ArticleProceedings. Biological sciences2015
Mountain uplift explains differences in Palaeogene patterns of mammalian evolution and extinction between North America and Europe.
Article in Proceedings. Biological sciences, 2015. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
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Who cites it
7 citing papers in PubMed.
- Multiple Ecological Niche Modeling Reveals Niche Conservatism and Divergence in East Asian Yew (Plants (Basel, Switzerland) · 2025Article
- Tectonic extension and paleoelevation influence mammalian diversity dynamics in the Basin and Range Province of western North America.Science advances · 2024Article
- Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition.Nature communications · 2023Article
- The legacy of Eastern Mediterranean mountain uplifts: rapid disparity of phylogenetic niche conservatism and divergence in mountain vipers.BMC ecology and evolution · 2021Article
- Why aren't rabbits and hares larger?Evolution; international journal of organic evolution · 2021Article
- Lepidosaurian diversity in the Mesozoic-Palaeogene: the potential roles of sampling biases and environmental drivers.Royal Society open science · 2018Article
- Twenty-million-year relationship between mammalian diversity and primary productivity.Proceedings of the National Academy of Sciences of the United States of America · 2016Article
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Authors and funding
4 authors.
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Abstract
Patterns of late Palaeogene mammalian evolution appear to be very different between Eurasia and North America. Around the Eocene-Oligocene (EO) transition global temperatures in the Northern Hemisphere plummet: following this, European mammal faunas undergo a profound extinction event (the Grande Coupure), while in North America they appear to pass through this temperature event unscathed. Here, we investigate the role of surface uplift to environmental change and mammalian evolution through the Palaeogene (66-23 Ma). Palaeogene regional surface uplift in North America caused large-scale reorganization of precipitation patterns, particularly in the continental interior, in accord with our combined stable isotope and ecometric data. Changes in mammalian faunas reflect that these were dry and high-elevation palaeoenvironments. The scenario of Middle to Late Eocene (50-37 Ma) surface uplift, together with decreasing precipitation in higher-altitude regions of western North America, explains the enigma of the apparent lack of the large-scale mammal faunal change around the EO transition that characterized western Europe. We suggest that North American mammalian faunas were already pre-adapted to cooler and drier conditions preceding the EO boundary, resulting from the effects of a protracted history of surface uplift.
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