developed jaw muscles suggest a high bite force, congruent with the large, very broad P3 and p3, which presumably had a crushing function.

A prominent nuchal crest, as seen in Anatoliadelphys, is usually interpreted as indicating strongly-developed neck musculature, indicative of powerful dorsoventral and lateral movements of the head and neck [45]. In turn, this has been argued to be suggestive of predatory behaviour; Didelphis, which shows a similar degree of development of the nuchal crest to that seen in Anatoliadelphys, subdues prey items by violently shaking them from side to side [152, 153], as do dasyurids [154, 155]. However, it may instead simply reflect the presence of a large head relative to body size, which requires well-developed neck muscles to support it.

In summary, the known craniodental morphology of Anatoliadelphys suggests that this animal was specialised for durophagy (based on its large, very broad P3 and p3), and was capable of generating high bite forces (based on its robust mandible and prominent jaw muscle attachments). However, it was probably not a hypercarnivore, but instead had a more generalised, meso- or hypo-carnivorous diet, based on the absence of a very elongate, notched postmetacrista and tall, notched paracristid, and the presence of a robust protocone and well-developed talonid.


The glenoid of the scapula of Anatoliadelphys is a cranially-elongated oval (“pear”) shape, as is typical of most mammals, with the exception of cursorially-specialised forms [43]. The rounded (rather than transversely compressed) humeral head that is slightly higher than the greater tubercle suggests considerable mobility of the shoulder, congruent with some degree of climbing ability [39, 43, 48]. The humeral head protrudes posteriorly further than in the aboreal didelphid Caluromys, which might indicate a lesser range of movement at the scapulo-humeral joint [43], but the articular surface faces more posteriorly than proximally, and the overall morphology is broadly similar to the condition in other didelphids and the stem-marsupials Pucadelphys and Mayulestes [43]. The well-developed teres tuberosity indicates a powerful M. teres major, which is a flexor of the shoulder; the teres tuberosity is large in both arboreal and semi-fossorial therian mammals [58], but is also associated with a relatively abducted forelimb position, which is likely plesiomorphic for therians. The deltopectoral crest is prominent, particularly at its distal end, but extends distally only to about the mid-point of the humerus (deltopectoral crest length/total humeral length = 0.47). A short but strongly-developed deltopectoral crest is characteristic of some arboreal didelphids (e.g. Caluromys, Glironia; [41, 43]), where it may reflect powerful grasping, but it is also seen in some semi-fossorial taxa, e.g. the sciurids Cynomys and Marmota [58].

The radial and olecranon fossae are deeper than in the arboreal didelphid Caluromys, and the olecranon fossa is slightly deeper than in the more scansorial Didelphis, but much shallower than in Dasyurus and Sarcophilus [43, 52]. The crests of the humeral trochlea are not particularly well-developed, although somewhat more prominent than in arboreal didelphids Caluromys and Glironia [41, 43], and the articular surface of the trochlea is not extensive proximally either cranially or caudally. Together with the relatively shallow trochlear notch and only moderately prominent anconeal process of the ulna, this indicates that the elbow joint of Anatoliadelphys was more stabilised than in arboreally-specialised marsupials, but less so than in the more terrestrially-adapted dasyurids and didelphid Metachirus, or the stem-marsupial Mayulestes. This suggests that Anatoliadelphys was capable of climbing, but that it did not have particularly agile, rapid movements.

The relatively spherical capitulum would allow considerable pronation and supination of the forearm. The entepicondyle is well-developed and protrudes medially, as in all didelphids except Metachirus [43, 48], indicating the presence of powerful flexors of the manus and digits; unlike the condition in the stem-marsupial Mayulestes, it does not protrude distomedially [39]. Although broken, the supinator crest is also prominent, suggesting that the extensors of the manus and digits, and the supinator of the forearm, were also well-developed.

The olecranon process of the ulna appears longer than in dasyurids and arboreal didelphids [43, 52]; proportionately, the relative size of the olecranon process appears similar to that of the terrestrial didelphid Monodelphis and the stem-marsupial Mayulestes [39, 43]. The olecranon process is not as long proportionately as in the semi-fossorial bandicoots and bilby [156] or in other semi-fossorial and fossorial mammals [76, 157], and nor is it obviously medially inflected, suggesting that Anatoliadelphys was not specialised for digging. The caudal margin of the olecranon is not inclined cranially towards its proximal end, whereas a strong incline is seen in arboreal didelphids and several other arboreal mammals [43, 48, 58]. The anconeal process is more prominent and the trochlear notch is deeper than in arboreal didelphids, but less than in the terrestrially-specialised Metachirus [43].

The radial head is rounded, similar in shape to those of Didelphis and Caluromys, whilst the facet for the humeral capitulum is deeper than that of Didelphis. This, together with the spherical capitulum, indicates considerable capacity for pronation and supination, which is suggestive of locomotion over uneven substrate, and probably also the capacity to climb [40, 47, 48]. This interpretation is supported by the very prominent bicipital tuberosity, and the strongly curved radial shaft (similar in morphology to that seen in the didelphid Monodelphis and the stem-marsupial Mayulestes [43]); the latter feature would have provided space for a very large M. flexor digitorum profundus [43].

The most striking feature of the os coxae (innominate bone) of Anatoliadelphys is the laterally everted ilium, which would have provided a larger insertion area for the M. longissimus dorsi (the major extensor of the back) and more space for the gluteal muscles [39, 44, 48, 58]. The ilia of most didelphids are relatively straight, but lateral eversion of the ilium is seen in the agile Metachirus, dasyurids and Mayulestes [39, 44, 48]. The presence of a laterally everted ilium, indicating more powerful epaxial musculature, has often been interpreted as evidence of greater agility, possibly including leaping [39, 44, 48, 58]. However, several non-agile mammals, such as the koala, wombat, bears and anteater, also exhibit a laterally everted ilium [39, 58], reflecting changes in the orientation of the lever-arm of the gluteal muscles [158]. Anatoliadelphys differs from agile mammals such as Metachirus in that the gluteal fossa does not appear to be much larger than the iliacus fossa, and the greater trochanter of the femur does not extend further proximally than the femoral head (see below). This, together with the general robustness of its postcranial skeleton, suggests that Anatoliadelphys was not a highly agile, leaping animal. The ischiatic spine is the origin of the M. biceps femoris, the M. semimembranosus, and the M. semitendinosus caput ventrale, all of which are powerful extensors of the hip [44, 48]; in agile and rapidly-moving (e.g. leaping, bounding or running) mammals, the ischiatic spine is usually prominent and everted [48], but it appears only very weakly developed and not obviously everted in Anatoliadelphys. A laterally everted ilium has also been associated with bipedalism [58], and it is possible that Anatoliadelphys was capable of periods of bipedal locomotion, perhaps in the context of climbing or scanning the environment.

A distinct tuberosity for the M. rectus femoris, anterior to the acetabulum, is present in Anatoliadelphys, as it is in dasyurids and in the stem-marsupials Herpetotherium, Pucadelphys and Mayulestes [39, 4850]. In didelphids, this tuberosity is absent or weakly developed in slow-moving arboreal forms such as Caluromys and Micoureus, but better developed in the agile Metachirus, which resembles Dasyurus in this regard [48]. The M. rectus femoris is a powerful extensor of the knee and flexor of the hip, and presence of a well-developed tuberosity has been interpreted as evidence of agility [39, 48, 49]. It might be an indication that Anatoliadelphys was capable of periods of relatively rapid locomotion, perhaps in pursuit of prey.

In the femur, the greater trochanter (the area of insertion of the gluteal muscles) extending proximally above the height of the femoral head is characteristic of agile taxa such as Metachirus and the bandicoot Perameles [48], and this feature is often associated with a much larger gluteal fossa than iliacus fossa [44, 48]. However, the greater trochanter is similar in height to the femoral head in Anatoliadelphys and the gluteal fossa does not appear greatly enlarged, and so it was probably not as agile as Metachirus or Perameles. The lesser trochanter is prominent and bladelike, and distally more extensive than in didelphids or Mayulestes, resembling dasyurids in this respect [39, 44, 52], which suggests that the M. iliacus and M. psoas major (which are flexors and external rotators and adductors of the leg [48]) were well-developed; a large lesser trochanter may be an indication of climbing ability [44, 48]. The apex of the lesser trochanter is positioned close to the femoral head, as in Dasyurus and Metachirus, suggesting rapid flexion [44]. In medial view, the lesser trochanter extends largely medially and only slightly caudally, as is typical for more scansorial/arboreal didelphids [41], although the exact functional significance of the orientation of the lesser trochanter is somewhat unclear [58].

Presence of a distinct third trochanter (which receives the insertion of the M. gluteus superficialis, an extensor and abductor of the femur) is probably plesiomorphic for Metatheria [47] but is absent in most crown-clade marsupials, with the exception of paucituberculatans, vombatids and notoryctids [47, 51, 80]. The third trochanter of Anatoliadelphys is laterally more extensive in Anatoliadelphys than in Mayulestes, Pucadelphys and paucituberculatans [39, 51, 159], extending beyond the lateral margin of the greater trochanter, but is similar in this regard to that of Herpetotherium [49, 50]. It is also relatively distally positioned, with its apex ~30% of the total length of the femur from the proximal end, broadly similar to its position in Pucadelphys, but further distal than in Mayulestes [39], Hereptotherium [49, 50] and paucituberculatans [51, 159]. A distal position of the third trochanter may indicate that the M. gluteus superficialis was acting more as an abductor than as an extensor [62]. A more distal location and greater degree of lateral extension of the third trochanter has been interpreted as evidence of greater terrestrial locomotion in tupaiid treeshrews [160], but evidence from other mammalian clades is more equivocal [62, 161]. Nevertheless, the third trochanter of Anatoliadelphys appears less prominent than in fossorially-specialised mammals [80, 161].

The crests of the femoral trochlea are more salient in Anatoliadelphys than in didelphids, including the relatively terrestrial Metachirus, but similar in this regard to Dasyurus, suggesting relatively rapid and powerful movements of the knee joint (the trochlear crests prevent dislocation of the tendon of the M. vasti and M. rectus femoris); however, the trochlea is not as deeply defined as the agile, terrestrial Perameles [39, 44].

In caudal view, although the medial condyle extends further proximally and distally than does the lateral condyle, the two condyles are of similar widths, with a ratio of medial condyle width to lateral condyle width of 0.90. This is greater than that of any didelphid measured by Muizon [39] or Argot [44], including the more terrestrial Monodelphis (0.83) and Metachirus (0.75), and also greater than that of Dasyurus (0.78), Mayulestes (0.73) and Pucadelphys (0.75–0.82). The terrestrial caenolestids and Perameles have condyles of roughly equal width [44, 47, 159], as in Anatoliadelphys, whilst the medial condyle is wider than the lateral condyle in the borhyaenoid Borhyaena, which has been interpreted to be terrestrial and digitigrade [53]. A lateral condyle that is wider than the medial condyle width is suggestive of a very abducted position for the femur, which may be plesiomorphic for mammals [39]; in therians, it may be an indication of arboreality [39, 44, 47, 48]. The relatively equal widths of the condyles in Anatoliadelphys suggests a less abducted femur, possibly indicative of more rapid, terrestrial locomotion.

The tendon of the M. quadriceps (a powerful extensor of the knee) inserts on the tibial tuberosity. In didelphids, the development of the tibial tuberosity is correlated with the degree of terrestriality [44, 48]. The tibial tuberosity of Anatoliadelphys is more prominent than that of the arboreal Caluromys, similar in size to that of the scansorial Didelphis, and less developed than that of the agile, terrestrial Metachirus. The tibial crest of Anatoliadelphys is also not as sharp as in Metachirus, again suggesting a lesser degree of agility [44, 48]. The sigmoidal shape of the tibia in craniocaudal view is likely plesiomorphic for therians and may be further indication of climbing ability [47, 48]; however, the tibia is sigmoidal in the relatively terrestrial Caenolestes and Sarcophilus and straight in the arboreal diprotodontians Phalanger and Phascolarctos [39], and so by itself this feature is of limited functional significance. The tibia of Anatoliadelphys is more strongly curved in mediolateral view (convex anteriorly, concave posteriorly) than in didelphids or dasyurids, but resembles Pucadelphys and Mayulestes in this regard; this would probably have resulted in a large space between the tibia and fibula, which may have been filled by a particularly well-developed M. flexor digitorum fibularis [44]. The medial tibial condyle is slightly lower than the lateral condyle, which helps to stabilise the knee joint; in didelphids, the difference in height is greater in terrestrial forms (e.g. Metachirus) than in arboreal forms (e.g. Caluromys) [44].

The large, flared proximal end of the fibula of Anatoliadelphys may be plesiomorphic for therians [47], and it suggests that the M. flexor fibularis and (particularly) M. peroneus longus were well-developed [44]. The proximal end of the fibula of Anatoliaelphys is smaller than that of Caluromys, but similar in size to that of Didelphis and larger than that of Metachirus (in which the hallux is still opposable) and dasyurids (in which the hallux is reduced and non-opposable) [44, 48]. However, the groove at the distal end of the fibula for the M. peroneus brevis, M. peroneus longus and M. extensor digitorum lateralis is less prominent than in Didelphis and much less so in Caluromys [44], suggesting a less powerful grasping ability. The pes is insufficiently preserved in AÜJM 2002–25 to reveal whether or not the hallux was opposable.

On the distal epiphysis of the tibia of Anatoliadelphys, the medial and lateral astragalotibial facets meet at a sharper angle than in didelphids, including the terrestrially-adapted Metachirus [56]. This suggests that the upper ankle joint of Anatoliadelphys was less mobile than in didelphids, congruent with more terrestrial locomotion. However, neither the left nor the right astragalus is preserved in AÜJM 2002–25, and so the degree of angulation between the astraglotibial and astragalofibular facets of the astragalus is unknown. Conversely, the short, deep, medially-inflected calcaneal tuber, and the prominent peroneal process with a very well-defined groove for the tendon of the M. peroneus longus, indicate that the hindfoot of Anatoliadelphys was capable of powerful grasping and inversion-eversion [39, 44, 56, 162, 163]. The ectal facet of Anatoliadelphys appears larger than the sustentacular facet, it has a prominent lateral border proximally, and it faces more medially than in the more terrestrial Metachirus, dasyurids and peramelids, but more dorsally than in the arboreal Caluromys [44, 48, 56].

A small calcaneofibular facet appears to be present in Anatoliadelphys; among marsupials, contact between the fibula and calcaneus probably helps stabilise the upper ankle joint, and it is generally found among more terrestrially-adapted taxa [56]. However, calcaneofibular contact is plesiomorphic for therian mammals [56], and so its apparent presence in Anatoliadelphys may be of limited functional significance. The broad, concave calcaneocuboid facet of Anatoliadelphys would have allowed considerable rotation of the pes at the transverse tarsal joint [44, 56], which may have facilitated climbing. However, it lacks the morphological specialisations of the calcaneocuboid facet to facilitate rotation at the transverse tarsal joint seen in didelphids (in which the calcanceocuboid facet is bipartite, to accommodate a distinct proximal extension of the cuboid) and plesiomorphic australidelphians (in which the facet is tripartite) [56, 125, 164].

In summary, there are features of the forelimb of Anatoliadelphys that would have facilitated pronation-supination movements (e.g. the spherical capitulum) and powerful grasping (e.g. the prominent medial epicondyle and supinator crest), suggesting an ability to climb (although it should be noted that these features are probably plesiomorphic for therians); however, they are less developed in Anatoliadelphys than in arboreal specialists such as the didelphid Caluromys. Some features of the hindlimb are also indicative of powerful grasping and inversion-eversion (e.g. the large peroneal process of the calcaneus with its very prominent groove for the tendon of the M. peroneus longus), but others (such as the laterally flaring ilium, well-developed tubercle for the M. rectus femoris, well-defined femoral trochlea, and femoral condyles that are of similar width) are typical of more agile, more terrestrial marsupials. Thus, we suggest that Anatoliadelphys was not an arboreal specialist, but was nevertheless capable of climbing. It may have had similar scansorial abilities to Didelphis, but was probably capable of more rapid, agile movements. In this regard, it may have resembled the living spotted quoll Dasyurus maculatus, which has a similar body mass to that estimated for Anatoliadelphys, and which is an agile predator that is predominantly terrestrial, but which is nevertheless capable of climbing well. However, the larger medial epicondyle and supinator crest of the humerus and the much larger peroneal process of the calcaneus of Anatoliadelphys suggest that it was capable of more powerful grasping than in D. maculatus in which (as in all dasyuromorphians) the hallux is reduced; nevertheless, D. maculatus and other dasyurids (including Sarcophilus) are capable of grasping [52, 154, 155, 165].

Our phylogenetically-flexible discriminant function analysis of locomotor mode based on a dataset of 24 postcranial indices (Table 5 and Fig 37) performed well at correctly classifying extant taxa, with only 16% misclassified. Based on the same dataset, this analysis classified Anatoliadelphys as having a probability of 77% of being scansorial, 17% of being semifossorial and 6% of being terrestrial. These results are therefore highly congruent with our qualitative analysis of its postcranial skeleton, which also supports scansorial locomotion.

Fig 37. Phylogenetically flexible discriminant analysis of postcranial indices for Anatoliadelphys maasae and modern mammals.

The modern mammals were classified as representing either arboreal, scansorial, semiaquatic, semifossorial or terrestrial locomotor modes. This analysis classified Anatoliadelphys as having a probability of 77% of being scansorial, 17% of being semifossorial and 6% of being terrestrial. The plot shows the first two discriminant axes (DAs) only.

Table 5. 24 postcranial indices from Chen and Wilson [76] calculated for Anatoliaelphys maasae, based on measurements from AÜJM 2002–25.

Phylogenetic relationships of Anatoliadelphys

Several metatherians show broadly similar craniodental adaptations to Anatoliadelphys, namely enlarged upper and lower third premolars and features associated with the generation of high bite forces; these include the Late Cretaceous North American stagodontids [29, 75, 101, 142, 145147], Eobrasilia coutoi, Didelphopsis cabrerai and Gaylordia macrocynodonta from the early Eocene Itaboraí fauna of Brazil [166172], various South American Cenozoic sparassodonts [148], the probable dasyuromorphian Malleodectes from the Miocene of Australia [150, 151], and the extant dasyurid Sarcophilus harrisii. Qualitative analysis of available data suggests that these similarities are most likely homoplastic, as discussed here.

Anatoliadelphys lacks the tall paraconid and high, bladelike paracristid with a “keyhole”-like carnassial notch characteristic of stagodontid lower molars, and there are major differences in the structure of the upper molars, with stagodontids having a straight centrocrista on M3 (strongly v-shaped in Anatoliadelphys, with the premetacrista contacting stylar cusp D) and well-developed conules (absent or indistinct in Anatoliadelphys) [66, 101, 147]. Isolated tarsals tentatively referred to the stagodontids Eodelphis and Didelphodon by Szalay [56] are highly distinctive, and exhibit a number of probable apomorphies absent in Anatoliadelphys, including a circular calcaneocuboid facet, and a distally-placed and obliquely-oriented sustentacular facet [56].

Eobrasilia is too poorly known to be meaningfully compared with Anatoliadelphys. An isolated right upper molar (DGM 896-M(a), an M2 or M3) was tentatively referred to E. coutoi by Marshall [167], but was subsequently referred by him to a separate taxon, Zeusdelphys complicatus [168, 169]. In any case, DGM 896-M(a) differs markedly from the upper molars of Anatoliadelphys: in DGM 896-M(a), StB and StD are both very large and subequal in height (StD is much larger than StB in Anatoliadelphys), and the enamel is heavily wrinkled, unlike in Anatoliadelphys, and it further differs from Anatoliadelphys in lacking distinct cingula anterior and posterior to the protocone. Didelphopsis cabrerai and Gaylordia macrocynodonta, meanwhile, lacks the strong posterior increase in molar size, enormous protoconid and very reduced paraconid and metaconid of Anatoliadelphys. Didelphopsis cabrerai and a second, less specialised Gaylordia species from Itaboraí, G. mater are characterised by a weakly v-shaped centrocrista on M3 (strongly v-shaped in Anatoliadelphys, with the premetacrista contacting stylar cusp D), and a prominent stylar cusp C (absent in Anatoliadelphys), and they lack prominent pre- and post-cingula [168172].

In the upper molars of sparassodonts, the centrocrista (where not lost through fusion of the paracone and metacone) is straight on all upper molars, unlike the strongly v-shaped centrocrista of the M3 of Anatoliadelphys, pre- and post-cingula are absent, and the protocone is often reduced, whilst in the lower molars, the paraconid is consistently well-developed in sparassodonts [32, 66]; there are also major differences in tarsal structure between sparassodonts and Anatoliadelphys [56].

Finally, Anatoliadelphys shares with most dasyuromorphians (including the durophagously-adapted Malleodectes [151]) the presence of a StD that is distinctly larger than StB on M3, but it lacks the characteristic australidelphian apomorphies seen in the tarsus of dasyuromorphians, most obviously the fusion of the ectal and sustentacular facets (the “continuous lower ankle joint pattern”) [56, 125, 164]. In summary, although Anatoliadelphys shares some derived craniodental features with a wide range of metatherians, it is likely that most (if not all) are convergent, reflecting the functional demands of a durophagous diet. Broadly similar adaptations have also evolved multiple times in eutherians, for example in the “condylarth” Periptychus [10] and the apternodontid “insectivore” Apternodus [173].

This qualitative interpretation is supported by the results of our Bayesian undated and “tip-and-node dating” analyses. In the both analyses, Anatoliadelphys falls within Marsupialiformes but outside Marsupialia, and it does not form a clade with Didelphodon or with the possible sparassodont Mayulestes. In the undated analysis, Anatoliadelphys is part of a trichotomy that also includes Peradectidae and a clade that includes Marsupialia, Didelphodon, Herpetotherium and Asiatherium. In the dated analysis, Anatoliadelphys forms a clade with Peradectidae, which receives moderate support (Bayesian posterior probability = 0.77), whilst Didelphodon is again closer to Marsupialia.

Overall, our phylogenetic results are broadly similar to other recent analyses [37, 75, 80, 103, 148, 174, 175], although some relationships within Marsupialiformes remain to be confidently resolved. Notably, our analyses recovered relationships within Marsupialia that are congruent with recent molecular studies [5, 176178], in contrast to the phylogenetic analysis of Wilson et al. [75], which failed to recover monophyly of Australidelphia.

Unambigous synapomorphies for Metatheria, Marsupialiformes, Marsupialia and (for the dated analysis) Anatoliadelphys+Peradectidae are given in Table 6. In the undated analysis, loss of the posterior cingulid optimises as an unambiguous synapomorphy of Marsupialia (secondarily reversed in dasyuromorphians), as previously proposed by Voss and Jansa [27]; Anatoliadelphys retains a very faint posterior cingulid on m3 and m4, supporting a position outside Marsupialia. In the dated analysis, meanwhile, the sole unambiguous synapomorphy of Marsupialia is subdivision of the calcaneocuboid facet of the calcaneus into three distinct facets; this morphology is present in australidelphians and paucituberculatans, whilst didelphids have distinct distal and proximal calcaneocuboid facets, and that of Herpetotherium also appears to be subdivided into two distinct facets (one laterodorsal and one medioventral [49, 56, 119, 125, 164, 179]). The simple, concave calcaneocuboid facet of Anatoliadelphys is congruent with a position outside Marsupialia. A full list of morphological synapomorphies for all clades present in our undated and dated analyses, under both Accelerated Transformation (ACCTRAN) and Delayed Transformation (DELTRAN), is given in S4 Text.

Table 6. Unambiguous morphological synapomorphies (identified using the maximum parsimony criterion in PAUP* 4.0a152) for selected clades recovered in our dated and undated phylogenetic analyses (see Figs 38 and 39).

A full list of morphological synapomorphies for all clades present in our undated and dated analyses, under both Accelerated Transformation (ACCTRAN) and Delayed Transformation (DELTRAN), is given in S4 Text.

Fig 38. Phylogeny of Metatheria based on Bayesian undated analysis of total evidence dataset.

The dataset comprises 259 morphological characters and 9012 bp of molecular sequence data from 5 nuclear genes (APOB, BRCA1, IRBP, RAG1 and VWF). The topology represents a 50% majority rule consensus tree of post-burn-in trees. Abbreviations: BPP, Bayesian posterior probability.

Fig 39. Phylogeny of Metatheria based on Bayesian “tip-and-node dating” analysis of total evidence dataset.

The dataset comprises 259 morphological characters and 9012 bp of molecular sequence data from 5 nuclear genes (APOB, BRCA1, IRBP, RAG1 and VWF), assuming a single Independent Gamma Rates (IGR) clock model, “diversity” sampling, and with temporal information provided in the form of tip ages and also constraints (specified as offset exponential distributions) on the ages of selected nodes. The topology represents a maximum clade credibility (MCC) tree. Nodes without Bayesian posterior probabilities were used as age constraints, which required them to be constrained as monophyletic a priori. Blue bars at nodes represent 95% Highest Posterior Densities (HPDs) on node ages. Abbreviations: BPP, Bayesian posterior probability.

The dated analysis resulted in divergence dates that are broadly congruent with recent molecular studies [5], with the first divergence within Marsupialia estimated at 68.2 MYA (95% HPD: 60.7–75.2 MYA). Anatoliadelphys was estimated as having diverged from Peradectidae 59.0 MYA (95% HPD 54.4–72.4 MYA).


Perhaps the most remarkable aspect of Anatoliadelphys maasae is its large size. With an estimated body mass of 3–4 kg, it is one of the largest metatherians known from the northern hemisphere, together with two North American species, namely the extant Virginia opossum (Didelphis virginiana; mean body mass 2.4 kg [70]), and the Late Cretaceous stagodontid Didelphodon vorax (estimated body mass 2.1–6.2 kg [75]). With the exception of D. virginiana (which dispersed to North America from South America <1 million years ago [22]), the largest Cenozoic metatherians previously known from the northern hemisphere were the early Eocene North American peradectids Mimoperadectes labrus and M. houdei [20, 180]), which probably weighed ~250g, i.e. an order of magnitude smaller than Anatoliadelphys.

Anatoliadelphys is also unusual in exhibiting obvious craniodental adaptations for carnivory (probably meso- or hypocarnivory, rather than hypercarnivory) and durophagy (perhaps for crushing bone, hard shelled invertebrates, or both). The Cretaceous northern hemisphere deltatheroidans and stagodontids were carnivorously adapted [6, 7, 9, 66], and the large, broad premolars of stagodontids also suggest durophagy [6, 29, 101, 145, 181]. Numerous carnivorous and durophagous metatherians are also known from the Cenozoic of South America and Australia [12, 15, 17, 32, 104, 148, 151, 182, 183]. However, prior to the discovery of Anatoliadelphys, all known Cenozoic fossil metatherians from the northern hemisphere were characterised by relatively generalised tribosphenic molars and unspecialised premolars [20, 21, 28, 184], suggesting that they were primarily insectivorous (although some peradectids may have been at least partially frugivorous [95]). Anatoliadelphys therefore reveals previously unsuspected ecomorphological diversity among northern hemisphere metatherians during the Cenozoic.

Anatoliadelphys demonstrates that at least one metatherian lineage evolved to successfully occupy a small-medium meso- or hypocarnivore niche in the northern hemisphere during the early Palaeogene. Numerous carnivorous fossil eutherians are known from the northern hemisphere during this time period, including carnivoromorphians, mesonychians, pantolestids, didymoconids, and oxyaenid and hyaenodontid creodonts [10, 185]. Hyaenodontids are also known from the early Palaeogene of Africa, where they likely originated [186]. Many of these carnivorous eutherians were similar in size (1–10 kg) to Anatoliadelphys, and so represent potential ecological competitors [185].

However, although still poorly known, the UCF mammal fauna appears to be highly endemic (Table 7), and carnivorous eutherians have yet to be found there. As noted by Metais et al. [94], the presence of multiple species of the pleuraspidotheriid Hilalia in the Lutetian (44–43 MYA) UCF mammal fauna is particularly striking: the youngest record of Pleuraspidotheriidae from Europe is latest Palaeocene, i.e. 12–14 million years older [189]. This “anachronistic” presence of pleuraspidotheriids suggests that the UCF may preserve a mammal fauna that evolved largely in isolation during the early Cenozoic, with only limited biogeographical connectivity to Laurasia and Africa [89, 94]. This is congruent with geological evidence that this region of Turkey was an island for at least part of the early Cenozoic [188, 190]. If Anatoliadelphys evolved as part of an isolated mammalian fauna in which carnivorous eutherians were absent, then it may in fact provide further support for the hypothesis that metatherians are competitively inferior to eutherians, due to differences in traits relating to reproductive mode and associated developmental constraints, and/or differences in metabolic rate [23, 191195]. This interpretation is reinforced by the apparent absence of mainland Laurasian metatherians that show similar specialisations to Anatoliadelphys.

Table 7. The mammal fauna described to date from the Uzunçarşidere Formation.

Supporting information

S1 File. Total evidence (morphological and molecular) character matrix for analysing phylogenetic relationships of metatherians using Bayesian undated and “tip-and-node dating” approaches.


S1 Text. Comparative material of modern and fossil metatherians examined in this study.


S2 Text. Morphological character scores of Anatoliadelphys and Didelphodon for phylogenetic analysis.


S3 Text. Assumed age ranges (in MYA) for fossil taxa included in phylogenetic analysis.


S4 Text. Morphological synapomorphies for all clades present in our undated and dated analyses, under both Accelerated Transformation (ACCTRAN) and Delayed Transformation (DELTRAN).



We thank Mary Maas (University of Texas at Austin) for inviting AMM to participate in fieldwork at Uzunçarşı and for graciously allowing us to study the specimen, Nizamettin Kazancı, Veysel Işik and Gürol Seyitoğlu (Ankara Üniversitesi) for their assistance with geological mapping and stratigraphy of the UCF and other Palaeogene continental deposits in Orhaniye, and the curators and collection managers at the American Museum of Natural History, National Museum of Natural History, Carnegie Natural History Museum, Australian Museum, and World Museum Liverpool for access to comparative specimens. We thank Christine Argot for assisting us in interpreting the morphology of the fibula, and Lars Schmitz for advice regarding phylogenetic flexible discriminant analysis. We also thank the editor Alistair Evans, and in particular the reviewers Guillermo Rougier and Greg Wilson for their detailed and constructive reviews.

Author Contributions

  1. Conceptualization: AMM.
  2. Formal analysis: RMDB.
  3. Funding acquisition: RMDB.
  4. Investigation: AMM RMDB.
  5. Methodology: AMM RMDB.
  6. Visualization: AMM RMDB.
  7. Writing – original draft: AMM RMDB.
  8. Writing – review & editing: AMM RMDB.


  1. 1. Luo Z-X, Yuan CX, Meng QJ, Ji Q. A Jurassic eutherian mammal and divergence of marsupials and placentals. Nature. 2011;476(7361):442–5. pmid:21866158
  2. 2. dos Reis M, Donoghue PCJ, Yang Z. Neither phylogenomic nor palaeontological data support a Palaeogene origin of placental mammals. Biol Lett. 2014;10(1):20131003. pmid:24429684
  3. 3. dos Reis M, Inoue J, Hasegawa M, Asher RJ, Donoghue PC, Yang Z. Phylogenomic datasets provide both precision and accuracy in estimating the timescale of placental mammal phylogeny. Proc R Soc B. 2012;279(1742):3491–500. pmid:22628470
  4. 4. Tarver JE, dos Reis M, Mirarab S, Moran RJ, Parker S, O'Reilly JE, et al. The interrelationships of placental mammals and the limits of phylogenetic inference. Genome Biology and Evolution. 2016;8(2):330–44. pmid:26733575
  5. 5. Meredith RW, Janecka JE, Gatesy J, Ryder OA, Fisher CA, Teeling EC, et al. Impacts of the Cretaceous Terrestrial Revolution and KPg extinction on mammal diversification. Science. 2011;334(6055):521–4. pmid:21940861
  6. 6. Kielan-Jaworowska Z, Cifelli RL, Luo Z-X. Mammals from the age of dinosaurs: origins, evolution, and structure. New York: Columbia University Press; 2004.
  7. 7. Wilson GP. Mammals across the K/Pg boundary in northeastern Montana, USA: dental morphology and body-size patterns reveal extinction selectivity and immigrant-fueled ecospace filling. Paleobiology. 2013;39(3):429–69.
  8. 8. Grossnickle DM, Newham E. Therian mammals experience an ecomorphological radiation during the Late Cretaceous and selective extinction at the K–Pg boundary. Proc R Soc B. 2016;283(1832).
  9. 9. Wilson GP. Mammalian extinction, survival, and recovery dynamics across the Cretaceous-Paleogene boundary in northeastern Montana, USA. In: Wilson GP, Clemens WA, Horner JR, Hartman JH, editors. Through the end of the Cretaceous in the type locality of the Hell Creek Formation in Montana and adjacent areas: Geological Society of America Special Paper 503: The Geological Society of America; 2014. p. 365–92.
  10. 10. Rose KD. The beginning of the age of mammals. Baltimore: Johns Hopkins University Press; 2006. i-xiv, 1–428 p.
  11. 11. Wilson DE, Reeder DM. Mammal species of the world. Third edition ed. Baltimore: John Hopkins University Press; 2005.
  12. 12. Goin FJ, Woodburne MO, Zimicz AN, Martin GM, Chornogubsky L. A brief history of South American metatherians: Evolutionary contexts and intercontinental dispersals. Dordrecht: Springer; 2016.
  13. 13. Case JA, Goin FJ, Woodburne MO. “South American” marsupials from the Late Cretaceous of North America and the origin of marsupial cohorts. J Mamm Evol. 2005;12(3–4):461–94.
  14. 14. Goin FJ, Zimicz AN, Forasiepi AM, Chornogubsky LC, Abello MA. The rise and fall of South American metatherians: contexts, adaptations, radiations, and extinctions. In: Rosenberger AL, Tejedor MF, editors. Origins and evolution of Cenozoic South American mammals. New York: Springer; in press.
  15. 15. Archer M, Hand SJ. The Australian marsupial radiation. In: Merrick JR, Archer M, Hickey GM, Lee MSY, editors. Evolution and biogeography of Australasian vertebrates. Sydney: Auscipub Pty Ltd; 2006. p. 575–646.
  16. 16. Archer M, Arena R, Bassarova M, Black K, Brammall J, Cooke B, et al. The evolutionary history and diversity of Australian mammals. Aust Mammal. 1999;21:1–45.
  17. 17. Archer M. The Australian marsupial radiation. In: Archer M, Clayton G, editors. Vertebrate zoogeography and evolution in Australasia. Perth: Hesperian Press; 1984. p. 633–808.
  18. 18. Black KH, Archer M, Hand SJ, Godthelp H. The rise of Australian marsupials: a synopsis of biostratigraphic, phylogenetic, palaeoecologic and palaeobiogeographic understanding. In: Talent JA, editor. Earth and Life: Global Biodiversity, Extinction Intervals and Biogeographic Perturbations Through Time. Dordrecht: Springer Verlag; 2012. p. 983–1078.
  19. 19. Long JA, Archer M, Flannery TF, Hand SJ. Prehistoric mammals of Australia and New Guinea: one hundred million years of evolution. Sydney: UNSW Press; 2002.
  20. 20. Korth WW. Marsupialia. In: Janis CM, Gunnell GF, Uhen MD, editors. Evolution of Tertiary mammals of North America Volume 2 Small mammals, xenarthrans, and marine mammals. Cambridge: Cambridge University Press; 2008. p. 39–48.
  21. 21. Crochet J-Y. Les Marsupiaux du Tertiare d'Europe. Paris: Editions Foundation Singer-Polinac; 1980.
  22. 22. Woodburne MO. The Great American Biotic Interchange: dispersals, tectonics, climate, sea level and holding pens. J Mamm Evol. 2010;17:245–64. pmid:21125025
  23. 23. Lillegraven JA, Thompson SD, McNab BK, Patton JL. The origin of eutherian mammals. Biol J Linn Soc. 1987;32:281–336.
  24. 24. Archibald JD. Extinction and radiation: how the fall of dinosaurs led to the rise of mammals. Baltimore: The Johns Hopkins University Press; 2011.
  25. 25. Fedorov A, Beichel R, Kalpathy-Cramer J, Finet J, Fillion-Robin JC, Pujol S, et al. 3D Slicer as an image computing platform for the Quantitative Imaging Network. Magn Reson Imaging. 2012;30(9):1323–41. pmid:22770690
  26. 26. Limaye A. Drishti: a volume exploration and presentation tool. In: Stock SR, editor. Proceedings of SPIE 8506, Developments in X-Ray Tomography VIII; October 17, 2012; San Diego, USA 2012. p. 85060X.
  27. 27. Voss RS, Jansa SA. Phylogenetic relationships and classification of didelphid marsupials, an extant radiation of New World metatherian mammals. Bull Am Mus Nat Hist. 2009;322:1–177.
  28. 28. Williamson TE, Brusatte SL, Wilson GP. The origin and early evolution of metatherian mammals: the Cretaceous record. Zookeys. 2014;465:1–76.
  29. 29. Clemens WA. Fossil mammals of the Type Lance Formation, Wyoming. Part II: Marsupialia. Univ Calif Publ Geol Sci. 1966;62:1–122.
  30. 30. Reig OA, Kirsch JAW, Marshall LG. Systematic relationships of the living and Neocenozoic American "opossum-like" marsupials (suborder Didelphimorphia), with comments on the classification of these and the Cretaceous and Paleogene New World and European metatherians. In: Archer M, editor. Possums and opossums: studies in evolution. Sydney: Surrey Beatty and Sons and the Royal Zoological Society of New South Wales; 1987. p. 1–89.
  31. 31. Archer M. The basicranial region of marsupicarnivores (Marsupialia), inter-relationships of carnivorous marsupials, and affinities of the insectivorous marsupial peramelids. Zool J Linn Soc. 1976;59(3):217–322.
  32. 32. Forasiepi AM. Osteology of Arctodictis sinclairi (Mammalia, Metatheria, Sparassodonta) and phylogeny of Cenozoic metatherian carnivores from South America. Monogr Mus Argent Cienc Nat. 2009;6:1–174.
  33. 33. Voss RS, Jansa SA. Phylogenetic studies on didelphid marsupials II. Nonmolecular data and new IRBP sequences: separate and combined analyses of didelphine relationships with denser taxon sampling. Bull Am Mus Nat Hist. 2003;276:1–82.
  34. 34. de Muizon C. Mayulestes ferox, a borhyaenoid (Metatheria, Mammalia) from the early Palaeocene of Bolivia: phylogenetic and palaeobiologic implications. Geodiversitas. 1998;20(1):19–142.
  35. 35. Wible JR. Late Cretaceous marsupial petrosal bones from North America and a cladistic analysis of the petrosal in therian mammals. J Vertebr Paleontol. 1990;10:183–205.
  36. 36. Wible JR. On the cranial osteology of the short-tailed opossum Monodelphis brevicaudata (Marsupialia, Didelphidae). Ann Carnegie Mus. 2003;72(3):137–202.
  37. 37. Beck RMD, Travouillon KJ, Aplin KP, Godthelp H, Archer M. The osteology and systematics of the enigmatic Australian Oligo-Miocene metatherian Yalkaparidon (Yalkaparidontidae; Yalkaparidontia;? Australidelphia; Marsupialia). J Mamm Evol. 2014;21(2):127–72.
  38. 38. Marshall LG, Muizon Christian de. Pucadelphys andinus (Marsupialia, Mammalia) from the early Paleocene of Bolivia. Mem Mus Natl Hist Nat. 1995;165:1–164.
  39. 39. Muizon C. de. Mayulestes ferox, a borhyaenoid (Metatheria, Mammalia) from the early Palaeocene of Bolivia: phylogenetic and palaeobiologic implications. Geodiversitas. 1998;20(1):19–142.
  40. 40. Flores DA. Phylogenetic analyses of postcranial skeletal morphology in didelphid marsupials. Bull Am Mus Nat Hist. 2009;320:1–81.
  41. 41. Flores DA, Díaz MM. Postcranial skeleton of Glironia venusta (Didelphimorphia, Didelphidae, Caluromyinae): description and functional morphology. Zoosystematics and Evolution. 2009;85(2):311–39.
  42. 42. Marshall LG, Sigogneau-Russell D. Postcranial skeleton. In: de Muizon C, editor. Pucadelphys andinus (Marsupialia, Mammalia) from the early Palaeocene of Bolivia. Memoires du Museum National d'Histoire Naturelle. Paris1995. p. 91–164.
  43. 43. Argot C. Functional-adaptive anatomy of the forelimb in the Didelphidae, and the paleobiology of the Paleocene marsupials Mayulestes ferox and Pucadelphys andinus. J Morphol. 2001;247(1):51–79. pmid:11124686
  44. 44. Argot C. Functional-adaptive analysis of the hindlimb anatomy of extant marsupials and the paleobiology of the Paleocene marsupials Mayulestes ferox and Pucadelphys andinus. J Morphol. 2002;253:76–108. pmid:11981806
  45. 45. Argot C. Functional-adaptive anatomy of the axial skeleton of some extant marsupials and the paleobiology of the Paleocene marsupials Mayulestes ferox and Pucadelphys andinus. J Morphol. 2003;255(3):279–300. pmid:12520547
  46. 46. Coues E. The osteology and myology of Didelphys virginiana. Memoirs of the Boston Society of Natural History. 1872;2:41–154.
  47. 47. Szalay FS, Sargis EJ. Model-based analysis of postcranial osteology of marsupials from the Palaeocene of Itaboraí (Brazil) and the phylogenetics and biogeography of Metatheria. Geodiversitas. 2001;23(2):139–302.
  48. 48. Muizon C. de, Argot C. Comparative anatomy of the Tiupampa didelphimorphs: an approach to locomotory habits of early marsupials. In: Jones M, Dickman C, Archer M, editors. Predators with pouches: the biology of carnivorous marsupials. Collingwood: CSIRO Publishing; 2003. p. 43–62.
  49. 49. Horovitz I, Ladevèze S, Argot C, Macrini TE, Martin T, Hooker JJ, et al. The anatomy of Herpetotherium cf. fugax Cope, 1873, a metatherian from the Oligocene of North America. Palaeontographica Abteilung A. 2008;284(4–6):109–41.
  50. 50. Sánchez-Villagra MR, Ladevèze S, Horovitz I, Argot C, Hooker JJ, Macrini TE, et al. Exceptionally preserved North American Paleogene metatherians: adaptations and discovery of a major gap in the opossum fossil record. Biol Lett. 2007;3(3):318–22. pmid:17426007
  51. 51. Abello MA, Candela AM. Postcranial skeleton of the Miocene marsupial Palaeothentes (Paucituberculata, Palaeothentidae): paleobiology and phylogeny. J Vertebr Paleontol. 2010;30(5):1515–27.
  52. 52. Argot C. Postcranial functional adaptations in the South American Miocene borhyaenoids (Mammalia, Metatheria): Cladosictis, Pseudonotictis and Sipalocyon. Alcheringa. 2003;27(4):303–56.
  53. 53. Argot C. Functional adaptations of the postcranial skeleton of two Miocene borhyaenoids (Mammalia, Metatheria), Borhyaena and Prothylacinus, from South America. Palaeontology. 2003;46:1213–67.
  54. 54. Argot C. Functional-adaptive analysis of the postcranial skeleton of a Laventan borhyaenoid, Lycopsis longirostris (Marsupialia, Mammalia). J Vertebr Paleontol. 2004;24(3):689–708.
  55. 55. Argot C, Babot J. Postcranial morphology, functional adaptations and palaeobiology of Callistoe vincei, a predaceous metatherian from the Eocene of Salta, north-western Argentina. Palaeontology. 2011;54(2):447–80.
  56. 56. Szalay FS. Evolutionary history of the marsupials and an analysis of osteological characters. Cambridge: Cambridge University Press; 1994. 481 p.
  57. 57. Evans HE. Miller’s anatomy of the dog. Philadelphia: W.B. Saunders; 1993.
  58. 58. Muizon C de, Billet G, Argot C, Ladevèze S, Goussard F. Alcidedorbignya inopinata, a basal pantodont (Placentalia, Mammalia) from the early Palaeocene of Bolivia: anatomy, phylogeny and palaeobiology. Geodiversitas. 2015;37(4):397–634.
  59. 59. Chester SGB, Sargis EJ, Szalay FS, Archibald JD, Averianov AO. Mammalian distal humeri from the Late Cretaceous of Uzbekistan. Acta Palaeontol Pol. 2010;55(2):199–211.
  60. 60. Chester SGB, Sargis EJ, Szalay FS, Archibald JD, Averianov AO. Therian femora from the Late Cretaceous of Uzbekistan. Acta Palaeontol Pol. 2012;57(1):53–64.
  61. 61. Szalay FS, Sargis EJ. Cretaceous therian tarsals and the metatherian-eutherian dichotomy. J Mamm Evol. 2006;13:171–210.
  62. 62. Candela AM, Picasso MB. Functional anatomy of the limbs of Erethizontidae (Rodentia, Caviomorpha): Indicators of locomotor behavior in Miocene porcupines. J Morphol. 2008;269(5):552–93. pmid:18157864
  63. 63. Dumont ER, Strait SG, Friscia AR. Abderitid marsupials from the Miocene of Patagonia: An assessment of form, function, and evolution. J Paleontol. 2000;74(6):1161–72.
  64. 64. Gordon CL. A first look at estimating body size in dentally conservative marsupials. J Mamm Evol. 2003;10(1–2):1–21.
  65. 65. Myers TJ. Prediction of marsupial body mass. Aust J Zool. 2001;49:99–118.
  66. 66. Muizon C. de, Lange-Badré B. Carnivorous dental adaptations in tribosphenic mammals and phylogenetic reconstruction. Lethaia. 1997;30:353–66.
  67. 67. Zimicz N. Avoiding competition: The ecological history of Late Cenozoic metatherian carnivores in South America. J Mamm Evol. 2014;21(4):383–93.
  68. 68. Zimicz AN. Ecomorfología de los marsupiales paleógenos de América del Sur. Unpublished PhD thesis: Universidad Nacional de La Plata; 2012.
  69. 69. Van Valkenburgh B. Iterative evolution of hypercarnivory in canids (Mammalia, Carnivora)—evolutionary interactions among sympatric predators. Paleobiology. 1991;17(4):340–62.
  70. 70. Jones KE, Bielby J, Cardillo M, Fritz SA, O'Dell J, Orme CDL, et al. PanTHERIA: a species-level database of life history, ecology, and geography of extant and recently extinct mammals. Ecology. 2009;9:2648.
  71. 71. Hammer Ø, Harper DAT, Ryan PD. PAST: Paleontological statistics software package for education and data analysis. Palaeontol Electron. 2001;4(1):4.
  72. 72. Thomason JJ. Cranial strength in relation to estimated biting forces in some mammals. Can J Zool. 1991;69:2326–33.
  73. 73. Wroe S, McHenry C, Thomason J. Bite club: comparative bite force in big biting mammals and the prediction of predatory behaviour in fossil taxa. Proc R Soc B. 2005;272(1563):619–25. pmid:15817436
  74. 74. Therrien F. Mandibular force profiles of extant carnivorans and implications for the feeding behaviour of extinct predators. J Zool. 2005;267:249–70.
  75. 75. Wilson GP, Ekdale EG, Hoganson JW, Calede JJ, Vander Linden A. A large carnivorous mammal from the Late Cretaceous and the North American origin of marsupials. Nature communications. 2016;7:13734. pmid:27929063
  76. 76. Chen M, Wilson GP. A multivariate approach to infer locomotor modes in Mesozoic mammals. Paleobiology. 2015;41(2):280–312.
  77. 77. Motani R, Schmitz L. Phylogenetic versus functional signals in the evolution of form-function relationships in terrestrial vision. Evolution. 2011;65(8):2245–57. pmid:21790572
  78. 78. Schmitz L, Motani R. Nocturnality in dinosaurs inferred from scleral ring and orbit morphology. Science. 2011;332(6030):705–8. pmid:21493820
  79. 79. Bininda-Emonds ORP, Cardillo M, Jones KE, MacPhee RDE, Beck RMD, Grenyer R, et al. The delayed rise of present-day mammals. Nature. 2007;446:507–12. pmid:17392779
  80. 80. Beck RMD, Warburton NM, Archer M, Hand SJ, Aplin KP. Going underground: postcranial morphology of the early Miocene marsupial mole Naraboryctes philcreaseri and the evolution of fossoriality in notoryctemorphians. Mem Mus Vic. 2016;74:151–71.
  81. 81. Ronquist F, Teslenko M, van der Mark P, Ayres DL, Darling A, Hohna S, et al. MrBayes 3.2: efficient Bayesian phylogenetic inference and model choice across a large model space. Syst Biol. 2012;61(3):539–42. pmid:22357727
  82. 82. Lanfear R, Calcott B, Ho SY, Guindon S. Partitionfinder: combined selection of partitioning schemes and substitution models for phylogenetic analyses. Mol Biol Evol. 2012;29(6):1695–701. pmid:22319168
  83. 83. Lewis PO. A likelihood approach to estimating phylogeny from discrete morphological character data. Syst Biol. 2001;50:913–25. pmid:12116640
  84. 84. Ronquist F, Klopfstein S, Vilhelmsen L, Schulmeister S, Murray DL, Rasnitsyn AP. A total-evidence approach to dating with fossils, applied to the early radiation of the Hymenoptera. Syst Biol. 2012;61(6):973–99. pmid:22723471
  85. 85. Pyron RA. Divergence time estimation using fossils as terminal taxa and the origins of Lissamphibia. Syst Biol. 2011;60(4):466–81. pmid:21540408
  86. 86. Zhang C, Stadler T, Klopfstein S, Heath TA, Ronquist F. Total-evidence dating under the fossilized birth-death process. Syst Biol. 2016;65(2):228–49. pmid:26493827
  87. 87. O'Reilly JE, Donoghue PC. Tips and nodes are complementary not competing approaches to the calibration of molecular clocks. Biol Lett. 2016;12(4). pmid:27095263
  88. 88. Rambaut A, Suchard MA, Xie D, Drummond AJ. Tracer v1.6. 2014.
  89. 89. Licht A, Coster P, Ocakoğlu F, Campbell C, Métais G, Mulch A, et al. Tectono-stratigraphy of the Orhaniye Basin, Turkey: Implications for collision chronology and Paleogene biogeography of central Anatolia. J Asian Earth Sci. in press.
  90. 90. Erdal O, Antoine P-O, Sen S. New material of Palaeoamasia kansui (Embrithopoda, Mammalia) from the Eocene of Turkey and a phylogenetic analysis of Embrithopoda at the species level. Palaeontology. 2016.
  91. 91. Kappelman J, Maas MC, Sen S, Alpagut B, Fortelius M, Lunkka JP. A new early Tertiary mammalian fauna from Turkey and its paleobiogeographic significance. J Vertebr Paleontol. 1996;16(3):592–5.
  92. 92. Maas MC, Thewissen JGM, Kappelman JW. Hypsamasia seni (Mammalia: Embrithopoda) and other mammals from the Eocene Kartal Formation of Turkey. In: Beard KC, Dawson MR, editors. Dawn of the age of mammals in Asia. Pittsburgh: Bulletin of Carnegie Museum of Natural History; 1998. p. 286–97.
  93. 93. Maas MC, Thewissen JGM, Sen S, Kazanci N, Kappelman J. Enigmatic new ungulates from the early middle Eocene of central Anatolia, Turkey. J Vertebr Paleontol. 2001;21(3):578–90.
  94. 94. Métais G, Beard K, Erdal O, Erturaç K. Tarsal morphology of the pleuraspidotheriid mammal Hilalia from the middle Eocene of Turkey. Acta Palaeontol Pol. 2017;62.
  95. 95. Kurz C. Ecomorphology of opossum-like marsupials from the Tertiary of Europe and a comparison with selected taxa. Kaupia—Darmstädter Beiträge zur Naturgeschichte. 2005;14:21–6.
  96. 96. Kurz C. The opossum-like marsupials (Didelphimorphia and Peradectia, Marsupialia, Mammalia) from the Eocene of Messel and Geiseltal—ecomorphology, diversity and palaeogeography. Kaupia. 2007;15:3–64.
  97. 97. Beck RMD. Current understanding of the phylogeny of Metatheria: A review. In: Goin FJ, Forasiepi AM, editors. New World marsupials and their extinct relatives: 100 million years of evolution: Springer; in press.
  98. 98. O'Leary MA, Bloch JI, Flynn JJ, Gaudin TJ, Giallombardo A, Giannini NP, et al. The placental mammal ancestor and the post-K-Pg radiation of placentals. Science. 2013;339(6120):662–7. pmid:23393258
  99. 99. Rougier GW, Wible JR, Novacek MJ. Implications of Deltatheridium specimens for early marsupial history. Nature. 1998;396:459–63. pmid:9853752
  100. 100. Bi S, Jin X, Li S, Du T. A new Cretaceous metatherian mammal from Henan, China. PeerJ. 2015;3:e896. pmid:25893149
  101. 101. Fox RC, Naylor BG. Stagodontid marsupials from the Late Cretaceous of Canada and their systematic and functional implications. Acta Palaeontol Pol. 2006;51(1):13–36.
  102. 102. Sánchez-Villagra M, Asher RJ. Cranio-sensory adaptations in small, faunivorous mammals, with special reference to olfaction and the trigeminal system. Mammalia. 2002;66(1):93–109.
  103. 103. Beck RMD. The skull of Epidolops ameghinoi from the early Eocene Itaboraí fauna, southeastern Brazil, and the affinities of the extinct marsupialiform order Polydolopimorphia. J Mamm Evol. 2016.
  104. 104. Forasiepi AM, Goin F, Martinelli AG. Contribution to the knowledge of the Sparassocynidae (Mammalia, Metatheria, Didelphoidea), with comments on the age of the Aisol Formation (Neogene), Mendoza Province, Argentina. J Vertebr Paleontol. 2009;29(4):1252–63.
  105. 105. Woodburne MO. The Alcoota Fauna, central Australia. Bulletin of the Bureau of Mineral Resources Geology and Geophysics, Australia. 1967;87:1–187.
  106. 106. Sánchez-Villagra MR, Wible JR. Patterns of evolutionary transformation in the petrosal bone and some basicranial features in marsupial mammals, with special reference to didelphids. J Zool Syst Evol Res. 2002;40:26–45.
  107. 107. Turnbull WD. Mammalian masticatory apparatus. Fieldiana: Geology. 1970;18:149–356.
  108. 108. Cope ED. On the foramina perforating the posterior part of the squamosal bone of the Mammalia. Proc Am Philos Soc. 1880;18:452–61.
  109. 109. Gregory WK. The orders of mammals. Bull Am Mus Nat Hist. 1910;27:1–524.
  110. 110. Pavan SE, Voss RS. A revised subgeneric classification of short-tailed opossums (Didelphidae: Monodelphis). Am Mus Novit. 2016;3868:1–44.
  111. 111. Muirhead J. Yaraloidea (Marsupialia, Peramelemorphia), a new superfamily of marsupial and a description and analysis of the cranium of the Miocene of Yarala burchfieldi. J Paleontol. 2000;74(3):512–23.
  112. 112. Koyabu D, Maier W, Sanchez-Villagra MR. Paleontological and developmental evidence resolve the homology and dual embryonic origin of a mammalian skull bone, the interparietal. Proc Natl Acad Sci U S A. 2012;109(35):14075–80. 10.1073/pnas.1208693109. pmid:22891324
  113. 113. Sánchez-Villagra MR. The cerebellar paraflocculus and the subarcuate fossa in Monodelphis domestica and other marsupial mammals–ontogeny and phylogeny of a brain-skull interaction. Acta Theriol. 2002;47(1):1–14.
  114. 114. Sigé B, Archer M, Crochet J-Y, Godthelp H, Hand S, Beck RMD. Chulpasia and Thylacotinga, late Paleocene-earliest Eocene trans-Antarctic Gondwanan bunodont marsupials: New data from Australia. Geobios. 2009;42(6):813–23.
  115. 115. Sánchez-Villagra MR, Smith KK. Diversity and evolution of the marsupial mandibular angular process. J Mamm Evol. 1997;4(2):119–44.
  116. 116. Hiiemae K, Jenkins FA Jr. The anatomy and internal architecture of the muscles of mastication in Didelphis marsupialis. Postilla. 1969;140:1–49.
  117. 117. Sánchez-Villagra MR, Narita Y, Kuratani S. Thoracolumbar vertebral number: the first skeletal synapomorphy for afrotherian mammals. Syst Biodivers. 2007;5(1):1–7.
  118. 118. Klima M. Early development of the shoulder girdle and sternum in marsupials (Mammalia, Metatheria). Advances in Anatomy, Embryology and Cell Biology. 1987;109:1–91.
  119. 119. Horovitz I, Sánchez-Villagra MR. A morphological analysis of marsupial mammal higher-level phylogenetic relationships. Cladistics. 2003;19:181–212.
  120. 120. Szalay FS, Trofimov B. The Mongolian Late Cretaceous Asiatherium, and the early phylogeny and paleobiogeography of Metatheria. J Vertebr Paleontol. 1996;16:474–509.
  121. 121. Samuels ME, Regnault S, Hutchinson JR. Evolution of the patellar sesamoid bone in mammals. PeerJ. 2017;5:e3103. pmid:28344905
  122. 122. Geiger M, Forasiepi AM, Koyabu D, Sanchez-Villagra MR. Heterochrony and post-natal growth in mammals—an examination of growth plates in limbs. J Evol Biol. 2014;27:98–115. pmid:24251599
  123. 123. Szalay FS, Decker RL. Origins, evolution, and function of the tarsus in Late Cretaceous Eutheria and Paleocene Primates. In: Jenkins FA Jr., editor. Primate Locomotion. New York: Academic Press; 1974. p. 223–59.
  124. 124. Horovitz I. The tarsus of Ukhaatherium nessovi (Eutheria, Mammalia) from the Late Cretaceous of Mongolia: an appraisal of the evolution of the ankle in basal therians. J Vertebr Paleontol. 2000;20(3):547–60.
  125. 125. Beck RMD. An 'ameridelphian' marsupial from the early Eocene of Australia supports a complex model of Southern Hemisphere marsupial biogeography. Naturwissenschaften. 2012;99(9):715–29. Epub 2012/08/07. pmid:22864962
  126. 126. Kermack KA. Molar evolution in Mesozoic mammals. J Dent Res. 1967;46:792–5. pmid:5234019
  127. 127. Butler PM. Tribosphenic molars in the Cretaceous. In: Smith P, Tchernov E, editors. Structure, Function and Evolution of Teeth. Tel Aviv, Israel: Freund Publishing House; 1992. p. 125–38.
  128. 128. Hillson S. Teeth. 2nd ed. New York: Cambridge University Press; 2005. xiv, 373 p. p.
  129. 129. Butler PM. Evolutionary radiation of the cheek teeth of Cretaceous placentals. Acta Palaeontol Pol. 1977;22(3):241–71.
  130. 130. Anderson PSL, Gill PG, Rayfield EJ. Modeling the effects of cingula structure on strain patterns and potential fracture in tooth enamel. J Morphol. 2011;272(1):50–65. pmid:20960463
  131. 131. Williamson TE, Brusatte SL, Carr TD, Weil A, Standhardt BR. The phylogeny and evolution of Cretaceous-Palaeogene metatherians: cladistic analysis and description of new early Palaeocene specimens from the Nacimiento Formation, New Mexico. J Syst Palaeontol. 2012;10(4):625–51.
  132. 132. Averianov AO, Archibald JD, Ekdale EG. New material of the Late Cretaceous deltatheroidan mammal Sulestes from Uzbekistan and phylogenetic reassessment of the metatherian-eutherian dichotomy. J Syst Palaeontol. 2010;8(3):301–30.
  133. 133. Marshall LG. First Pliocene record of the water opossum, Chironectes minimus (Didelphidae, Marsupialia). J Mammal. 1977;58(3):434–6.
  134. 134. Simpson GG. Didelphidae from the Chapadmalal Formation in the Museo Municipal de Ciencias Naturales de Mar del Plata. Revista del Museo Municipal de Ciencias Naturales de Mar del Plata. 1972;2:1–40.
  135. 135. Reig OA. Descripcion previa de nuevos ungulados y marsupiales fosiles del Plioceno y del Eocuartario Argentinos. Revista del Museo Municipal de Ciencias Naturales y Tradicional de Mar del Plata. 1952;1:119–29.
  136. 136. Travouillon KJ, Gurovich Y, Beck RMD, Muirhead J. An exceptionally well-preserved short-snouted bandicoot (Marsupialia; Peramelemorphia) from Riversleigh’s Oligo-Miocene deposits, northwestern Queensland, Australia. J Vertebr Paleontol. 2010;30(5):1528–46.
  137. 137. Abello MA, De Los Reyes M, Candela AM, Pujos F, Voglino D, Quispe BM. Description of a new species of Sparassocynus (Marsupialia: Didelphoidea: Sparassocynidae) from the late Miocene of Jujuy (Argentina) and taxonomic review of Sparassocynus heterotopicus from the Pliocene of Bolivia. Zootaxa. 2015;3937(1):147–60. pmid:25947465
  138. 138. Marshall LG. Review of the Hathlyacyninae, an extinct subfamily of South American “dog-like” marsupials. Fieldiana Geology, new series. 1981;7:1–120.
  139. 139. Lillegraven JA. Latest Cretaceous mammals of the upper part of Edmonton Formation of Alberta, Canada, and review of marsupial-placental dichotomy in mammalian evolution. The University of Kansas Paleontological Contributions. 1969;50:1–122.
  140. 140. Archibald JD. A study of Mammalia and geology across the Cretaceous-Tertiary boundary in Garfield County, Montana. Univ Calif Publ Geol Sci. 1982;122:1–286.
  141. 141. Matthew WD. A marsupial from the Belly River Cretaceous. With critical observations upon the affinities of the Cretaceous mammals. Bull Am Mus Nat Hist. 1916;35:475–521.
  142. 142. Fox RC. Mammals from the Upper Cretaceous Oldman Formation, Alberta.V. Eodelphis Matthew, and the evolution of the Stagodontidae (Marsupialia). Can J Earth Sci. 1981;18(2):350–65.
  143. 143. Muirhead J, Wroe S. A new genus and species, Badjcinus turnbulli (Thylacinidae: Marsupialia), from the late Oligocene of Riversleigh, northern Australia, and an investigation of thylacinid phylogeny. J Vertebr Paleontol. 1998;18:612–26.
  144. 144. Murray PF, Megirian D. Cranial morphology of the Miocene thylacinid Mutpuracinus archibaldi (Thylacinidae, Marsupialia) and relationships within the Dasyuromorphia). Alcheringa. 2006;Special Issue 1:229–76.
  145. 145. Lofgren DL. Upper premolar configuration of Didelphodon vorax (Mammalia, Marsupialia, Stagodontidae). J Paleontol. 1992;66(1):162–4.
  146. 146. Clemens WA. A mandible of Didelphodon vorax (Marsupialia, Mammalia). Los Angeles County Museum Contributions in Science. 1968;133:1–11.
  147. 147. Scott CS, Fox RC. Review of Stagodontidae (Mammalia, Marsupialia) from the Judithian (Late Cretaceous) Belly River Group of southeastern Alberta, Canada. Can J Earth Sci. 2015;52(8):682–95.
  148. 148. Forasiepi AM, Babot MJ, Zimicz N. Australohyaena antiqua (Mammalia, Metatheria, Sparassodonta), a large predator from the Late Oligocene of Patagonia. J Syst Palaeontol. 2014.
  149. 149. Attard MR, Parr WC, Wilson LA, Archer M, Hand SJ, Rogers TL, et al. Virtual reconstruction and prey size preference in the mid Cenozoic thylacinid, Nimbacinus dicksoni (Thylacinidae, Marsupialia). PLoS ONE. 2014;9(4):e93088. pmid:24718109
  150. 150. Arena DA, Archer M, Godthelp H, Hand SJ, Hocknull S. Hammer-toothed 'marsupial skinks' from the Australian Cenozoic. P Roy Soc B-Biol Sci. 2011;278(1724):3529–33. pmid:21508033
  151. 151. Archer M, Hand SJ, Black KH, Beck RM, Arena DA, Wilson LA, et al. A new family of bizarre durophagous carnivorous marsupials from Miocene deposits in the Riversleigh World Heritage Area, northwestern Queensland. Sci Rep-Uk. 2016;6:26911. pmid:27229325
  152. 152. Oliveira ME, Santori RT. Predatory behavior of the opossum Didelphis albiventris on the pitviper Bothrops jararaca. Stud Neotrop Fauna Environ. 1999;34(2):72–5.
  153. 153. Roberts WW, Steinberg ML, Means LW. Hypothalamic mechanisms for sexual aggressive and other motivational behaviors in opossum Didelphis virginiana. J Comp Physiol Psych. 1967;64(1):1–&.
  154. 154. Pellis SM, Officer RCE. An analysis of some predatory behaviour patterns in four species of carnivorous marsupials (Dasyuridae), with comparative notes on the eutherian cat Felis catus. Ethology. 1987;75(3):177–96.
  155. 155. Pellis SM, Nelson JE. Some aspects of predatory behaviour of the quoll Dasyurus viverrinus. Aust Mammal. 1984;7:5–15.
  156. 156. Warburton NM, Gregoire L, Jacques S, Flandrin C. Adaptations for digging in the forelimb muscle anatomy of the southern brown bandicoot (Isoodon obesulus) and bilby (Macrotis lagotis). Aust J Zool. 2013;61:402–19.
  157. 157. Hopkins SSB, Davis EB. Quantitative morphological proxies for fossoriality in small mammals. J Mammal. 2009;90(6):1449–60.
  158. 158. Elftman HO. Functional adaptations of the pelvis in marsupials. Bull Am Mus Nat Hist. 1929;58:189–232.
  159. 159. Osgood WH. A monographic study of the American marsupial Caenolestes. Field Museum of Natural History Zoological Series. 1921;14:1–162.
  160. 160. Sargis EJ. Functional morphology of the hindlimb of tupaiids (Mammalia, Scandentia) and its phylogenetic implications. J Morphol. 2002;254(2):149–85. pmid:12353299
  161. 161. Salton JA, Sargis EJ. Evolutionary morphology of the Tenrecoidea (Mammalia) hindlimb skeleton. J Morphol. 2009;270(3):367–87. pmid:19107938
  162. 162. Godinot M, Prasad GVR. Discovery of Cretaceous arboreal eutherians. Naturwissenschaften. 1994;81(2):79–81.
  163. 163. Prasad GVR, Godinot M. Eutherian tarsal bones from the Late Cretaceous of India. J Paleontol. 1994;68(4):892–902.
  164. 164. Szalay FS. A new appraisal of marsupial phylogeny and classification. In: Archer M, editor. Carnivorous marsupials. Mosman, New South Wales: Royal Zoological Society of New South Wales; 1982. p. 621–40.
  165. 165. Buchmann OLG, E.R. Behaviour and ecology of the Tasmanian devil, Sarcophilus harrisii. In: Stonehouse B, Gilmore D, editors. The biology of marsupials. Baltimore: University Park Press; 1977. p. 155–68.
  166. 166. Simpson GG. A new Eocene marsupial from Brazil. Am Mus Novit. 1947;1357:1–7.
  167. 167. Marshall LG. The lower jaw of Eobrasilia coutoi Simpson, 1947, a unique didelphoid (not borhyaenoid). J Paleontol. 1984;58(1):173–7.
  168. 168. Marshall LG. Systematics of Itaboraian (middle Paleocene) age "opossum-like" marsupials from the limestone Quarry at Sao Jose de Itaborai, Brazil. In: Archer M, editor. Possums and opossums: studies in evolution. Sydney: Surrey Beatty and Sons and the Royal Zoological Society of New South Wales; 1987. p. 91–160.
  169. 169. Oliveira EV, Goin FJ. A reassessment of bunodont metatherians from the Paleogene of Itaboraí (Brazil): systematics and age of the Itaboraian SALMA. Revista Brasileira de Paleontologia. 2011;14(2):105–36.
  170. 170. Oliveira EV, Goin FJ. A new species of Gaylordia Paula Couto (Mammalia, Metatheria) from Itaboraí, Brazil. Rev Bras Paleontol. 2015;18(1):97–108.
  171. 171. Paula Couto C. de. Fossil mammals from the beginning of the Cenozoic in Brazil. Marsupialia: Didelphidae. Am Mus Novit. 1952;1567:1–26.
  172. 172. Oliveira EV, Goin FJ. Marsupiais do início do Terciário do Brasil: origem, irradiação e história biogeográfica. In: Cáceres NC, Monteiro Filho ELA, editors. Os Marsupiais do Brasil: biologia, ecologia e evolução. Campo Grande: UFMS; 2006. p. 299–320.
  173. 173. Asher RJ, McKenna MC, Emry RJ, Tabrum AR, Kron DG. Morphology and relationships of Apternodus and other extinct, zalambdodont, placental mammals. Bull Am Mus Nat Hist. 2002;273:1–117.
  174. 174. Rougier GW, Davis BM, Novacek MJ. A deltatheroidan mammal from the Upper Cretaceous Baynshiree Formation, eastern Mongolia. Cretaceous Res. 2015;52:167–77.
  175. 175. Ni X, Li Q, Stidham TA, Li L, Lu X, Meng J. A late Paleocene probable metatherian (?deltatheroidan) survivor of the Cretaceous mass extinction. Sci Rep. 2016;6:38547. pmid:27924847
  176. 176. Mitchell KJ, Pratt RC, Watson LN, Gibb GC, Llamas B, Kasper M, et al. Molecular phylogeny, biogeography, and habitat preference evolution of marsupials. Mol Biol Evol. 2014;31(9):2322–30. pmid:24881050
  177. 177. Gallus S, Janke A, Kumar V, Nilsson MA. Disentangling the relationship of the Australian marsupial orders using retrotransposon and evolutionary network analyses. Genome Biology and Evolution. 2015;7(4):985–92. pmid:25786431
  178. 178. Nilsson MA, Churakov G, Sommer M, Tran NV, Zemann A, Brosius J, et al. Tracking marsupial evolution using archaic genomic retroposon insertions. PLoS Biol. 2010;8(7):e1000436. pmid:20668664
  179. 179. Beck RMD, Godthelp H, Weisbecker V, Archer M, Hand SJ. Australia’s oldest marsupial fossils and their biogeographical implications. PLoS ONE. 2008;3(3):e1858. pmid:18365013
  180. 180. Horovitz I, Martin T, Bloch J, Ladevèze S, Kurz C, Sánchez-Villagra MR. Cranial anatomy of the earliest marsupials and the origin of opossums. PLoS ONE. 2009;4(12):e8278. pmid:20016823
  181. 181. Clemens WA. Marsupialia. In: Lillegraven JA, Kielan-Jaworowska Z, Clemens WA, editors. Mesozoic mammals: the first two-thirds of mammalian history. Berkeley: University of California Press; 1979. p. 192–220.
  182. 182. Van Dyck S, Strahan R, editors. The mammals of Australia. Third edition. Sydney: New Holland Publishers; 2008.
  183. 183. Reig OA, Simpson GG. Sparassocynus (Marsupialia, Didelphidae), a peculiar mammal from the late Cenozoic of Argentina. J Zool. 1972;167(Aug):511–39.
  184. 184. Korth WW. Middle Tertiary marsupials (Mammalia) from North America. J Paleontol. 1994;68(2):376–97.
  185. 185. Morlo M, Gunnell GF, Nagel D. Ecomorphological analysis of carnivore guilds in the Eocene through Miocene of Laurasia. In: Goswami A, Friscia A, editors. Carnivoran evolution: new views on phylogeny, form and funtion. Cambridge: Cambridge University Press; 2010. p. 269–310.
  186. 186. Gheerbrant E, Rage JC. Paleobiogeography of Africa: How distinct from Gondwana and Laurasia? Palaeogeogr Palaeoclimatol Palaeoecol. 2006;241(2):224–46.
  187. 187. Gül A. Orhaniye-Güvenc¸ civarindaki (Ankara KB’si) karasal Paleojen birimlerinin stratigrafisi ve sedimantolojisi. 2003.
  188. 188. Sen S. Dispersal of African mammals in Eurasia during the Cenozoic: Ways and whys. Geobios. 2013;46(1–2):159–72.
  189. 189. Smith T, Quesnel F, De Ploeg G, De Franceschi D, Metais G, De Bast E, et al. First Clarkforkian equivalent Land Mammal Age in the latest Paleocene basal Sparnacian facies of Europe: fauna, flora, paleoenvironment and (bio)stratigraphy. PLoS ONE. 2014;9(1):e86229. pmid:24489703
  190. 190. Barrier E, Vrielynck B. Palaeotectonic maps of the Middle East. Tectonosedimentary-palinspastic maps from late Norian to Pliocene. Paris: CGMW/CCGM; 2008.
  191. 191. McNab BK. Uniformity in the basal metabolic rate of marsupials: its causes and consequences. Rev Chil Hist Nat. 2005;78:183–98.
  192. 192. Sears KE. Constraints on the morphological evolution of marsupial shoulder girdles. Evolution. 2004;58(10):2353–70. pmid:15562696
  193. 193. Bennett CV, Goswami A. Statistical support for the hypothesis of developmental constraint in marsupial skull evolution. BMC Biol. 2013;11. pmid:23622087
  194. 194. Echarri S, Prevosti FJ. Differences in mandibular disparity between extant and extinct species of metatherian and placental carnivore clades. Lethaia. 2015;48(2):196–204.
  195. 195. Goswami A, Randau M, Polly PD, Weisbecker V, Bennett CV, Hautier L, et al. Do developmental constraints and high integration limit the evolution of the marsupial oral apparatus? Integr Comp Biol. 2016;56(3):404–15. pmid:27260858