Stable isotopic composition of fossil mammal teeth and environmental change in southwestern South Africa during the Pliocene and Pleistocene

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Stable isotopic composition of fossil mammal teeth and environmental change in southwestern South Africa during the Pliocene and Pleistocene

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作者：Sophie B. Lehmann^a ; ^{slehman4@jhu.edu" class="auth_mail" title="E-mail the corresponding author} ; David R. Braun^b ; ^c ; ^d ; ^{david.braun@uct.ac.za" class="auth_mail" title="E-mail the corresponding author} ; Kate J. Dennis^e ; ^{katejdennis@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; David B. Patterson^f ; ^{dbpatter@gwmail.gwu.edu" class="auth_mail" title="E-mail the corresponding author} ; Deano D. Stynder^c ; ^{Deano.Stynder@uct.ac.za" class="auth_mail" title="E-mail the corresponding author} ; Laura C. Bishop^g ; ^{l.c.bishop@ljmu.ac.uk" class="auth_mail" title="E-mail the corresponding author} ; Frances Forrest^h ; ^{francesforrest@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; Naomi E. Levin^a ; ^{naomi.levin@jhu.edu" class="auth_mail" title="E-mail the corresponding author}
关键词：Pliocene-Pleistocene climate ; Stable isotopes ; Tooth enamel ; South Africa ; C4 vegetation
刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
出版年：2016
出版时间：1 September 2016
年：2016
卷：457
期：Complete
页码：396-408
全文大小：1183 K

文摘

•: Grazing herbivores in southwestern South Africa ate substantial amounts of C₃ grasses and minor amounts of C₄ grasses.
•: Winter rainfall has persisted in southwestern South Africa since at least 5 Ma.
•: Elandsfontein was likely buffered from regional aridity during the mid-Pleistocene.

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