Estimating the extinction risk from climate change
DOI: 10.1063/pt.uwaf.apmp
To learn how Earth’s species go extinct, scientists have often focused on organisms’ intrinsic traits—body size or the geographic range of a habitat, for example. Yet some of the largest mass extinctions in the geologic past have also been connected to climate change. Some previous studies have assessed
The artistic reconstruction shows a late-Triassic coral reef (left) before and (right) after a rise in ocean temperature (represented by the color bar) led to mass extinction.
Maija Karala
To disentangle various causes of extinction, it would help to understand interactions between extrinsic and intrinsic factors from the geologic past and apply them to the modern era. Now Cooper Malanoski and Erin Saupe of the University of Oxford and their colleagues have analyzed extinction risk
The researchers analyzed marine invertebrates, because they have been continuously preserved in the fossil record, making them the ideal model organisms for studying extinction dynamics over geologic time scales. The Phanerozoic eon, which began about 540 million years ago, has witnessed multiple extinction events, some associated with large swings in global temperature.
Using observations of more than 9000 extinct and living genera—archived at a public database
All the traits that were studied are statistically significant for predicting the last occurrence of a genus in the fossil record. Geographic range, in particular, was the strongest contributor. The traits also interact with each other, which highlights the complexity of how organisms may respond to extinction pressure. The effects of traits, however, weren’t sufficient to explain the total observed extinction: The magnitude of climate change, the researchers found, independently contributes to extinction risk. That may mean that, if the magnitude of modern anthropogenic climate change is large enough, marine life may be threatened by extinction regardless of the traits that they have. (C. M. Malanoski et al., Science 383, 1130, 2024
More about the Authors
Alex Lopatka. alopatka@aip.org