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URN to cite this document: urn:nbn:de:bvb:703-epub-5962-5
Title data
Mathes, Gregor H. ; Kiessling, Wolfgang ; Steinbauer, Manuel:
Deep-time climate legacies affect origination rates of marine genera.
In: Proceedings of the National Academy of Sciences.
Vol. 118
(7 September 2021)
Issue 36
.
ISSN Print: 0027-8424 Electronic: 1091-6490
DOI der Verlagsversion: https://doi.org/10.1073/pnas.2105769118
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Project information
| Project title: |
Project's official title Project's id Humans on Planet Earth (Hope) 741413 FOR 2332: Temperature-related stressors as a unifying
principle in ancient extinctions (Tersane) 269895748 CoralTrace: A new approach to understanding climate-induced reef crises KI 806/16-1 PastKey: Evolutionary and environmental history explaining temperature related extinctions in marine biota STE 2360/2-1 |
|---|---|
| Project financing: |
Deutsche Forschungsgemeinschaft European Research Council Deutsche Forschungsgemeinschaft Deutsche Forschungsgemeinschaft Deutsche Forschungsgemeinschaft |
Abstract
Biodiversity dynamics are shaped by a complex interplay between current conditions and historic legacy. The interaction of short- and long-term climate change may mask the true relationship of evolutionary responses to climate change if not specifically accounted for. These paleoclimate interactions have been demonstrated for extinction risk and biodiversity change, but their importance for origination dynamics remains untested. Here, we show that origination probability in marine fossil genera is strongly affected by paleoclimate interactions. Overall, origination probability increases by 27.8% [95% CI (27.4%, 28.3%)] when a short-term cooling adds to a long-term cooling trend. This large effect is consistent through time and all studied groups. The mechanisms of the detected effect might be manifold but are likely connected to increased allopatric speciation with eustatic sea level drop caused by sustained global cooling. We tested this potential mechanism through which paleoclimate interactions can act on origination rates by additionally examining a proxy for habitat fragmentation. This proxy, continental fragmentation, has a similar effect on origination rates as paleoclimate interactions, supporting the importance of allopatric speciation through habitat fragmentation in the deep-time fossil record. The identified complex nature of paleoclimate interactions might explain contradictory conclusions on the relationship between temperature and origination in the previous literature. Our results highlight the need to account for complex interactions in evolutionary studies both between and among biotic and abiotic factors.
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