The earliest colubroid-dominated snake fauna from Africa: perspectives from the Late Oligocene Nsungwe Formation of southwestern Tanzania.
The extant snake fauna has its roots in faunal upheaval occurring across the Paleogene-Neogene transition. On northern continents, this turnover is well established by the late early Miocene. However, this transition is poorly documented on southern landmasses, particularly on continental Africa, wh...
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| Auteurs principaux: | , , |
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| Format: | article |
| Langue: | EN |
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Public Library of Science (PLoS)
2014
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| Accès en ligne: | https://doaj.org/article/1567ecad55084e459e275ea4fc5b6539 |
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