Temnospondyls are one of the earliest radiations of limbed vertebrates. Skeletal remains of more than 190 genera have been identified from late Paleozoic and early Mesozoic rocks. Paleozoic temnospondyls comprise mainly small to medium sized forms of diverse habits ranging from fully aquatic to fully terrestrial. Accordingly, their ichnological record includes tracks described from many Laurasian localities. Mesozoic temnospondyls, in contrast, include mostly medium to large aquatic or semi-aquatic forms. Exceedingly few fossil tracks or trackways have been attributed to Mesozoic temnospondyls, and as a consequence very little is known of their locomotor capabilities on land.
We report a ca. 200 Ma trackway, Episcopopus ventrosus, from Lesotho, southern Africa that was made by a 3.5 m-long animal. This relatively long trackway records the trackmaker dragging its body along a wet substrate using only the tips of its digits, which in the manus left characteristic drag marks. Based on detailed mapping, casting, and laser scanning of the best-preserved part of the trackway, we identified synapomorphies (e.g., tetradactyl manus, pentadactyl pes) and symplesiomorphies (e.g., absence of claws) in the Episcopopus trackway that indicate a temnospondyl trackmaker.
Our analysis shows that the Episcopopus trackmaker progressed with a sprawling posture, using a lateral-sequence walk. Its forelimbs were the major propulsive elements and there was little lateral bending of the trunk. We suggest this locomotor style, which differs dramatically from the hindlimb-driven locomotion of salamanders and other extant terrestrial tetrapods can be explained by the forwardly shifted center of mass resulting from the relatively large heads and heavily pectoral girdles of temnospondyls.
Citation: Marsicano CA, Wilson JA, Smith RMH (2014) A Temnospondyl Trackway from the Early Mesozoic of Western Gondwana and Its Implications for Basal Tetrapod Locomotion. PLoS ONE9(8): e103255. https://doi.org/10.1371/journal.pone.0103255
Editor: David Carrier, University of Utah, United States of America
Received: March 5, 2014; Accepted: June 28, 2014; Published: August 6, 2014
Copyright: © 2014 Marsicano 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: This research was partially supported by grants Universidad de Buenos Aires Ciencia y Técnica (to CAM), a Woodrow Wilson National Fellowship Foundation Career Enhancement Fellowship for Junior Faculty (to JAW), and Palaeontological Scientific Trust (to RMHS) which also supported our field work during 2005-2008. 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 Moyeni tracksite in Lesotho, southern Africa, preserves a diverse assemblage of large- and medium-sized tetrapod tracks (Fig. 1). The site lies within the lower part of the upper Elliot Formation of the Stormberg Group, whose age has been generally accepted as Early Jurassic based on correlations of its ichnotaxa with those of North America  as well as on the comparative evolutionary grade of its tetrapod fauna . The Moyeni tracksite was first described by Paul Ellenberger , who mapped the surface and identified numerous tetrapod trackways made by several trackmakers preserved in what he interpreted as an emergent sandbank formed at the mouth of a river flowing into a large lake (Fig. 2). The Moyeni tracksite constitutes one of best preserved and diverse tracksites from the Triassic-Jurassic in Gondwana.
Top, paleogeographic reconstruction of southern Pangea during the Late Triassic, 200 Ma (map produced at the University of Texas Institute for Geophysics, 2012; http://www.ig.utexas.edu/research/projects/plates/). Locality is indicated by a star. Bottom, Google Earth image of southern Lesotho showing location of Moyeni tracksite (building indicated by arrow) just outside the town of Quthing. A2 and A4 are major roadways leading to Quthing. Abbreviations: AF, Africa; AN, Antarctica; EU-AS, Eurasia; IN-MA, Indo-Madagascar; NA, North America; SA, South America.
Track surface exposed during 1960s and 1970s, with original interpretations of tracks and surface morphology by Ellenberger (; foldout e). Current position of footbridge and Visitor Center are shown schematically by translucent gray polygons. The trackway of Episcopopus ventrosus is highlighted in blue, and the first and last recorded steps are indicated.
During geological and paleontological field work at Moyeni from 2005 to 2008, we reinterpreted the depositional setting of the tracksite as a meandering fluvial channel on the lower slope of a point bar  and studied the locomotor capabilities of dinosaur trackmakers relative to differences in substrate inclination and slipperiness . The footprints at Moyeni were imprinted into cohesive, fine-grained sand on an exposed scroll bar covered with ripples formed under rapidly waning flood flow. As water levels dropped, the shallow water flowing over the bar top washed-out the ripples and replaced them with current lineation. The flanks of the bar remained sculpted by low amplitude, small current ripples orientated tangential to slope. These surfaces were subsequently draped with a veneer of silty clay that settled out of suspension. A short period of subaerial exposure of the bar is evidenced by wrinkle marks in the claystone veneer, run-off rills, and a distinctive, pustular, surface texture imprinted by shrinkage of a microbial mat that was lowered onto the bar surface .
In addition to saurischian and ornithischian dinosaurs, non-dinosaur tetrapod tracks have been identified at Moyeni. Episcopopus ventrosus tracks were made by a large, slow-moving quadruped with a low body carriage (see , p. 347; pl. 6, fig. 70). The generic name is derived from the Greek word episkopus, which refers “bishop” according to Ellemberger (, p. 53) due to the resemblance between the arcuate limb drag marks and a bishop's crook. The specific name refers to the trackmaker's “heavy belly” (venter, Latin), which flattened the ground below it. The brevity of the initial description of Episcopopus and other Stormberg ichnotaxa  has led some to regards several of these ichnotaxa as nomina nuda . However, given the detailed description provided later , we agree with Porchetti & Nicosia  that “following the spirit of the meaning of priority as well as the ethics of scientific propriety,” the ichnotaxa established by Ellenberger (1970) should be “considered as valid in principle but in need of amendment” (p. 221).
Episcopopus ventrosus is a rare and enigmatic ichnotaxon that has only been reported from the Moyeni tracksite, where only a single, long trackway was recorded. There are no Episcopopus-like trackways known from elsewhere in Lesotho, southern Africa, or indeed from Pangea—not even from the Newark Supergroup, which shares many ichnotaxa with Moyeni . The identity of the Episcopopus trackmaker has remained enigmatic. Ellenberger ,  entertained the possibility of crocodilian, chelonian, or even dinosaurian trackmakers, but subsequent interpretations narrowed the identity to a basal chelonian , .
In this paper, we describe the ichnomorphology of the Episcopopus ventrosus trackway, which we attribute to a ca. 3.5 meter-long temnospondyl. Our re-investigation of Episcopopus used a combination of traditional mapping and laser-scanning techniques. The high-resolution surface scans revealed for the first time details of the footprints and belly drag. We conclude that Episcopopus represents the first definitive temnospondyl trackway from the Mesozoic and provides useful comparisons with the locomotor patterns of extant salamanders, which are frequently used as the model for basal tetrapod locomotion.
The map in Figure 3 was made from three-dimensional data collected on site using a HandyScan HZ portable laser scanner at 0.63–0.88 mm resolution. Individual 50×50 cm squares were scanned, edited in Materialise Magics 14, and then stitched together in Materialise 3-Matic 4.4. Two-dimensional images were created from the modified three-dimensional data. Interpretation of track morphology was based on our in situ observations as well as images of three-dimensional data created with a controlled light source. The corresponding permits for field work in Quting area were issued by the Secretary of the Protection & Preservation Commission, Department of Culture of Lesotho.
Trackway measurements reported in Table S1 follow the standard protocols. Stride length is the distance between homologous points on successive prints of the same foot. Pace length is the distance between homologous points on the prints of the left and right manus or pes. The pace angle is formed by successive paces (i.e., R–L–R or L–R–L). Linear measurements were made to the nearest 0.5 centimeter and were measured in situ unless noted; angular measurements were made to the nearest 0.5 degree using the digital map of the trackway surface.
SAM, Iziko South African Museum, Cape Town, South Africa; UCMP, University of California Museum of Paleontology, Berkeley, California, U.S.A.; UMMP, University of Michigan Museum of Paleontology, Ann Arbor, Michigan, U.S.A.; UMMZ, University of Michigan Museum of Zoology, Ann Arbor, Michigan, U.S.A.
Ichnogenus Episcopopus Ellenberger 1970
Scanned image (top) and interpretive line drawing (bottom) of manus-pes pairs 65–70. Odd numbers represent left manus-pes pairs; even numbers indicate right manus-pes pairs. Direction of travel and left (L) and right (R) are indicated by the arrow at right. Abbreviations: I–V, digits; An., Anamoepus; Gr., Grallator; m, manus; p, pes. White arrowheads indicate straight drag marks probably made by the base of the tail; black and white arrowheads indicate manual digit drag marks. Scale equals 1 m. m.
Right manus-pes pair 56 demonstrating the superposition of the pes print over the manus drag. Note that this is photograph of a cast (positive), with light directed from the upper left. The pentadactly pes (I–V) is positioned forward of the tetradactyl manus (I–IV) and oversteps truncates the digital drag marks (dd) of the manus. The microbial-matted surface (mm) has been smoothed in the immediate vicinty of the tracks. Scale equals 5 cm. cm.
Sinusoidal manus drag between successive footfalls. Image at left shows right manus-pes pair 68 and and right manus 70. The rightmost edge of the belly drag, which smoothed the microbially-matted surface, can be seen at left. The interpretive drawing at right shows schematic outlines (filled in black) of the right manus and pes along with a dotted line indicating the arc of curvature of the drag. Abbreviations: I–V, digit numbers; dd, digit drag; m, manus; p, pes.
Belly drag between manus-pes pairs 65–70. In this photograph of a plaster cast of the trackway, made on site by the authors, the belly drag was recognized by the smoothing of the microbial-matted surface between the successive footfalls. Our interpretation, which is marked in the translucent white tone bordered by a dotted line, differs from that portrayed by Ellenberger across nearly the same interval (: fig. 70, pl. I), which was continuous, broader, and slightly more regularly undulating. That is, our interpretation is that the belly drag was narrower, more discontinuous, and irregular. The scale bar is in centimeters (lower central portion of image).
Moyeni tracksite, Quthing District, Lesotho, southern Africa. In addition to the original prints, there are plaster casts of different sections of the trackway that were made by Ellenberger (Collection Paul Ellenberger—Pistes du Stormberg, Laboratoire de Paléontologie, Institut de Sciences de l'Evolution, Université Montpellier II; ) and by the authors (SAM-PT-K10949). The digital archive of the northern portion of the trackway is stored at the University of Michigan Museum of Paleontology.
ca. 3.5 m-long quadrupedal trackmaker with four manual digits and five pedal digits, all of which lack claws. The digital impressions of the manus and pes are convex anteriorly; together the manual digit impressions form a chevron shape, and together the pedal digit impressions form a rounded arch. The pes oversteps the manus of the previous stride (i.e., secondary overstepping), implying the trackmaker had a relatively long body with short limbs. The body drag is broad and lacks evidence of undulation.
Other distinctive features of Episcopopus may be related to behavior and substrate in this exemplar. These include the lack of registration on the surface by the proximal phalanges or metapodials, as well as the drag marks associated with manus and pes, which differ from one another. The drag marks associated with the manus are sigmoid, elongate, and distally converging, whereas those associated with the pes are short, straight, and non-converging. These latter features are not diagnostic of the ichnotaxon, but provide information about its locomotion, as discussed below.
Ellenberger ,  made interpretations of the Episcopopus tracks that differ substantially from to the one we present below. Some of the more salient differences include the identification of the manus and pes, the number of digits, the presence of claws, and the interpretation of the body drag (see “Description” below).
Ellenberger  described 82 successive manus-pes pairs on the Episcopopus trackway, which he numbered sequentially (Fig. 2). According to him , the trackway starts subaqueously at the southern extreme of the tracksite, on the lower ripple-marked portion of the bar, and climbs tangentially up the western margin of the bar until it emerges from the water just south of the position of the footbridge that now crosses the site. We were not able to identify any definitive Episcopopus tracks south of the bridge as the surface has been eroded since it was studied by Ellenberger in the 1960s. At that time, only the deepest parts of the tracks were visible . The Episcopopus trackway continues northwards from the current position of the bridge across the emergent microbial-matted bar top. This microbial mat has a uniform pustular texture , and surface scan images show that this part of the surface was very gently undulated by low-amplitude ripples oriented perpendicular to the trackway axis. The northernmost 3 m of the trackway, which records the last steps made by the Episcopopus trackmaker on this surface, is now hidden beneath the Visitors' Center building (see ). Thus, due to natural weathering and the new construction, our sample of the Episcopopus trackway is limited to 22 manus-pes pairs exposed between the bridge and Visitors' Center, which correspond to manus-pes pairs 49–70 in Ellenberger's  sequence (Fig. 2). Although this is a smaller sample than that studied by Ellenberger , the tracks that are available to us are still well preserved and offer insights into the identity and mode of locomotion of the Episcopopus trackmaker (Fig. 4).
The Episcopopus trackway records a quadruped animal with a sprawling gait, moving steadily northward (i.e., in the direction of current) with a regular stride length (ca. 110 cm) and pace angulation (ca. 72°) for both manus and pes (see Table S1). The manus and pes prints are well separated from the midline and the low-slung ventral surface of the trackmaker's body left drag marks between its footprints.
The tracks were imprinted on a microbial mat, which bears signs of subaerial exposure in the shrinkage puckering [11-13]. Dragging of the belly and digits over the microbial mat has smoothed its puckered surface (Fig. 4). We conclude that there was no standing water on the bar top when the trackmaker moved across the matted surface; thus the Episcopopus trackmaker was engaging in terrestrial locomotion, not aquatic locomotion or bottom-walking.
The direction of travel is deduced from the shape of the manus and pes digit impressions, both of which form an arc with the convexity facing the same direction. We assume here that the convex side of the manus and pes impressions indicates the forward direction of travel, because we know of no tetrapod has a manus or pes in which lateralmost and medialmost digits are longer than central digits, or that makes anteriorly concave manus and pes impressions. We distinguished between manus and pes impressions by their cross-cutting relationships. In a forward-moving trackmaker, the pes can superpose the manus impression, but not vice versa. Detailed observations of the trackway surface, laser scans, and plaster casts allows us to identify the pes as the more tightly-arched structure that consistently oversteps the manus and crosscuts the manus drag impressions (Fig. 5). Our identification of the manus and pes in the trackway is exactly opposed to Ellenberger's  interpretation, in which the manus print is positioned in front of the pes print (see “Comments” above).
Relative measurements of trackway width, size of the prints, and stride length were used to calculate the body size of the Episcopopus trackmaker (Table S1). The ca. 130 cm glenoacetabular distance and relative shortness of the limbs suggests that the pes-manus overstep is probably second phase; that is, the pes oversteps the manus of the previous stride (Fig. 8). This has been referred to as “long coupling” . In this case, the fairly regular print impressions and constant trackway width (ca. 65 cm) suggest that the secondary overstep is due to the relatively short limbs in the trackmaker rather than a very long-bodied animal or a running “short coupled” gait, as noted by Peabody  in his study on salamander locomotion.
The illustration shows the underside of a stereospondyl as it progresses along a hypothetical trackway surface. The lower portion of the illustration shows the sequence of impressions made by the right and left manus (RM, LM) and pes (RP, LP) leading up to the moment just before the left pes contacts the substrate. Note that in this ‘long-coupled’ form the pes oversteps the manus of the previous stride. We infer that the Episcopopus trackmaker made tracks in this fashion.
The manus prints are preserved as shallow impressions of the tips of the digits (I to IV) and their associated drag marks. No digit impression or drag marks are preserved lateral to these, so we conclude that the trackmaker had a four-digit manus. Occasionally, only the drag marks of the digits are present (e.g., manus print number 68). Not a single palm impression was observed in any of the 22 manus prints studied, nor were they noted by Ellenberger  in the rest of the trackway. It follows that either the palm did not contact the substrate, or it made contact but did not bear enough weight to imprint the surface, which preserves digit drag marks. The digits are clawless, with gently rounded tips. The combined impressions of the digit tips form an inwardly oriented /\-shape that is ca. 25 cm wide by ca. 15 cm long (Figs. 4–6). The apex of the /\ is formed by the digit III print. The digit IV print is located just lateral to the apex, and digits II and I are positioned progressively posterior and medial to it. The outer digits (i.e., III, IV) made deeper, more distinctive impressions than did the inner digits (i.e., I, II). Consequently, in the less well preserved, shallower prints, it is the outer digits, especially digit IV, that are most readily identified (e.g., manus print 69). The impression of digit II could be consistently identified when the light source and contrast of the scanned images were manipulated, but the impression of digit I could only be identified in four instances. All digit impressions are deepest anterolaterally, perhaps as a result of pressure exerted during the “stance phase” of the step cycle , .
All manus prints have distinctive sinusoidal (i.e., “crook-shaped”), forwardly-directed drags for which the genus name of the track was derived (see above; Figs. 2–6). These drag marks were created during the “swing phase” of the step cycle , . They originate from the anterior ends of digits II, III, and IV and converge just in front of the manus print. This convergence of digit impressions implies that the digits faced laterally when planted on the substrate, but superposed one another as the manus was lifted from the substrate and moved inwards at the beginning of its swing. Later, as the forelimb moved forward, the trailing digits impressed a pronounced concave arc that swung outwards before ending with a slight inward movement towards the midline. In some of the best preserved tracks, the end of these trailing digit impressions lead into to the next manus (Fig. 6). Similar S-shaped drag marks are registered by the pes of the living salamander Taricha sp., especially when walking on “soft” substrates or when the animal is fatigued .
Episcopopus pes prints record only the impressions of the tips of five digits; no trace of the sole could be detected in any of the scans. These digit impressions are rounded to somewhat laterally elongated, and like the manual digits, they lack claws. Typically, all five digits are recognizable, and the impressions of digits II–V are arranged in an arc that is ca. 20 cm wide by 20 cm long. The arc is orientated slightly inwards, with the digit I imprinted just posterior to digit II. The interior three digits (i.e., II–IV) make deeper, more distinct impressions, whereas digits I and V make more subtle impressions. Digit I in particular is commonly only visible after the light source and contrast are adjusted. Similar to the manus digits, the pedal digit prints deepen anterolaterally and they also have trailing digit impressions. However, these are shorter, weakly impressed in the sediment, and only associated with digits II and III (Fig. 5). The pedal digit drags are anteriorly directed and run nearly parallel to one another without converging distally. There is no discernible curvature to the pedal digit drag marks, which could be attributed to either their relative shortness or more likely to the absence of significant lateral motion of the pes as it was lifted from the substrate (Figs. 4–6).
The Episcopopus trackway is also characterized by the presence of a median body drag mark (ca. 40 cm wide), which is particularly evident on the microbial-matted bar top surface (Figs. 4, 7). The belly drag was described by Ellenberger , who considered it a diagnostic character of the ichnospecies and attributed its apparent alternating lobes to “balancing” of the animal body during progression. The casts and laser scans demonstrated that the alternating lobes of the body drag were the result of the trackmaker's ventral surface contacting the crests of low-angled ripples (Fig. 7). The ripples cover the paleosurface (see above) and are oriented perpendicular to the axis of elongation of the bar form and tangential to the direction of locomotion of the Episcopopus trackmaker. Thus, variations in the width and depth of the belly drag traces are due to undulations in the surface topography rather than any vertical or lateral movement of the body.
Close to the middle of the broad, shallowly impressed body drag, there is a long, narrow groove that is flanked by a shorter groove along part of its length. Ellenberger  interpreted these as tail impressions, perhaps due to their resemblance to the broad, shallow furrow with lateral ridges made by the tail of ambystomatid salamanders . Another possible explanation is that the elongate groove was made by a single ridge of the tail, but the tip of the tail occasionally contacted the substrate to create a parallel groove. The linear form of these ridges suggests that the proximal portion of tail, which made the drags, was not swinging from side to side. In his study on living salamander trackways, Peabody  observed that even when undulatory movement of the body is not evident in the trackways, its presence can be detected by lateral undulation of the tail. Nevertheless, in Episcopopus, both the body and tail drags lack lateral undulation, indicating that the belly and tail were moving forwards in a straight line when in contact with the sediment. The only evidence of lateral undulation in the locomotion comes from the marked S-shaped manus drags. Although there are short drag marks associated with the pedal digits, they do not indicate any sideways movement of the pes during the step cycle. Thus it appears that only the forelimbs were strongly swung inwards and then outwards during progression.
In the original description of Episcopopus ventrosus, Ellenberger  identified the trackmaker as a primitive crocodilian or possibly a turtle. Later, in his monograph on the footprints and trackways from Lesotho, Ellenberger  provided a full description of Episcopopus and attributed it to a basal crocodilian, based on the resemblance to body fossil taxa described from the same stratigraphic interval (“Upper Stormberg”). Although Ellenberger  could not rule out the possibility that the Episcopopus trackway was made by an ornithischian dinosaur, he rejected his previous hypothesis of a chelonian trackmaker. Later, Olsen and Galton  re-evaluated Ellenberger's ichnotaxonomy of Upper Stormberg footprints, synonomizing 19 of his ichnotaxa with forms from the Newark Supergroup, identifying 26 as indeterminate, and recognizing only one, Episcopopus ventrosus, as “distinct but possibly indeterminate” (p. 94). Olsen and Galton  recognized a superficial similarity to chelonian tracks, which was supported by the presence of proganochelyid body fossils in the same strata . Knoll  likewise suggested an austrochelyid trackmaker for Episcopopus tracks.
Our approach to trackmaker identification hinges on recognizing features preserved in the tracks and trackway that indicate body fossil morphology (i.e., manus, pes, abdomen, tail) and using those proxies to identify the trackmaker clade . Synapomorphies and symplesiomorphies preserved in Episcopopus suggest that it was produced by a quadrupedal basal tetrapod, most probably a temnospondyl. Symplesiomorphies include wide-gauge, sprawling gait, and belly drag, the latter of which results from the combination of a relatively long, stout body and short limbs. In addition, the sinuous impressions made by the trailing manual digits support the hypothesis that the trackmaker did not walk with an erect posture. This type of progression is primitive for tetrapods but is also present in some groups that have secondarily adapted to a semi-aquatic mode-of-life, such as modern crocodilians . It is absent in therapsids and dinosaurs, thus excluding them as potential trackmakers. The absence of claws in both manus and pes is another symplesiomorphy present in amphibians (Fig. 9) that indicates a basal tetrapod trackmaker and excludes amniote trackmakers such as crocodilians and turtles. The presence of a four-digit manus and five-digit pes is a synapomorphy of Amphibia (i.e., Temnospondyli + Lissamphibia) and is also present in some Paleozoic lepospondyls (microsaurs, nectridians) and the Carboniferous colosteid stem-tetrapods , . Although the absence of toe impressions in footprints can be a taphonomic anomaly, we are confident that a fifth manual digit was not present in the Episcopopus trackmaker because high resolution laser scanning was unable to detect even the most subtle impression at either the medial or lateral edge of the manus. We discount nectridean and microsaur lepospondyls as potential trackmakers because they are much smaller than the Episcopopus trackmaker. The largest microsaurs are ca. 10x smaller, and the largest nectrideans are ca. 5x smaller; they are also ca. 50 Ma older than the Triassic-Jurassic age of the Moyeni tracksite, which would imply a lengthy ghost lineage.
Photographs show the impressions left by the undersides of the right manus and pes of the salamander Dicamptodon ensatus (UMMZ 135631). Roman numerals indicate digit number. Scale equals 1 cm. cm.
In light of this combination of synapomorphies, symplesiomorphies, and by process of elimination, the most likely candidate trackmaker is a relatively large temnospondyl amphibian. During the Mesozoic, temnospondyls were represented by the stereospondyls, a highly diverse clade of semi-aquatic to aquatic amphibians . Their aquatic mode of life is characterized by the presence of relatively small and poorly ossified limbs. It is probable that aquatic stereospondyls were incapable of elevating their ventral surface from the ground during locomotion. In addition, the well-defined manus drag-marks are consistent with an animal that had a forwardly-located center of mass and bore more weight on its anterior limbs, due to a relatively large skull and heavy pectoral girdle.
We estimate the total body length of the Episcopopus trackmaker to be approximately 350 cm (Fig. 10), based on the calculated glenoacetabular distance (ca. 130 cm) and comparisons with complete skeletons of Mesozoic stereospondyls, such as the Australian chigutisaurid Siderops  and the European capitosauroid Mastodonsaurus . Cranial fragments of a large, Siderops-like chigutisaurid were found in strata from South Africa  that are coeval with the Moyeni tracksite.
Skeletal silhouettes are shown in ventral view. We calculated the glenoacetabular distance for the temnospondyl to be ca. 130 cm, and its body form is based on comparisons with complete skeletons of Mesozoic stereospondyls, such as the Australian chigutisaurid Siderops  and the European capitosauroid Mastodonsaurus . The salamander body is based on Dicamptodon ensatus (UMMZ 135631) and skeletal information from http://digimorph.org/specimens/Ambystoma_tigrinum/whole/. Important differences between these two include relative size and ossification of the skull and pectoral girdle, robustness of dorsal ribs, and degree of ossification of carpal, tarsal, and metapodial elements. Silhouette reconstructions are not to scale; see schematics at the bottom right size proportions.
Mesozoic Temnospondyl Track Record
The rarity of trackways attributed to temnospondyls in the Mesozoic, particularly during the Triassic, contrasts with the relative abundance of their body fossils, which comprise ca. 160 genera described from Mesozoic levels . Until now there have been no definitive Mesozoic temnospondyl ichnofossils, despite descriptions of several putative temnospondyl tracks, discussed below.
The first Mesozoic temnospondyl footprints were reported from Lower Triassic exposures in Germany , . The isolated footprint figured by Spitz  (Fig. 11B) was discovered on a geological excursion during a conference at Tübingen attended by F. von Huene, E. Hennig, O. Abel, and F. Nopcsa. It was collected from an Upper Buntsandstein outcropping near Kappel, Baden-Württemberg (southern Germany). Apart from the field sketch (drawn by Huene), no description was provided, and the track was not given a name. According to Spitz , Hennig attributed the print to a temnospondyl trackmaker based on the presence of skeletal remains of the temnospondyl Mastodonsaurus cappelensis in the same unit.
A, aubold (1971); B, Pohlig (1893); C, Peabody (1948); D, Fuglewicz et al. (1990). Scale bar equals 10 cm for A and C; 5 cm for D. The original image in B was published without a scale.
Haubold ,  later described two trackways, one with 5 manus-pes pairs and the other with 3 manus-pes pairs, from slightly lower strata (Middle Buntsandstein) exposed at Bernburg near the Saale River in central Germany (Fig. 11A). Haubold  created the new ichnogenus and ichnospecies Capitosauroides bernburgensis to encompass the new trackways, as well as the isolated tracks reported earlier ,  because they were similar in form and provenance. All the German Capitosauroides tracks appear to lack claws. The trackways, in which the manus and pes can be unambiguously identified, were reported to preserve a pentadactyl manus. However, the presence of the lateral-most manual digit (i.e., digit V) is difficult to confirm from available photographs (see , pls. 1–2). Although most temnospondyls have a tetradactyl manus, Haubold  nonetheless attributed the tracks to that group, citing examples of temnospondyls that were at that time restored with five manual digits.
Fuglewicz and colleagues  described a cf. Capitosauroides trackway from Middle Buntsandstein levels at Wióry, in the Holy Cross Mountains of Poland (Fig. 11D). The material includes a trackway consisting of four left manus-pes pairs plus one isolated manus and four right successive pes impressions that lack the posterior margin due to poor preservation . On the left side, the manus prints are slightly smaller and positioned somewhat laterally to the corresponding pes print. The tips of the digits are clearly outlined in each print, and no metapodial impressions were observed . The Polish specimen was reported to be similar to the German Capitosauroides tracks, but differs from them in its larger trackway width and overstepping of the manus by the pes. We could not corroborate the number of manual or pedal digits reported by Fuglewicz et al.  from the photographs they provided; none of the impressions appear to be clearly preserved.
The European tracks attributed to the ichnotaxon Capitosauroides cannot be definitively attributed to a temnospondyl amphibian trackmaker, although some features are consistent with this identification (e.g., absence of claw marks, wide-gauged gait). The wide-gauge gait and absence of claws, however, are not exclusive to temnospondyls. They are primitive features that are expected to be present in non-amniote tetrapods. Moreover, demonstrating the absence of claw marks can be quite difficult, requiring good preservation of several footsteps to offer the best opportunity to preserve those structures. We were not able to confirm that the above-mentioned Capitosauroides specimens definitively lack claws. The presence of a pentadactyl manus is inconsistent with a temnospondyl trackmaker, which would be expected to possess only four functional digits.
Moenkopi capitosaurid tracks.
Peabody  described two isolated manus-pes pairs from the Early Triassic Moenkopi Formation of North America (Fig. 11C). The prints included only the tips of the toes, which were reported to lack claws, and were attributed to a capitosaurid trackmaker in part based on the presence of skeletal remains (UCMP 36718) collected from the same formation . Capitosaurids are crocodile-like, aquatic temnospondyls that include forms such as Mastodonsaurus , the presumed German Capitosauroides trackmaker. The Moenkopi capitosaurid skeleton (UCMP 36713), which is now called Wellesaurus peabodyi , , was reported to have five digits on the manus . The manus-pes pairs that Peabody attributed to a capitosaurid trackmaker were interpreted to have a pentadactyl manus and pes, like Wellesaurus. Notably, several of the preserved manual and pedal digit traces are associated with very narrow, straight drag marks.
The Moenkopi tracks were originally assigned to a temnospondyl trackmaker mainly because the presence of skeletal remains of these animals in the same stratigraphic levels. As occurs with Capitosauroides, the wide-gauged gait and the lack of claw marks are consistent with a temnospondyl trackmaker but do not provide a conclusive identification. The uncertainty surrounding the number of digits in the manus (see , pl. 27A), prevents unequivocally assigning the Moenkopi tracks to temnospondyl amphibians.
Paucity of Mesozoic Temnospondyl Tracks.
Most of the Mesozoic ichnofossils attributed to temnospondyls are isolated tracks, and only a single trackway has been described. In all cases, the tracks appear to lack traces of claws and are quite small in comparison to Episcopopus (Fig. 5). In no case, however, could a tetradactyl manus be unambiguously identified. Rather, in most cases a pentadactyl condition was inferred. Apart from the Moenkopi capitosaurid skeleton, the only other putative pentadactyl temnospondyl described is the Australian stereospondyl Paracyclotosaurus . Although it is not impossible that some temnospondyls had a pentadactyl manus, there is no specimen from the Mesozoic that definitively demonstrates the presence of five manual digits (CAM pers. obs.). Even if some basal temnospondyls did possess a pentadactyl manus, we consider it unlikely that the entirety of the temnospondyl track record would be made up of specimens possessing this condition.
In contrast, the Paleozoic temnospondyl footprint record includes a diverse collection of predominantly small tracks described from several Laurasian localities and stratigraphic levels extending from the Mississipian to the latest Permian [28,35-45]. All of these trackways indicate a trackmaker with a tetradactyl manus and a pentadactyl pes, which was considered diagnostic of “Amphibia” sensu lato or Temnospondyli . In some cases, a temnospondyl trackmaker was inferred due to the relatively large size of the tracks . Other referrals to temnospondyl trackmakers were based on correlation with the body fossil record , , , .
As previously mentioned, the paucity of footprints and trackways attributed to Mesozoic stereospondyls is striking in light of their relatively rich body fossil record, and several explanations are possible. Stereospondyls were predominantly semi-aquatic to aquatic tetrapods, with relatively weak limbs and probably limited capability of locomotion on land , , . The low preservation potential of footprints in saturated sediments, as well as the poor registration of anatomical detail on such surfaces , probably contributes to their rarity. At Moyeni, the cross-cutting relationships with sedimentary structures, emergence features, and other biogenic traces indicate that the Episcopopus tracks were made after the ripple forms had stopped migrating, just after emergence of the bar surface. The unique track preservation and the plasticity of the sediment was probably the result of more than one factor (e.g., sediment composition and granulometry, absence of erosional processes) but certainly enhanced by the microbial mat that covered the bar top where the tracks are strikingly well preserved .
Salamanders have been regarded as the living animals that most closely resemble the ancestral condition for Tetrapoda in terms of locomotion due to their retention of sprawling gait with limbs of equal size, elongated trunk, and a tail [15,48-53]. Salamanders are usually capable of both aquatic and terrestrial locomotion. When walking on land, they have a sprawling posture and produce “standing waves” of body undulations that increase their stride length. When swimming, they use axial undulation of the trunk and tail to produce “travelling waves.” The limbs are held against the trunk to reduce drag and play no active role in propulsion , , .
According to the present understanding of the interrelationships of temnospondlys and their closest relatives , , stereospondyl temnospondyls are close relatives of crown-group amphibians (i.e., frogs, salamanders, caecilians). In this context, the Moyeni tracksite provides a rare opportunity to compare the locomotion of extinct tetrapods against a closely-related extant analogue. Nevertheless, it must be kept in mind that the Episcopopus trackway represents a single exemplar, made by an individual at one time in one place. The resultant ichnomorphology is a function of the interaction between the particular conditions of the Moyeni substrate (e.g., substrate wetness, inclination, grain size) and the Episcopopus trackmaker (e.g., body mass, morphology, behavior), as well as the subsequent modifications (e.g., taphonomic processes during burial and subsequent exposure). Taking into account all these considerations, the Episcopopus trackway preserved at Moyeni still differs in important ways from trackways made by living salamanders.
As previously mentioned, the Episcopopus trackway reveals a sprawling quadruped moving in a straight line. The footfall pattern and other trackway parameters are consistent across the 22 tracks scanned and studied here (Table S1). The underside of the body was not completely elevated from the substrate during locomotion, as evidenced by the well-marked body drag, which occupies a large part of the space between right and left manus and pes prints. None of the manus or pes prints overprint or were overprinted by the body drag, indicating that the limbs were directed laterally and the manus did not reach very far anteriorly during progression. There is little to no transverse movement captured by the body drag, tail drag, or pes drag. The lack of sinuosoidal movement in the pedal digit drags, which are straight and do not converge, and the regular, wide-gauge posture suggests that the rear part of the body did not undulate during locomotion. Moreover, the longitudinal grooves interpreted as part of the tail drag are also straight. In contrast, the arcuate manual digit drags indicate that at least part of the body, the pectoral girdle, was translated transversely during locomotion. The manus drags are asymmetrically S-shaped, with a short medial excursion preceding a longer, more arcuate lateral excursion. Successive manus drags form a more or less sinusoidal pattern whose amplitude indicates the extent of transverse movement of the shoulder girdle. Any sinusoidal movement of the pectoral region of the body might have been overprinted (and obscured) by the straight drag of the rear part of the body and tail.
Very similar drag marks were recorded  in trackways of the salamanders Taricha and Triturus (see , pl. 11), with the crucial difference that it is their pedes that make the sinusoidal drag marks and have a more regular footfall pattern than does the manus. In these and other living terrestrial sprawling tetrapods, both the forelimbs and hindlimbs have a similar weight-bearing capacity, but the hindlimbs are the primary propulsors. The forelimbs, in contrast, mainly provide deceleration during the step cycle [57-60]. Hind limb-driven locomotion depends on the size of the tail, which can produce important frictional forces ,  that influence in the position of the center of mass in reptiles , . In contrast to hind limb-driven locomotors, in semi-aquatic stereospondyls the center of mass was most probably positioned anteriorly due to the relatively larger skull, heavier pectoral girdle, and less massive pelvic girdle , . Moreover, tail size relative to the body length (from the tip of the snout to the first caudal vertebrae) is substantially smaller in stereospondyls (ca. 50%, CAM pers. obs.) than the higher proportions (>80%) reported for salamanders and crocodiles  (Fig. 10). Together, the more forward position of the center of mass and the sinusoidal manus drags indicate that the forelimb, not the hindlimb, was the main propulsive element in the Episcopopus trackmaker, and possibly in other stereospondyls.
A second distinctive difference between Episcopopus and modern salamander tracks is that the former lacks impressions of the proximal phalanges and metapodials. The Episcopopus manus and pes prints are well-marked but consist of only the tips of digits, all of which lack claw marks as well as any evidence of cornified structures that are present occasionally in some salamander and anuran genera . The absence of proximal phalanges and metapodials in the manus and pes prints may reflect a difference related to the substrate condition, behavior, or morphology. Temnospondyl skeletons (Paleozoic and Mesozoic) rarely preserve ossified carpals and tarsals, although they are present in certain heavily ossified forms that have been interpreted to be more terrestrial , . Nevertheless, most Paleozoic footprints and trackways attributed to temnospondyls show conspicuous palm and sole impressions, and variations appear to be related to substrate consistency [35,37-41,44,45]. In living salamanders (e.g., Triturus torosus) imprinting of the manus and pes also varies with substrate consistency, as does the presence of drag marks, particularly on saturated sediments (e.g., UCMP V4133-36752 and V4133-36745; ). On soft or slippery surfaces, Triturus torosus leaves drags marks when the manus/pes sink more deeply in the sediment during the “stance phase” of the step cycle , . In contrast, “tips only” prints are associated with firm or cohesive substrates, where only the part of the autopodium that exerts the most pressure on the substrate, in this case the tips of the digits, is imprinted , .
According to our investigations of the Moyeni tracksite, at the time of imprinting, the surface of the emergent part of the sand bar was moist but not saturated and covered in a microbial mat . Therefore, we consider that this unique trackway morphology reflects the ability of the Episcopopus trackmaker to “pull” its body over the slippery microbial-matted surface using its forelimbs as the main propulsive elements, with the hindlimbs mainly giving support to the rear part of body and tail. We propose that this form of forelimb-driven locomotion allowed these large, heavy, semi-aquatic animals with relatively weak limbs to engage in intermittent bouts of terrestrial locomotion.
Implications for basal tetrapod locomotion
Recent discussions of ancient tetrapod locomotion focused on the sequence of changes in the fins and limbs during the transition from swimming to walking on land , , specifically on which of the two sets of paired appendages was first enlisted in terrestrial locomotion. King and colleagues  argued that the use of pelvic appendages as major propulsors as a characteristic of terrestrial tetrapod locomotion arose in sarcopterigian fishes, before the evolution of digited limbs. In contrast, Pierce and colleagues  in their studies on Ichthyostega locomotor performance suggested that the forelimb was the first enlisted in land locomotion, with hindlimb-powered terrestrial locomotion acquired in later stages of tetrapod evolution. These authors  suggested that because the hindlimbs of Devonian stem-tetrapods were adapted for swimming, rather than for interaction with the substrate, they were unable to employ a modern tetrapod quadrupedal progression on land. They ,  concluded that salamanders might be appropriate “model organisms” for the study of locomotor function in crown-group tetrapods, but they might not be reliable for early stages of the water-land transition in stem-tetrapods.
Fossil tracks and trackways, although preserving only a small portion of trackmaker anatomy, can under certain conditions provide more direct evidence of paleobiology than can be inferred from the fossil body record. This strength is balanced by the taxonomic coarseness with which trackmakers can be identified using synapomophies of body fossil taxa , . In the present case, the Episcopopus trackmaker has been interpreted to be a relatively large, semi-aquatic stereospondyl that was moving along the top of a partially emerged sand bar at the bend in a river. The animal progressed with a sprawling posture, using a lateral-sequence walk without a substantial bending of the trunk. Our analysis suggests that its forelimbs were the major propulsive elements, which dramatically differs from hindlimb-driven locomotion of salamanders and other extant terrestrial tetrapods. If this is true, then salamanders might not be good “model organisms” to study the locomotor behavior of early aquatic and semi-aquatic crown-group tetrapods. Stereospondyls were suitable to perform quadrupedal walking on land, as other sprawling extant tetrapods (i.e. salamanders), but differences in their skeletal plan that likely influence the position of the center of mass resulted in completely different locomotor behaviors (Fig. 10). Further detailed investigations on Paleozoic trackways, in concert with studies of locomotor performance in fossil basal tetrapods, will shed light on the question of how and when the locomotor behavior observed in extant terrestrial sprawling tetrapods evolved.
Approximately 200 million years ago in the part of western Gondwana that is now the southern African country of Lesotho, a partially emerged, microbial-matted sand bar on the inner bank of a river bend was repeatedly traversed by dinosaurs and other tetrapods. The first animal to make tracks across the bar soon after it was subaerially exposed a large stereospondyl amphibian. The tracks, known as Episcopopus ventrosus, represent one of the only definitive temnospondyl trackways known from the Mesozoic Era. The Mesozoic record of temnospondyl tracks is extremely sparse compared to their Paleozoic record, which is relatively much more abundant and spatiotemporally wide-ranging. One possible explanation for this disparity between Paleozoic and Mesozoic track abundance is that the temnospondyls from these respective eras differed in their terrestrial capabilities. Large temnospondyls of the Mesozoic have been inferred to be more aquatic, based on their flattened skulls with dorsally-facing eyes and their poorly ossified distal limb skeleton.
The Episcopopus trackway records a 3.5 m long animal dragging its belly across a wet substrate. In addition to a well-marked body drag, manual digits recorded sinuous drag marks. A detailed study of the trackway has led us to conclude that the animal was reaching with the tips of its fingers to pull its body over the surface and probably using the slippery wet surface to facilitate its progression. This locomotor behavior differs from those observed in living salamanders moving on slippery surfaces, which has been used as living models to interpret basal tetrapod locomotion. The differences between temnospondyl locomotion inferred from trackways and observed salamander locomotion can be explained by major differences in the body shape, size, and skeletal plan of these two groups, which strongly influenced their terrestrial capabilities.
Measurements of Episcopopus trackway at Moyeni, Lesotho. Numbers identifying the successive manus (m) and pes (p) in the trackway follow original Ellenberger'  numbering. Linear measurements are expressed in centimeters and angles in degrees; em-dash denotes missing datum due to preservation bias.
We thank Dr. A. Warren for discussion on temnospondyl forelimbs. We would also like to thank the support of the Lesotho Director of Culture, Ms Khitsane, and Sir David Ambrose for allowing us access to his invaluable archive of the trackways of Lesotho. We thank B. Miljour for her assistance with Figures 2 and 11 and Gabriel Lio with Figures 8 and 10. S. O'Grady and the UM 3D lab provided assistance with the laser scanner and imaging. T. O'Connell and J. Whitlock stitched together individual 50×50 cm scans. This is CAM's R-122 contribution to the Instituto de Estudios Andinos “Don Pablo Groeber”.
Conceived and designed the experiments: CAM JAW RMHS. Performed the experiments: CAM JAW RMHS. Analyzed the data: CAM JAW RMHS. Contributed reagents/materials/analysis tools: CAM JAW RMHS. Wrote the paper: CAM JAW RMHS.
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