The Middle and Later Stone Age faunal remains from Diepkloof Rock Shelter, Western Cape, South Africa

被引:80
|
作者
Steele, Teresa E. [1 ]
Klein, Richard G. [2 ]
机构
[1] Univ Calif Davis, Dept Anthropol, Davis, CA 95616 USA
[2] Stanford Univ, Program Human Biol, Stanford, CA 94305 USA
基金
美国国家科学基金会;
关键词
Faunal analysis; Middle Stone Age; Later Stone Age; Stone Age ecology; Western Cape; South Africa; Modern human origins; STILL BAY INDUSTRY; HOWIESONS POORT; HUMAN-BEHAVIOR; SIBUDU CAVE; EXPLOITATION; PROVINCE; EXCAVATION; CHRONOLOGY; SEQUENCE; CONTEXT;
D O I
10.1016/j.jas.2013.01.001
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
The faunal sample from the Middle Stone Age (MSA) and overlying Later Stone Age (LSA) deposits of Diepkloof Rock Shelter (Western Cape Province, South Africa) includes at least 40 taxa, mostly mammals, but also tortoises, snakes, birds (especially ostrich represented by eggshell), and intertidal mollusks. The LSA sample contains only species that occurred nearby historically, including domestic sheep, which LSA people introduced to the region by 1800 years ago. In contrast, like other Western Cape MSA faunas, the Diepkloof MSA sample has more species and it is especially notable for five large extralimital grazing species. These imply a greater-than-historic role for grasses in the local vegetation, particularly in the post-Howiesons Poort (latest MSA) interval where the grazers appear most abundant. Extreme fragmentation and dark-staining impedes analysis of the MSA bones, but cut-marks, abundant burning, and numerous associated artifacts suggest that people were the main accumulators. Rare coprolites imply that carnivores could have contributed some bones, and concentrations of small mammal bones, particularly near the bottom of the MSA sequence, suggest a role for raptors. Tortoise bones are common throughout the sequence, and the MSA specimens tend to be especially large, as in other MSA assemblages. The LSA specimens are smaller, probably because LSA human populations were denser and preyed on tortoises more intensively. The most surprising aspect of the Diepkloof assemblage is its marine component. The coast is currently 14 km away and it would have been even more distant during much of the MSA when sea levels were often lower. Intertidal mollusks, particularly black mussels and granite limpets, are concentrated in the LSA and in the Late and Post-Howiesons Poort layers. Only LSA shells are complete enough for measurement, and the limpets are small as at other LSA sites. The implication is again for more intense LSA collection by relatively dense human populations. Both the LSA and MSA deposits also contain bones of shorebirds and Cape fur seals. Whale barnacles and occasional dolphin bones indicate that MSA people scavenged beached cetaceans. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3453 / 3462
页数:10
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