A 35 ka pollen and isotope record of environmental change along the southern margin of the Kalahari from a stalagmite and animal dung deposits in Wonderwerk Cave, South Africa

被引:78
作者
Brook, G. A. [1 ]
Scott, L. [2 ]
Railsback, L. B. [3 ]
Goddard, E. A. [4 ]
机构
[1] Univ Georgia, Dept Geog, Athens, GA 30602 USA
[2] Univ Orange Free State, Dept Plant Sci, ZA-9300 Bloemfontein, South Africa
[3] Univ Georgia, Dept Geol, Athens, GA 30602 USA
[4] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA
基金
美国国家科学基金会; 新加坡国家研究基金会;
关键词
Archaeology; Caves; Dung; Paleoclimate; Pollen; Southern Africa; Speleothem; RADIOCARBON CALIBRATION; MILLENNIAL-SCALE; SUMMER MONSOON; SAVANNA BIOME; EQUUS CAVE; PRECIPITATION; VARIABILITY; CLIMATE; PLEISTOCENE; SPELEOTHEM;
D O I
10.1016/j.jaridenv.2009.11.006
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A 0.6-m-long horizontal core from a stalagmite in the entrance area of Wonderwerk Cave in South Africa, a National Heritage Site, has provided a 35 ka record of environmental change. A pollen sequence from the stalagmite, and two animal dung deposits, is longer and more detailed for the end of the Pleistocene than previous palynological reports from the southern Kalahari region. This pollen record closely matches information from spring peats at Wonderkrater in Northern Province indicating that speleothem pollen can provide reliable paleovegetation data. The delta O-18 and delta C-13 records resemble those from Cold Air Cave in Northern Province and parallel variations in Greenland Ice Sheet GISP2 paleotemperature. This indicates that past climate changes in southern Africa were linked to changes in global atmospheric and oceanic circulation patterns possibly triggered by conditions in the North Atlantic region. The Wonderwerk data suggest wetter conditions at ca. 33 ka, from 23 to 17 ka, and from 4 ka to present. Conditions were drier 17-13 ka, when microstromatolitic carbonate was deposited on the flank of the stalagmite, and possibly also during depositional hiatuses from 33 to 23 ka and 13 to 4 ka. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:870 / 884
页数:15
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