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• W2034422182 abstract "The transformation from low-crowned to high-crowned horse teeth during the Miocene has traditionally been interpreted as an adaptive response to the spread of savanna grasslands during the middle Miocene by about 15 m.y. ago. Carbon isotope data from 50 North American horse teeth spanning Eocene to Pleistocene age indicate that savanna grasslands, presumably dominated by C4 grasses as they are today, first became widespread much later than do horses with high-crowned teeth. Prior to ∼ 7 m.y., horses had a C3-based diet and after 7 m.y. horses started eating C4 grasses. This change in diet occurred when the major drop in the diversity of horses occurs during the late Miocene. The change in vegetation reflected in horses' diet may be related to a significant reduction in atmospheric CO2 level toward the end of the Miocene which provided the C4 grasses with an adaptive advantage and led to their expansion at the expense of C3 plants." @default.
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• W2034422182 date "1994-02-01" @default.
• W2034422182 modified "2023-10-05" @default.
• W2034422182 title "Fossil horses and carbon isotopes: new evidence for Cenozoic dietary, habitat, and ecosystem changes in North America" @default.
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• W2034422182 doi "https://doi.org/10.1016/0031-0182(94)90099-x" @default.
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