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- W2000900726 abstract "Recent paleontological investigations of six sections fringing the Deccan volcanic outcrops of the Indian peninsula indicate that terrestrial faunas during the Cretaceous-Paleocene transition lacked the endemism predicted by geophysical models of an oceanically isolated Indian subcontinent. At the generic and familial level there is a close correspondence between the Cretaceous vertebrates of peninsular India, Africa, and Madagascar. This suggests that a dispersal corridor, consisting of presently submerged aseismic elements (the Mascarene Plateau and the Chagos-Laccadive Ridge), existed between these landmasses about 80 million years ago as India drifted close to eastern Africa." @default.
- W2000900726 created "2016-06-24" @default.
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- W2000900726 date "1984-10-26" @default.
- W2000900726 modified "2023-09-24" @default.
- W2000900726 title "Cretaceous-Paleocene Terrestrial Faunas of India: Lack of Endemism During Drifting of the Indian Plate" @default.
- W2000900726 cites W1995766053 @default.
- W2000900726 doi "https://doi.org/10.1126/science.226.4673.441" @default.
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