4.6 Article

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

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PEERJ
卷 9, 期 -, 页码 -

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PEERJ INC
DOI: 10.7717/peerj.12577

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Extinction time; Fossilized-birth-death model; Permo-Carboniferous synapsids; Mass extinction events; Permian; Ophiacodontidae; Edaphosauridae; Sphenacodontidae; Amniotes; Fossil record

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The new method takes into account the possibility of diversification before extinction and estimates extinction times using the entire phylogenetic tree, resulting in more accurate confidence intervals. The approach is applied to study the extinction time of three Permo-Carboniferous synapsid taxa, supporting the idea of a progressive decline in biodiversity throughout the late Kungurian.
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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