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A diverse diapsid tooth assemblage from the Early Triassic (Driefontein locality, South Africa) records the recovery of diapsids following the end-Permian mass extinction

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dc.contributor.authorHoffman, Devin K.en
dc.contributor.authorHancox, John P.en
dc.contributor.authorNesbitt, Sterling J.en
dc.date.accessioned2023-07-31T17:32:28Zen
dc.date.available2023-07-31T17:32:28Zen
dc.date.issued2023-05en
dc.description.abstractMass extinctions change the trajectory of evolution and restructure ecosystems. The largest mass extinction, the end-Permian, is a particularly interesting case due to the hypothesized delay in the recovery of global ecosystems, where total trophic level recovery is not thought to have occurred until 5-9 million years after the extinction event. Diapsids, especially archosauromorphs, play an important role in this recovery, filling niches left vacant by therapsids and anapsids. However, the nature of lineage and ecological diversification of diapsids is obscured by the limited number of continuous, well-dated stratigraphic sections at the Permian-Triassic boundary and continuing through the first half of the Triassic. The Karoo Basin of South Africa is one such record, and particularly the late Early Triassic (Olenekian) Driefontein locality fills this gap in the diapsid fossil record. We collected a total of 102 teeth of which 81 are identified as diapsids and the remaining 21 as identified as temnospondyls. From the sample, seven distinct tooth morphotypes of diapsids are recognized, six of which are new to the locality. We used a combination of linear measurements, 3D geomorphometrics, and nMDS ordination to compare these morphotypes and made inferences about their possible diets. Although the morphotypes are readily differentiated in nMDS, the overall morphological disparity is low, and we infer five morphotypes are faunivorous with the other two potentially omnivorous or piscivorous based on their morphological similarities with dentitions from extant diapsids, demonstrating an unsampled taxonomic and ecological diversity of diapsids in the Early Triassic based on teeth. Although ecological specialization at Driefontein may be low, it records a diversity of diapsid taxa, specifically of archosauromorph lineages.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.doihttps://doi.org/10.1371/journal.pone.0285111en
dc.identifier.issn1932-6203en
dc.identifier.issue5en
dc.identifier.othere0285111en
dc.identifier.pmid37126508en
dc.identifier.urihttp://hdl.handle.net/10919/115951en
dc.identifier.volume18en
dc.language.isoenen
dc.publisherPublic Library of Scienceen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectbeaufort-groupen
dc.subjectkaroo basinen
dc.subjectcomplexityen
dc.subjectarchosauren
dc.subjecthistoryen
dc.subjectpatternen
dc.subjectteethen
dc.titleA diverse diapsid tooth assemblage from the Early Triassic (Driefontein locality, South Africa) records the recovery of diapsids following the end-Permian mass extinctionen
dc.title.serialPlos Oneen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten

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