Paleoenvironmental and biogeographic implications of terminal Pleistocene large mammals from the Ziway-Shala Basin, Main Ethiopian Rift, Ethiopia
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- 作者：José ; phine Lesura ; jolesur@mnhn.fr" class="auth_mail" title="E-mail the corresponding author ; J. Tyler Faithb ; j.faith@uq.edu.au" class="auth_mail" title="E-mail the corresponding author ; Franç ; ois Bonc ; bon@univ-tlse2.fr" class="auth_mail" title="E-mail the corresponding author ; Assamerew Dessied ; ato.asamerew.dessie@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Clé ; ment Mé ; narde ; menard.clement@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Laurent Bruxellesc ; f ; g ; laurent.bruxelles@inrap.fr" class="auth_mail" title="E-mail the corresponding author
- 关键词：Horn of Africa ; Main Ethiopian Rift ; Terminal Pleistocene ; Biogeography ; Damaliscus
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 May 2016
- 年：2016
- 卷：449
- 期：Complete
- 页码：567-579
- 全文大小：2492 K
文摘
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Faunas from B1s1 and B1s4 document paleoenvironments during the terminal Pleistocene.
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Faunal assemblages are dominated by bovids of the tribes Alcelaphini and Antilopini.
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Fauna includes Damaliscus hypsodon, a small extinct alcelaphine.
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B1s1 and B1s4 faunal remains are indicative of widespread arid grasslands.
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Arid-adapted species disappear or shift their range at the onset of the Holocene.