An examination of the impact of Olson’s extinction on tetrapods from Texas

It has been suggested that a transition between a pelycosaurian-grade synapsid dominated fauna of the Cisuralian (early Permian) and the therapsid dominated fauna of the Guadalupian (middle Permian) was accompanied by, and possibly driven by, a mass extinction dubbed Olson’s Extinction. However, thi...

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Main Author: Neil Brocklehurst
Format: Article
Language:English
Published: PeerJ Inc. 2018-05-01
Series:PeerJ
Subjects:
Online Access:https://peerj.com/articles/4767.pdf
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spelling doaj-79f85fca2256417596c05a0307d95e772020-11-24T23:52:41ZengPeerJ Inc.PeerJ2167-83592018-05-016e476710.7717/peerj.4767An examination of the impact of Olson’s extinction on tetrapods from TexasNeil Brocklehurst0Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Berlin, GermanyIt has been suggested that a transition between a pelycosaurian-grade synapsid dominated fauna of the Cisuralian (early Permian) and the therapsid dominated fauna of the Guadalupian (middle Permian) was accompanied by, and possibly driven by, a mass extinction dubbed Olson’s Extinction. However, this interpretation of the record has recently been criticised as being a result of inappropriate time-binning strategies: calculating species richness within international stages or substages combines extinctions occurring throughout the late Kungurian stage into a single event. To address this criticism, I examine the best record available for the time of the extinction, the tetrapod-bearing formations of Texas, at a finer stratigraphic scale than those previously employed. Species richness is calculated using four different time-binning schemes: the traditional Land Vertebrate Faunachrons (LVFs); a re-definition of the LVFs using constrained cluster analysis; individual formations treated as time bins; and a stochastic approach assigning specimens to half-million-year bins. Diversity is calculated at the genus and species level, both with and without subsampling, and extinction rates are also inferred. Under all time-binning schemes, both at the genus and species level, a substantial drop in diversity occurs during the Redtankian LVF. Extinction rates are raised above background rates throughout this time, but the biggest peak occurs in the Choza Formation (uppermost Redtankian), coinciding with the disappearance from the fossil record of several of amphibian clades. This study, carried out at a finer stratigraphic scale than previous examinations, indicates that Olson’s Extinction is not an artefact of the method used to bin data by time in previous analyses.https://peerj.com/articles/4767.pdfTetrapodsTexasTime binsOlson’s extinctionRedtankianPermian
collection DOAJ
language English
format Article
sources DOAJ
author Neil Brocklehurst
spellingShingle Neil Brocklehurst
An examination of the impact of Olson’s extinction on tetrapods from Texas
PeerJ
Tetrapods
Texas
Time bins
Olson’s extinction
Redtankian
Permian
author_facet Neil Brocklehurst
author_sort Neil Brocklehurst
title An examination of the impact of Olson’s extinction on tetrapods from Texas
title_short An examination of the impact of Olson’s extinction on tetrapods from Texas
title_full An examination of the impact of Olson’s extinction on tetrapods from Texas
title_fullStr An examination of the impact of Olson’s extinction on tetrapods from Texas
title_full_unstemmed An examination of the impact of Olson’s extinction on tetrapods from Texas
title_sort examination of the impact of olson’s extinction on tetrapods from texas
publisher PeerJ Inc.
series PeerJ
issn 2167-8359
publishDate 2018-05-01
description It has been suggested that a transition between a pelycosaurian-grade synapsid dominated fauna of the Cisuralian (early Permian) and the therapsid dominated fauna of the Guadalupian (middle Permian) was accompanied by, and possibly driven by, a mass extinction dubbed Olson’s Extinction. However, this interpretation of the record has recently been criticised as being a result of inappropriate time-binning strategies: calculating species richness within international stages or substages combines extinctions occurring throughout the late Kungurian stage into a single event. To address this criticism, I examine the best record available for the time of the extinction, the tetrapod-bearing formations of Texas, at a finer stratigraphic scale than those previously employed. Species richness is calculated using four different time-binning schemes: the traditional Land Vertebrate Faunachrons (LVFs); a re-definition of the LVFs using constrained cluster analysis; individual formations treated as time bins; and a stochastic approach assigning specimens to half-million-year bins. Diversity is calculated at the genus and species level, both with and without subsampling, and extinction rates are also inferred. Under all time-binning schemes, both at the genus and species level, a substantial drop in diversity occurs during the Redtankian LVF. Extinction rates are raised above background rates throughout this time, but the biggest peak occurs in the Choza Formation (uppermost Redtankian), coinciding with the disappearance from the fossil record of several of amphibian clades. This study, carried out at a finer stratigraphic scale than previous examinations, indicates that Olson’s Extinction is not an artefact of the method used to bin data by time in previous analyses.
topic Tetrapods
Texas
Time bins
Olson’s extinction
Redtankian
Permian
url https://peerj.com/articles/4767.pdf
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