Taxonomy and paleoecology of fossil Bovidae (Mammalia, Artiodactyla) from the Kibish Formation, southern Ethiopia: Implications for dietary change, biogeography, and the structure of the living bovid faunas of East Africa

被引:23
作者
Rowan, John [1 ]
Faith, J. Tyler [2 ]
Gebru, Yemane [3 ]
Fleagle, John G. [4 ]
机构
[1] Arizona State Univ, Sch Human Evolut & Social Change, Tempe, AZ 85282 USA
[2] Univ Queensland, Sch Social Sci, Archaeol Program, Brisbane, Qld 4072, Australia
[3] Univ Addis Ababa, Paleoanthropol & Paleoenvironm Program, Addis Ababa, Ethiopia
[4] SUNY Stony Brook, Dept Anat Sci, Stony Brook, NY 11794 USA
基金
美国国家科学基金会;
关键词
Biogeography; Bovidae; Mesowear; Kibish Forrnation; Late Quaternary paleoecology; LATE PLEISTOCENE; PLIOCENE BOVIDAE; LAKE VICTORIA; OMO I; PHYLOGEOGRAPHY; REGION; SITES; AGE; MITOCHONDRIAL; HYBRIDIZATION;
D O I
10.1016/j.palaeo.2014.12.017
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Kibish Formation of southern Ethiopia has yielded the earliest fossils of Homo sapiens, ca. 196 ka, and has thus figured prominently in discussions of the origins of modern humans. Here we describe the fossil Bovidae from the Kibish Formation, a record that spans the late Middle Pleistocene to the early to mid-Holocene, and reconstruct aspects of their dietary ecology using mesowear analyses. All of the Kibish bovids represent extant taxa with the exception of the extinct blesbok-like alcelaphin Damaliscus hypsodon; extinct arid-adapted forms Syncerus antiquus and Megalotragus, common in other Late Quaternary sites, are notably absent. Mesowear of the Kibish bovids suggests that the late Quaternary specimens were characterized by diets with considerably more abrasion-dominated wear relative to their extant conspecifics. Finally, the Kibish record provides supporting evidence for recent phylogeographic hypotheses by demonstrating significant range expansions of Aepyceros melampus, Connochaetes taurinus, Hippotragus equinus, and, to a lesser extent. Kobus kob in the late Middle Pleistocene through the early to mid-Holocene coincident with humid phases that punctuated dry spells of the late Quaternary. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:210 / 222
页数:13
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