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The '''Stereospondyli''' are a group of extinct [[Temnospondyli|temnospondyl]] [[amphibian]]s. Relative to other early tetrapods ([[labyrinthodont]]s), they had simplified backbones, where the whole vertebra was made of a single [[intercentrum]], topped by a [[neural arch]]. The whole vertebral structure was rather weak, meaning that most stereospondyls were aquatic. The family [[Plagiosauridae]] appear to have been wholly aquatic and retained their larval [[gill]]s in adulthood.
The '''Stereospondyli''' are a group of extinct [[Temnospondyli|temnospondyl]] [[amphibian]]s that existed primarily during the [[Mesozoic]] period. They are known from all seven continents and were common components of many Triassic ecosystems, likely filling a similar ecological niche to modern [[Crocodilia|crocodilians]] prior to the diversification of [[Pseudosuchia|pseudosuchian]] [[Archosaur|archosaurs]].


⚫
== Classification and anatomy ==
Stereospondyls first appeared during the [[Late Permian]]. During this time, the two major groups of stereospondyls, [[capitosauria]]ns and [[trematosauria]]ns, appeared. Stereospondyls were relatively uncommon in the [[Paleozoic]], outnumbered by the more diverse [[euskelia]]ns. During this time, they were endemic to Gondwana. Many early groups of temnospondyls became extinct during the [[Permian-Triassic extinction event]] but stereospondyls likely survived in [[Australia]] or [[Antarctica]], radiating worldwide in the [[Triassic]].
The group was first defined by Zittel (1888)<ref>{{Cite book|last=von Zittel|first=Karl A.|title=Handbuch der Paläontologie. Abteilung 1. Paläozoologie Band III: Vertebrata (Pisces, Amphibia, Reptilia, Aves).|publisher=Oldenbourg|year=1888|isbn=|location=Munich & Leipzig|pages=1-890}}</ref> on the recognition of the distinctive vertebral anatomy of the best known stereospondyls of the time, such as ''[[Mastodonsaurus]]'' and ''[[Metoposaurus]]''. The term 'stereospondylous' as a descriptor of vertebral anatomy was coined the following year by Fraas<ref>{{Cite book|last=FRAAS, Eberhard.|url=http://worldcat.org/oclc/559337958|title=Die Labyrinthodonten der schwäbischen Trias. [With plates.].|date=1889|oclc=559337958}}</ref>, referring to a vertebral position consisting largely or entirely of the intercentrum in addition to the neural arch. While the name 'Stereospondyli' is derived from the stereospondylous vertebral condition, there is a diversity of vertebral morphologies among stereospondyls, including the diplospondylous ('[[Tupilakosauridae|tupilakosaurid]]') condition,<ref>{{Cite journal|last=Warren|first=Anne|last2=Rozefelds|first2=Andrew C.|last3=Bull|first3=Stuart|date=2011-07-01|title=Tupilakosaur-like vertebrae in Bothriceps australis, an Australian brachyopid stereospondyl|url=https://doi.org/10.1080/02724634.2011.590563|journal=Journal of Vertebrate Paleontology|volume=31|issue=4|pages=738–753|doi=10.1080/02724634.2011.590563|issn=0272-4634}}</ref> where the arch sits between the corresponding intercentrum and pleurocentrum, and the [[Plagiosauridae|plagiosaurid]] condition, where a single large centrum ossification (identity unknown) is present, and the arch sits between subsequent vertebral positions<ref>{{Cite journal|last=Danto|first=Marylène|last2=Witzmann|first2=Florian|last3=Pierce|first3=Stephanie E.|last4=Fröbisch|first4=Nadia B.|date=2017-05-18|title=Intercentrum versus pleurocentrum growth in early tetrapods: A paleohistological approach|url=http://dx.doi.org/10.1002/jmor.20709|journal=Journal of Morphology|volume=278|issue=9|pages=1262–1283|doi=10.1002/jmor.20709|issn=0362-2525}}</ref>. The concept of Stereospondyli has thus undergone repeated and frequent revisions by different workers. Defining features include a tight articulation between the parasphenoid and the pterygoid and a stapedial groove<ref name=":0">{{Cite journal|last=Eltink|first=Estevan|last2=Schoch|first2=Rainer R.|last3=Langer|first3=Max C.|date=2019-04-16|title=Interrelationships, palaeobiogeography and early evolution of Stereospondylomorpha (Tetrapoda: Temnospondyli)|url=http://dx.doi.org/10.1007/s41513-019-00105-z|journal=Journal of Iberian Geology|volume=45|issue=2|pages=251–267|doi=10.1007/s41513-019-00105-z|issn=1698-6180}}</ref>.


== Evolutionary history ==
Stereospondyls were the latest-surviving temnospondyl group. With the diversification of crocodile-like [[archosaur]]s and an [[Triassic-Jurassic extinction event|extinction event]] at the end of the Triassic, most other temnospondyls disappeared. Two families of stereospondyls survived into the [[Jurassic]], and some appear to have survived into the [[Early Cretaceous]] in [[Gondwana]]. ''[[Koolasuchus]]'' is the latest known stereospondyl, living during the late Early Cretaceous in what is now [[Australia]] in areas that would then have been too cool for crocodiles. Some groups, such as the ''[[Metoposaurus]]'', are often associated to mass mortality and [[bone bed]]s.<ref>Brusatte, S. L., Butler R. J., Mateus O., & Steyer S. J. (2015). A new species of Metoposaurus from the Late Triassic of Portugal and comments on the systematics and biogeography of metoposaurid temnospondyls. Journal of Vertebrate Paleontology. e912988., 2015:</ref>
Stereospondyls first definitively appeared during the [[early Permian]], as represented by fragmentary remains of a [[Rhinesuchidae|rhinesuchid]] from the Pedra de Fogo Formation of [[Brazil]]<ref>{{Cite journal|last=Cisneros|first=Juan C.|last2=Marsicano|first2=Claudia|last3=Angielczyk|first3=Kenneth D.|last4=Smith|first4=Roger M. H.|last5=Richter|first5=Martha|last6=Fröbisch|first6=Jörg|last7=Kammerer|first7=Christian F.|last8=Sadleir|first8=Rudyard W.|date=2015-11-05|title=New Permian fauna from tropical Gondwana|url=http://dx.doi.org/10.1038/ncomms9676|journal=Nature Communications|volume=6|issue=1|doi=10.1038/ncomms9676|issn=2041-1723}}</ref>. Rhinesuchids are one of the earliest groups of stereospondyls to appear in the fossil record and are predominantly a [[late Permian]] clade, with only one species, ''[[Broomistega putterilli]],'' from the [[Early Triassic]] of [[South Africa]]. However, almost all other groups of stereospondyls are not known from any Paleozoic deposits, which remained dominated by non-stereospondyl [[Stereospondylomorpha|stereospondylomorphs]]. The taxonomically unresolved ''[[Peltobatrachus pustulatus]],'' which has historically been regarded as a stereospondyl, is also known from the late Permian of [[Tanzania]]<ref>{{Cite journal|date=1959-01-29|title=A new armoured amphibian from the Upper Permian of East Africa|url=http://dx.doi.org/10.1098/rstb.1959.0005|journal=Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences|volume=242|issue=691|pages=207–281|doi=10.1098/rstb.1959.0005|issn=2054-0280}}</ref>. Several more fragmentary records are known from horizons spanning the Permo-Triassic boundary in South America, such as the rhinesuchid-like ''[[Arachana nigra]]'' from Uruguay<ref>{{Cite journal|last=Piñeiro|first=Graciela|last2=Ramos|first2=Alejandro|last3=Marsicano|first3=Claudia|date=2012-01|title=A rhinesuchid-like temnospondyl from the Permo-Triassic of Uruguay|url=http://dx.doi.org/10.1016/j.crpv.2011.07.007|journal=Comptes Rendus Palevol|volume=11|issue=1|pages=65–78|doi=10.1016/j.crpv.2011.07.007|issn=1631-0683}}</ref> and an indeterminate mastodonsaurid<ref>{{Cite journal|last=Piñeiro|first=Graciela|last2=Marsicano|first2=Claudia A.|last3=Damiani|first3=Damiani|date=2007|title=Mandibles of mastodonsaurid temnospondyls from the Upper Permian–Lower Triassic of Uruguay|url=|journal=Acta Palaeontologica Polonica|volume=52|pages=695-703|via=}}</ref> from Uruguay.
''[[Chinlestegophis]]'', a putative Triassic stereospondyl considered to be related to [[Metoposauroidea|metoposauroids]] such as ''[[Rileymillerus]]'', has been noted to share many features with [[caecilian]]s, a living group of legless burrowing amphibians. If ''Chinlestegophis'' is indeed both an advanced stereospondyl and a relative of caecilians, this means that stereospondyls (in the form of caecilians) survived to the present day.<ref>{{Cite journal|last=Pardo|first=Jason D.|last2=Small|first2=Bryan J.|last3=Huttenlocker|first3=Adam K.|date=2017-07-03|title=Stem caecilian from the Triassic of Colorado sheds light on the origins of Lissamphibia|journal=Proceedings of the National Academy of Sciences|language=en|volume=114|issue=27|pages=E5389–E5395|doi=10.1073/pnas.1706752114|issn=0027-8424|pmid=28630337|pmc=5502650}}</ref>


Following the Permo-Triassic mass extinction, stereospondyls are abundantly represented in the fossil record, particularly from Russia, South Africa, and Australia. This led Yates & Warren (2000) to propose that stereospondyls had sheltered in a high-latitude refugium that would have been somewhat shielded from the global effects of the extinction, and that they subsequently radiated from present-day Australia or Antarctica<ref>{{Cite journal|last=YATES|first=ADAM M.|last2=WARREN|first2=A. ANNE|date=2000-01|title=The phylogeny of the ‘higher’ temnospondyls (Vertebrata: Choanata) and its implications for the monophyly and origins of the Stereospondyli|url=http://dx.doi.org/10.1111/j.1096-3642.2000.tb00650.x|journal=Zoological Journal of the Linnean Society|volume=128|issue=1|pages=77–121|doi=10.1111/j.1096-3642.2000.tb00650.x|issn=0024-4082}}</ref>. Recent discoveries of a diverse rhinesuchid community in South America alongside non-stereospondyl stereospondylomorphs have led to an alternative hypothesis for a radiation from western Gondwana in South America<ref name=":0" />. By the end of the Early Triassic, virtually all major clades of stereospondyls had appeared in the fossil record, although some were more geographically localized (e.g., [[Lapillopsidae|lapillopsids]], [[Rhytidosteidae|rhytidosteids]]) than those with cosmopolitan distributions (e.g., [[Capitosauroid|capitosauroids]], [[Trematosauroidea|trematosauroids]]).
⚫
==Classification==

Stereospondyls were the latest-surviving temnospondyl group. With the diversification of crocodile-like [[archosaur]]s and an [[Triassic-Jurassic extinction event|extinction event]] at the end of the Triassic, most other temnospondyls disappeared. [[Chigutisauridae|Chigutisaurid]] [[Brachyopoidea|brachyopoids]] persisted into the Jurassic in Asia and Australia<ref>{{Cite journal|date=1983-09-13|title=The last Labyrinthodont? A new brachyopoid (Amphibia, Temnospondyli) from the early Jurassic Evergreen formation of Queensland, Australia|url=http://dx.doi.org/10.1098/rstb.1983.0080|journal=Philosophical Transactions of the Royal Society of London. B, Biological Sciences|volume=303|issue=1113|pages=1–62|doi=10.1098/rstb.1983.0080|issn=0080-4622}}</ref><ref>{{Cite journal|last=Buffetaut|first=Eric|last2=Tong|first2=Haiyan|last3=Suteethorn|first3=Varavudh|date=1994-07-13|title=First post-Triassic labyrinthodont amphibian in South East Asia: a temnospondyl intercentrum from the Jurassic of Thailand|url=http://dx.doi.org/10.1127/njgpm/1994/1994/385|journal=Neues Jahrbuch für Geologie und Paläontologie - Monatshefte|volume=1994|issue=7|pages=385–390|doi=10.1127/njgpm/1994/1994/385|issn=0028-3630}}</ref><ref>{{Cite journal|last=Maisch|first=Michael W.|last2=Matzke|first2=Andreas T.|date=2005-06|title=Temnospondyl amphibians from the Jurassic of the Southern Junggar Basin (NW China)|url=http://dx.doi.org/10.1007/bf02990189|journal=Paläontologische Zeitschrift|volume=79|issue=2|pages=285–301|doi=10.1007/bf02990189|issn=0031-0220}}</ref>, including ''[[Koolasuchus]],'' the youngest known stereospondyl (late Early Cretaceous) from what is now [[Australia]]<ref>{{Cite journal|last=Warren|first=Anne|last2=Rich|first2=Thomas H.|last3=Vickers-Rich|first3=Patricia|date=1997|title=The last last labyrinthodonts|url=|journal=Palaeontolographica Abteilung A-Stuttgart|volume=247|pages=1-24|via=}}</ref>. There is also sparse evidence for the persistence of some trematosauroids into the Jurassic of Asia<ref>{{Cite journal|last=Maisch|first=Michael W.|last2=Matzke|first2=Andreas T.|last3=Sun|first3=Ge|date=2004-09-24|title=A relict trematosauroid (Amphibia: Temnospondyli) from the Middle Jurassic of the Junggar Basin (NW China)|url=http://dx.doi.org/10.1007/s00114-004-0569-x|journal=Naturwissenschaften|volume=91|issue=12|pages=589–593|doi=10.1007/s00114-004-0569-x|issn=0028-1042}}</ref>. If the recent hypothesis that ''[[Chinlestegophis]],'' a Late Triassic stereospondyl from North America, is indeed a stem [[caecilian]] is correct, then stereospondyls would survive to the present day.

== Lifestyle and ecology ==
Stereospondyls were particularly diverse during the Early Triassic, with small-bodied taxa such as lapillopsids and [[Lydekkerinidae|lydekkerinids]] that were likely more terrestrially capable present alongside larger taxa that would continue into the Middle Triassic, such as [[Brachyopoidea|brachyopoids]] and trematosauroids. The vast majority of stereospondyls, particularly the large-bodied taxa, have been inferred to have been obligately aquatic based on features of the external anatomy such as a well-developed lateral line system<ref>{{Cite journal|last=Moodie|first=Roy L.|date=1908-10|title=The lateral line system in extinct amphibia|url=http://dx.doi.org/10.1002/jmor.1050190206|journal=Journal of Morphology|volume=19|issue=2|pages=511–540|doi=10.1002/jmor.1050190206|issn=0362-2525}}</ref>, poorly ossified postcranial skeleton<ref>{{Cite journal|last=WITZMANN|first=FLORIAN|last2=SCHOCH|first2=RAINER R.|date=2006-11|title=THE POSTCRANIUM OF ARCHEGOSAURUS DECHENI, AND A PHYLOGENETIC ANALYSIS OF TEMNOSPONDYL POSTCRANIA|url=http://dx.doi.org/10.1111/j.1475-4983.2006.00593.x|journal=Palaeontology|volume=49|issue=6|pages=1211–1235|doi=10.1111/j.1475-4983.2006.00593.x|issn=0031-0239}}</ref>, and occasional preservation of proxies of external gills<ref>{{Cite journal|last=Witzmann|first=Florian|date=2013-07|title=Phylogenetic patterns of character evolution in the hyobranchial apparatus of early tetrapods|url=http://dx.doi.org/10.1017/s1755691013000480|journal=Earth and Environmental Science Transactions of the Royal Society of Edinburgh|volume=104|issue=2|pages=145–167|doi=10.1017/s1755691013000480|issn=1755-6910}}</ref>. Many taxa also reflect adaptations for an aquatic lifestyle as evidence in bone histology, which is [[Pachyostosis|pachyostotic]] in many taxa<ref>{{Cite journal|last=Danto|first=Marylène|last2=Witzmann|first2=Florian|last3=Fröbisch|first3=Nadia B.|date=2016-04-13|title=Vertebral Development in Paleozoic and Mesozoic Tetrapods Revealed by Paleohistological Data|url=http://dx.doi.org/10.1371/journal.pone.0152586|journal=PLOS ONE|volume=11|issue=4|pages=e0152586|doi=10.1371/journal.pone.0152586|issn=1932-6203}}</ref>, although some studies suggest a greater terrestrial ability than historically inferred<ref>{{Cite journal|last=FORTUNY|first=J.|last2=MARCÉ-NOGUÉ|first2=J.|last3=DE ESTEBAN-TRIVIGNO|first3=S.|last4=GIL|first4=L.|last5=GALOBART|first5=À.|date=2011-06-24|title=Temnospondyli bite club: ecomorphological patterns of the most diverse group of early tetrapods|url=http://dx.doi.org/10.1111/j.1420-9101.2011.02338.x|journal=Journal of Evolutionary Biology|volume=24|issue=9|pages=2040–2054|doi=10.1111/j.1420-9101.2011.02338.x|issn=1010-061X}}</ref><ref>{{Cite journal|last=Mukherjee|first=Debarati|last2=Ray|first2=Sanghamitra|last3=Sengupta|first3=Dhurjati P.|date=2010-01-29|title=Preliminary observations on the bone microstructure, growth patterns, and life habits of some Triassic temnospondyls from India|url=http://dx.doi.org/10.1080/02724630903409121|journal=Journal of Vertebrate Paleontology|volume=30|issue=1|pages=78–93|doi=10.1080/02724630903409121|issn=0272-4634}}</ref><ref>{{Cite journal|last=Mukherjee|first=Debarati|last2=Sengupta|first2=Dhurjati P.|last3=Rakshit|first3=Nibedita|date=2019-06-28|title=New biological insights into the Middle Triassic capitosaurs from India as deduced from limb bone anatomy and histology|url=http://dx.doi.org/10.1002/spp2.1263|journal=Papers in Palaeontology|volume=6|issue=1|pages=93–142|doi=10.1002/spp2.1263|issn=2056-2802}}</ref>. Most of the aquatic taxa resided in freshwater environments, but some trematosauroids in particular are thought to have been [[euryhaline]] based on their preservation in marine sediments with marine organisms <ref>{{Cite journal|last=JOHNSON|first=G. A. L.|date=1981-07|title=GEOGRAPHICAL EVOLUTION FROM LAURASIA TO PANGAEA|url=http://dx.doi.org/10.1144/pygs.43.3.221|journal=Proceedings of the Yorkshire Geological
Society|volume=43|issue=3|pages=221–252|doi=10.1144/pygs.43.3.221|issn=0044-0604}}</ref><ref>{{Citation|last=Hammer|first=W. R.|title=Paleoecology and Phylogeny of the Trematosauridae|date=2013-03-18|url=http://dx.doi.org/10.1029/gm041p0073|work=Gondwana Six: Stratigraphy, Sedimentology, and Paleontology|pages=73–83|place=Washington, D. C.|publisher=American Geophysical Union|isbn=978-1-118-66425-4|access-date=2020-09-23}}</ref>. While stereospondyls are often compared to modern crocodilians, the presence of multiple temnospondyls in some environments and the range of morphologies across Stereospondyli indicates that at least some clades occupied drastically different ecological niches, such as benthic ambush predators<ref>{{Cite journal|last=WITZMANN|first=FLORIAN|last2=SCHOCH|first2=RAINER R.|last3=HILGER|first3=ANDRÉ|last4=KARDJILOV|first4=NIKOLAY|date=2011-11-25|title=Braincase, palatoquadrate and ear region of the plagiosaurid Gerrothorax pulcherrimus from the Middle Triassic of Germany|url=http://dx.doi.org/10.1111/j.1475-4983.2011.01116.x|journal=Palaeontology|volume=55|issue=1|pages=31–50|doi=10.1111/j.1475-4983.2011.01116.x|issn=0031-0239}}</ref>. Some groups, such as [[Metoposauridae|metoposaurids]], are often recovered from large monotaxic [[bone bed]]s interpreted as evidence of aggregation prior to mass death<ref>{{Cite journal|last=Lucas|first=Spencer G.|last2=Rinehart|first2=Larry F.|last3=Krainer|first3=Karl|last4=Spielmann|first4=Justin A.|last5=Heckert|first5=Andrew B.|date=2010-12|title=Taphonomy of the Lamy amphibian quarry: A Late Triassic bonebed in New Mexico, U.S.A.|url=http://dx.doi.org/10.1016/j.palaeo.2010.10.025|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|volume=298|issue=3-4|pages=388–398|doi=10.1016/j.palaeo.2010.10.025|issn=0031-0182}}</ref><ref>Brusatte, S. L., Butler R. J., Mateus O., & Steyer S. J. (2015). A new species of Metoposaurus from the Late Triassic of Portugal and comments on the systematics and biogeography of metoposaurid temnospondyls. Journal of Vertebrate Paleontology. e912988., 2015:</ref>.

==Relationships==


===Phylogeny===
===Phylogeny===
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==References==
==References==
{{Reflist}}
{{Reflist}}{{Portal|Paleontology}}
*Yates, A. M. & Warren, A. A. (2000), The phylogeny of the 'higher' temnospondyls (Vertebrata: Choanata) and its implications for the monophyly and origins of the Stereospondyli. ''Zoological Journal of the Linnean Society'' 128: 77-121.

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Revision as of 18:14, 23 September 2020

Stereospondyls
Temporal range: 272.95–120 Ma Possible descendant taxon Apoda (caecilians) survives to present
Life restoration of Siderops kehli, a chigutisaurid
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Order: †Temnospondyli
Clade: †Stereospondylomorpha
Suborder: †Stereospondyli
Subgroups[1]

The Stereospondyli are a group of extinct temnospondyl amphibians that existed primarily during the Mesozoic period. They are known from all seven continents and were common components of many Triassic ecosystems, likely filling a similar ecological niche to modern crocodilians prior to the diversification of pseudosuchian archosaurs.

Classification and anatomy

The group was first defined by Zittel (1888)[2] on the recognition of the distinctive vertebral anatomy of the best known stereospondyls of the time, such as Mastodonsaurus and Metoposaurus. The term 'stereospondylous' as a descriptor of vertebral anatomy was coined the following year by Fraas[3], referring to a vertebral position consisting largely or entirely of the intercentrum in addition to the neural arch. While the name 'Stereospondyli' is derived from the stereospondylous vertebral condition, there is a diversity of vertebral morphologies among stereospondyls, including the diplospondylous ('tupilakosaurid') condition,[4] where the arch sits between the corresponding intercentrum and pleurocentrum, and the plagiosaurid condition, where a single large centrum ossification (identity unknown) is present, and the arch sits between subsequent vertebral positions[5]. The concept of Stereospondyli has thus undergone repeated and frequent revisions by different workers. Defining features include a tight articulation between the parasphenoid and the pterygoid and a stapedial groove[6].

Evolutionary history

Stereospondyls first definitively appeared during the early Permian, as represented by fragmentary remains of a rhinesuchid from the Pedra de Fogo Formation of Brazil[7]. Rhinesuchids are one of the earliest groups of stereospondyls to appear in the fossil record and are predominantly a late Permian clade, with only one species, Broomistega putterilli, from the Early Triassic of South Africa. However, almost all other groups of stereospondyls are not known from any Paleozoic deposits, which remained dominated by non-stereospondyl stereospondylomorphs. The taxonomically unresolved Peltobatrachus pustulatus, which has historically been regarded as a stereospondyl, is also known from the late Permian of Tanzania[8]. Several more fragmentary records are known from horizons spanning the Permo-Triassic boundary in South America, such as the rhinesuchid-like Arachana nigra from Uruguay[9] and an indeterminate mastodonsaurid[10] from Uruguay.

Following the Permo-Triassic mass extinction, stereospondyls are abundantly represented in the fossil record, particularly from Russia, South Africa, and Australia. This led Yates & Warren (2000) to propose that stereospondyls had sheltered in a high-latitude refugium that would have been somewhat shielded from the global effects of the extinction, and that they subsequently radiated from present-day Australia or Antarctica[11]. Recent discoveries of a diverse rhinesuchid community in South America alongside non-stereospondyl stereospondylomorphs have led to an alternative hypothesis for a radiation from western Gondwana in South America[6]. By the end of the Early Triassic, virtually all major clades of stereospondyls had appeared in the fossil record, although some were more geographically localized (e.g., lapillopsids, rhytidosteids) than those with cosmopolitan distributions (e.g., capitosauroids, trematosauroids).

Stereospondyls were the latest-surviving temnospondyl group. With the diversification of crocodile-like archosaurs and an extinction event at the end of the Triassic, most other temnospondyls disappeared. Chigutisaurid brachyopoids persisted into the Jurassic in Asia and Australia[12][13][14], including Koolasuchus, the youngest known stereospondyl (late Early Cretaceous) from what is now Australia[15]. There is also sparse evidence for the persistence of some trematosauroids into the Jurassic of Asia[16]. If the recent hypothesis that Chinlestegophis, a Late Triassic stereospondyl from North America, is indeed a stem caecilian is correct, then stereospondyls would survive to the present day.

Lifestyle and ecology

Stereospondyls were particularly diverse during the Early Triassic, with small-bodied taxa such as lapillopsids and lydekkerinids that were likely more terrestrially capable present alongside larger taxa that would continue into the Middle Triassic, such as brachyopoids and trematosauroids. The vast majority of stereospondyls, particularly the large-bodied taxa, have been inferred to have been obligately aquatic based on features of the external anatomy such as a well-developed lateral line system[17], poorly ossified postcranial skeleton[18], and occasional preservation of proxies of external gills[19]. Many taxa also reflect adaptations for an aquatic lifestyle as evidence in bone histology, which is pachyostotic in many taxa[20], although some studies suggest a greater terrestrial ability than historically inferred[21][22][23]. Most of the aquatic taxa resided in freshwater environments, but some trematosauroids in particular are thought to have been euryhaline based on their preservation in marine sediments with marine organisms [24][25]. While stereospondyls are often compared to modern crocodilians, the presence of multiple temnospondyls in some environments and the range of morphologies across Stereospondyli indicates that at least some clades occupied drastically different ecological niches, such as benthic ambush predators[26]. Some groups, such as metoposaurids, are often recovered from large monotaxic bone beds interpreted as evidence of aggregation prior to mass death[27][28].

Relationships

Phylogeny

Gallery

References

  1. ^ Eltink, Estevan; Schoch, Rainer R.; Langer, Max C. (June 2019). "Interrelationships, palaeobiogeography and early evolution of Stereospondylomorpha (Tetrapoda: Temnospondyli)". Journal of Iberian Geology. 45 (2): 251–267. doi:10.1007/s41513-019-00105-z.
  2. ^ von Zittel, Karl A. (1888). Handbuch der Paläontologie. Abteilung 1. Paläozoologie Band III: Vertebrata (Pisces, Amphibia, Reptilia, Aves). Munich & Leipzig: Oldenbourg. pp. 1–890.
  3. ^ FRAAS, Eberhard. (1889). Die Labyrinthodonten der schwäbischen Trias. [With plates.]. OCLC 559337958.
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