ArticleProceedings. Biological sciences2021
Increase in marine provinciality over the last 250 million years governed more by climate change than plate tectonics.
Article in Proceedings. Biological sciences, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
6 citing papers in PubMed.
- Global patterns are key to understanding macroevolution.Communications biology · 2026Article
- Diverging selection on body size in specialist terrestrial mammals.Nature ecology & evolution · 2026Article
- Unveiling the underlying drivers of Phanerozoic marine diversification.Proceedings. Biological sciences · 2024Article
- Article
- Global diversity dynamics in the fossil record are regionally heterogeneous.Nature communications · 2022Article
- Increase in marine provinciality over the last 250 million years governed more by climate change than plate tectonics.Proceedings. Biological sciences · 2021Article
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Authors and funding
5 authors.
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No grant is acknowledged in the PubMed record.
Abstract
Amidst long-term fluctuations of the abiotic environment, the degree to which life organizes into distinct biogeographic provinces (provinciality) can reveal the fundamental drivers of global biodiversity. Our understanding of present-day biogeography implies that changes in the distribution of continents across climatic zones have predictable effects on habitat distribution, dispersal barriers and the evolution of provinciality. To assess marine provinciality through the Phanerozoic, here we (a) simulate provinces based on palaeogeographic reconstructions and global climate models and (b) contrast them with empirically derived provinces that we define using network analysis of fossil occurrences. Simulated and empirical patterns match reasonably well and consistently suggest a greater than 15% increase in provinciality since the Mesozoic era. Although both factors played a role, the simulations imply that the effect of the latitudinal temperature gradient has been twice as important in determining marine provinciality as continental configuration.
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Registered trials
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