Hatfield, Jack H and Allen, Bethany J and Carroll, Tadhg and Dean, Christopher D and Deng, Shuyu and Gordon, Jonathan D and Guillerme, Thomas and Hansford, James P and Hoyal Cuthill, Jennifer F and Mannion, Philip D and Martins, Inês S and Payne, Alexander RD and Shipley, Amy and Thomas, Chris D and Thompson, Jamie B and Woods, Lydia and Davis, Katie E (2025) The Greatest Extinction Event in 66 Million Years? Contextualising Anthropogenic Extinctions. Global Change Biology, 31 (9). e70476-. DOI https://doi.org/10.1111/gcb.70476
Hatfield, Jack H and Allen, Bethany J and Carroll, Tadhg and Dean, Christopher D and Deng, Shuyu and Gordon, Jonathan D and Guillerme, Thomas and Hansford, James P and Hoyal Cuthill, Jennifer F and Mannion, Philip D and Martins, Inês S and Payne, Alexander RD and Shipley, Amy and Thomas, Chris D and Thompson, Jamie B and Woods, Lydia and Davis, Katie E (2025) The Greatest Extinction Event in 66 Million Years? Contextualising Anthropogenic Extinctions. Global Change Biology, 31 (9). e70476-. DOI https://doi.org/10.1111/gcb.70476
Hatfield, Jack H and Allen, Bethany J and Carroll, Tadhg and Dean, Christopher D and Deng, Shuyu and Gordon, Jonathan D and Guillerme, Thomas and Hansford, James P and Hoyal Cuthill, Jennifer F and Mannion, Philip D and Martins, Inês S and Payne, Alexander RD and Shipley, Amy and Thomas, Chris D and Thompson, Jamie B and Woods, Lydia and Davis, Katie E (2025) The Greatest Extinction Event in 66 Million Years? Contextualising Anthropogenic Extinctions. Global Change Biology, 31 (9). e70476-. DOI https://doi.org/10.1111/gcb.70476
Abstract
<jats:title>ABSTRACT</jats:title><jats:p>Biological communities are changing rapidly in response to human activities, with the high rate of vertebrate species extinction leading many to propose that we are in the midst of a sixth mass extinction event. Five past mass extinction events have commonly been identified across the Phanerozoic, with the last occurring at the end of the Cretaceous, 66 million years ago (Ma). However, life on Earth has always changed and evolved, with most species ever to have existed now extinct. The question is, are human activities increasing the rate and magnitude of extinction to levels rarely seen in the history of life? Drawing on the literature on extinctions primarily over the last 66 million years (i.e., the Cenozoic), we ask: (1) what comparisons can meaningfully be drawn? and (2) when did the Earth last witness an extinction event on this scale? We conclude that, although challenging to address, the available evidence suggests that the ongoing extinction episode still falls a long way short of the devastation caused by the bolide impact 66 Ma, but that it has likely surpassed most other Cenozoic events in magnitude, with the possible exception of the Eocene–Oligocene transition (34 Ma), about which much uncertainty remains. Given the number of endangered and at‐risk species, the eventual magnitude of the current event will depend heavily on humanity's response and how we interact with the rest of the biosphere over the coming millennia.</jats:p>
Item Type: | Article |
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Uncontrolled Keywords: | Anthropocene; biodiversity; Cenozoic; extinction; mass extinction; sixth mass extinction |
Subjects: | Z Bibliography. Library Science. Information Resources > ZR Rights Retention |
Divisions: | Faculty of Science and Health Faculty of Science and Health > Life Sciences, School of |
SWORD Depositor: | Unnamed user with email elements@essex.ac.uk |
Depositing User: | Unnamed user with email elements@essex.ac.uk |
Date Deposited: | 17 Sep 2025 15:04 |
Last Modified: | 18 Sep 2025 01:51 |
URI: | http://repository.essex.ac.uk/id/eprint/41575 |
Available files
Filename: Hatfield_et_al_GCB_accepted.pdf
Licence: Creative Commons: Attribution 4.0