15 Jul 2013: Bardet N, Jalil NE, de Lapparent de Broin F, Germain D, Lambert O, et al. (2013) Correction: A Giant Chelonioid Turtle from the Late Cretaceous of Morocco with a Suction Feeding Apparatus Unique among Tetrapods. doi: info:doi/10.1371/annotation/b4b475f1-6bcc-424a-87dc-aa5fabcc9288 View correction
Secondary adaptation to aquatic life occurred independently in several amniote lineages, including reptiles during the Mesozoic and mammals during the Cenozoic. These evolutionary shifts to aquatic environments imply major morphological modifications, especially of the feeding apparatus. Mesozoic (250–65 Myr) marine reptiles, such as ichthyosaurs, plesiosaurs, mosasaurid squamates, crocodiles, and turtles, exhibit a wide range of adaptations to aquatic feeding and a broad overlap of their tooth morphospaces with those of Cenozoic marine mammals. However, despite these multiple feeding behavior convergences, suction feeding, though being a common feeding strategy in aquatic vertebrates and in marine mammals in particular, has been extremely rarely reported for Mesozoic marine reptiles.
A relative of fossil protostegid and dermochelyoid sea turtles, Ocepechelon bouyai gen. et sp. nov. is a new giant chelonioid from the Late Maastrichtian (67 Myr) of Morocco exhibiting remarkable adaptations to marine life (among others, very dorsally and posteriorly located nostrils). The 70-cm-long skull of Ocepechelon not only makes it one of the largest marine turtles ever described, but also deviates significantly from typical turtle cranial morphology. It shares unique convergences with both syngnathid fishes (unique long tubular bony snout ending in a rounded and anteriorly directed mouth) and beaked whales (large size and elongated edentulous jaws). This striking anatomy suggests extreme adaptation for suction feeding unmatched among known turtles.
The feeding apparatus of Ocepechelon, a bony pipette-like snout, is unique among tetrapods. This new taxon exemplifies the successful systematic and ecological diversification of chelonioid turtles during the Late Cretaceous. This new evidence for a unique trophic specialization in turtles, along with the abundant marine vertebrate faunas associated to Ocepechelon in the Late Maastrichtian phosphatic beds of Morocco, further supports the hypothesis that marine life was, at least locally, very diversified just prior to the Cretaceous/Palaeogene (K/Pg) biotic crisis.
Citation: Bardet N, Jalil N-E, de Lapparent de Broin F, Germain D, Lambert O, Amaghzaz M (2013) A Giant Chelonioid Turtle from the Late Cretaceous of Morocco with a Suction Feeding Apparatus Unique among Tetrapods. PLoS ONE 8(7): e63586. doi:10.1371/journal.pone.0063586
Editor: Laurent Viriot, Team 'Evo-Devo of Vertebrate Dentition', France
Received: July 20, 2012; Accepted: March 25, 2013; Published: July 11, 2013
Copyright: © 2013 Bardet et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: Funding for this project was obtained from the French-Moroccan International Program of Scientific Cooperation between the CNRS and the CNRST (PICS n° 4892 for NB and NEJ) and from the CNRS UMR 7207, Département Histoire de la Terre (MNHN, Paris, France). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
The Phosphates of Morocco: a Hotspot of Vertebrate Palaeobiodiversity at the K/Pg Turnover
The Late Cretaceous - Early Palaeogene Phosphates of Morocco are part of the ‘Mediterranean Tethyan Phosphogenic Province’, a large belt of sedimentary rocks deposited around palaeolatidude 20°S, outshore of the NW part of the African Craton . These phosphatic deposits currently crop out widely in the Middle East, North and West Africa, up to the Pernambuco Province of Brazil, where they are exploited as a valuable economical resource.
Beyond their economical interest, the Phosphates of Morocco are characterized by their extreme richness (both in terms of taxonomical diversity and specimen abundance) in Maastrichtian to Ypresian marine vertebrate taxa, which include selachians, osteichthyan fishes, both continental and marine reptiles (including birds), as well as terrestrial mammals , . Around 96% of the taxa found are of marine origin. Near-shore high productivity during periods of intense upwelling probably played an important role to explain this important paleobiodiversity and the plethora of described species .
Among these vertebrate remains, reptiles, and especially marine forms are, with selachians, the most diversified and abundant. They are represented by more than fifty species along the Maastrichtian-Ypresian Phosphatic series, which represents about one fourth of the total vertebrate species known in the Phosphates of Morocco. During the Maastrichtian, mosasaurid squamates were the most abundant and diversified, representing half the total of species found  (see Table 1).
As far as chelonians are concerned, the Maastrichtian taxa remain poorly known (see Table 1) and their record is scarce compared to that of the very abundant and highly diversified Palaeogene ones , . They include both bothremydid pleurodirans and chelonioid cryptodirans. Up to now, they are only known by a skull of the cheloniid Euclastes , a hyoplastron of an indeterminate ‘dermochelyid’  that might prove to belong to the same taxon as described here or to a closely related one (see Text S1, p. 11–13, in Supporting Information S1), indeterminate forms of cheloniids and bothremydids  (pers. obs.), as well as a new Dermochelyoidae currently under study (Lapparent et al., in prep.) (see Table 1).
The Sea Turtle Fossil Record
Sea turtles, the Chelonioidea (Cryptodira), are known in the fossil record since the Early Cretaceous  or the Late Jurassic ,  and constitute the main group of modern marine reptiles. Their highest diversity occurred during the Late Cretaceous – Early Palaeogene interval, when they were represented by a large number of taxa showing diverse ecological adaptations to an aquatic life, including a large variety of predators, though being edentulous forms .
In Africa, Cretaceous cryptodiran turtles are rather scarce and, apart from the taxa from the Maastrichtian Phosphates of Morocco above mentioned, the only other record is Angolachelys Mateus et al., 2009 from the Turonian of Angola .
Here we describe a new genus and species of marine chelonian found in the Late Maastrichtian of the Oulad Abdoun Basin, central Morocco. It represents not only one of the best records of the rare cryptodiran turtles from the Cretaceous of Africa, but also a new giant form of Chelonioidea recorded just prior to the K/Pg biological crisis, and most notably, a taxon exemplifying a suction feeding apparatus unique among tetrapods.
Materials and Methods
The Phosphates of Morocco Sites
The Phosphates of Morocco crop out in several basins, the most important being the Oulad Abdoun and the Ganntour basins, in central Morocco (Figure 1A). These phosphatic deposits stratigraphically extend from the Late Cretaceous (Maastrichtian) to the base of the middle Eocene (Lutetian), spanning the largest interval of all Tethyan phosphates . The Maastrichtian phosphatic level of the Oulad Abdoun Basin is called Couche III (Level CIII). It is considerably condensed in the eastern part of the basin (Figure 1B–C), being only about 2 to 5 meters thick. It includes two exploited levels of soft phosphates: the yellowish Lower Level III (LLIII), and the greyish Upper Level III (ULIII) (Figure 1C). The series is Late (but not latest) Maastrichtian in age.
Ocepechelon has been found in the Upper Level III (Upper Maastrichtian) phosphatic deposits of the Sidi Chennane area, SE part of the Oulad Abdoun Basin, central Morocco. A, general geographical map of Morocco showing the main phosphatic basins (Ganntour and Oulad Abdoun basins); B, details of the Oulad Abdoun Basin with the northeastern main exploited areas (Daoui, Meraa El Arach, Sidi Chennane); C, synthetical stratigraphical column of the Maastrichtian phosphatic series in the northeastern part of the Oulad Abdoun Basin. Abbreviations : LLIII, Lower Level III; ULIII, Upper Level III; Ph, phosphates; Ma, marls; Li, limestones. The black star indicates the stratigraphical occurrence of Ocepechelon bouyai gen. et sp. nov.
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 “http://zoobank.org/”. The LSID for this publication is: urn:lsid:zoobank.org:pub: DA469295-7A8F-4DD1-A59F-090FC9DB4754. 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.
The phylogenetic analyses have been performed with PAUP*, NONA (winclada interface), and TNT, with all characters considered unordered. The used matrix is modified from Hiramaya  and Kear & Lee . Several rootings have been tried: with and without the hypothetical taxon and the other outgroups. Principal results of the phylogenetical analyses are presented below, with different cladograms obtained according to the variable inclusion of the outgroups. It appears that the results are more congruent with the current knowledge of turtle evolution if the hypothetical taxon is retained in all the tested examples, and particularly for the matrix with two outgroups (hypothetical taxon and Chelomacryptodira). The inclusion of Chelomacryptodira (including both Trionychoidea and Testudinoidea) in the analysis allows the identification of potential homoplasies of a negligible importance between Chelonioidea (including Ocepechelon) and some Chelomacryptodira (see Text S2 in Supporting Information S1).
The main and indispensable synapomorphies of each monophyletic chelonioid group, which are clearly evidenced even if the groups are variably assembled, are presented in the Text S2 and Figure S1 in Supporting Information S1.
Chelonii Latreille, 1800.
Cryptodira Cope, 1868.
Chelonioidea Oppel, 1811.
Dermochelyoidae Baur, 1888.
Ocepechelon gen. nov.
Ocepechelon bouyai sp. nov.
OCP DEK/GE 516, Holotype, Phosphates (Upper Level III, Upper Maastrichtian, uppermost Cretaceous), Sidi Chennane area (Oulad Abdoun Basin, Morocco). Photographs and interpretative drawings. Abbreviations: Boc, basioccipital; Bsph, basisphenoid; Cho, choanae; En, external nare; Fpci, foramen posterior canalis carotici interni; Fr, frontal; Ica, incisura columellae auris; Ju, jugal; Mx, maxilla; Na, nasal; Op, opisthotic; Pa, parietal; Pal, palatine; Pfr, prefrontal; Pmx, premaxilla; Po, postorbital; pr tro ot, processus trochlearis oticus; Pt, pterygoid; Ptw, pterygoid wing; Q, quadrate; Qj, quadratojugal; Ra, marks of the rhamphotheca; Sq, squamosal; Vo, vomer. Scale = 20 cm.
OCP DEK/GE 516, Holotype, Phosphates (Upper Level III, Upper Maastrichtian, uppermost Cretaceous), Sidi Chennane area (Oulad Abdoun Basin, Morocco). Photograph and interpretative drawing. Abbreviations: En, external nare; Fr, frontal; Ica, incisura columellae auris; Ju, jugal; Mx, maxilla; Na, nasal; Pa, parietal; Pal, palatine; Pfr, prefrontal; Pmx, premaxilla; Po, postorbital; Pt, pterygoid; Q, quadrate; Qj, quadratojugal; Ra, marks of the rhamphotheca; Sq, squamosal. Scale = 20 cm.
OCP DEK/GE 516, Holotype, Phosphates (Upper Level III, Upper Maastrichtian, uppermost Cretaceous), Sidi Chennane area (Oulad Abdoun Basin, Morocco). Photographs. Abbreviation: pr tro ot, processus trochlearis oticus. Scale = 20 cm.
OCP DEK/GE 516, Holotype, Phosphates (Upper Level III, Upper Maastrichtian, uppermost Cretaceous), Sidi Chennane area (Oulad Abdoun Basin, Morocco). A, lateroventral view of the skull (left side), showing the processus trochlearis oticus above the processus articularis quadrati. B, posteroventral view of the skull (left side) showing the widely opened fenestra postotica. Abbreviations: c occ, condylus occipitalis; fj, foramen jugulare posterior; fm, foramen magnum; fpci, foramen posterior canalis carotici interni; fpost, fenestra postotica; pr art q, processus articularis quadrati; pr tro ot, processus trochelearis oticus; pt fl, pterygoid flanges; Q, processus articularis quadrati. Scale = 5 cm.
(Published with the permission of C. Letenneur/MNHN under a CC-BY license).
Ocepechelon is a remote relative of the extant leatherback turtle Dermochelys coriacea and of fossil protostegids.
ZooBank life science identifer (LSID) for genus.
ZooBank life science identifer (LSID) for species.
Genus name from OCP, acronym for the Groupe Office Chérifien des Phosphates, the mining company exploiting phosphatic deposits in Morocco, and from Χελώνη (chelone), meaning turtle in Greek; species name from Mr. Baâdi Bouya, engineer geologist, head of the OCP Geological Survey in Khouribga, for his help during our fieldwork.
OCP DEK/GE 516, a complete skull found isolated, Office Chérifien des Phosphates collections, Khouribga (Morocco).
Type locality and horizon.
Trench 2 (N32° 39, 516′; W 06° 38, 280′), Sidi Chennane area, SE part of the Oulad Abdoun Basin, Khouribga Province, Morocco (Figure 1A–B); Phosphatic deposits, base of the Upper Level III (ULIII), Upper Maastrichtian (uppermost Cretaceous) (Figure 1C) , .
For genus and species, by monotypy. Ocepechelon bouyai gen. nov. sp. nov. differs from all other turtles in: a bony pipette-like snout consisting of an elongated arched rostrum with dorsoventrally compressed dermal bones ending anteriorly by a hemitubular and anteriorly directed snout opening; fused horizontal premaxillae and curved ventrolaterally maxillae, located in front of a flattened and wide skull table, that is posterolaterally elongated into large squamosal wings. Posterodorsally placed external nares, partly situated between the anterior part of the orbits and surimposed to the choanae. Flattened nasal cavity. External nare-vomer-choanae-palatine area curved and smooth up to the ventral maxillary margins that bear the marks of a rhamphotheca, ventrally forming thin ‘triturating’ surfaces, that constitute a structure appropriate for flow regulation rather than for prey capture or food processing. Large orbits facing obliquely, located close to the dorsal roof surface and superimposed to the fossae temporalis inferiores, without any bony floor; orbit immediately medial to the cheek emargination with a posterior margin at the vertical level of the anterior border of the well forward located processus articularis quadrati; vertically flattened jugal ventral to the orbit. Strongly developed vertical pterygoid flanges, located medial to the short processus articularis quadrati, and extending ventrally beyond this process. Extensive quadratojugal, quadrate and squamosal, stretched forward and backward, thus arranged horizontally and obliquely rather than vertically; low and prominent processus trochlearis oticus constituted by the quadrate without any prootic contribution, its borders delimited by right angles, forming a wide dorsal subrectangular and slightly concave facet. Incisura columellae auris ventrally facing in a wide semicircular notch of the meatus quadrati. Posterior extremity of the quadrate sutured with the squamosal at the horizontal level of the condylus mandibularis. Skull roof widened and flattened, inducing a wide cerebral cavity and a lateral wall of the cavum cranii bowed anteromedially; ascending epipterygoid also laterally directed and contacting the similarly laterally directed descending processus inferior parietalis; foramen nervi trigemini located at the extremity of a short canal anterolaterally issued from the cavum cranii. Ventrally elongated basicranium: pterygoids and basioccipital, enclosing the basisphenoid, extend far posterior to the condylus mandibularis quadrati, which bears a wide and deep biconcave articular facet; basioccipital tubercles elongated with a protuberant, wide and flattened biconvex condylus occipitalis located between the elongated and widened paroccipital processes of the opisthotic and the squamosal wings. Large size (holotype skull 70 cm long and 43 cm wide).
Comparisons and Phylogenetic Relationships
A detailed description of Ocepechelon bouyai gen. et sp. nov. (Figures 2–5) is available in Text S1 of Supporting Information S1. A detailed phylogenetic analysis (Figure 7, Figure S1) is provided in Text S2 of Supporting Information S1. A life reconstruction is provided in Figure 6.
As a result, on the basis of its skull, Ocepechelon is clearly a cryptodire and not a pleurodire because of: 1) the presence of a processus trochelaris oticus, well visible in frontal view through the orbit, backward to the orbit which is fully open posteriorly; 2) a preserved epipterygoid contact; 3) a posterior extension of the pterygoid (Figures 2, 4, 5A).
Despite the presence of pterygoid flanges (here convergently acquired), Ocepechelon is definitively not a pleurodire because of all the above mentioned characters and because of the absence of a processus trochlearis pterygoideus laterally protruding into the inferior temporal fossa. Upward curled, this process forms in pleurodires a groove (the sulcus palatino-pterygoideus), dorsally opened and connecting the orbit to the inferior temporal fossa, laterally to the braincase and medially to the closed posterior wall of the orbit. In the absence of any posterior wall and groove, it is fully open in Ocepechelon up to the braincase.
It is a Chelonioidea because of the absence of foramina praepalatina and the presence of closely set foramina anteriora canalium carotici interni located in the sella turcica, anterior to the dorsum sellae; although relatively low and wide (possibly as a consequence of the autapomorphic skull flattening), the dorsum sellae is separated from the sella turcica by an oblique crest in conformity with the condition in Chelonioidea.
It is a stem Dermochelyoidae sensu  because of the absence of any ventral medial contact between the fully ventrally reduced jugal and the palatal elements (palatine and pterygoid) linked to a full reduction of the foramen palatinum posterius (as in protostegines and Dermochelys), and because of the vomer no longer contacting the pterygoids.
The foramen palatinum posterius is absent like in some cheloniids but, in these, this absence is due to the presence of a secondary palate and the contact jugal-pterygoid is preserved. The well-developed rodlike rostrum basisphenoidale raising off from the pterygoid floor is similar to that of advanced cheloniids.
Ocepechelon is not a protostegid because the pterygoid, although taking part into the articular process of the quadrate, is not lowered up to the mandibular condyle, and because of the posterior position of the posterior carotid foramen that is fully embedded in the pterygoid. The small and anteriorly rounded ventral basisphenoid is like that of protostegids, but differs in being located posteriorly to the incisura columellae auris. The short dorsal parietal-squamosal contact is similar to that of Protostega but the small parietal posterodorsal emargination is not deep. The Ocepechelon skull, lateroposteriorly prolonged by the squamosal wings, gives an erroneous aspect of a strong emargination, while this is barely larger than in Dermochelys, as shown by the short medial posterior protrusion of the parietals (covering the supraoccipital). Like in at least Corsochelys (undescribed structure in other protostegids), the wide fenestra postotica includes the foramen jugulare posterius and the hypoglossi nerve foramens, because the recessus scalae tympani is not closed posteriorly by any lateroventral extension of the exoccipital toward the basioccipital and the pterygoid (Figure 5B).
Suction Feeding Adaptations of Ocepechelon
Despite the tremendous diversity in form and function of the turtle skulls , , , the skull of Ocepechelon bouyai is one of the most unusual. Although the lower jaw and hyoid apparatus of this species remain unknown, the diet and feeding mechanics of Ocepechelon can be inferred from the architecture of its large and highly specialized skull (see Text S1 of Supporting Information S1 and Figures 2–5) . The flattened, streamlined shape of the cranium, combined with the dorsal position and orientation of the orbits and external nares, suggest that Ocepechelon was an epipelagic turtle hunting close to the sea surface, as for example crocodilians. Its marine behaviour is supported by both the sedimentological context of the type locality and the chelonioid skull anatomy. As a Dermochelyoidae, Ocepechelon much likely possessed limbs modified into flippers, allowing an active swimming ecology in open-sea. Possibly referable postcranial material found in the same Maastrichtian Level III of the Oulad Abdoun Basin further supports this anatomical deduction (see Text S1, p 11–13, in Supporting Information S1).
The most intriguing feature of Ocepechelon is its pipette-like longirostrine bony snout. The thin, tubular snout of Ocepechelon was embedded ventro-laterally in a deep and non-triturating rhamphotheca, as indicated by an area covered by nutritive foramina and short longitudinal sulci. But the absence of cutting, shearing or triturating structures in the upper jaw precludes any use for direct capture or processing of food items.
Ocepechelon has a large head, an elongated upper jaw without food triturating structures, and a mouth aperture in a plan perpendicular to the forward movement, all morphological features characteristic of ram feeding tetrapods . Nevertheless, ram feeders tend to have an oral orifice with a very large cross-sectional area. The snout of Ocepechelon, ending with a relatively small rounded forward-facing-mouth aperture, is reminiscent of the rostrum and mandible of the much smaller syngnathiform fishes (seahorses, pipefishes, and allies), which represent efficient designs for suction feeding –.
Suction feeding is frequent in aquatic vertebrates (chondrichthyans, osteichthyans, amphibians, aquatic turtles and marine mammals) , , –. The aspiration tube of suction feeders is variably formed by the snout, independently from the presence of teeth. It is documented in living short-snouted freshwater turtles such as Chelus and Chelydra, and among extant marine mammals, in the long-snouted sperm whale Physeter and beaked whales (Odonteceti, Ziphiidae), as well as in more or less short-snouted species such as various delphinoids and walruses. In all these groups, the buccal tunnel is at least partly made of soft tissues; examples include the mucosa issued from an external adductor muscle in the freshwater turtle Chelus, the Mundplätte (figures in ), or the large gums, and extensive lower lips that line the mouth opening in beaked whales (diagrams for species of Mesoplodon, figs. 2 and 3 in , figures (partly) and diagrams in , including fig. 3 for a generalized odontocete). Because the tubular rostrum of Ocepechelon is made of bone, it is therefore unique among marine tetrapods.
Ocepechelon differs significantly from other suction feeding turtles , in its unique cranial architecture. It particularly shares some interesting resemblances with beaked whales. Ocepechelon and most beaked whales are large animals, and, as in all other extant cetaceans and Ocepechelon, the nostrils of beaked whales are posterodorsally shifted (Figures 2, 3, 6). They also share similarities on their feeding apparatus: elongated jaws (without triturating surfaces in Ocepechelon and toothless in most extant beaked whales, except for one or two pairs of apical teeth modified in tusks in adult males) and a small gape . The mouth gape of Ocepechelon can be inferred from the diameter of the tube (about 6 cm). It is worth emphasizing the disproportion between the tiny size of the mouth opening and the large size of the skull (70 cm long). The snout diameter predicts that Ocepechelon was a small-prey hunter (e.g., small fishes, cephalopods and jellyfishes). In pipefishes the snout length is inversely related to the mouth cross-section and is considered as an evolutionary advantage since it reduces the time to reach the prey . In Ocepechelon, the elongated rostrum and the round and small mouth much likely increased the velocity of the water influx .
Suction feeding does not require strong biting and is often associated with weakly developed jaw adductor muscles, as seen in edentulous odontocetes. According to the different suction feeding processes, the different parts of the jaw adductor muscles are not equally developed, as seen with the developed mucosa in Chelus , . Dominant muscles in Ocepechelon were attached to the pterygoids, as suggested by the conspicuous large ventral pterygoid flanges of these bones, comparable in development to those of pleurodiran Podocnemididae. In these turtles, the pars ventralis of the muscle pterygoideus (anterior part of the Musculus adductor mandibulae internus), inserted between the developed flanges, has a special function of protraction of the lower jaw, acting in synergy with the rectracting component of the external adductor muscle . Situated above the hyoid apparatus, this muscle couple could also have acted in combination with the piston function of the hyoid and tongue in the swallowing process. By deduction, the same system might have worked convergently in Ocepechelon. However, the muscular bauplan is basically identical for swallowing process in turtles, such as it is figured in the sharpening feeder pleurodire Podocnemis  (fig. 11) (which possesses pterygoid flanges) and the crushing feeder cryptodire Chelonia  (fig. 10).
Moreover, in Ocepechelon, the squamosals are exceptionally developed into broad posterolateral wings, providing large surfaces for visceral muscle attachment , much likely for an important hyoid and tongue musculature, as in other living turtles such as the leatherback Dermochelys ,  and notably the suction feeder Chelus , . The hyoid apparatus and associated musculature are also remarkably developed in cetaceans, especially in suction feeding beaked whales (diagrams and figs. in , , ).
The remarkable and unique anatomy of Ocepechelon, including a unique bony pipette-like longirostrine snout, exceptionnaly large pterygoid flanges and posteriorly developed squamosal wings, suggests a feeding strategy that was later paralleled by several cetaceans, including the beaked whales , , . We hypothesize that it fed, as the latter, by generating a fast, large-amplitude depression within its buccopharyngeal cavity. Given the narrow tubular shape of its upper jaw, Ocepechelon probably performed small-gape suction (with minimally opened mouth), thereby enhancing the suction force for attracting and ingesting the prey (Figures 2, 3, 6, Video S1). In general, a small and circular mouth opening generates greater negative intraoral pressure than a laterally open and larger mouth. A part of the marine mammals, excluding beaked whales, perform a circular mouth opening through shortening and widening of the rostrum and jaws ,  (e.g. odontocete mandibular bluntness studied in details in Werth ).
In aquatic turtles, the expansion of the buccal and pharyngeal cavities plays an important role, since the highly distensible oesophagus may serve as a water reservoir and entrap prey until the closure of the mouth, before swallowing the prey and finally expelling the water, a behaviour that we propose for Ocepechelon –,  (Video S1). Many living turtles, including marine forms such as Dermochelys, have keratinized buccopharyngeal papillae that allow both filtering water and entrapping prey . Beaked whales also possess lingual or palatal horny papillae that may help retaining the prey against the palate . Ocepechelon could have possessed mouth papillae.
During the Mesozoic, large marine carnivorous reptiles such as ichthyopterygians, sauropterygians, mosasaurid squamates and crocodyliformes exhibited a wide range of feeding strategies based on their tooth morphologies, from benthic crushing feeders to huge open-sea generalist predators . However, despite this considerable diversity in the Mesozoic marine reptile modes of predation , , as well as a broad overlap of their tooth morphospaces with those of Cenozoic marine mammals, indicating multiple feeding behavior convergences , suction feeding, though being a common feeding strategy in aquatic vertebrates  has been extremely rarely reported among Mesozoic marine reptiles. It has been hypothesized (but without any concrete argument) for Hupesuchus, a small marine reptile from the Middle Triassic of China  and recently postulated for Shonisaurus ,  and Shastasaurus , both large toothless Triassic ichthyosaurs, interpreted as suction feeders also comparable to many extant odontocetes.
The unique anatomy and ecology of Ocepechelon suggest a prey capture behavior similar to that of several extant suction feeding odontocetes. Furthermore it is the only bony pipette-feeder ever reported among tetrapods. Irrespective of its feeding strategy, Ocepechelon dramatically illustrates the anatomical and taxonomic diversification of chelonioid turtles during the Late Cretaceous (Figures 6, 7). It combines turtle morphology with a feeding device that parallels the adaptation of modern pipefishes and some living odontocetes.
With its peculiar morphology, Ocepechelon likely occupied a different ecological niche compared to other coeval marine reptiles , , , . Its specialization further emphasizes the tremendous diversity that prevailed among the fishes and reptiles in the shallow marine environments of the Late Maastrichian Phosphates of Morocco, shortly before the K/Pg mass extinction event , .
Detailed description, phylogenetical analysis, additional references and Figure S1. Text S1: Detailed description. Text S2: Phylogenetical analysis (based on a slightly modified existing data matrix of morphological characters) including the list of characters, their discussion, the matrix and the details of the analysis with bootstrap values. Additional references: for detailed description and phylogenetical analysis. Figure S1: Chosen examples of cladograms obtained from the modified Kear & Lee (2006) matrix ; S1.1, removing outgroups one after the other, except the hypothetical taxon (cladograms not presented here display only minor changes compared to the ones illustrated); S1.2, Additional tree tested from the matrix of Figure S1.1 (C1 and C2), with the hypothetic taxon and Chelomacryptodira as outgroups; As in the strict consensus (Figure S1.1–C1), L = 207, Ci = 54, Ri = 62.
Animated 3D reconstruction of the suction feeding process in Ocepechelon (Maxon Cinema 4D).
This work is part of an official French-Moroccan Palaeontological Convention between the Muséum National d’Histoire Naturelle/Centre National de la Recherche Scientifique (MNHN/CNRS, Paris), the Office Chérifien des Phosphates (OCP, Casablanca), the Ministère de l’Energie, des Mines, de l’Eau et de l’Environnement (MEMEE, Rabat), and the Universities Cadi Ayyad (UCAM, Marrakech) and Chouaîb Doukkali (UCDJ, El Jadida). We thank E. Gheerbrant, P. Janvier, and C. de Muizon for their advices on the manuscript, O. Selloum for field data concerning the specimen, R. Vacant for the preparation of the specimen, C. Letenneur and C. Lemzaouda for the illustrations, as well as S. Bailon, L. Pierre, J.-F. Voisin and L. Vives, for the access to the collections under their care (all MNHN, Paris). Finally, we thank A. Louchart (ENS, Lyon), J. Claude (UM2, Montpellier) and E. Cadena (North Carolina State University) for their reviews that have permitted to improve our manuscript.
Provided the logistic facilities during field work: MA. Provided the animated 3D reconstruction: DG. Conceived and designed the experiments: NB NEJ FLB DG OL. Performed the experiments: NB NEJ FLB DG OL. Analyzed the data: NB NEJ FLB DG OL. Contributed reagents/materials/analysis tools: NB NEJ FLB DG OL. Wrote the paper: NB NEJ FLB DG OL.
- 1. Lucas J, Prévôt-Lucas L (1996) Tethyan phosphates and bioproductites. In: Nairn AEM et al.., editors. Volume 8: The Tethys Ocean - The Ocean basins and Margins. New York: Plenum Press. 367–391.
- 2. Arambourg C (1952) Les vertébrés fossiles des gisements de phosphates (Maroc-Algérie-Tunisie). Notes Mém Serv Géol Maroc 92: 1–372.
- 3. Bardet N, Pereda Suberbiola X, Jouve S, Bourdon E, Vincent P, et al. (2010) Reptilian assemblages from the latest Cretaceous - Palaeogene phosphates of Morocco: from Arambourg to present time. Hist Biol 22: 186–199. doi: 10.1080/08912961003754945
- 4. Gaffney ES, Tong H, Meylan PS (2006) Evolution of the side-necked turtles: the families Bothremydidae, Euraxemydidae, and Araripemydidae. Bull Am Mus Nat Hist 300: 1–700. doi: 10.1206/0003-0090(2006)300[1:eotstt]2.0.co;2
- 5. Tong H, Hirayama R (2008) A new species of Argillochelys (Testudines: Cryptodira: Cheloniidae) from the Ouled Abdoun phosphate Basin, Morocco. Bull Soc Géol France 179: 623–630. doi: 10.2113/gssgfbull.179.6.623
- 6. Gmira S (1995) Etude des Chéloniens fossiles du Maroc. Anatomie, systématique, phylogénie. Paris: Cahiers de paleontology. 140 p.
- 7. Tong H, Hirayama R (2004) First Cretaceous dermochelyid turtle from Africa. Rev Paléobiologie 9: 55–59.
- 8. Lapparent de Broin F de (2000) African chelonians from the Jurassic to the Present. A preliminary catalog of the African fossil chelonians. Paleontol Afr 36: 43–82.
- 9. Hirayama R (1997) Distribution and diversity of Cretaceous chelonioids. In: Callaway JM, Nicholls EL, editors. Ancient Marine Reptiles. San Diego: Academic Press. 225–241.
- 10. De La Fuente M, Fernández MS (2011) An unusual pattern of limb morphology in the Tithonian marine turtle Neusticemys neuquina from the Vaca Muerta Formation, Neuquén Basin, Argentina. Lethaia 44(1): 15–25. doi: 10.1111/j.1502-3931.2010.00217.x
- 11. Lapparent de Broin F de (2001) The European turtle fauna from the Triassic to the Present. Dumerilia 4(3): 155–216.
- 12. Parham JF, Pyenson ND (2010) New Sea Turtle from the Miocene of Peru and the Iterative Evolution of Feeding Ecomorphologies since the Cretaceous. Jour Pal 84(2): 231–247. doi: 10.1666/09-077r.1
- 13. Mateus O, Jacobs L, Polcyn M, Schulp A, Vineyyard D, et al. (2009) The oldest African eucryptodiran turtle, Angolachelys ombeu, from the Cretaceous of Angola. Acta Pal Pol 54(4): 581–588. doi: 10.4202/app.2008.0063
- 14. Hirayama R (1998) Oldest known sea turtle. Nature 392 (6677): 705–708. doi: 10.1038/33669
- 15. Kear P, Lee MSY (2006) A primitive protostegid from Australia and early sea turtle evolution. Biol Let 2: 116–119. doi: 10.1098/rsbl.2005.0406
- 16. Jalil NE, Lapparent de Broin F de, Bardet N, Vacant R, Bouya B, et al. (2009) Euclastes acutirostris, a new species of marine turtle (Cryptodira, Cheloniidae) from the Palaeocene phosphates of Morocco (Oulad Abdoun Basin, Danian-Thanetian). C R Palevol 8(5): 447–459. doi: 10.1016/j.crpv.2009.03.002
- 17. Bour R, Dubois A (1986) Nomenclature ordinale et familiale des Tortues (Reptilia). Note complémentaire. Bull mens Soc Lin Lyon 55(3): 87–90.
- 18. Ernst CH, Barbour RW (1989) Turtles of the World. Washington, DC: Smithsonian Institution Press.
- 19. Gaffney ES (1979) Comparative cranial morphology of recent and fossil turtles. Bull Am Mus Nat Hist 164: 65–376.
- 20. Benton MJ (2010) studying function and behavior in the fossil record. Plos Biology 8(3): e1000321 doi:10.1371/journal.pbio.1000321.
- 21. Sanderson SL, Wassersug R (1993) Convergent and alternative designs for vertebrate suspension feeding. In: Hanken G, Hall BK, editors. The skull, Vol 3 Functional and Evolutionary Mechanusms. Chicago, IL: University of Chicago Press.
- 22. Bergert BA, Wainwright PC (1997) Morphology and kinematics of prey capture in the syngnathid fishes Hippocampus erectus and Syngnathus floridae. Marine Biol 127: 563–570. doi: 10.1007/s002270050046
- 23. Lussanet MHE de, Muller M (2007) The smaller your mouth, the longer your snout: predicting the snout length of Syngnathus acus, Centriscus scutatus and other pipette feeders. J R Soc Interface 4: 561–573. doi: 10.1098/rsif.2006.0201
- 24. Heyning JE, Mead JG (1996) Suction feeding in beaked whales: morphological and observationnal evidence. Contr Science 464: 1–12.
- 25. Werth AJ (2006a) Odontocete suction feeding: experimental analysis of water flow and head shape. J Morphol 267: 1415–1428. doi: 10.1002/jmor.10486
- 26. Van Wassenbergh S, Roos G, Ferry L (2011) An adaptive explanation for the horse-like shape of seahorses. Nat Commun 2: 164, 10.1038/ncomms1168.
- 27. Werth AJ (2000) Feeding in Marine Mammals. In: Schwenk K, editor. Feeding: Form, Function, and Evolution in Tetrapod Vertebrates. San Diego: Academic Press, 487–526.
- 28. Lambert O, Bianucci G, Post K, de Muizon C, Salas-Gismondi R, et al. (2010) The giant bite of a new raptorial sperm whale from the Miocene epoch of Peru. Nature 466: 105–108. doi: 10.1038/nature09067
- 29. Lauder GV (1985) Aquatic feeding in lower vertebrates. In: Hildebrand M, Bramble DM, Liem KF, Wake DB, editors. Functional Vertebrate Morphology. Cambridge, MA: Harvard University Press, 210–229.
- 30. Lauder GV, Prendergast T (1992) Kinematics of aquatic prey capture in the snapping turtle Chelydra serpentina.. J Exp Biol 164: 55–78.
- 31. Summers AP, Darouian KF, Richmond AM, Brainerd EL (1998) Kinematics of aquatic and terrestrial prey capture in Terrapene carolina, with implications for the evolution of feeding in cryptodire Turtles. J Exp Zool 281: 280–287. doi: 10.1002/(sici)1097-010x(19980701)281:4<280::aid-jez4>3.0.co;2-k
- 32. Lemell P, Lemmell C, Snelderwaard P, Gumpenberger M, Wochesländer R, et al. (2002) Feeding patterns of Chelus fimbriatus (Pleurodira: Chelidae). J Exp Biol 205: 1495–1506. doi: 10.1163/156853810790457803
- 33. Lemell P, Beisser CJ, Gumpenberger M, Snelderwaard P, Gemel R, et al. (2010) The feeding apparatus of Chelus fimbriatus (Pleurodira: Chelidae) – adaptation perfected? Amphibia-Reptilia 31: 97–107. doi: 10.1163/156853810790457803
- 34. Werth AJ (2006b) Mandibular and dental variation and the evolution of suction feeding in Odontoceti. J Mammal 87: 579–588. doi: 10.1644/05-mamm-a-279r1.1
- 35. Schumacher GH (1973) The head muscles and hyolaryngeal skeleton of turtles and crocodilians. In: Gans C, Parsons TS, editors. Biology of Reptilia, Vol. 4. New York: Academic Press.
- 36. Gervais P (1872) Ostéologie de Sphargis luth. Nouv Arch Muséum Mém 8: 199–228.
- 37. Reidenberg JS, Laitman JT (1994) Anatomy of the hyoid apparatus in Odontoceti (toothed whales): specializations of their skeleton and musculature compared with those of terrestrial mammals. Anat Rec 240: 598–624. doi: 10.1002/ar.1092400417
- 38. Van Damme J, Aerts P (1997) Kinematics and Functional Morphology of Aquatic Feeding in Australian Snake-Necked Turtles (Pleurodira; Chelodina). J Morphol 233: 113–125. doi: 10.1002/(sici)1097-4687(199708)233:2<113::aid-jmor3>3.0.co;2-7
- 39. Winokur RM (1988) The buccopharyngeal mucosa of the turtles (Testudines). J Morphol 196: 33–52. doi: 10.1002/jmor.1051960105
- 40. Massare JA (1987) Tooth morphology and prey preference of Mesozoic marine reptiles. J Vert Pal 7: 121–137. doi: 10.1080/02724634.1987.10011647
- 41. Massare JA (1988) Swimming capabilities of Mesozoic marine reptiles: implications for method of predation. Paleobiology 14: 187–205.
- 42. Ciampaglio CN, Wray GA, Corliss BH (2005) A toothy tale of evolution: convergence in tooth morphology among Mesozoic–Cenozoic sharks, reptiles and mammals. Sedimentary Rec 3(4): 4–8.
- 43. Carroll RL, Dong ZM (1991) Hupehsuchus, an enigmatic aquatic reptile from the Triassic of China, and the problem of establishing relationships. Phil Trans Royal Soc London B 28(331): 131–153. doi: 10.1098/rstb.1991.0004
- 44. Collin R, Janis CM (1997) Morphological Constraints on Tetrapod Feeding Mechanisms: Why Were There No Suspension-Feeding Marine Reptiles? In Callaway JM, Nicholls EL, editors. Ancient Marine Reptiles. San Diego: Academic Press, 451–466.
- 45. Nicholls E, Manabe M (2004) Giant species of the Triassic – a new species of Shonisaurus from the Pardonet Formation (Norian: Late Triassic) of British Columbia. J Vert Pal 24: 838–849. doi: 10.1671/0272-4634(2004)024[0838:giottn]2.0.co;2
- 46. Sander PM, Chen X, Cheng L, Wang X (2011) Short-snouted toothless ichthyosaur from China suggests Late Triassic diversification of suction feeding. Plos One 6(5): 1–10. doi: 10.1371/journal.pone.0019480
- 47. Jouve S, Bardet N, Jalil NE, Pereda Suberbiola X, Bouya B, et al. (2008) The oldest African crocodylian: phylogeny, palaeobiogeography, and differential survivorship of marine reptiles through the Cretaceous-Tertiary boundary. J Vert Pal 28: 409–421. doi: 10.1671/0272-4634(2008)28[409:toacpp]2.0.co;2
- 48. Vincent P, Bardet N, Pereda Suberbiola X, Bouya B, Amaghzaz M, et al. (2011) Zarafasaura oceanis, a new elasmosaurid (Reptilian: Sauropterygia) from the Maastrichtian Phosphates of Morocco and the palaeobiogeography of latest Cretaceous plesiosaurs. Gond Res 19: 1062–1073. doi: 10.1016/j.gr.2010.10.005