How predictable are mass extinction events?

William Foster*, Bethany Allen, Niklas Kitzmann, Jannes Munchmeyer, Tabea Rettelbach, James D Witts, Rowan Whittle, Ekaterina Larina, Matthew Clapham, Alexander Dunhill

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

10 Citations (Scopus)

Abstract

Many modern extinction drivers are shared with past mass extinction events, such as rapid climate warming, habitat loss, pollution and invasive species. This commonality presents a key question: can the extinction risk of species
during past mass extinction events inform our predictions for a modern biodiversity crisis? To investigate if it is possible to establish which species were more likely to go extinct during mass extinctions, we applied a functional trait-based model of extinction risk using a machine learning algorithm to datasets of marine fossils for the end-Permian, end-Triassic and end-Cretaceous mass extinctions. Extinction selectivity was inferred across each individual mass extinction event, before testing whether the selectivity patterns obtained could be used to ‘predict’ the extinction selectivity exhibited during the other mass extinctions. Our analyses show that, despite some similarities in extinction selectivity patterns between ancient crises, the selectivity of mass extinction events is inconsistent, which leads to a poor predictive performance. This lack of predictability is attributed to evolution in marine ecosystems particularly during Mesozoic marine revolution, associated with shifts in community structure alongside coincident Earth system changes. Our results suggest that past extinctions are unlikely to be informative for predicting extinction risk during a projected mass extinction.
Original languageEnglish
Article number221507
JournalRoyal Society Open Science
Volume10
Issue number3
DOIs
Publication statusPublished - 15 Mar 2023

Bibliographical note

Funding Information:
W.J.F. is funded by the Deutsche Forschungsgemeinschaft (project no. FO1297/1-1). B.J.A. was supported by a Natural Environment Research Council Studentship (grant no. NE/L002574/1) and an ETH+ grant (BECCY) funded by ETH Zürich. N.H.K. is funded by the Geo.X Young Academy. J.M. and T.R. were funded by the Helmholtz Einstein International Berlin Research School in Data Sciences (HEIBRiDS). Acknowledgements

Publisher Copyright:
© 2023 The Authors.

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