Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction

The Main Karoo Basin of South Africa contains a near-continuous sequence of continental deposition spanning ~80 Myr from the mid-Permian to the Early Jurassic. The terrestrial vertebrates of this sequence provide a high-resolution stratigraphic record of regional origination and extinction, especial...

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Main Authors: Day, M, Benson, R, Kammerer, C, Rubidge, B
Format: Journal article
Published: Cambridge University Press 2018
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author Day, M
Benson, R
Kammerer, C
Rubidge, B
author_facet Day, M
Benson, R
Kammerer, C
Rubidge, B
author_sort Day, M
collection OXFORD
description The Main Karoo Basin of South Africa contains a near-continuous sequence of continental deposition spanning ~80 Myr from the mid-Permian to the Early Jurassic. The terrestrial vertebrates of this sequence provide a high-resolution stratigraphic record of regional origination and extinction, especially for the mid–late Permian. Until now, data have only been surveyed at coarse stratigraphic resolution using methods that are biased by nonuniform sampling rates, limiting our understanding of the dynamics of diversification through this important time period. Here, we apply robust methods (gap-filler and modified gap-filler rates) for the inference of patterns of species richness, origination rates, and extinction rates to a subset of 1321 reliably-identified fossil occurrences resolved to approximately 50 m stratigraphic intervals. This data set provides an approximate time resolution of 0.3–0.6 Myr and shows that extinction rates increased considerably in the upper 100 m of the mid-Permian Abrahamskraal Formation, corresponding to the latest part of the Tapinocephalus Assemblage Zone (AZ). Origination rates were only weakly elevated in the same interval and were not sufficient to compensate for these extinctions. Subsampled species richness estimates for the lower part of the overlying Teekloof Formation (corresponding to the Pristerognathus and Tropidostoma AZs) are low, showing that species richness remained low for at least 1.5–3 million years after the main extinction pulse. A high unevenness of the taxon abundance–frequency distribution, which is classically associated with trophically unstable postextinction faunas, in fact developed shortly before the acme of elevated extinction rates due to the appearance and proliferation of the dicynodont Diictodon. Our findings provide strong support for a Capitanian (“end-Guadalupian”) extinction event among terrestrial vertebrates and suggest that further high-resolution quantitative studies may help resolve the lack of consensus among paleobiologists regarding this event.
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spelling oxford-uuid:b21c5037-e26d-4e97-b29e-1f49a5530fb32022-03-27T04:09:21ZEvolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstructionJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:b21c5037-e26d-4e97-b29e-1f49a5530fb3Symplectic Elements at OxfordCambridge University Press2018Day, MBenson, RKammerer, CRubidge, BThe Main Karoo Basin of South Africa contains a near-continuous sequence of continental deposition spanning ~80 Myr from the mid-Permian to the Early Jurassic. The terrestrial vertebrates of this sequence provide a high-resolution stratigraphic record of regional origination and extinction, especially for the mid–late Permian. Until now, data have only been surveyed at coarse stratigraphic resolution using methods that are biased by nonuniform sampling rates, limiting our understanding of the dynamics of diversification through this important time period. Here, we apply robust methods (gap-filler and modified gap-filler rates) for the inference of patterns of species richness, origination rates, and extinction rates to a subset of 1321 reliably-identified fossil occurrences resolved to approximately 50 m stratigraphic intervals. This data set provides an approximate time resolution of 0.3–0.6 Myr and shows that extinction rates increased considerably in the upper 100 m of the mid-Permian Abrahamskraal Formation, corresponding to the latest part of the Tapinocephalus Assemblage Zone (AZ). Origination rates were only weakly elevated in the same interval and were not sufficient to compensate for these extinctions. Subsampled species richness estimates for the lower part of the overlying Teekloof Formation (corresponding to the Pristerognathus and Tropidostoma AZs) are low, showing that species richness remained low for at least 1.5–3 million years after the main extinction pulse. A high unevenness of the taxon abundance–frequency distribution, which is classically associated with trophically unstable postextinction faunas, in fact developed shortly before the acme of elevated extinction rates due to the appearance and proliferation of the dicynodont Diictodon. Our findings provide strong support for a Capitanian (“end-Guadalupian”) extinction event among terrestrial vertebrates and suggest that further high-resolution quantitative studies may help resolve the lack of consensus among paleobiologists regarding this event.
spellingShingle Day, M
Benson, R
Kammerer, C
Rubidge, B
Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title_full Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title_fullStr Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title_full_unstemmed Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title_short Evolutionary rates of mid-Permian tetrapods from South Africa and the role of temporal resolution in turnover reconstruction
title_sort evolutionary rates of mid permian tetrapods from south africa and the role of temporal resolution in turnover reconstruction
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AT bensonr evolutionaryratesofmidpermiantetrapodsfromsouthafricaandtheroleoftemporalresolutioninturnoverreconstruction
AT kammererc evolutionaryratesofmidpermiantetrapodsfromsouthafricaandtheroleoftemporalresolutioninturnoverreconstruction
AT rubidgeb evolutionaryratesofmidpermiantetrapodsfromsouthafricaandtheroleoftemporalresolutioninturnoverreconstruction