Paleoenvironment and archaeology of Drotsky's cave: Western kalahari desert, Botswana

被引:35
作者
Robbins, LH
Murphy, ML
Stevens, NJ
Brook, GA
Ivester, AH
Haberyan, KA
Klein, RG
Milo, R
Stewart, KM
Mattiesen, DG
Winkler, AJ
机构
[1] SUNY STONY BROOK,DEPT ANTHROPOL,STONY BROOK,NY 11794
[2] UNIV GEORGIA,DEPT GEOG,ATHENS,GA 30602
[3] TROY STATE UNIV,DEPT BIOL,TROY,AL 36082
[4] STANFORD UNIV,DEPT ANTHROPOL,STANFORD,CA 94305
[5] UNIV CHICAGO,DEPT ANTHROPOL,CHICAGO,IL 60637
[6] CANADIAN MUSEUM NAT,OTTAWA,ON K1P 6P4,CANADA
[7] UNIV FLORIDA,DEPT ZOOL,GAINESVILLE,FL 32611
[8] SO METHODIST UNIV,SHULER MUSEUM PALEONTOL,DALLAS,TX 75275
基金
美国国家科学基金会;
关键词
Drotsky's cave; southern African prehistory; terminal Pleistocene Holocene climate change; Kalahari desert; NORTHWEST KALAHARI; NORTHERN BOTSWANA; MIDDLE KALAHARI; STONE-AGE; SITE;
D O I
10.1006/jasc.1996.0002
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Test excavations conducted at Drotsky's Cave have provided important new information on the paleoenvironment and archaeology of the western Kalahari desert during the late and terminal Pleistocene. An occupation layer dated to the terminal Pleistocene was rich in Late Stone Age artefacts, pieces of ostrich egg shell, the remains of carnivorous bullfrogs, springhare, and other fauna. A detailed sediment study, along with the evidence of Angoni vlei rat, climbing mouse, an aquatic Xenopus frog, and side neck turtle confirms that conditions were for the most part, substantially more moist than at present between approximately 30,000 and 11,000 years ago. Analysis of a diatom assemblage dated to the terminal Pleistocene implies that the currently dry Gcwihaba Valley was most likely flowing for much of the year. Our evidence supports findings made at other localities in the Kalahari documenting the existence of especially moist conditions during the terminal Pleistone. (C) 1996 Academic Press Limited
引用
收藏
页码:7 / 22
页数:16
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