Editing Permian (section)

===Terrestrial biota===
Terrestrial life in the Permian included diverse plants, [[Fungus|fungi]], [[arthropod]]s, and various types of [[List of Permian tetrapods|tetrapods]]. The period saw a massive desert covering the interior of [[Pangaea]]. The warm zone spread in the northern hemisphere, where extensive dry desert appeared.<ref name="ucmp.berkeley.edu">{{cite web|url=http://www.ucmp.berkeley.edu/permian/permian.php|title=The Permian Period|work=berkeley.edu|access-date=2015-04-09|archive-date=2017-07-04|archive-url=https://web.archive.org/web/20170704140229/http://www.ucmp.berkeley.edu/permian/permian.php|url-status=live}}</ref> The rocks formed at that time were stained red by iron oxides, the result of intense heating by the sun of a surface devoid of vegetation cover. A number of older types of plants and animals died out or became marginal elements.

The Permian began with the Carboniferous flora still flourishing. About the middle of the Permian a major transition in vegetation began. The [[swamp]]-loving [[Lycopodiophyta|lycopod]] trees of the Carboniferous, such as ''[[Lepidodendron]]'' and ''[[Sigillaria]]'', were progressively replaced in the continental interior by the more advanced [[Pteridospermatophyta|seed ferns]] and early [[Pinophyta|conifers]] as a result of the [[Carboniferous rainforest collapse]]. At the close of the Permian, lycopod and [[Equisetopsida|equisete]] swamps reminiscent of Carboniferous flora survived only in [[Cathaysia]], a series of equatorial islands in the [[Paleo-Tethys Ocean]] that later would become [[South China (continent)|South China]].<ref>Xu, R. & Wang, X.-Q. (1982): Di zhi shi qi Zhongguo ge zhu yao Diqu zhi wu jing guan (Reconstructions of Landscapes in Principal Regions of China). Ke xue chu ban she, Beijing. 55 pages, 25 plates.</ref>

The Permian saw the radiation of many important conifer groups, including the ancestors of many present-day families. Rich forests were present in many areas, with a diverse mix of plant groups. The southern continent saw extensive seed fern forests of the ''[[Glossopteris]]'' flora. Oxygen levels were probably high there. The [[Ginkgoopsida|ginkgos]] and [[cycad]]s also appeared during this period.

====Insects====
[[File:Permocupes sojanensis holotype and reconstruction.jpg|thumb|Fossil and life restoration of ''[[Permocupes|Permocupes sojanensis]]'', a [[Permocupedidae|permocupedid]] beetle from the Middle Permian of Russia]]
Insects, which had first appeared and become abundant during the preceding Carboniferous, experienced a dramatic increase in diversification during the Early Permian. Towards the end of the Permian, there was a substantial drop in both origination and extinction rates.<ref name="Labandeira-2018">{{Citation|last=Labandeira|first=Conrad C.|title=The Fossil History of Insect Diversity|date=2018-05-23|url=https://onlinelibrary.wiley.com/doi/10.1002/9781118945582.ch24|work=Insect Biodiversity|pages=723–788|place=Chichester, UK|publisher=John Wiley & Sons, Ltd|language=en|doi=10.1002/9781118945582.ch24|isbn=978-1-118-94558-2|access-date=2021-07-25|archive-date=2021-07-25|archive-url=https://web.archive.org/web/20210725130020/https://onlinelibrary.wiley.com/doi/10.1002/9781118945582.ch24|url-status=live}}</ref> By the start of the Permian, there was already an active coevolutionary arms race between insects and plant reproductive structures, evidenced by both insect-caused damage in plants and defensive structures in plants aimed at minimising predation by insects.<ref>{{Cite journal |last1=Santos |first1=Artai A. |last2=Wappler |first2=Torsten |last3=McLoughlin |first3=Stephen |date=14 October 2024 |editor-last=Cascales-Miñana |editor-first=Borja |title=Earliest evidence of granivory from China (Shanxi Formation) points to seeds as a food source and nursing habitat for insects in the earliest Permian humid tropical forests of Cathaysia |journal=[[PLOS ONE]] |language=en |volume=19 |issue=10 |pages=e0311737 |doi=10.1371/journal.pone.0311737 |doi-access=free |issn=1932-6203 |pmc=11472943 |pmid=39401203 |bibcode=2024PLoSO..1911737S }}</ref> The dominant insects during the Permian Period were early representatives of [[Palaeoptera|Paleoptera]], [[Polyneoptera]], and [[Paraneoptera]]. [[Palaeodictyopteroidea]], which had represented the dominant group of insects during the Carboniferous, declined during the Permian. This is likely due to [[Competition (biology)|competition]] by [[Hemiptera]], due to their similar mouthparts and therefore ecology. Primitive relatives of [[Damselfly|damselflies]] and [[Dragonfly|dragonflies]] ([[Meganisoptera]]), which include the largest flying insects of all time, also declined during the Permian.<ref name="Schachat-2021">{{Cite journal|last1=Schachat|first1=Sandra R|last2=Labandeira|first2=Conrad C|date=2021-03-12|editor-last=Dyer|editor-first=Lee|title=Are Insects Heading Toward Their First Mass Extinction? Distinguishing Turnover From Crises in Their Fossil Record|url=https://academic.oup.com/aesa/article/114/2/99/6056214|journal=[[Annals of the Entomological Society of America]]|language=en|volume=114|issue=2|pages=99–118|doi=10.1093/aesa/saaa042|issn=0013-8746|doi-access=free|access-date=2021-07-25|archive-date=2021-07-25|archive-url=https://web.archive.org/web/20210725130021/https://academic.oup.com/aesa/article/114/2/99/6056214|url-status=live}}</ref> [[Holometabola]], the largest group of modern insects, also diversified during this time.<ref name="Labandeira-2018" /> "[[Grylloblattida|Grylloblattidans]]", an extinct group of winged insects thought to be related to modern [[Ice crawler|ice crawlers]], reached their apex of diversity during the Permian, representing up to a third of all insects at some localities.<ref name=":0">{{Cite journal |last1=Cui |first1=Yingying |last2=Bardin |first2=Jérémie |last3=Wipfler |first3=Benjamin |last4=Demers-Potvin |first4=Alexandre |last5=Bai |first5=Ming |last6=Tong |first6=Yi-Jie |last7=Chen |first7=Grace Nuoxi |last8=Chen |first8=Huarong |last9=Zhao |first9=Zhen-Ya |last10=Ren |first10=Dong |last11=Béthoux |first11=Olivier |date=2024-03-07 |title=A winged relative of ice-crawlers in amber bridges the cryptic extant Xenonomia and a rich fossil record |url=https://onlinelibrary.wiley.com/doi/10.1111/1744-7917.13338 |journal=Insect Science |volume=31 |issue=5 |pages=1645–1656 |language=en |doi=10.1111/1744-7917.13338 |pmid=38454304 |bibcode=2024InsSc..31.1645C |issn=1672-9609}}</ref> [[Mecoptera]] (sometimes known as scorpionflies) first appeared during the Early Permian, going on to become diverse during the Late Permian. Some Permian mecopterans, like [[Mesopsychidae]] have long proboscis that suggest they may have pollinated gymnosperms.<ref>{{Citation |last1=Lin |first1=Xiaodan |title=Mecoptera – Scorpionflies and Hangingflies |date=2019-04-29 |work=Rhythms of Insect Evolution |pages=555–595 |editor-last=Ren |editor-first=Dong |url=https://onlinelibrary.wiley.com/doi/10.1002/9781119427957.ch24 |access-date=2024-09-21 |edition=1 |publisher=Wiley |language=en |doi=10.1002/9781119427957.ch24 |isbn=978-1-119-42798-8 |last2=Shih |first2=Chungkun |last3=Li |first3=Sheng |last4=Ren |first4=Dong |editor2-last=Shih |editor2-first=Chung Kun |editor3-last=Gao |editor3-first=Taiping |editor4-last=Yao |editor4-first=Yunzhi}}</ref> The earliest known [[beetle]]s appeared at the beginning of the Permian. Early beetles such as members of [[Permocupedidae]] were likely [[xylophagous]], feeding on decaying wood. Several lineages such as Schizophoridae expanded into aquatic habitats by the Late Permian.<ref>{{Cite journal|last1=Ponomarenko|first1=A. G.|last2=Prokin|first2=A. A.|date=December 2015|title=Review of paleontological data on the evolution of aquatic beetles (Coleoptera)|url=http://link.springer.com/10.1134/S0031030115130080|journal=[[Paleontological Journal]]|language=en|volume=49|issue=13|pages=1383–1412|doi=10.1134/S0031030115130080|bibcode=2015PalJ...49.1383P |s2cid=88456234|issn=0031-0301|access-date=2021-07-26|archive-date=2023-07-16|archive-url=https://web.archive.org/web/20230716091929/https://link.springer.com/article/10.1134/S0031030115130080|url-status=live}}</ref> Members of the modern orders [[Archostemata]] and [[Adephaga]] are known from the Late Permian.<ref>{{Cite journal|last1=Ponomarenko|first1=A. G.|last2=Volkov|first2=A. N.|date=November 2013|title=Ademosynoides asiaticus Martynov, 1936, the earliest known member of an extant beetle family (Insecta, Coleoptera, Trachypachidae)|url=http://dx.doi.org/10.1134/s0031030113060063|journal=Paleontological Journal|volume=47|issue=6|pages=601–606|doi=10.1134/s0031030113060063|bibcode=2013PalJ...47..601P |s2cid=84935456|issn=0031-0301|access-date=2021-07-25|archive-date=2023-07-16|archive-url=https://web.archive.org/web/20230716091930/https://link.springer.com/article/10.1134/S0031030113060063|url-status=live}}</ref><ref>{{Cite journal|last1=Yan|first1=Evgeny Viktorovich|last2=Beutel|first2=Rolf Georg|last3=Lawrence|first3=John Francis|last4=Yavorskaya|first4=Margarita Igorevna|last5=Hörnschemeyer|first5=Thomas|last6=Pohl|first6=Hans|last7=Vassilenko|first7=Dmitry Vladimirovich|last8=Bashkuev|first8=Alexey Semenovich|last9=Ponomarenko|first9=Alexander Georgievich|date=2020-09-13|title=Archaeomalthus -(Coleoptera, Archostemata) a 'ghost adult' of Micromalthidae from Upper Permian deposits of Siberia?|url=https://www.tandfonline.com/doi/full/10.1080/08912963.2018.1561672|journal=[[Historical Biology]]|language=en|volume=32|issue=8|pages=1019–1027|doi=10.1080/08912963.2018.1561672|bibcode=2020HBio...32.1019Y |s2cid=91721262|issn=0891-2963|access-date=2021-07-25|archive-date=2019-12-15|archive-url=https://web.archive.org/web/20191215170246/https://www.tandfonline.com/doi/full/10.1080/08912963.2018.1561672|url-status=live}}</ref> Complex wood boring traces found in the Late Permian of China suggest that members of [[Polyphaga]], the most diverse group of modern beetles, were also present by the Late Permian.<ref>{{Cite journal|last1=Feng|first1=Zhuo|last2=Wang|first2=Jun|last3=Rößler|first3=Ronny|last4=Ślipiński|first4=Adam|last5=Labandeira|first5=Conrad|date=2017-09-15|title=Late Permian wood-borings reveal an intricate network of ecological relationships|journal=[[Nature Communications]]|language=en|volume=8|issue=1|pages=556|doi=10.1038/s41467-017-00696-0|pmid=28916787|issn=2041-1723|pmc=5601472|bibcode=2017NatCo...8..556F}}</ref>


====Tetrapods====
[[File:Weigeltisaurus reconstruction.png|left|thumb|Restoration of ''[[Weigeltisaurus jaekeli]]'', a [[Weigeltisauridae|weigeltisaurid]] from the Late Permian of Europe. Weigeltisaurids represent the oldest known gliding vertebrates.]]
The terrestrial fossil record of the Permian is patchy and temporally discontinuous. Early Permian records are dominated by equatorial Europe and North America, while those of the Middle and Late Permian are dominated by temperate [[Karoo Supergroup]] sediments of South Africa and the Ural region of European Russia.<ref name="Brocklehurst-2020">{{Cite journal |last=Brocklehurst |first=Neil |date=2020-06-10 |title=Olson's Gap or Olson's Extinction? A Bayesian tip-dating approach to resolving stratigraphic uncertainty |journal=[[Proceedings of the Royal Society B: Biological Sciences]] |language=en |volume=287 |issue=1928 |pages=20200154 |doi=10.1098/rspb.2020.0154 |issn=0962-8452 |pmc=7341920 |pmid=32517621}}</ref> Early Permian terrestrial faunas of North America and Europe were dominated by primitive [[pelycosaur]] [[synapsid]]s including the herbivorous [[Edaphosauridae|edaphosaurids]], and carnivorous [[Sphenacodontidae|sphenacodontids]], [[Diadectidae|diadectids]] and [[amphibian]]s.<ref name="Huttenlocker, A. K. 2012. Pp. 90">Huttenlocker, A. K., and E. Rega. 2012. The Paleobiology and Bone Microstructure of Pelycosaurian-grade Synapsids. Pp. 90–119 in A. Chinsamy (ed.) Forerunners of Mammals: Radiation, Histology, Biology. Indiana University Press.</ref><ref>{{cite web|url=http://www.ucmp.berkeley.edu/napc/abs23.html#SumidaS|title=NAPC Abstracts, Sto - Tw|work=berkeley.edu|access-date=2014-03-31|archive-date=2020-02-26|archive-url=https://web.archive.org/web/20200226163702/https://ucmp.berkeley.edu/napc/abs23.html#SumidaS|url-status=live}}</ref> Early Permian reptiles, such as [[Acleistorhinidae|acleistorhinids]], were mostly small insectivores.<ref>{{cite journal |last1=Modesto |first1=Sean P. |last2=Scott |first2=Diane M. |last3=Reisz |first3=Robert R. |date=1 July 2009 |title=Arthropod remains in the oral cavities of fossil reptiles support inference of early insectivory |journal=[[Biology Letters]] |volume=5 |issue=6 |pages=838–840 |doi=10.1098/rsbl.2009.0326 |pmid=19570779 |pmc=2827974 }}</ref>

====Amniotes====
[[Synapsid]]s (the group that would later include mammals) thrived and diversified greatly during the Cisuralian. Permian synapsids included some large members such as ''[[Dimetrodon]]''. The special adaptations of synapsids enabled them to flourish in the drier climate of the Permian and they grew to dominate the vertebrates.<ref name="Huttenlocker, A. K. 2012. Pp. 90"/> A faunal turnover occurred around the transition between the Cisuralian and Guadalupian, with the decline of amphibians and the replacement of pelycosaurs (a [[paraphyletic]] group) with more advanced [[therapsid]]s,<ref name="Didier&Laurin_2021" /> although the decline of early synapsid clades was apparently a slow event that lasted about 20 Ma, from the [[Sakmarian]] to the end of the [[Kungurian]].<ref name="Didier & Laurin 2024">{{cite journal |last1=Didier |first1=Gilles |last2=Laurin |first2=Michel |title=Testing extinction events and temporal shifts in diversification and fossilization rates through the skyline Fossilized Birth-Death (FBD) model: The example of some mid-Permian synapsid extinctions |journal=Cladistics |date=June 2024 |volume=40 |issue=3 |pages=282–306 |doi=10.1111/cla.12577 |language=en |issn=0748-3007|doi-access=free }}</ref> Predator-prey interactions among terrestrial synapsids became more dynamic.<ref>{{Cite journal |last1=Singh |first1=Suresh A. |last2=Elsler |first2=Armin |last3=Stubbs |first3=Thomas L. |last4=Rayfield |first4=Emily J. |last5=Benton |first5=Michael James |date=17 February 2024 |title=Predatory synapsid ecomorphology signals growing dynamism of late Palaeozoic terrestrial ecosystems |journal=[[Communications Biology]] |language=en |volume=7 |issue=1 |page=201 |doi=10.1038/s42003-024-05879-2 |issn=2399-3642 |pmc=10874460 |pmid=38368492 }}</ref> If terrestrial deposition ended around the end of the Cisuralian in North America and began in Russia during the early Guadalupian, a continuous record of the transition is not preserved. Uncertain dating has led to suggestions that there is a global hiatus in the terrestrial fossil record during the late Kungurian and early [[Roadian]], referred to as "Olson's Gap" that obscures the nature of the transition. Other proposals have suggested that the North American and Russian records overlap,<ref>{{cite journal |last1=Reisz |first1=Robert R. |last2=Laurin |first2=Michel |title=The reptile Macroleter: First vertebrate evidence for correlation of Upper Permian continental strata of North America and Russia |journal=GSA Bulletin |date=1 September 2001 |volume=113 |issue=9 |pages=1229–1233 |doi=10.1130/0016-7606(2001)113<1229:TRMFVE>2.0.CO;2 |bibcode=2001GSAB..113.1229R |url=https://doi.org/10.1130/0016-7606%282001%29113%3C1229%3ATRMFVE%3E2.0.CO%3B2 |issn=0016-7606 |access-date=17 January 2022 |archive-date=16 July 2023 |archive-url=https://web.archive.org/web/20230716092442/https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/113/9/1229/183805/The-reptile-Macroleter-First-vertebrate-evidence?redirectedFrom=fulltext |url-status=live }}</ref><ref name="Lozovsky 2005">{{cite journal |last1=Lozovsky |first1=Vladlen R. |title=Olson's gap or Olson's bridge, that is the question |journal=New Mexico Museum of Natural History and Science Bulletin |date=1 January 2005 |volume=30, The Nonmarine Permian |pages=179–184 |url=https://books.google.com/books?id=EmPvCQAAQBAJ&dq=Olson%27s+gap+or+Olson%27s+bridge%2C+that+is+the+question&pg=PA179 |publisher=New Mexico Museum of Natural History and Science |language=en}}</ref><ref>{{cite journal |last1=Brocklehurst |first1=Neil |date=10 June 2020 |title=Olson's Gap or Olson's Extinction? A Bayesian tip-dating approach to resolving stratigraphic uncertainty |url=https://doi.org/10.1098/rspb.2020.0154 |url-status=live |journal=[[Proceedings of the Royal Society B: Biological Sciences]] |volume=287 |issue=1928 |pages=20200154 |doi=10.1098/rspb.2020.0154 |pmc=7341920 |pmid=32517621 |archive-url=https://web.archive.org/web/20200713165459/https://royalsocietypublishing.org/doi/10.1098/rspb.2020.0154 |archive-date=13 July 2020 |access-date=17 January 2022}}</ref><ref name="Laurin & Hook 2022">{{cite journal |last1=Laurin |first1=Michel |last2=Hook |first2=Robert W. |title=The age of North America's youngest Paleozoic continental vertebrates: a review of data from the Middle Permian Pease River (Texas) and El Reno (Oklahoma) Groups |journal=BSGF - Earth Sciences Bulletin |date=2022 |volume=193 |pages=10 |doi=10.1051/bsgf/2022007 |url=https://doi.org/10.1051/bsgf/2022007 |language=en}}</ref> with the latest terrestrial North American deposition occurring during the Roadian, suggesting that there was an extinction event, dubbed "[[Olson's Extinction]]".<ref>{{Cite journal|last=Lucas|first=S.G.|date=July 2017|title=Permian tetrapod extinction events|url=https://linkinghub.elsevier.com/retrieve/pii/S0012825217300600|journal=[[Earth-Science Reviews]]|language=en|volume=170|pages=31–60|doi=10.1016/j.earscirev.2017.04.008|bibcode=2017ESRv..170...31L|access-date=2021-04-18|archive-date=2021-05-06|archive-url=https://web.archive.org/web/20210506060019/https://linkinghub.elsevier.com/retrieve/pii/S0012825217300600|url-status=live}}</ref> 

The Middle Permian faunas of South Africa and Russia are dominated by therapsids, most abundantly by the diverse [[Dinocephalia]]. Dinocephalians become extinct at the end of the Middle Permian, during the [[Capitanian mass extinction event]]. Late Permian faunas are dominated by advanced therapsids such as the predatory sabertoothed [[gorgonopsia]]ns and herbivorous beaked [[dicynodont]]s, alongside large herbivorous [[pareiasaur]] [[Parareptilia|parareptiles]].<ref>{{Cite journal|date=2017-07-01|title=Permian tetrapod extinction events|url=https://www.sciencedirect.com/science/article/abs/pii/S0012825217300600|journal=[[Earth-Science Reviews]]|language=en|volume=170|pages=31–60|doi=10.1016/j.earscirev.2017.04.008|issn=0012-8252|last1=Lucas|first1=S.G.|bibcode=2017ESRv..170...31L|access-date=2021-08-18|archive-date=2021-08-18|archive-url=https://web.archive.org/web/20210818230353/https://www.sciencedirect.com/science/article/abs/pii/S0012825217300600|url-status=live}}</ref> The [[Archosauromorpha]], the group of reptiles that would give rise to the [[pseudosuchia]]ns, [[dinosaur]]s, and [[pterosaur]]s in the following Triassic, first appeared and diversified during the Late Permian, including the first appearance of the [[Archosauriformes]] during the latest Permian.<ref>{{Cite journal|last1=Spiekman|first1=Stephan N. F.|last2=Fraser|first2=Nicholas C.|last3=Scheyer|first3=Torsten M.|date=2021-05-03|title=A new phylogenetic hypothesis of Tanystropheidae (Diapsida, Archosauromorpha) and other "protorosaurs", and its implications for the early evolution of stem archosaurs|journal=[[PeerJ]]|language=en|volume=9|pages=e11143|doi=10.7717/peerj.11143|pmid=33986981|issn=2167-8359|pmc=8101476|doi-access=free }}</ref> [[Cynodont]]s, the group of therapsids ancestral to modern [[mammal]]s, first appeared and gained a worldwide distribution during the Late Permian.<ref>{{Cite journal|last1=Huttenlocker|first1=Adam K.|last2=Sidor|first2=Christian A.|date=2020-12-01|title=A Basal Nonmammaliaform Cynodont from the Permian of Zambia and the Origins of Mammalian Endocranial and Postcranial Anatomy|url=https://www.tandfonline.com/doi/full/10.1080/02724634.2020.1827413|journal=[[Journal of Vertebrate Paleontology]]|language=en|volume=40|issue=5|pages=e1827413|doi=10.1080/02724634.2020.1827413|bibcode=2020JVPal..40E7413H|s2cid=228883951|issn=0272-4634|access-date=2021-08-18|archive-date=2021-11-07|archive-url=https://web.archive.org/web/20211107151159/https://www.tandfonline.com/doi/full/10.1080/02724634.2020.1827413|url-status=live}}</ref> Another group of therapsids, the [[therocephalia]]ns (such as ''[[Lycosuchus]]''), arose in the Middle Permian.<ref>{{cite journal | author = Huttenlocker A. K. | year = 2009 | title = An investigation into the cladistic relationships and monophyly of therocephalian therapsids (Amniota: Synapsida) | journal = [[Zoological Journal of the Linnean Society]] | volume = 157 | issue = 4| pages = 865–891 | doi=10.1111/j.1096-3642.2009.00538.x| doi-access = free }}</ref><ref>{{cite journal |author1=Huttenlocker A. K. |author2=Sidor C. A. |author3=Smith R. M. H. | year = 2011 | title = A new specimen of Promoschorhynchus (Therapsida: Therocephalia: Akidnognathidae) from the lowermost Triassic of South Africa and its implications for therocephalian survival across the Permo-Triassic boundary | journal = [[Journal of Vertebrate Paleontology]] | volume = 31 |issue=2 | pages = 405–421 | doi=10.1080/02724634.2011.546720|bibcode=2011JVPal..31..405H |s2cid=129242450 }}</ref> There were no flying vertebrates, though the extinct lizard-like reptile family [[Weigeltisauridae]] from the Late Permian had extendable wings like modern [[Draco (lizard)|gliding lizards]], and are the oldest known gliding vertebrates.<ref name="Pritchard-2021">{{Cite journal |last1=Pritchard |first1=Adam C. |last2=Sues |first2=Hans-Dieter |last3=Scott |first3=Diane |last4=Reisz |first4=Robert R. |date=20 May 2021 |title=Osteology, relationships and functional morphology of Weigeltisaurus jaekeli (Diapsida, Weigeltisauridae) based on a complete skeleton from the Upper Permian Kupferschiefer of Germany |journal=[[PeerJ]] |language=en |volume=9 |pages=e11413 |doi=10.7717/peerj.11413 |pmid=34055483 |issn=2167-8359 |pmc=8141288 |doi-access=free }}</ref><ref>{{Cite journal |last1=Bulanov |first1=V. V. |last2=Sennikov |first2=A. G. |date=1 October 2006 |title=The first gliding reptiles from the upper Permian of Russia |url=https://link.springer.com/article/10.1134/S0031030106110037 |journal=[[Paleontological Journal]] |language=en |volume=40 |issue=5 |pages=S567–S570 |doi=10.1134/S0031030106110037 |bibcode=2006PalJ...40S.567B |issn=1555-6174 |s2cid=84310001 |access-date=3 November 2023}}</ref>

<gallery class="center">
File:EdaphosaurusDB.jpg|''[[Edaphosaurus|Edaphosaurus pogonias]]'' and ''[[Platyhystrix]]'' – Early Permian, North America and Europe
File:Dimetr eryopsDB.jpg|''[[Dimetrodon|Dimetrodon grandis]]'' and ''[[Eryops]]'' – Early Permian,  North America
File:Ocher fauna DB.jpg|Ocher fauna, ''[[Estemmenosuchus|Estemmenosuchus uralensis]]'' and ''[[Eotitanosuchus]]'' – Middle Permian, Ural Region
File:Titanophoneus 3.jpg|''[[Titanophoneus]]'' and ''[[Ulemosaurus]]'' – Ural Region
File:Inostrancevia 4DB.jpg|''[[Inostrancevia|Inostrancevia alexandri]]'' and ''[[Scutosaurus]]'' – Late Permian, North European Russia (Northern Dvina)
</gallery>

====Amphibians====
Permian stem-amniotes consisted of [[lepospondyli]] and [[Batrachosauria|batrachosaurs]], according to some phylogenies;<ref name="Ruta & Coates 2007">{{cite journal |last1=Ruta |first1=Marcello |last2=Coates |first2=Michael I. |title=Dates, nodes and character conflict: Addressing the Lissamphibian origin problem |journal=Journal of Systematic Palaeontology |date=January 2007 |volume=5 |issue=1 |pages=69–122 |doi=10.1017/S1477201906002008 |bibcode=2007JSPal...5...69R |url=https://doi.org/10.1017/S1477201906002008 |language=en |issn=1477-2019}}</ref> according to others, stem-amniotes are represented only by [[Diadectomorpha|diadectomorphs]].<ref name="Marjanović & Laurin 2019">{{cite journal |last1=Marjanović |first1=David |last2=Laurin |first2=Michel |title=Phylogeny of Paleozoic limbed vertebrates reassessed through revision and expansion of the largest published relevant data matrix |journal=PeerJ |date=4 January 2019 |volume=6 |pages=e5565 |doi=10.7717/peerj.5565 |doi-access=free |pmid=30631641 |pmc=6322490 |language=en |issn=2167-8359}}</ref> 

Temnospondyls reached a peak of diversity in the Cisuralian, with a substantial decline during the Guadalupian-Lopingian following Olson's extinction, with the family diversity dropping below Carboniferous levels.<ref>{{Cite journal|last1=Ruta|first1=Marcello|last2=Benton|first2=Michael J.|title=Calibrated Diversity, Tree Topology and the Mother of Mass Extinctions: The Lesson of Temnospondyls|date=November 2008|journal=[[Palaeontology (journal)|Palaeontology]]|language=en|volume=51|issue=6|pages=1261–1288|doi=10.1111/j.1475-4983.2008.00808.x|bibcode=2008Palgy..51.1261R|s2cid=85411546|doi-access=free}}</ref>

[[Embolomeri|Embolomeres]], a group of aquatic crocodile-like limbed vertebrates that are [[Reptiliomorpha|reptilliomorphs]] under some phylogenies. They previously had their last records in the Cisuralian, are now known to have persisted into the Lopingian in China.<ref>{{Cite journal|last1=Chen|first1=Jianye|last2=Liu|first2=Jun|date=2020-12-01|title=The youngest occurrence of embolomeres (Tetrapoda: Anthracosauria) from the Sunjiagou Formation (Lopingian, Permian) of North China|journal=[[Fossil Record]]|volume=23|issue=2|pages=205–213|doi=10.5194/fr-23-205-2020|bibcode=2020FossR..23..205C |issn=2193-0074|doi-access=free}}</ref>

Modern amphibians ([[lissamphibia]]ns) are suggested to have originated during Permian, descending from a lineage of [[Dissorophoidea|dissorophoid]] temnospondyls<ref>{{Cite journal|last=Schoch|first=Rainer R.|date=January 2019|title=The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls|journal=[[Journal of Paleontology]]|language=en|volume=93|issue=1|pages=137–156|doi=10.1017/jpa.2018.67|bibcode=2019JPal...93..137S |issn=0022-3360|doi-access=free}}</ref> or [[Lepospondyli|lepospondyls]].<ref name="Marjanović & Laurin 2019"></ref>