Distributions of extinction times from fossil ages and tree topologies: the example of mid-Permian synapsid extinctions

被引:6
作者
Didier, Gilles [1 ]
Laurin, Michel [2 ]
机构
[1] Univ Montpellier, CNRS, IMAG, Montpellier, France
[2] Sorbonne Univ, CR2P Ctr Rech Sur Paleobiodiversite & Paleoenviro, Museum Natl Hist Nat, CNRS MNHN UPMC,UMR 7207, Paris, France
来源
PEERJ | 2021年 / 9卷
关键词
Extinction time; Fossilized-birth-death model; Permo-Carboniferous synapsids; Mass extinction events; Permian; Ophiacodontidae; Edaphosauridae; Sphenacodontidae; Amniotes; Fossil record; 6TH MASS EXTINCTION; CONFIDENCE-INTERVALS; STRATIGRAPHIC RANGES; VERTEBRATE EVIDENCE; CONTINENTAL STRATA; REPTILE MACROLETER; DIVERGENCE TIMES; ASSEMBLAGE ZONE; NORTH-AMERICA; KAROO BASIN;
D O I
10.7717/peerj.12577
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Given a phylogenetic tree that includes only extinct, or a mix of extinct and extant taxa, where at least some fossil data are available, we present a method to compute the distribution of the extinction time of a given set of taxa under the Fossilized Birth-Death model. Our approach differs from the previous ones in that it takes into account (i) the possibility that the taxa or the clade considered may diversify before going extinct and (ii) the whole phylogenetic tree to estimate extinction times, whilst previous methods do not consider the diversification process and deal with each branch independently. Because of this, our method can estimate extinction times of lineages represented by a single fossil, provided that they belong to a clade that includes other fossil occurrences. We assess and compare our new approach with a standard previous one using simulated data. Results show that our method provides more accurate confidence intervals. This new approach is applied to the study of the extinction time of three Permo-Carboniferous synapsid taxa (Ophiacodontidae, Edaphosauridae, and Sphenacodontidae) that are thought to have disappeared toward the end of the Cisuralian (early Permian), or possibly shortly thereafter. The timing of extinctions of these three taxa and of their component lineages supports the idea that the biological crisis in the late Kungurian/early Roadian consisted of a progressive decline in biodiversity throughout the Kungurian.
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页数:39
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