Stable isotope paleoecology of Late Pleistocene Middle Stone Age humans from the Lake Victoria basin, Kenya

被引:37
作者
Garrett, Nicole D. [1 ]
Fox, David L. [2 ]
McNulty, Kieran P. [1 ]
Faith, J. Tyler [4 ]
Peppe, Daniel J. [5 ]
Van Plantinga, Alex [5 ,6 ]
Tryon, Christian A. [3 ]
机构
[1] Univ Minnesota, Dept Anthropol, Hubert H Humphrey Ctr 395, Minneapolis, MN 55455 USA
[2] Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
[3] Harvard Univ, Dept Anthropol, Peabody Museum Archaeol & Ethnol, Cambridge, MA 02138 USA
[4] Univ Queensland, Sch Social Sci, Brisbane, Qld 4072, Australia
[5] Baylor Univ, Dept Geol, Waco, TX 76798 USA
[6] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA
基金
美国国家科学基金会;
关键词
Paleoenvironment; Human dispersal; Quaternary; Rusinga island; Mfangano island; SOIL ORGANIC-MATTER; AFRICA RIFT-VALLEY; CARBON ISOTOPES; OXYGEN ISOTOPES; LATE QUATERNARY; EAST-AFRICA; ENVIRONMENTAL-CHANGE; ENAMEL CARBONATE; C-13/C-12; RATIOS; ATMOSPHERIC CO2;
D O I
10.1016/j.jhevol.2014.10.005
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Paleoanthropologists have long argued that environmental pressures played a key role in human evolution. However, our understanding of how these pressures mediated the behavioral and biological diversity of early modern humans and their migration patterns within and out of Africa is limited by a lack of archaeological evidence associated with detailed paleoenvironmental data. Here, we present the first stable isotopic data from paleosols and fauna associated with Middle Stone Age (MSA) sites in East Africa. Late Pleistocene (similar to 100-45 ka, thousands of years ago) sediments on Rusinga and Mfangano Islands in eastern Lake Victoria (Kenya) preserve a taxonomically diverse, non-analog faunal community associated with MSA artifacts. We analyzed the stable carbon and oxygen isotope composition of paleosol carbonate and organic matter and fossil mammalian tooth enamel, including the first analyses for several extinct bovids such as Rusingoryx atopocranion, Damaliscus hypsodon, and an unnamed impala species. Both paleosol carbonate and organic matter data suggest that local habitats associated with human activities were primarily riverine woodland ecosystems. However, mammalian tooth enamel data indicate that most large-bodied mammals consumed a predominantly C-4 diet, suggesting an extensive C-4 grassland surrounding these riverine woodlands in the region at the time. These data are consistent with other lines of paleoenvironmental evidence that imply a substantially reduced Lake Victoria at this time, and demonstrate that C-4 grasslands were significantly expanded into equatorial Africa compared with their present distribution, which could have facilitated dispersal of human populations and other biotic communities. Our results indicate that early populations of Homo sapiens from the Lake Victoria region exploited locally wooded and well-watered habitats within a larger grassland ecosystem. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1 / 14
页数:14
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