A high resolution and continuous isotopic speleothem record of paleoclimate and paleoenvironment from 90 to 53 ka from Pinnacle Point on the south coast of South Africa

被引:153
作者
Bar-Matthews, Miryam [1 ]
Marean, Curtis W. [2 ]
Jacobs, Zenobia [3 ]
Karkanas, Panagiotis
Fisher, Erich C. [4 ]
Herries, Andy I. R. [5 ]
Brown, Kyle [2 ,6 ]
Williams, Hope M.
Bernatchez, Jocelyn
Ayalon, Avner [1 ]
Nilssen, Peter J. [7 ]
机构
[1] Geol Survey Israel, IL-95501 Jerusalem, Israel
[2] Arizona State Univ, Inst Human Origins, Sch Human Evolut & Social Change, Tempe, AZ 85287 USA
[3] Univ Wollongong, Ctr Archaeol Sci, Sch Earth & Environm Sci, Wollongong, NSW 2522, Australia
[4] Univ Florida, Dept Anthropol, Gainesville, FL 32611 USA
[5] Univ New S Wales, Sch Med Sci, UNSW Archaeomagnetism Lab, Sydney, NSW 2052, Australia
[6] Univ Cape Town, Dept Archaeol, ZA-7701 Rondebosch, South Africa
[7] Ctr Heritage & Archaeol Resource Management, ZA-6500 Mossel Bay, South Africa
基金
美国国家科学基金会;
关键词
MIDDLE-STONE-AGE; MODERN HUMAN-BEHAVIOR; LATE QUATERNARY; BLOMBOS CAVE; HOWIESONS-POORT; PLANT DIVERSITY; KLASIES RIVER; CAPE-PROVINCE; ROCK SHELTER; LUMINESCENCE;
D O I
10.1016/j.quascirev.2010.05.009
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Coastal South Africa draws interdisciplinary interests due to the co-occurrence of a rich record for early human behavioral modernity, hyper-diverse vegetation with very high endemism (the Cape Floral Region), and globally influential oceanic and climate systems. High resolution and continuous climate and environmental records are needed to provide the context for the evolution of behavioral modernity and this diverse flora. Here we present the first such record for climate and environmental change from 90 000 to 53 000 years ago from the southern Cape coast. This important time span covers a burst of expression of several indicators of human behavioral modernity, as well as several key cycles in global climate change. Our research location is ideally placed near the location of several critical archaeological sites, near the boundary of the winter and summer rainfall regimes, and close to isotopically distinct floral zones. We used isotopic analysis of precisely dated speleothems to document shifting vegetation and rainfall, and show that the presence of winter rain and C3 grasses waxes and wanes in response to Southern Hemisphere shifts in SSTs and global temperature. When proxies of global temperatures indicate warmer conditions, delta O-18 and delta C-13 indicate more winter rain and more C3 grasses, respectively, and vice versa. This record displays abrupt and short-term changes previously undocumented. It is often argued that the Cape Floral Region partially owes its high diversity to relative climatic stability. Our record shows isotopic variability that at least matches that displayed in the Levantine Mediterranean system, so climatic stability may not have characterized the south coast. One short-lived phase of human technological innovation (the Still Bay) associated with early evidence for behavioral modernity occurs synchronous with an abrupt environmental perturbation. Early modern humans in this region confronted a variable climate and adapted quickly in a manner similar to behaviorally modern humans. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2131 / 2145
页数:15
相关论文
共 129 条
[1]  
Aitken M.J., 1998, An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence, DOI DOI 10.1017/S0016756899551777
[2]  
Ambrose StanleyH., 1990, The Emergence of Modern Humans: An Archaeological Perspective, P3
[3]  
[Anonymous], 2006, AGULHAS CURRENT, DOI DOI 10.1007/3-540-37212-1
[4]  
[Anonymous], 1983, SPECIAL PUBLICATIONS
[5]  
[Anonymous], [No title captured]
[6]   A re-appraisal of micromammalian data from South Africa [J].
Avery, DM .
QUATERNARY INTERNATIONAL, 1999, 57-8 :175-183
[7]   Rainfall-recharge relationships within a karstic terrain in the eastern Mediterranean semi-arid region, Israel:: δ18O and δD characteristics [J].
Ayalon, A ;
Bar-Matthews, M ;
Sass, E .
JOURNAL OF HYDROLOGY, 1998, 207 (1-2) :18-31
[8]   Middle Stone Age bone tools from the Howiesons Poort Layers, Sibudu Cave, South Africa [J].
Backwell, Lucinda ;
d'Errico, Francesco ;
Wadley, Lyn .
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 2008, 35 (06) :1566-1580
[9]  
Bakker E. M., 1978, Biogeography and ecology of Southern Africa. Vol.1., P131
[10]   Sea-land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals [J].
Bar-Matthews, M ;
Ayalon, A ;
Gilmour, M ;
Matthews, A ;
Hawkesworth, CJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2003, 67 (17) :3181-3199