As a single stratigraphic source and site of high-fidelity vertebrate trackways and superbly preserved skeletons, the Lower Permian Tambach Formation, lowermost unit of the Upper Rotliegend, of the Bromacker locality in the middle part of the Thuringian Forest near Gotha, central Germany, provides a unique opportunity of matching late Paleozoic trackways with their trackmakers. Here the track-trackmaker association is firmly established between two species of the ichnogenus Ichniotherium, Ichniotherium cottae and Ichniotherium sphaerodactylum, and the skeletal fossils of the closely related diadectids Diadectes absitus and Orobates pabsti, respectively. These are the first well-documented species-level identifications of the trackmakers of Paleozoic trackways. The Ichniotherium ichnospecies are principally separated by the relative lengths of the digits of the pes imprint and the degree of overstepping of the pes and manus imprints. Both characters are shown to be clearly due to differences in the number and lengths of phalangeal elements and the number of presacral vertebrae of the diadectid species. The unique methods employed here in establishing the track-trackmaker associations provide not only an innovative data source for studying the evolutionary biology, paleo-biogeography, and locomotor behaviour of the trackmakers, but also a valuable methodology for evaluating taxonomic concepts in vertebrate ichnology.
Tetrapod footprints are a common phenomenon in late Paleozoic terrestrial deposits, having been documented by several thousand specimens from Africa, Europe, European Russia, North America, and South America. Due to their abundant record, global distribution, and autochthonous origin vertebrate tracks are often used as collateral evidence in reconstructing terrestrial tetrapod communities for paleoecological, biostratigraphic, and biogeographic analyses (e.g., Matsukawa et al., 2005; Van Allen et al., 2005). The accuracy of such studies is facilitated by confident identification of a biospecies as the progenitor of an ichnospecies. Unfortunately, this approach is typically obstructed severely by two commonly encountered obstacles: (1) biotaxa are typically based mainly on cranial features, whereas ichnotaxa are based strictly on features of the tracks and trackways; and (2) even if the structures of the manus and pes of a biotaxon are well known, there remains the difficulty of matching them to imprints that reflect a soft-tissue encasement of skeletal structures. Due to this taphonomic bias, tetrapod ichnogen-era and ichnospecies are usually more or less vaguely referred to families or orders within paleobiological classifications (Haubold, 2000). This practice is necessitated in essence by an insufficient skeletal fossil record. Despite the large number of late Paleozoic track sites and tracks, there is only a small portion of sufficiently well-preserved specimens to which anatomical differences of the imprint morphology or trackway pattern can be used to differentiate ichnospecies. On the other hand, the skeletal fossil record typically lacks sufficiently preserved postcrania to allow detailed comparisons with ichnospecimens. Moreover, relevant tracks and skeletal remains are predominantly preserved in different sedimentary fades and often in different formations that are widely separated stratigraphically and spatially, further raising the suspicion about the accuracy of track-trackmaker associations.
Here we present well-documented examples in which the origins of two vertebrate ichnospecies of Ichniotherium can be ascribed to two biospecies of closely related genera of Diadectidae that occur with tracks at essentially the same stratigraphic level of the Lower Permian Tambach Formation of the Bromacker locality in central Germany. These are the first such examples of Paleozoic track-trackmaker associations at the species level and are based on anatomical features of the trackmaker's postcranial skeleton that are clearly transcribed in the imprint morphology and trackway pattern of the ichnotaxa.
MATERIALS AND METHODS
This study is based on 53 trackways of the Permo-Carboniferous tetrapod ichnogenus Ichniotherium Pohlig, 1892, which include 11 specimens of Ichniotherium cottae (Pohlig, 1885) and 42 of Ichniotherium sphaerodactylum (Pabst, 1895) collected from the Lower Permian Tambach Formation of the Bromacker locality in Thuringia, central Germany. Collectively, these specimens comprise more than 600 manus and pes imprints, as well as several hundred Ichniotherium tracks of incompletely preserved trackways. The difference in the abundances of the two ichnospecies trackways does not reflect a selective bias of the specimens studied, but rather a tally of all the Ichniotherium trackways encountered by the senior author during a 5-year research program of reviewing Permo-Carboniferous tet-rapod footprints. To assess the variability of the trackways, they were photographed both in overview and as individual imprints. Most importantly, the trackways were outlined on transparency film in order to record measurements of 28 different parameters of imprint morphology and trackway pattern (Appendices 1, 2). All of the measurements are widely accepted as standard, procedural practice and have been fully described in other such studies (e.g., Haubold, 1971; Leonardi, 1987; Voigt and Haubold, 2000).
The Tambach Formation of the Bromacker locality has yielded about a dozen partial to complete, articulated skeletons of the diadectids Diadectes absitus Berman, Sumida, and Martens, 1998, and Orobates pabsti Berman, Henrici, Kissel, Sumida, and Martens, 2004 (see Appendix 3), which are described here as the trackmakers of the ichnospecies Ichniotherium cottae and Ichniotherium sphaerodactylum, respectively. Before the description of Diadectes Cope, 1878, from the Bromacker locality (Berman et al., 1998), this well-known genus had an exclusively North American distribution, whereas the occurrence of Orobates (Berman et al., 2004) is restricted to the Bromacker locality. Unfortunately, only a few specimens of the two Bromacker diadectids are useful in identifying them as the trackmakers of I. cottae and I. sphaerodactylum. Of the Bromacker D. absitus specimens, the greater portion of the articulated postcranial skeleton of MNG 7721 provides the first example of a complete, articulated manus (a right). Examples of the pes in D. absitus, however, are limited to a partial right tarsus in the holotype MNG 8853, which consists of the greater portion of an articulated skeleton with skull, and a partial pes in MNG 10650, which consists of an articulated right tibia, fibula, partial tarsus, and metatarsals 1–4 (Berman et al., 1998; Berman and Henrici, 2003). In the absence of an example of a complete pes in D. absitus the present analysis uses a large, mature Diadectes sp. specimen, CM 41700, from the Permo-Carboniferous of North America that consists of a superbly preserved, dorsally exposed, articulated posterior half of the postcranial skeleton (Berman, 1993; Eberth and Berman, 1993; Berman and Henrici, 2003). In this specimen both hind limbs are extended directly outward from the pelvis and the pedes are splayed out and present mirrored images of one another. Except for a missing medial centrale in the left tarsus, the pedes exhibit the full complement of elements in their correct relative positions to each other. This substitution is justified by the fact that the partial pedes in the Bromacker specimens MNG 8853 and 10650 exhibit no noticeable deviations from those in CM 41700 (Berman and Henrici, 2003) and that there is only one Diadectes species, D. absitus, known from the locality. CM 41700 is also important to this study in possessing a complete, articulated tail, which is not preserved fully in any of the D. absitus specimens.
The holotype of Orobates pabsti, MNG 10181, a complete, superbly preserved, articulated skeleton, exhibits all the structures necessary for this study in dorsal view: (1) a complete vertebral column that includes the presacral region and the entire tail; (2) both manus, with the right exposed in dorsal view, and all the elements in nearly their correct relative positions to each other; and (3) both hind limbs extend outward from the pelvis with the pedes exposed splayed out and presenting mirrored images of one another with all the elements occupying their correct positions relative to each other. Because the North American and German Diadectes specimens are structurally identical in their postcranial characters (Berman et al., 1998), they collectively provide a reliable basis for comparison with O. pabsti. All of the measurements of postcranial structures included herein have been made directly from the study specimens.
BGR, Bundesanstalt fur Geow-issenschaften und Rohstoffe; Außenstelle Berlin-Spandau, Germany; BUW, Bauhaus-Universitat Weimar, Germany; CM, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, U.S.A.; FG, Geologisches Institut der Technischen Universitat Bergakademie, Freiberg, Germany; GZG, Geowissenschaftliches Zentrum Gottingen, Germany; HF, Institut für Geologische Wissenschaften und Geiseltalmuseum, Martin-Luther-Universität Halle-Wittenberg, Germany; HLMD, Hessisches Landesmuseum Darmstadt, Germany; LMJG, Landesmuseum Joanneum Graz, Austria; MB, Naturkundemuseum Berlin, Germany; MLP, Museum of Natural History La Plata, Argentina; MNG, Museum der Natur Gotha, Germany; MSEO, Museum Schloß Ehrenstein, Ohrdruf, Germany; NHMM, Naturhistorisches Museum Magdeburg, Germany; NHMS, Naturhistorisches Museum Schloß Bertholdsburg Schleusingen, Germany; NHMW, Naturhistorisches Museum Wien, Austria; NME, Naturkundemuseum Erfurt, Germany; PMJ, Phyletisches Museum Jena, Germany; RE, Ruhrlandmuseum Essen, Germany; SMMGD, Staatliches Museum für Mineralogie und Geologie Dresden, Germany; UGBL, Urweltmuseum Geoskop Burg Lichtenberg, Thallichtenberg, Germany.
as, astragalus; ca, calcaneum; fe, femur; fi, fibula; h, humerus; i, intermedium or its portion of astragalus; lc, lateral centrale; mc, medial centrale; pc, proximal centrale or its portion of astragalus; pi, pisiform; r, radius; ra, radiale; ti, tibia; tib, tibiale or its portion of astragalus; u, ulna; ul, ulnare; 1–4, distal carpals and tarsals.
A, distance between manus and pes; B, width of pace; C, apparent body length; m, manus imprint; mb, width of manus imprint; ml, length of manus imprint; ml to mV, length of digit I to V of the manus imprint; P, length of pace; p, pes imprint; pb, width of pes imprint; pl, length of pes imprint; pI to pV, length of digit I to V of the pes imprint; S, length of stride; α, pace angulation; β, divarication of manus or pes from midline, plus = outward rotation, minus = inward rotation; γ, interdigital angle I–V; I–II–III–IV–V, first to fifth digit, numbered from medial to lateral side of imprint.
With one exception (postcranial skeletal of Diadectes, CM 41700) the present study is based entirely on vertebrate skeletal fossils and tracks or trackways from the Lower Permian Bromacker locality, an area of small abandoned and intermittently active quarries scattered over an area of less than 0.5 km2 in the middle part of the Thuringian Forest approximately 1.5 km north of the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany (Fig. 1). This is the type locality of the Tambach Sandstone, a 50–100 m thick, mid-member of an informal, tripartite division the Tambach Formation, which forms the base of the Upper Rotliegend Group or Series in this area and comprises a 200–400 m thick unit of conglomerates, sandstones, and mudstones. The red beds of the Tambach Formation, whose outcrops are now restricted to an area of about 50 km2, were deposited in a small, internally drained paleograben, termed the Tambach Basin, approximately 250 km2 in original aerial extent. The Bromacker locality lies near the center of the former Tambach Basin. The vertebrate tracks and skeletons occur in a 10 m thick stratigraphic interval of the Tambach Sandstone exposed in the commercial quarries of the Bromacker locality. Eberth and colleagues (2000) interpreted the deposition of the Bromacker sediments and its associated fossil assemblage of the Tambach Basin as representing a rarely described paleoenvironment of a ‘truly upland’ terrestrial setting that was far removed and up-dip from coal-swamps or extensive coastal or alluvial plains bordering non–coal-forming wetlands, which has been the overwhelming source of Late Pennsylvanian-Early Permian vertebrates.
Based on different facies content the Bromacker section was divided into two conformable stratigraphic intervals by Eberth and colleagues (2000; Fig. 1), a sandstone-dominated Lower Beds and a mudstone-dominated Upper Beds. The Lower Beds consist of several decimeter-thick massive to bedded sandstones with millimeter-to-centimeter thick laterally-extensive mud-drapes along which they are easily split into the commercial sandstones slabs. Desiccation cracks, macroplant and jellyfish impressions, invertebrate trace fossils, the vertebrate tracks for which the Bromacker locality is famous, as well as evaporation and raindrop marks, are commonly preserved on the lower surface of the sandstone slabs (Haubold, 1973b; Martens, 1975; Barthel and Rößler, 1994; Eberth et al., 2000; Voigt, 2002b). The sandstone bodies alternate with decimeter-thick laminated to bedded siltstones. The Upper Beds are dominated by two facies: basal, decimeter-scaled massive siltstones to very fine-grained sandstones, which are sharply overlain by beds of finely laminated siltstone and claystone. Essentially all of the hundreds of vertebrate skeletal specimens collected from the Bromacker, ranging from isolated elements to partial and complete, articulated skeletons, including the diadectid specimens that are the subject of this study (e.g., Boy and Martens, 1991; Berman and Martens, 1993; Berman et al., 1998, 2004; Berman, Henrici, et al., 2000; Berman, Reisz, et al., 2000), were recovered from two closely associated sheetflood deposits within a stratigraphic interval of 1.2 m within the massive siltstones of the Upper Beds. The overlying facies of very finely interlaminated siltstone and claystone beds, up to 15 cm thick, have yielded impressions of conchostracans, insect wings, and myriapod fragments (Martens et al., 1981).
According to Eberth and colleagues (2000) the red beds of the Bromacker locality were probably deposited on an upland alluvial plain with minor stream channels. Fossil biota and bedding plane markings indicate seasonal wet-dry cycles of a savanna-type climate. The sandstone sheets and their mudstone drapes of the Lower Beds were interpreted as recurrent alluvial paleochannel and interfluvial deposition, respectively. The sandstones sheets were deposited as low-sinuosity, shallow, paleochannel fills during high-energy flooding events. A cessation of the flooding events due to a blockage or back up of the channels was followed by mud-laden, slack-water conditions that drowned the channels and resulted in the laterally extensive deposition of the mud drapes. The Upper Beds were interpreted as an upper-flow-regime sheetflood deposit and waning flood deposits in an ephemeral-lacustrine to flood basin setting. The sheetfloods probably originated at the margins of the Tambach Basin and, when sufficiently intense, spread across the low-sloping land surface of the basin center. The fine-grained sandstone lenses were interpreted as shallow, locally developed, channel fills. Because the depositional style of the Lower and Upper Beds represents cyclic deposition of coarser-grained flood sediments followed by slack-water conditions with suspension deposition that are very similar to one another, sedimentation of the Bromacker red-bed succession from the Lower Beds to the Upper Beds is thought to have occurred without a significant stratigraphic break. On this basis it is probable that the taxa represented by the skeletal remains in the Upper Beds are the same as those that made the tracks in the Lower Beds.
BROMACKER TETRAPOD ICHNOTAXA RECORD
Preservation and Ichnofauna
The Bromacker locality has long been known for exceptionally well-preserved tetrapod footprints (Pohlig, 1892; Pabst, 1895, 1908; Voigt, 2002a). Approximately 300 large trackway slabs that collectively include thousands of single imprints have been recovered during the past 120 years of commercial quarrying activities in the area (e.g., Müller, 1954; Steiner and Schneider, 1963; Haubold, 1973b; Fichter, 1998). The superb preservation and abundance of the tracks in the Lower Beds was undoubtedly the result of the unusual sedimentary conditions in which they were made: (1) the tracks were made on the uppermost surface of thin, mm-to-cm-thick drying mud layers of the mud drapes and, therefore, represent true surface footprints with the potential of preserving ultra-fine anatomical details such as skin impressions; (2) the underlying sandy substrate of the paleochannel fill was sufficiently coarse-grained and thick-layered to provide firm support and only shallow penetration by the trackmakers; and (3) the sand grains of the overlying channel fill that filled in the imprints were of sufficient fineness to form detailed natural casts of the tracks. The tetrapod tracks of the Tambach Sandstone are, therefore, exclusively preserved as convex hyporeliefs on the bottom surface of the sandstone channel fills. The Bromacker locality can be regarded as presenting optimum conditions for the preservation of tetrapod tracks.
To date, five vertebrate ichnogenera are currently recognized from the Tambach Sandstone of the Bromacker locality (Haubold, 1998; Voigt, 2005): (1) Amphisauropus Haubold, 1970, referred to the seymouriamorph amphibians; (2) Ichniotherium Pohlig, 1892, referred to the diadectomorph Diadectidae; (3) Dimetropus Romer and Price, 1940, referred to the primitive basal synapsid sphenacodontids or caseids; (4) Varanopus Moodie, 1929, referred to the reptilian Captorhinomorpha; and (5) Tambachichnium Müller, 1954, of uncertain origin and tentatively referred to the parareptilian bolosaurids or primitive basal synapsid Varanopidae (Haubold, 1998; Voigt, 2005). Ichniotherium is by far the most common ichnogenus from the Tambach Sandstone, representing more than 95% of all tetrapod footprints recovered (Haubold, 1998).
Ichniotherium Pohlig, 1892
Since the beginning of ichnologic studies of the Bromacker site in the late 19th century, researchers discerned minor morphological differences in the Ichniotherium footprint record, which they used as a basis for ichnospecies recognition. Shortly following the description of Ichniotherium cottae (Pohlig, 1885), two additional ichnospecies or ichnosubspecies of Ichniotherium were recognized (Pabst, 1895, 1908) at the Bromacker locality, the more common Ichniotherium sphaerodactylum (Pabst, 1895) and the rather rare I. sphaerodactylum minor (Pabst, 1895). Nopcsa (1923), Lotze (1928), and Korn (1933) not only accepted the subspecific separation of the Bromacker Ichniotherium tracks, but also proposed a greater ichnotaxonomic separation on the basis of differences in trackway patterns. Haubold (1971, 1973a) initially argued that I. sphaerodactylum, I. sphaerodactylum minor, and I. cottae are the tracks of a single species which reflected different gaits, and so he synonymized the former two ichnospecies with Ichniotherium cottae, the first named ichnotaxon (Pohlig, 1885, 1892). However, in a recent revision of the Ichniotherium assemblage of the Bromacker locality Voigt and Haubold (2000) recognised two morphotypes of Ichniotherium that they referred to as A and B, which differ in the relative length of digit V of the pes imprint and the trackway pattern. They noted that the imprints of the more common morphotype A exhibits a longer digit V and a trackway pattern indicative of a slow to moderate rate of locomotion by the trackmaker, whereas the imprints of the rarer morphotype B exhibits a shorter digit V and a trackway pattern indicative of a more rapid rate of locomotion. On this basis Voigt and Haubold (2000) concluded, as Haubold (1971, 1973a) had earlier, that morphotypes A and B were made by individuals of the same species, and their differences merely reflect different gaits and speeds. The short digit V of the morphotype B, which is represented only by the rounded imprint of the digit tip, was interpreted by Voigt and Haubold (2000) as indicating a greater speed and less plantigrade gait of the trackmaker. This explanation for the differences in the two types of Ichniotherium tracks was abandoned, however, with the discovery in 2002 of the second most prolific Ichniotherium track site in the Permo-Pennsylvanian red beds of the Maroon Formation near Maroon Bells, central Colorado (Voigt et al., 2005). Here numerous trackway segments and hundreds of isolated imprints of Ichniotherium were recorded that are identical to the morphotype B tracks of the Bromacker locality. Thus, it was concluded (Voigt et al., 2005) that morphotypes A and B of Ichniotherium were made by very closely related animals that differ in some post-cranial characters, such as the relative length of digit V of the pes and the ratio of the body length to that of the limbs. This significant expansion of the ichnological database revealed clearly that two different ichnospecies of Ichniotherium occur at the Bromacker locality: I. sphaerodactylum (Pabst, 1895) and I. cottae (Pohlig, 1885), which are synonymous with morphotypes A and B, respectively, of Voigt and Haubold (2000). The taxonomy of both ichnospecies is complex and beyond the goal of this study (cf. Voigt, 2005). Yet, it can be stated that Ichniotherium undoubtedly represents the best example of all late Palaeozoic tetrapod ichnogenera in which ichnospecies can be distinguished on anatomically controlled characters of the imprint morphology and trackway pattern that correlate with well-preserved body fossils.
Based on the abundant track record from the Bromacker locality Ichniotherium is the trackway of a quadrupedal tetrapod with pentadactyle, plantigrade footprints between 5.5 and 13.0 cm in length (Fig. 2). In both the manus and pes footprints digits I–IV exhibit a serial increase in length, whereas the length of digit V is ichnospecies specific in being either shorter than II or as long as III. In well-preserved manus and pes tracks the digits, particularly their proximal portions, are segmented transversely by short, very narrow, slightly irregularly curved grooves. The distal portions of digits II–IV of the manus imprint are distinct from those of the pes in being more strongly bent or angled toward the trackway midline. The manus and pes impressions of Ichniotherium can be easily recognized by a large, mediolaterally expanded, oval solepad impression that is clearly separated from the digit impressions. In contrast to the solepad impression of the manus, however, that of the pes is more clearly defined marginally and is larger in relief. Also typical of the pes, the digits terminate in expanded, rounded margins that give them a drumstick-like outline. The length of the manus imprint is about 80% of that of the pes, with a width that exceeds its length by about 20%, whereas the pes imprint is about as long as it is wide.
Other than the manus imprint always being positioned in front of the pes track, the trackway pattern of Ichniotherium is variable. Trackways with a long manus-pes separation are usually characterised by the manus imprint of one side being contra lateral to the pes imprint of the opposite side (=alternating arrangement of single imprints). The shorter the manus-pes separation the greater is the tendency for an alternating arrangement of coupled manus-pes imprints (Fig. 2A). Although primary overstepping occurs in trackways showing a distinctly alternating arrangement of footprint sets, it is, however, never greater than partial, with the digits of the pes imprint never reaching the base of the digits of the manus imprint. The trackway width and length of pace of the manus imprints are somewhat smaller than those of the pes imprints. The pace angulation ranges between 70° and 130°, the ratio of the stride length to pes length is 2.5–5.5:1, and the ratio of the stride length to the apparent body length is 0.8–1.7:1. Both the manus and pes imprints are directed inward, approximately 25° and 8°, respectively. A tail-drag mark is very rare and always discontinuously preserved.
Ichniotherium cottae (Pohlig, 1885) Characterization
The most diagnostic features of the manus and pes imprint morphology of Ichniotherium cottae are the lengths of digit V and the shape of the sole pad. In both the manus and pes imprints digit V is short, measuring about 50% of the length of digit IV (Fig. 3A–C, Appendix 1). The sole pad impression of the manus track exhibits an oval-to-subcircular outline with a mediolateral width that exceeds only slightly its proximodistal length and lies opposite digits II and III. Preservation of the sole pad impression of the pes track occurs as two, cojoined semicircular outlines: a medial, oval-to-subcircular outline that lies opposite digits II–IV and a smaller outline that joins its proximolateral margin as an oval-to-semicircular extension that lies opposite digit V (Fig. 3A–C). The appearance of the latter portion of the impression is apparently dependent on the impression of the sole pad being sufficiently deep to include it. The entire sole pad impression has a greatest mediolateral width that exceeds its greatest proximo-distal length by about 53%. The manus and pes lengths range between 5.5 and 7.6 cm and 6.6 and 8.4 cm, respectively (see Appendix 1).
The trackway pattern ranges from a nearly alternating arrangement of single imprints to an alternating arrangement of coupled manus-pes imprints (Fig. 4A–C). The latter pattern is more common and may exhibit a partial overstepping of the pes up to the proximal margins of the manus digits. The pace angulation ranges between 80° and 130°, the ratio of the stride length to pes length ranges from 3.5–5.5:1, and the ratio of the stride length, based on pes imprints, to the apparent body length ranges from 1.2–1.7:1. A tail-drag mark has never been reported in Bromacker specimens of Ichniotherium cottae nor has it been observed in this study.
Ichniotherium sphaerodactylum (Pabst, 1895) Characterization
The manus and pes imprints of Ichniotherium sphaerodactylum exhibit a relatively long digit V, measuring about 66% and 80% the length of digit IV in the manus and pes, respectively (Fig. 3D–F). The sole impression of the pes can be distinguished by its greatly expanded, mediolateral oval outline that measures approximately twice its proximodistal length and lies opposite digits II–V. In the manus imprint there is often a comparable but much smaller, less clearly defined sole impression that is narrower and positioned opposite digits II and III, although it sometimes appears to be elongated proximolaterally to about the level of the mid-width of digit IV. Typically, the distal portions of the manus digits II–IV are narrowly pointed, sharply bent or angled medially, and sub-parallel with each other. Commonly, the outline of the entire imprint of the first manus digit is narrowly triangular. The manus and pes lengths range between 4.4 and 10.6 cm and 5.7 and 12.9 cm, respectively (Appendix 2).
Trackway pattern ranges from an alternating arrangement of single imprints to an alternating arrangement of coupled manus-pes imprints (Fig. 4D–F). However, even trackways with a distinctly alternating arrangement of coupled manus-pes imprints exhibit only minor overstepping in which the digit tips of the pes imprints at most overlap slightly the proximal posterior margin of the manus imprints. The pace angulation ranges between 70° and 110°, the ratio of the stride length to the pes length ranges from 2.5–4.4:1, and the ratio of the stride length, based on pes imprints, to the apparent body length ranges from 0.8–1.4:1. A discontinuous tail-drag mark may be present (e.g., BUW 1, MB.ICV.2).
BROMACKER TETRAPOD BIOTAXA REPRESENTATION
Preservation and Faunal Composition
Vertebrate bone fragments were first found at the Bromacker locality in 1974 (Martens, 1980, 1982), more than 80 years after the first recovery of tetrapod tracks from the Bromacker. This initiated a program of systematic excavation of the Tambach Formation at the Bromacker locality, which yielded the first articulated vertebrate remains in 1979, a nearly complete, partially disarticulated postcranial skeleton of Diadectes (Martens et al., 1981; Berman et al., 1998). In terms of abundance of specimens, diversity of taxa, and quality of preservation the Bromacker locality had become the most productive locality for Lower Permian terrestrial vertebrates in Europe by the end of the century (Martens, 1988, 1994, 2001a, b; Boy and Martens, 1991; Berman and Martens, 1993; Berman et al., 1998, 2001; Berman, Henrici, et al., 2000; Berman, Reisz, et al., 2000; Sumida et al., 1996, 1998; Eberth et al., 2000). To date, a minimum of 11 vertebrate taxa have been identified from the Bromacker locality that are collectively represented by 50 or more partial-to-complete skeletons and hundreds of isolated elements (Eberth et al., 2000; Martens et al., 2005). Anamniotes (amphibians) include the trematopid Tambachia trogallas, Sumida, Berman, and Martens, 1998, unidentified dissorophids (Anderson et al., 2004), and the seymouriamorph Seymouria sanjuanensis Vaughn, 1966, (Berman and Martens, 1993; Berman, Henrici, et al., 2000; Martens et al., 2005; Klembara et al., 2005, 2006). Amniotes are represented by two diadectids, Diadectes absitus Berman, Sumida, and Martens, 1998, and Orobates pabsti Berman, Henrici, Kissel, Sumida, and Martens, 2004, the captorhinomorph Thuringothyris mahlendorffae Boy and Martens, 1991, the bolosaurid Eudibamus cursoris Berman, Reisz, Scott, Henrici, Sumida, and Martens, 2000, the primitive basal synapsid Dimetrodon teutonis Berman, Reisz, Martens, and Henrici, 2001, and two undescribed primitive basal synapsids, a caseid and varanopid (Berman et al., 2004; Martens et al., 2005).
Although the Bromacker vertebrate assemblage shares many taxa in common with those of well-documented, lowland terrestrial environments (almost exclusively found in the United States), it is unique in exhibiting marked differences in the composition and abundances of its constituents that suggest a direct relationship between their paleobiology and occurrence in a ‘truly upland’ paleoenvironment (Berman, Henrici, et al., 2000; Eberth et al., 2000; Martens et al., 2005): (1) a complete absence of aquatic and semi-terrestrial forms (fish and obligatory aquatic and semi-terrestrial amphibians); (2) an unusually high abundance and variety of herbivores (Diadectes, Orobates, Eudibamus, and the undescribed caseid) capable of subsisting on a diet of high-fiber plants; and (3) an unusually low abundance and variety of top predators (Dimetrodon and the undescribed varanopid).
The Bromacker is uniquely characterised by a remarkable abundance of specimens that occur fully or nearly complete, articulated, and exceptionally well preserved in fully extended, near natural poses (e.g., Fig. 5C; Berman et al., 2001, 2004; Berman, Henrici, et al., 2000; Eberth et al., 2000). This indicates that death and burial were in these instances almost certainly coeval events. Often two, three, or four articulated specimens of one or two taxa were preserved in small groups or clusters. These observations indicate that rates of sedimentation were high and the specimens were not transported great distances during the flooding events that preserved them in the sheet-flood deposits. It was also reasoned that those specimens clustered together occurred together at the time of death and probably indicate gregarious behavior. Furthermore, specimens represented by isolated bones of reworked carcasses were transported with little or no sub-aerial exposure from proximal to more central parts of the basin. Also judging from the description of the paleoenvironment of the Tambach Basin and its Bromacker locality (Eberth et al., 2000), there is reasonably good evidence to assume that the vertebrates are representatives of a single, local community: (1) most significantly, the sheet-flood deposit in which the vertebrates occur represent essentially a single, catastrophic flooding event that was restricted to the internally drained Tambach Basin and was of very short duration but had a very wide aerial extent and an apparent magnitude capable of preserving individuals much larger than those recovered; and (2) specimens of specific taxa are randomly distributed throughout the sheet-flood deposits without any signs of taphonomic sorting to a particular level. Taken together, these taphonomic features suggest strongly that the Bromacker quarry not only preserves only those vertebrates that inhabited the Tambach Basin, but also provides a fairly reliable census of their diversity, relative abundances, and maximum sizes. Until now, these two aspects of the Bromacker assemblage have never before been demonstrated in an Early Permian terrestrial assemblage, and they strongly indicate that the tetrapod taxa preserved in the Upper Beds most likely also represent those whose numerous tracks are preserved in the sandstone facies of the Lower Beds.
The Late Pennsylvanian to Early Permian Diadectidae, along with the Late Pennsylvanian Limnoscelidae and Early Permian Tseajaiidae, best or solely represented by the type genera Limnoscelis and Tseajaia (Vaughn, 1964; Moss, 1972; Fracasso, 1983; Berman and Sumida, 1990; Berman, 2000) comprise one of the best-known and most diverse late Paleozoic tetrapod clades, the Diadectomorpha. Although widely regarded as the sister group to all amniotes (e.g., Carroll, 1995; Laurin and Reisz, 1995,1997), Berman and colleagues (1992) and Berman (2000) placed the Diadectomorpha within Amniota as sharing a most recent common ancestor with Synapsida, as well as linking them as the sister clade of Reptilia. Diadectids include five more or less well-established genera, Diadectes Cope, 1878, Desmatodon Case, 1908, Diasparactus Case, 1910, Orobates Berman, Henrici, Kissel, Sumida, and Martens, 2004, and Ambedus Kissel and Reisz, 2004, and all are exclusively known from the Permo-Carboniferous of North America except for the Bromacker occurrence of Diadectes and the exclusively Bromacker occurrence of Orobates (Olson, 1947; Berman et al., 1992, 1998; Berman and Sumida, 1995). A combination of autapomorphic and plesiomor-phic characters, mainly cranial but also some postcranial, clearly distinguishes Orobates pabsti not only as most closely related to Diadectes among the diadectids, but also as the sister taxon to all other diadectids (Berman et al., 2004), with the possible exception of Ambedus Kissel and Reisz (2004), which is based solely on jaw elements with teeth similar to diadectids. Phanerosaurus Meyer, 1860, and Stephanospondylus Stappenbeck, 1905, are poorly defined diadectids from Germany, and about all that can be said of them is that they are probably diadectids (Berman et al., 1998).
The Bromacker locality is unique among Early Permian terrestrial vertebrate localities not only in having yielded a very large number of diadectid specimens (Appendix 3), but also in the great abundance of diadectids compared to the other members of the Bromacker assemblage (Eberth et al., 2000). Based on a count of minimal number of individuals, diadectids represent 35% of the Bromacker vertebrate population with Diadectes absitus and Orobates pabsti comprising 24% and 11% of this total, respectively. Most significantly, using the same abundance index, the herbivores (Diadectes, Orobates, Eudibamus, and the undescribed caseid) outnumbered the top predators (Dimetrodon and the undescribed varanopid) 7:1.
Diadectid Postcranial Characters and Implications for Ichnospecies Identification
Diadectes absitus Berman, Sumida, and Martens, 1998
An unusual character of the axial skeleton of Diadectes among late Paleozoic tetrapods, including the holotype of Diadectes absitus (MNG 8853; Fig. 5A), is the reduction of the number of presacral vertebrae to 21. The postaxial presacral neural arches are of the type typically referred to as swollen, with the zygapophyses extending well beyond the lateral margins of the centra. In addition to the two sacral vertebrae, at least 34 caudals are present in the complete tail of the North American specimen CM 41700 (Fig. 5B). The ulna exceeds the radius in length by about 20%, whereas the fibula exceeds the tibia in length by 10% (Appendix 4).
As far as is known, the right manus in the Bromacker Diadectes absitus MNG 7721 includes the only known example of a complete, or nearly complete, articulated carpus of the genus (Berman et al, 1998) and comprises all the expected elements, an ulnare, intermedium, radiale, lateral centrale, and distal carpals 1–5, except for perhaps the medial centrale and pisiform (Fig. 6A). The pisiform may be present, however, as a displaced element located between the metacarpals 2 and 3. The carpal elements are tightly packed and the five distal carpals provide a strong bony link between the carpus and digital complex. In size the oval ulnare is clearly the dominate element of the carpus. Because the proximodistally elongated distal carpal 2 is unusually large and contacts not only nearly the entire medial margin of the lateral centrale, but also the distal end of the radiale, it was suspected of either including or excluding the medial centrale. Distal carpal 4 is typical in being large with a broad contact with metacarpal 4, but is unusual in having a proximally extended angular margin that wedges partially between the medial centrale and the ulnare. In general, the metacarpals and digits exhibit a gradual serial increase in size from the first to the fourth. The fifth digit is shorter than the fourth, but its exact length is unknown due to probable incomplete preservation. Only two phalanges are present in the digit V, but a count of three is suspected to be the correct number, inasmuch as this is would give Diadectes the typical phalangeal formula of late Palaeozoic terrestrial vertebrates of 2-3-4-5-3 (e.g., Sumida, 1997). All of the phalanges are short and broad and decrease serially in length distally, but with an extreme shortening of the penultimate phalanges of digits II–IV. The terminal phalanges end in a bluntly rounded margin, giving them a spade-like outline in which the width slightly exceeds the length, but are longer than the nonterminal phalanges.
As noted earlier in this paper, the description of the pes in Diadectes absitus relies heavily on the superbly preserved examples in the Diadectes sp. specimen CM 41700 from the Permo-Carboniferous of North America (Figs. 5B, 7A; Berman and Henrici, 2003). The tarsus exhibits a reduction in the number of elements to five: astragalus, calcaneum, medial centrale, and distal tarsals 1 and 4. The partial Bromacker pes of D. absitus MNG 10650 may represent an exception to this pattern, in that an extremely small ossification may represent the fifth distal tarsal (Berman and Henrici, 2003:fig. 5). The obvious reduction in size or lack of ossification of some elements has resulted in large unoccupied areas. These spaces were presumably occupied by the standard series of tarsals, either totally represented by cartilage or as greatly reduced ossifications surrounded by a thick envelope of cartilage. The astragalus is extremely thick and, as is typical of late Paleozoic terrestrial amniotes, is L-shaped, although the vertical and horizontal limbs are greatly shortened. Its origin is clearly the result of a fusion of the amphibian tibiale, intermedium, and proximal centrale (Berman and Henrici, 2003). The calcaneum is oval in outline and considerably thinner than the astragalus, but the two elements have a broad contact with one another and were probably bound strongly together by ligaments and a peg-and-socket locking mechanism (Berman and Henrici, 2003). The greatest mediolateral width of the pair exceeds their greatest proximodistal length by about 30%. A small, oval, nodular medial centrale lies adjacent to the distomedial curvature of the astragalus. The small, oval distal tarsals 1 and 4 are apparently the only bony links between the proximal tarsal elements and the metatarsals. The first through fourth metatarsals and digits gradually increase in size serially, with the fifth being subequal to the second. The non-terminal phalangeal elements are short and broad, and decrease serially in size distally except for, as in the manus, an extreme shortening of the penultimate phalanges of digits II–IV. The terminal phalanges, as in the manus, are spade-like in outline with the width slightly exceeding the length, but are longer than the non-terminal phalanges (Fig. 7A). The phalangeal formula of the pes is 2–3–4–5-3, and thus identical to that of the manus.
Orobates pabsti Berman, Henrici, Kissel, Sumida, and Martens, 2004
The vertebral column of Orobates pabsti consists of 26 presacral and 2 sacral vertebrae, and a caudal count that apparently varies widely, with counts of 34 and 46 for the holotype MNG 10181 and paratype MNG 8980, respectively. The postaxial, presacral neural arches are of the type typically referred to as swollen, with the zygapophyses extending well beyond the lateral margins of the centra. The ulna exceeds the radius in length by about one fourth to one third, whereas the fibula exceeds the tibia in length by about 13% (see Appendix 4).
The carpus of Orobates pabsti is believed to consist of ten elements that include the radiale, intermedium, ulnare, medial and lateral centrales, distal carpals 1–4, and pisiform (Fig. 6B). There is an unusual reduction or even absence of ossification of some elements, which has resulted in large unoccupied areas. These spaces were presumably occupied by the standard series of carpal elements either totally represented by cartilage or as greatly reduced ossifications surrounded by a thick envelope of cartilage. The ulnare and intermedium are the dominant elements of the carpus, whereas in comparison the oval radiale is relatively small. Berman and colleagues (2004) assumed that the fourth distal carpal provided the only bony link, albeit weak, between the carpus and the digital complex. The first through fourth metacarpals and digits gradually increase in size serially, with the fifth being intermediate between the first and second. The non-terminal phalanges are short and broad and exhibit very little serial decrease in size distally, with 1 and 2 of the second digit, 2 and 3 of the third digit, and 2–4 of the fourth digit being subequal. The terminal phalanges are slightly longer than wide and considerable longer than the non-terminal phalanges and terminate in a bluntly pointed margin. Terminal phalanges of the digits I–IV are unique among diadectids in possessing a small, proximally directed, narrow, triangular extension at their proximolateral corner, giving them an asymmetrical appearance (Fig. 6B). The phalangeal formula of the manus is 2–3–4–5-3.
The tarsus of Orobates pabsti is reduced to six elements: tibiale, intermedium, proximal centrale, calcaneum (=amphibian fibulare), medial centrale, and fourth distal tarsal (Fig. 7B). The tibiale, intermedium, and proximal centrale are tightly united suturally into a single structural unit considered to be the equivalent of the amniote astragalus (Berman and Henrici, 2003). The greatest mediolateral width of the astragalus-calcaneum pair exceeds its greatest proximodistal length by about 70%. The slightly oval fourth distal tarsal articulates between the proximal centrale and the fourth metatarsal to provide the only bony link between the tarsus and the digital complex. An extremely small, oval-shaped element, presumably the medial centrale, lies adjacent to the distolateral corner of the tibiale portion of the astragalus. Thus, the tarsus, as in the carpus, exhibits large, unoccupied areas for which the same explanation was offered (Berman and Henrici, 2003). The first through fourth digits and metatarsals gradually increase in size serially, with the fifth of both being subequal to the third. The non-terminal phalangeal elements are short and broad and decrease serially in size distally, although the first and second penultimate phalanges of the third and fourth digits are subequal in size. As in the manus, the terminal phalanges are slightly longer than wide and considerably longer than the non-terminal phalanges. Also as in the manus, the terminal phalanges of digits I–IV possess a small, proximally directed, narrow, triangular extension at their proximolateral corner, giving them an asymmetrical appearance (Fig. 7B). The phalangeal formula of the pes is 2–3–4–5-4.
Biotaxon Correlation With Ichniotherium
The ichnotaxon Ichniotherium has been referred to very different groups of late Paleozoic tetrapods since its first description 120 years ago. Pohlig (1885, 1887, 1892, 1893) interpreted Ichniotherium alternately as the tracks of protorosaurs, archegosaurs, and branchiosaurs. Fritsch (1887, 1901) preferred a relationship to temnospondyls, first proposing a ‘giant salamander’, then a melanerpetontid branchiosaur as the possible trackmaker. Whereas the diagnosis of Nopcsa (1923) more correctly recognised a relationship to eryopids and diadectids, Lotze (1928) stressed a closer relationship to the latter on the basis of the pentadactyle imprints and the inferred, reptilian-like phalangeal formula of manus and pes. Schmidt (1927) was the first to presume a primitive or pelycosaurian-grade basal synapsid origin of the Ichniotherium trackmaker. Based on detailed anatomical studies Romer and Byrne (1931) rejected a relationship to diadectids, because they reconstructed the pes of Diadectes with the digit tips pointing at a vertical angle to the ground, which they reasoned would produce somewhat shorter digit impressions rather than the plantigrade, long-toed imprints of Ichniotherium. Nevertheless, subsequent studies preferred a relationship to diadectids (e.g., Korn, 1933; Abel, 1935; Czyzewska, 1955; Schmidt, 1959; Steiner and Schneider, 1963) or the lesser likelihood of a relationship to procolophonids (Korn, 1933; Müller, 1955). Haubold (1971, 1973a, b, 1996) opposed the diadectid trackmaker, referring to the study of Romer and Byrne (1931), and instead proposed a primitive basal synapsid origin, such as edaphosaurids or caseid precursors. Fichter (1983) and Gand (1988) followed this interpretation. The recovery of abundant and excellently preserved diadectid remains from the Bromacker locality during the 1990s presented the crucial turning point in the biotaxon interpretation of Ichniotherium trackways. A striking coincidence in the size distribution, anatomy, and abundance of the diadectid specimens from the Bromacker locality provided quickly accepted, convincing evidence of a diadectid-origin of Ichniotherium trackways (Fichter, 1998; Haubold, 1998, 2000; Eberth et al., 2000; Voigt and Haubold, 2000; Voigt, 2001, 2005; Berman et al., 2004; Voigt et al., 2005).
Biotaxa Correlations with Ichniotherium cottae and Ichniotherium sphaerodactylum
Comparisons of the Ichniotherium record at the Bromacker locality suggests the presence of two very closely related species of diadectid trackmakers. The ichnospecies Ichniotherium cottae (Pohlig, 1885) and Ichniotherium sphaerodactylum (Pabst, 1895) differ in some details of their manus and pes morphologies and trackway patterns, but most significantly in the: (1) relative lengths of digits I and V of the manus and pes; (2) shape of the terminal phalanges of digits II–IV; (3) shape of the distal portions of digits II–IV of the manus and the degree of their orientation toward the midline of the trackway; (4) shape and size of the sole pad; (5) degree of overstepping of the manus and pes; and (6) presence or absence of a tail drag mark. Despite numerous differences between the postcrania of Diadectes absitus and Orobates pabsti, albeit many of seemingly minor importance (Berman et al., 1998, 2004; Berman and Henrici, 2003), only a few can be directly or potentially related to the differences in the tracks and trackway patterns of the two ichnospecies of Ichniotherium. As noted earlier, because a complete pes of D. absitus was not available for this study, those of the superbly preserved mature Diadectes sp. specimen CM 41700 (Figs. 5B, 7A; Berman and Henrici, 2003) from the Permo-Carboniferous of North America provide much of the basis for the following comparisons.
Footprint Morphology versus Autopod Skeletal Anatomy
An association of the ichnospecies Ichniotherium cottae and Ichniotherium sphaerodactylum with the biospecies Diadectes absitus and Orobates pabsti, respectively, is supported strongly by the relative lengths of the pes digits (Fig. 8) when expressed as a percentage of the length of digit IV (Appendices 5, 6). This is especially true of digit V in the pes, which in I. cottae and D. absitus have lengths equal to about 48 and 52% of digit IV, respectively, compared to 80 and 79% in I. sphaerodactylum and O. pabsti, respectively. Differences in the relative lengths of digit V of the pes can be attributed to, at least in part, the smaller phalangeal count of three in D. absitus compared to four in O. pabsti. Similarly, the length of digit I in the pedes of I. cottae and presumably D. absitus are 35 and 38% of digit IV, respectively, whereas in I. sphaerodactylum and O. pabsti the respective measurements are 45 and 48%. There is also a strong correlation between the relative lengths of digits II and III compared to that of digit IV in the pes of I. cottae and presumably D. absitus of 62 and 58%, and 82 and 78%, respectively, whereas in I. sphaerodactylum and O. pabsti the same measurements are 67 and 60%, and 86 and 81%.
The associations between ichno- and biospecies is less clear based on the lengths of the manus digits (see Fig. 8) expressed as a percentage of the length of digit IV of the manus (Appendices 5, 6). Using this measure of comparison, there is a considerable discrepancy between the relative lengths of digits I–III in Ichniotherium cottae and Diadectes absitus. This could be due to an affectation of preservation, since in the only complete carpus of D. absitus available for this study, MNG 7721, the distal phalanges are hyperflexed against the plantar surface of manus with some being slightly telescoped on each other (digit III), and the two phalanges of digit I were lost due to weathering and restored using their enclosing matrix as a natural mold to cast them in epoxy (Berman et al., 1998). In the same manner, the only significant discrepancy between the relative lengths of digit V the ichno- and biospecies is the higher value of I. sphaerodactylum compared to that in O. pabsti. Disregarding a few apparent minor discrepancies, the relative lengths of the middle digits of the manus of I. sphaerodactylum and O. pabsti exceed those of I. cottae and D. absitus by fairly consistent values.
There are two anatomical features that may have contributed to why the manus and pes digit traces in Ichniotherium cottae are relatively shorter than those in Ichniotherium sphaerodactylum, assuming their respective origins are Diadectes absitus and Orobates pabsti: (1) in D. absitus there is a unique, extreme shortening of the penultimate phalanges of digits I–IV of the manus and pes (see Figs. 6, 7); and (2) the terminal phalanges of digits II–IV in D. absitus end in a bluntly rounded margin, giving them a spade-like outline in which the width slightly exceeds the length, whereas in O. pabsti the terminal phalanges are bluntly pointed and the length exceeds slightly the width.
The size and shape of the sole pad imprint of the pes in both Ichniotherium species are undoubtedly moulded, probably entirely, by the closely articulated astragalus (or its tightly sutured component elements) and calcaneum, which greatly dominate the tarsus. Outlines enclosing the articulated astragalus and calcaneum in Diadectes CM 41700 and Orobates pabsti MNG 10181 have a strong similarity to the outlines of the soles pad imprints of the pedes in Ichniotherium cottae and Ichniotherium sphaerodactylum, respectively (compare Figs. 3 and 7). A distinctive feature of the sole pad impression of the pes track of I. cottae is its partial division into two, co-joined impressions (Fig. 3C): an oval-to-subcircular medial impression and a smaller, semi-oval to semi-circular impression that extends from its proximolateral margin that were likely made by the astragalus and calcaneum, respectively. As already noted, the appearance of the latter portion of the impression was apparently dependent on the sole pad being pressed deep enough into the substrate to include it. This is seemingly due to a much greater vertical thickening of the ventral surface of the astragalus over that of the calcaneum. In Diadectes, although the dorsal surfaces of the articulated astraga-lus-calcaneum occupy essentially a single horizontal plane, the astragalus is about 60% thicker, giving it a much greater ventral dimension and undoubtedly a more dominant influence than the calcaneum in the formation of the sole pad impression (Berman and Henrici, 2003). On the other hand, the astragalus and calcaneum in Orobates pabsti are about equal thicknesses, and when articulated their dorsal and ventral surfaces occupy essentially parallel planes (Berman et al., 2004).
The trackways of both species of Ichniotherium indicate a plantigrade contact of the autopodes with the substrate at the initiation of the power stroke with a uniform medial divarication toward the midline of the trackway that averages about 25° and 5–10° for the manus and pes, respectively (Appendices 1, 2). The lesser degree of angulation of the pes toward the midline might be accounted for by a highly mobile joint between the epipodials and proximal tarsal elements, particularly between the tibia and the astragalus, which is not only present in the diadectids, including Diadectes absitus and Orobates pabsti, but also in Paleozoic amniotes as well (Berman and Henrici, 2003). Here a condyle-like tibial facet on the medial half of the dorsal surface of the astragalus is unusual in being much larger than the opposing facet on the distal end of the tibia, allowing for a rotational sliding motion of the pes about the long axis of the tibia. This permitted the pes to remain directed nearly anteriorly at all phases of the power stroke, so as to maximize the force of the posterior thrust during locomotion. A similar or comparable joint is not apparent between the epipodials and proximal carpal elements of the manus and may account for the higher medial divarication of the manus.
A distinctive feature of the imprints of the manus in Ichniotherium sphaemdactylum that distinguishes it from that of Ichniotherium cottae is the greater and more abrupt medial angulation or bending of the distal portions of digits II–IV, whereas this feature is negligible in the pes tracks of both ichnospecies. Differences in the expression of this feature may be attributable to differences in the ranges of rotational movement at joints between the epipodials and the proximal carpals and tarsals and between the distal carpals and tarsals and the metapodials. It is assumed that at the termination of the power stroke and the initiation of the retraction of the limbs to begin the next power stroke, the autopodes were lifted from the substrate progressively from their proximal margin to their digit tips. Just before the distal portions of the digits lost contact with the substrate, particularly the longer digits I–IV, there would have been a tendency for them to rotate significantly medially through a horizontal plane as the upper portion of the limb was swung anteriorly. In the pedes of both Diadectes absitus and Orobates pabsti this tendency might have been diminished strongly not only by a well-developed joint between the epipodials and the proximal tarsals, but also by an unusually mobile joint between the distal tarsals and metatarsals. Berman and Henrici (2003) proposed that large areas of reduction or absence of ossification of some of the central and distal tarsal bones in D. absitus and O. pabsti (at that time unnamed) provided a unique structural pattern in which the only bony link between the tarsus and the digital complex is via the fourth distal tarsal. This, they argued, produced a crude facsimile of the highly mobile lacertilian mesotarsal joint that served, along with the joint between the epipodials and the proximal tarsals, to maintain an anteriorly directed pes during the power stroke to maximize the force of the posterior thrust during locomotion. In the manus of O. pabsti, although there is some reduction in the number and ossification of the central and distal carpals, the mobility at the mesocarpal joint would have been far less than that at the mesotarsal joint. This, combined with the far less mobile epipodial-carpal joint compared to the equivalent joint of the hind limb, may account for the strong medial bending of the distal portions of digits II–IV of the manus imprint of I. sphaerodactylum. However, in D. absitus the carpal elements are strongly ossified and tightly packed, which likely minimized or eliminated any horizontal rotation of the digital complex about the mesocarpal joint. Yet, the distal portions of the imprints of digits II–IV of the manus of I. cottae exhibit little medial angulation or bending. Perhaps this is due in part to the relatively shorter digits in Diadectes, allowing for a more abrupt lifting of the manus from the substrate at the initiation of the limb retraction. The greater degree of medial bending or angulation of the distal portions of the digital imprints of the manus in I. sphaerodactylum than in I. cottae may also be directly related to a greater lateral undulation or flexion of the vertebral column during locomotion in O. pabsti than in D. absitus. In tetrapods with a sprawling-limb type of posture the degree of lateral undulation of the presacral vertebral column during locomotion is directly related to its length. Inasmuch as vertebral structure in Diadectes absitus and Orobates pabsti is essentially identical, the greater number of 26 presacral vertebrae in the latter, compared to 21 in the former, might have significantly increased its degree of lateral undulation during locomotion and therefore the medial bending or angulation of the distal portions of the digit imprints of the manus.
Trackway Pattern versus Axial Skeletal Anatomy
The two ichnospecies are distinguishable by consistent patterns of overstepping (Fig. 9). In Ichniotherium cottae overstepping is partial, with the pes track reaching the proximal ends of the manus digit impressions, whereas in Ichniotherium sphaerodactylum overstepping is minor, with the pes track reaching at its maximum the posterior margin of the manus sole impression (see Fig. 4). Differences in the extent of overstepping can be attributable to three variables: (1) the locomotory speed of the trackmaker, (2) length ratios of the limbs to the presacral portion of the vertebral column (=glenoid-acetabular distance), and (3) the length of the presacral vertebral column. Considering the abundant ichnological data examined for both ichnospecies, which includes 53 trackways, the full range of variation of their trackway patterns is probably represented. For this reason the differences in the upper limits of the range of overstepping exhibited by the two ichnospecies is considered to be of anatomical origin rather than differences in locomotory speed. Differences in the length proportions of the limbs to the presacral vertebral column can also be ruled out, as the proportional relationships of the propodials to the epipodials in Diadectes absitus and Orobates pabsti are identical (see Appendix 4). The third alternative explanation, however, dealing with differences in the glenoid-acetabular distance of the trackmakers, can be verified. The presacral columns in D. absitus and O. pabsti differ essentially only in the number of vertebra, with 21 in the former and 26 in the latter. Assuming equal-sized limbs in both genera, it is clear that the relatively shorter trunk in D. absitus would explain the more pronounced overstepping of its trackway pattern. In addition, trackway measurements of the ratio of the pes stride length to the apparent body length (glenoid-acetabular distance) of both ichnospecies of Ichniotherium indicate clearly that the trackmaker of Ichniotherium cottae was capable of significantly longer strides relative to its body length than the trackmaker of Ichniotherium sphaerodactylum (see Fig. 4).
The occasional inclusion of a tail-drag impression with the trackways of Ichniotherium sphaerodactylum and its absence in trackways of Ichniotherium cottae may be due to simply a difference in the tail lengths of their presumed trackmakers. The tail of the Diadectes CM 41700 (see Fig. 5B) appears to be complete and possesses 32 vertebrae, whereas counts of 34 and 46 were reported (Berman et al., 2004) for the holotype (see Fig. 5C) and paratype, respectively, of Orobates pabsti, which appear to represent complete or nearly complete counts. If it is assumed that the presence or absence of a tail-drag mark in I. cottae and I. sphaerodactylum is related to their tail lengths, then it would support their biospecies identifications as D. absitus and O. pabsti, respectively.
Ichnospecies as Indicators of Relative Body Size and Abundance of Biospecies
The maximum sizes of the manus and pes imprints of Ichniotherium cottae are significantly smaller than those of Ichniotherium sphaerodactylum (Appendices 1B, 2B), which, because of the close relationship of the ichnospecies, would be expected to reflect a corresponding similarity in the overall body sizes of Diadectes absitus and Orobates pabsti. However, the size distinction based on tracks is not reflected in the Bromacker skeletal record of D. absitus and O. pabsti if skull size is used, as the maximum skull size of the former exceeds substantially that of the latter (see Appendix 3). Several explanations can be offered for this apparent contradiction: (1) shortening of digits in Diadectes due to a reduced number of phalangeal elements and an extreme proximodistal shortening in some; (2) trackways of the I. cottae studied herein often lack the proximo-lateral extension of the pes sole pad, which obscures their true length; and (3) the skeletal record is typically far inferior to the ichnological record in providing complete size distribution data.
From another perspective, the long head, short trunk and tail, and long limbs and feet in Diadectes compared to the reversed body proportions in Orobates might be explained by morphodynamic and heterochronic developmental patterns, as demonstrated for example in dinosaurs and dinosaur tracks (Lockley, 2005; Lockley and Kukihara, 2005). This approach considers the organism as an integrated complex system ruled by extrinsic, as well as intrinsic, shape affecting factors. That means, if the trunk of Diadectes has been shortened and the limbs have been extended due to the acquirement of a more efficient locomotion, then the shortening of the tail and feet, as well as the extension of the head, may represent non-functional, corresponding or compensatory morphologic changes due to growth dynamics.
Inasmuch as all of the trackway specimens of this study were collected from the Bromacker locality and were selected on the basis of providing adequate data for comparisons, the numerical disparity of 11 Ichniotherium cottae and 42 Ichniotherium sphaerodactlyum specimens is strong reason to expect an approximately 1:4 ratio in the local community abundances of the trackmakers Diadectes absitus and Orobates pabsti. Furthermore, Ichniotherium is reported to represent more than 95% of all tetrapod footprints recovered from the Bromacker (Haubold, 1998). Yet, as already noted above, minimum number of individuals counts indicate that D. absitus outnumbered O. pabsti by a nearly 2:1 ratio and that in abundance they collectively represented about 35% of the Bromacker population.
There are several possible explanations for disparity between abundances based on trackways and skeletal fossils: (1) tracks are not necessarily good census indicators, as one individual can make numerous trackways; (2) the high percentage of Ichniotherium trackways may indicate that the diadectids were more successful than other vertebrates at reoccupying the alluvial plain of the Tambach Basin after flooding events; (3) the track-bearing mudflats were exposed for weeks to months, recording continuous activity by the same animals, whereas death and burial of the vertebrates by the sheetfloods were essentially coeval events representing a very brief moment of time and that preserved a relatively accurate census of the diversity and abundances of the Bromacker vertebrate community; and (4) the recovery of skeletal fossils by quarrying is best described as serendipitous or the result of fortunate, accidental discoveries influenced by strongly biased techniques that may produce a skewed picture of relative abundances and size ranges. The above comments are intended to indicate that at present tracks cannot be relied on to determine accurately the body size distributions and relative abundances of the trackmakers, just as the body fossil record may not accurately reflect the track census.
An extensive record of tetrapod tracks and articulated vertebrate remains from the Lower Permian Bromacker locality of central Germany provides strong evidence for a diadectid trackmaker of Ichniotherium footprints. Cross-checked comparative analysis of imprint morphology based on autopod structure and trackway pattern based on axial skeleton structure firmly establishes the track-trackmaker association between two species of the ichnogenus Ichniotherium Pohlig, 1892, Ichniotherium cottae (Pohlig, 1885) and Ichniotherium sphaerodactylum (Pabst, 1895), and the skeletal fossils of the closely related diadectids Diadectes absitus and Orobates pabsti, respectively. These are the first well-documented species-level correlations between trackmakers and Paleozoic trackways.
Orobates pabsti and Ichniotherium sphaerodactylum are known only from the Bromacker locality. On the other hand, Ichniotherium cottae occurs in all six formations of the Thuringian Forest Permo-Carboniferous succession that precedes the Tambach Formation (Voigt, 2005). This stratigraphic distribution is unexpected, inasmuch as Orobates is, with the possible exception of Ambedus Kissel and Reisz, 2004, the basal-most members of Diadectidae, which are known in North America from the Upper Pennsylvanian to the Lower Permian (Berman et al., 2004). In this context it is noteworthy that the accumulation of the clastic sediments of the Tambach Formation began after a significant break in sedimentation that was accompanied by denudation and remarkable tectonic movements (Knoth, 1970; Lutzner, 1981). Undoubtedly, it was this change in basin configuration and the creation of unique paleoenvironmental and paleobiological conditions that allowed Orobates pabsti, as well as other members of the Bromacker vertebrate assemblage, to colonize the Tambach Basin, which has been described as representing the earliest and best documented example of the rarely encountered ‘truly upland’ paleoecosystem (Eberth et al., 2000; Berman et al., 2001). In this scenario O. pabsti probably existed outside the Tambach Basin area long before the time span represented by the Lower Permian sedimentary rocks of the Tambach Formation. Therefore, the discovery of O. pabsti or I. sphaerodactylum at any other locality of Permo-Carboniferous beds in the world could provide an important key to the geographic origin and dispersal routes of diadectids (see also Berman et al., 1997). This goal could realistically be achieved by a careful restudy of the global Ichniotherium record, which is presently restricted to Europe and North America.
In addition, the recognition of the close relation between Ichniotherium species and diadectid genera offers a unique opportunity to evaluate principals and taxonomic concepts in vertebrate ichnology. Permian tetrapod footprints, which alone have been assigned to nearly 400 ichnospecies (Haubold, 2000), are based mostly on poorly preserved specimens and rely on obscure, weakly defined, or little understood features of imprint morphology and trackway pattern, as well as stratigraphic or even geographic occurrences. In several aspects, the superb Ichniotherium record from the Bromacker locality is an outstanding example of why those practices should be rejected in favor of diagnoses based on an abundant record of well-preserved tracks and trackways. Only then can anatomically controlled characters be clearly recognized and rigidly defined, so as to provide the most reliable criteria for diagnosing tetrapod ichnotaxa. Moreover, due to the extensive database available for Ichniotherium, it promises to be an invaluable and welcome subject to test the accuracy of bivariate and multivariate statistical methods often argued as the most objective and modern approach in recognizing tetrapod ichnotaxa (e.g., Demathieu and Demathieu, 2002; Tucker and Smith, 2004).
Sincere thanks are due the collection managers of the numerous natural history museums and related collection repositories in Europe and North and South America for access to Ichniotherium track-bearing slabs from the Tambach Sandstone and for technical support and help in unravelling the historical background of collections. SV gratefully acknowledges B. Small (Denver Museum of Nature and Science), his crew of volunteers, as well as the United States Forest Service, for enabling the study of the abundant Ichniotherium track record of the Maroon Formation both in their care and in the field, which was vital in clarifying the taxonomic differences of the Ichniotherium ichnospecies of the Tambach Formation. Frederik Spindler, Freiberg, is greatly acknowledged for preparing the diadectid illustrations of the last figure. Funding for this project was made available by the National Geographic Society and the Edward O'Neil Endowment Fund of the Carnegie Museum of Natural History (to DSB and ACH). Reviewers Martin Lockley and Hartmut Haubold made constructive suggestions for improvement of the manuscript.
- O. Abel 1935. Vorzeitliche Lebensspuren. Fischer, Jena, 644 pp. Google Scholar
- J. Anderson, S. S. Sumida, D. S. Berman, A. C. Henrici, and T. Martens . 2004. The dissorophoid temnospondyls from the Early Permian of Bromacker, Germany. Journal of Vertebrate Paleontology 24:334A. Google Scholar
- M. Barthel and R. Rößler . 1994. Calamiten im Oberrotliegend des Thtiringer Waldes. Was ist Walchia imbricatal? Veröffentlichungen des Naturhistorischen Museums Schleusingen 9:69–80. Google Scholar
- D. S. Berman 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. New Mexico Museum of Natural History and Science Bulletin 2:11–21. Google Scholar
- D. S. Berman 2000. Origin and early evolution of the amniote occiput. Journal of Paleontology 74:938–956. Google Scholar
- D. S. Berman and A. C. Henrici . 2003. Homology of the astragalus and structure and function of the tarsus of Diadectidae. Journal of Paleontology 77:172–188. Google Scholar
- D. S. Berman and T. Martens . 1993. First occurrence of Seymouria (Amphibia, Batrachosauria) in the Lower Permian Rotliegend of central Germany. Annals of Carnegie Museum 62:63–79. Google Scholar
- D. S. Berman and S. S. Sumida . 1990. A new species of Limnoscelis (Amphibia, Diadectomorpha) from the Late Pennsylvanian Sangre de Cristo Formation of central Colorado. Annals of Carnegie Museum 59:303–341. Google Scholar
- D. S. Berman and S. S. Sumida . 1995. New cranial material of the rare diadectid Desmatodon hesperis (Diadectomorpha) from the Late Pennsylvanian of central Colorado. Annals of Carnegie Museum 64:315–336. Google Scholar
- D. S. Berman, S. S. Sumida, and R. E. Lombard . 1992. Reinterpretation of the temporal and occipital regions in Diadectes and the relationships of diadectomorphs. Journal of Paleontology 66:481–499. Google Scholar
- D. S. Berman, S. S. Sumida, and R. E. Lombard . 1997. Biogeography of primitive amniotes. pp. 85–139 in S. S. Sumida and K. L. Martin (eds.), Amniote origins: completing the transition to land. Academic Press, San Diego, California. Google Scholar
- D. S. Berman, S. S. Sumida, and T. Martens . 1998. Diadectes (Diadectomorpha, Diadectidae) from the Early Permian of central Germany, with description of a new species. Annals of Carnegie Museum 67:53–93. Google Scholar
- D. S. Berman, A. C. Henrici, S. S. Sumida, and T. Martens . 2000. Redescription of Seymouria sanjuanensis (Seymouriamorpha) from the Lower Permian of Germany based on complete, mature specimens with a discussion of paleoecology of the Bromacker locality assemblage. Journal of Vertebrate Paleontology 20:253–268. Google Scholar
- D. S. Berman, R. R. Reisz, T. Martens, and A. C. Henrici . 2001. A new species of Dimetrodon (Synapsida: Sphenacodontidae) from the Lower Permian of Germany records first occurrence of genus outside of North America. Canadian Journal of Earth Sciences 38:803–812. Google Scholar
- D. S. Berman, A. C. Henrici, R. A. Kissel, S. S. Sumida, and T. Martens . 2004. A new diadectid (Diadectomorpha), Orobates pabsti, from the Early Permian of central Germany. Bulletin of Carnegie Museum of Natural History 35:1–36. Google Scholar
- D. S. Berman, R. R. Reisz, D. Scott, A. C. Henrici, S. S. Sumida, and T. Martens . 2000. Early Permian bipedal reptile. Science 290:969–972. Google Scholar
- J. A. Boy and T. Martens . 1991. Ein neues captorhinomorphes Reptil aus dem thüringischen Rotliegend (Unter-Perm; Ost-Deutschland). Paläontologische Zeitschrift 65:363–389. Google Scholar
- R. L. Carroll 1995. Problems of the phylogenetic analysis of Paleozoic choanates. Bulletin du Muséum National d'Histoire Naturelle 17:389–445. Google Scholar
- T. Czyzewska 1955. [Permian tetrapod footprints from Wambierzyce (Lower Silesia)]. Acta Geologica Polonica 5:131–160. [Polish]. Google Scholar
- G. Demathieu and P. Demathieu . 2002. Concerning the erection of ichnogenera and ichnospecies in vertebrate ichnotaxonomy. Ichnos 9:117–121. Google Scholar
- D. A. Eberth and D. S. Berman . 1993. Stratigraphy, sedimentology, and vertebrate paleoecology of the Cutler Formation redbeds (Pennsylvanian-Permian) of north-central New Mexico. New Mexico Museum of Natural History and Science Bulletin 2:33–49. Google Scholar
- D. A. Eberth, D. S. Berman, S. S. Sumida, and H. Hopf . 2000. Lower Permian terrestrial paleoenvironments and vertebrate paleoecology of the Tambach Basin (Thuringia, central Germany): the upland holy grail. Palaios 15:293–313. Google Scholar
- J. Fichter 1983. Tetrapodenfährten aus dem saarpfälzischen Rotliegenden (Ober-Karbon–Unter-Perm; Sudwest-Deutschland) II: Fahrten der Gattungen Foliipes, Varanopus, Ichniotherium, Dimetropus, Palmichnus, Phalangichnus, cf. Chelichnus, cf. Laoporus und Anhomoiichnium. Mainzer Naturwissenschaftliches Archiv 21:125–186. Google Scholar
- J. Fichter 1998. Bericht über die Bergung einer 20 t schweren Fährten-platte aus dem Tambacher Sandstein (Unter Perm) des Thüringer Waldes und erste Ergebnisse ichnologischer Studien. Philippia 8:147–208. Google Scholar
- M. Fracasso 1983. Cranial osteology, functional morphology, systematics and paleoenvironment of Limnoscelis paludis Williston. Ph.D. dissertation, Yale University, New Haven, Connecticut, 624 pp. Google Scholar
- A. Fritsch 1887. [Giant Permian tetrapod footprints]. Vesmir 16:121–122. [Czech]. Google Scholar
- A. Fritsch 1901. Die Fauna der Gaskohle und der Kalksteine der Perm-formation Böhmens. Rivnac, Prag, 101 pp. Google Scholar
- G. Gand 1988. Les traces de vertébrés tétrapodes du Permien francais. Ph.D. dissertation, University of Bourgogne, Dijon, 341 pp. Google Scholar
- H. Haubold 1971. Ichnia Amphibiorum et Reptiliorum fossilium. Encyclopedia of Palaeoherpetology 18:1–124. Google Scholar
- H. Haubold 1973a. Die Tetrapodenfährten aus dem Perm Europas. Freiberger Forschungshefte C 285:5–55. Google Scholar
- H. Haubold 1973b. Lebewelt und Ökologie des Tambacher Sandsteins (Unteres Perm, Saxon) im Rotliegenden des Thüringer Waldes. Zeitschrift für geologische Wissenschaften 1:247–268. Google Scholar
- H. Haubold 1996. Ichnotaxonomie und Klassifikation von Tetrapodenfährten aus dem Perm. Hallesches Jahrbuch für Geowissenschaften B 18:23–88. Google Scholar
- H. Haubold 1998. The Early Permian tetrapod ichnofauna of Tambach, the changing concepts in ichnotaxonomy. Hallesches Jahrbuch für Geowissenschaften B 20:1–16. Google Scholar
- H. Haubold 2000. Tetrapodenfährten aus dem Perm-Kenntnisstand und Progress 2000. Hallesches Jahrbuch für Geowissenschaften B 22:1–16. Google Scholar
- R. A. Kissel and R. R. Reisz . 2004. Ambedus pusillus, new genus, new species, a small diadectid (Tetrapoda: Diadectomorpha) from the Lower Permian of Ohio, with a consideration of Diadectomorpha phylogeny. Annals of Carnegie Museum 73:197–212. Google Scholar
- J. Klembara, D. S. Berman, A. C. Henrici, and A. Čerňansky . 2005. New structures and reconstructions of the skull of the seymouriamorph Seymouria sanjuanensis, Vaughn. Annals of Carnegie Museum 74:1–8. Google Scholar
- J. Klembara, D. S. Berman, A. C. Henrici, A. Čerňansky, and R. Werneburg . 2006. Comparison of cranial anatomy and proportions of similarly sized Seymouria sanjuanensis and Discosauriscus austriacus. Annals of Carnegie Museum 75:37–49. Google Scholar
- W. Knoth 1970. Zur Lithologie und Paläogeographie des höheren Rotliegenden im Thüringer Wald. Berichte der deutschen Gesellschaft für geologische Wissenschaften A 15:47–65. Google Scholar
- H. Korn 1933. Eine für die Kenntnis der Cotylosaurier des deutschen Perms bedeutsame Schwimmfährte von Tambach. Palaeobiologica 5:169–201. Google Scholar
- M. Laurin and R. R. Reisz . 1995. A reevaluation of early amniote phylogeny. Zoological Journal of the Linnean Society 113:165–223. Google Scholar
- M. Laurin and R. R. Reisz . 1997. A new perspective on tetrapod phylogeny. pp. 9–59 in S. S. Sumida and K. L. Martin (eds.), Amniote origins: completing the transition to land. Academic Press, San Diego, California. Google Scholar
- G. Leonardi (ed.). 1987. Glossary and manual of tetrapod footprint. Departemento Nacional da Produção Mineral, Brasilia, Brazil, 117 pp. Google Scholar
- M. G. Lockley 2005. Relationships between feet, footprints, limbs and the whole body: What morphodynamics tell us about the whole organism. Abstract book, International Symposium on dinosaurs and other vertebrates Palaeoichnology, October 4–8th 2005, Fumanya, Barcelona: 19–20. Google Scholar
- M. G. Lockley and R. Kukihara . 2005. A morphodynamic analysis of the Triassic theropod dinosaur Coelophysis: Dimorphism provides clues to intrinsic biological organization in saurischian dinosaurs. Abstracts Volume, Tracking dinosaur origins, The Triassic-Jurassic terrestrial transition, March 14–16th 2005, St. George, Utah: 11–12. Google Scholar
- F. Lotze 1928. Die Tambacher Sphaerodactylum-Fährten. Paläontologische Zeitschrift 9:170–175. Google Scholar
- H. Lützner 1981. Sedimentation der variszischen Molasse im Thüringer Wald. Schriftenreihe für geologische Wissenschaften 17:1–217. Google Scholar
- T. Martens 1975. Zur Taxonomie, Ökologie und Biostratigraphie des Oberrotliegenden (Saxon) der Tambacher Mulde in Thüringen. Freiberger Forschungshefte C 309:115–133. Google Scholar
- T. Martens 1980. Beitrag zur Taxonomie und Ökologie des Oberrotliegenden im Elgersburger Becken in Thüringen. Abhandlungen und Berichte des Museums der Natur Gotha 10:21–32. Google Scholar
- T. Martens 1982. Zur Stratigraphie, Taxonomie, Ökologie und Klimaentwicklung des Oberrotliegenden (Unteres Perm) im Thüringer Wald (DDR). Abhandlungen und Berichte des Museums der Natur Gotha 11:33–57. Google Scholar
- T. Martens 1988. Die Bedeutung der Rotsedimente für die Analyse der Lebewelt des Rotliegenden. Zeitschrift für geologische Wissenschaften 16:933–938. Google Scholar
- T. Martens 1994. 20 Jahre Sauriergrabung im Oberrotliegend (Unteres Perm) am Bromacker bei Tambach-Dietharz/Thüringer Wald. Abhandlungen und Berichte des Museums der Natur Gotha 18:15–26. Google Scholar
- T. Martens 2001a. Permokarbonische Tetrapodenfaunen in Pangaea—ein ungleicher Erforschungsgrad? Hallesches Jahrbuch für Geowissenschaften B 23:45–68. Google Scholar
- T. Martens 2001b. Paläontologie, Biostratigraphie und Paläogeographie der Tambach-Formation (Oberrotliegend, Unterperm) im Thüringer Wald—ein Überblick. Beiträge zur Geologie von Thüringen 8:181–212. Google Scholar
- T. Martens, J. Schneider, and H. Walter . 1981. Zur Paläontologie und Genese fossilführender Rotsedimente—der Tambacher Sandstein, Oberrotliegendes, Thüringer Wald (DDR). Freiberger Forschungshefte C 363:75–100. Google Scholar
- T. Martens, D. S. Berman, A. C. Henrici, and S. S. Sumida . 2005. The Bromacker quarry—the most important locality of Lower Permian terrestrial vertebrate fossils outside of North America. New Mexico Museum of Natural History and Science Bulletin 30:214–215. Google Scholar
- M. Matsukawa, K. Shibata, R. Kukihara, K. Koarai, and M. G. Lockley . 2005. Review of Japanese dinosaur track localities: implications for ichnotaxonomy, palaeogeography and stratigraphic correlation. Ichnos 12:201–222. Google Scholar
- J. L. Moss 1972. The morphology and phylogenetic relationships of the Lower Permian tetrapod Tseajaia campi Vaughn (Amphibia: Seymouriamorpha). University of California Publications in Geological Sciences 98:1–72. Google Scholar
- A. H. Müller 1954. Zur Ichnologie und Stratonomie des Oberrotliegenden von Tambach (Thüringen). Paläontologische Zeitschrift 28:189–203. Google Scholar
- A. H. Müller 1955. Eine kombinierte Lauf- und Schwimmfährte von Korynichnium aus dem Oberrotliegenden von Tambach (Thüringen). Geologie 4:490–496. Google Scholar
- F. B v Nopcsa 1923. Die Familien der Reptilien. Fortschritte der Geologie und Paläontologie der Rheinlande und Westfalens 2:1–210. Google Scholar
- E. C. Olson 1947. The family Diadectidae and its bearing on the classification of reptiles. Fieldiana 11:3–53. Google Scholar
- W. Pabst 1895. Thierfährten aus dem Rothliegenden von Friedrichroda, Tambach und Kabarz in Thüringen. Zeitschrift der deutschen geologischen Gesellschaft 47:570–576. Google Scholar
- W. Pabst 1908. Die Tierfährten in dem Rotliegenden, Deutschlands'. Nova Acta Leopoldina 89:315–481. Google Scholar
- H. Pohlig 1885. Saurierfährten in dem Unteren Rotliegenden von Friedrichroda. Verhandlungen des naturhistorischen Vereins der preussischen Rheinlande und Westfalens 42:285–286. Google Scholar
- H. Pohlig 1887. Thierfährten und Medusenabdrücke aus dem unteren Rothliegenden des Thüringer Waldes. Zeitschrift der deutschen geologischen Gesellschaft 39:644–645. Google Scholar
- H. Pohlig 1892. Altpermische Saurierfährten, Fische und Medusen der Gegend von Friedrichroda i. Thüringen; pp. 59–64 in Anonymous (ed.). Festschrift zum 70. Geburtstag von Rudolf Leuckardt. Engelmann, Leipzig, Germany. Google Scholar
- H. Pohlig 1893. Vorlage von Fliesspapierabdrücken fossiler Wirbeltier-Fussstapfen. Verhandlungen des naturhistorischen Vereins der preussischen Rheinlande und Westfalens 50:82–83. Google Scholar
- A. S. Romer and F. Byrne . 1931. The pes of Diadectes. Palaeobiologie 4:25–48. Google Scholar
- H. Schmidt 1927. Fährten der ältesten Saurier. Natur und Museum 57:517–526. Google Scholar
- H. Schmidt 1959. Die Cornberger Fährten im Rahmen der Vierfüßler-Entwicklung. Abhandlungen des Hessischen Landesamtes für Bodenforschung 28:1–137. Google Scholar
- W. Steiner and H. E. Schneider . 1963. Eine neue Lauffährte mit Schwanzschleppspur aus dem Ober-Rotliegenden von Tambach. Geologie 11:715–731. Google Scholar
- S. S. Sumida 1997. Locomotor features of taxa spanning the origin of amniotes. pp. 353–398 in S. S. Sumida and K. L. Martin (eds.), Amniote origins: completing the transition to land. Academic Press, San Diego, California. Google Scholar
- S. S. Sumida, D. S. Berman, and T. Martens . 1996. Biostratigraphic correlations between the Lower Permian of North America and central Europe using the first record of terrestrial tetrapods from Germany. PaleoBios 17:1–12. Google Scholar
- S. S. Sumida, D. S. Berman, and T. Martens . 1998. A new trematopid amphibian from the Lower Permian of central Germany. Palaeontology 41:605–629. Google Scholar
- L. Tucker and M. P. Smith . 2004. A multivariate taxonomic analysis of the Late Carboniferous vertebrate ichnofauna of Alveley, southern Shropshire, England. Palaeontology 47:679–710. Google Scholar
- H. E K. Van Allen, J. H. Calder, and A. P. Hunt . 2005. The trackway record of a tetrapod community in a walchian conifer forest from the Permo-Carboniferous of Nova Scotia. New Mexico Museum of Natural History and Science Bulletin 30:322–332. Google Scholar
- P. P. Vaughn 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38:567–583. Google Scholar
- S. Voigt 2001. Variation and preservation of Ichniotherium in the Tambach Sandstone. Natura Bresciana 25:221–225. Google Scholar
- S. Voigt 2002a. Zur Geschichte der Tetrapodenfährtenfunde in den Sandsteinbrüchen bei Tambach-Dietharz (1887–1908). Abhandlungen und Berichte des Museums der Natur Gotha 22:47–58. Google Scholar
- S. Voigt 2002b. Erstnachweis von fossilen Hydromedusen aus dem Tambacher Sandstein (Rotliegend, Unteres Perm, Thüringen). Freiberger Forschungshefte C 497:45–57. Google Scholar
- S. Voigt 2005. Die Tetrapodenichnofauna des kontinentalen Oberkarbon und Perm im Thüringer Wald—Ichnotaxonomie, Paläoökologie und Biostratigraphie. Cuvillier Verlag, Göttingen, Germany, 179 pp. Google Scholar
- S. Voigt and H. Haubold . 2000. Analyse zur Variabilität der Tetrapodenfährte Ichniotherium cottae aus dem Tambacher Sandstein (Rotliegend, Unterperm, Thüringen). Hallesches Jahrbuch für Geowissenschaften B 22:17–58. Google Scholar
- S. Voigt, B. Small, and F. Sanders . 2005. A diverse terrestrial ichnofauna from the Maroon Formation (Pennsylvanian-Permian), Colorado: Biostratigraphic and paleoecological significance. New Mexico Museum of Natural History and Science Bulletin 30:342–351. Google Scholar