The fossil record of North American mammals: Evidence for a Paleocene evolutionary radiation

被引:203
作者
Alroy, J [1 ]
机构
[1] Smithsonian Inst, Dept Paleobiol, MRC 121, Washington, DC 20560 USA
关键词
body mass; Cenozoic; Cretaceous; diversification; extinction; Mammalia; molecular clock;
D O I
10.1080/106351599260472
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Paleontologists long have argued that the most important evolutionary radiation of mammals occurred during the early Cenozoic, if not that all eutherians originated from a single common post-Cretaceous ancestor. Nonetheless, several recent molecular analyses claim to show that because several interordinal splits occurred during the Cretaceous, a major therian radiation was then underway This claim conflicts with statistical evidence from the well-sampled latest Cretaceous and Cenozoic North American fossil record. Paleofaunal data confirm that there were fewer mammalian species during the latest Cretaceous than during any interval of the Cenozoic, and that a massive diversification took place during the early Paleocene, immediately after a mass extinction. Measurement data show that Cretaceous mammals were on average small and occupied a narrow range of body sizes; after the Cretaceous-Tertiary mass extinction, there was a rapid and permanent shift in the mean. The fact that there was an early Cenozoic mammalian radiation is entirely compatible with the existence of a few Cretaceous splits among modern mammal lineages.
引用
收藏
页码:107 / 118
页数:12
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