Late Pleistocene monsoon variability in northwest Thailand: an oxygen isotope sequence from the bivalve Margaritanopsis laosensis excavated in Mae Hong Son province

被引:46
作者
Marwick, Ben [1 ]
Gagan, Michael K. [2 ]
机构
[1] Australian Natl Univ, Res Sch Pacific & Asian Studies, Dept Archaeol & Nat Hist, Canberra, ACT 0200, Australia
[2] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
关键词
Late Pleistocene; Thailand; Archaeology; Palaeomonsoon; Freshwater bivalve; Geochemistry; Oxygen-18; EAST-ASIAN MONSOON; FRESH-WATER BIVALVES; PAPUA-NEW-GUINEA; HIGH-RESOLUTION; EARLY HOLOCENE; ARCTICA-ISLANDICA; GROWTH INCREMENTS; MILLENNIAL-SCALE; CLIMATE; RECORD;
D O I
10.1016/j.quascirev.2011.07.007
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Long, continuous records of Late Quaternary environmental change are rare in Southeast Asia, yet they are crucial for understanding the nature of early human dispersal and occupation in the Australasian region. We present a new record of palaeomonsoon activity extending back to 35,000 BP (years before the present), based on the analysis of oxygen isotope ratios (delta O-18) in the freshwater bivalve Margaritanopsis laosensis excavated from the Tham Lod and Ban Rai rockshelters in Mae Hong Son Province, northwest Thailand. Long-term changes in the M. laosensis delta O-18 record reflect changes in the delta O-18 of the river water in which these organisms grew, and correlate well with changes in speleothem delta O-18 records of east Asian monsoon rainfall from Hulu Cave and Dongge Cave in China. The new northwest Thailand delta O-18 sequence indicates wetter and relatively unstable climatic conditions from 35,000 to 20,000 BP, followed by drier conditions from 20,000 to 11,500 BP. A period of peak aridity occurred around 15,600 BP during Heinrich Event 1, suggesting that the intertropical convergence zone shifted southward when the North Atlantic region cooled. However, there is little evidence for the Younger Dryas event at similar to 12,800-11,500 BP. After 9,800 BP, precipitation increased substantially and climatic variability declined. Our findings provide an improved baseline against which to gauge interactions between early humans and climate change in Southeast Asia. For example, there was no significant change in the prehistoric flake stone technology used at Tham Lod and Ban Rai despite the bivalve delta O-18 evidence for substantial climate change in the region. Also, the climatic impact of the Younger Dryas event appears to have been less intense in northwest Thailand compared to the cooling and drying observed in China, and may explain why agriculture made a relatively late appearance in Thailand, possibly involving migrants from China. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3088 / 3098
页数:11
相关论文
共 105 条
[1]   Stable isotope evidence for moisture sources in the Asian summer monsoon under present and past climate regimes -: art. no. L08203 [J].
Aggarwal, PK ;
Fröhlich, K ;
Kulkarni, KM ;
Gourcy, LL .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (08) :L082031-4
[2]   ISOTOPE SIGNATURES ASSOCIATED WITH EARLY METEORIC DIAGENESIS [J].
ALLAN, JR ;
MATTHEWS, RK .
SEDIMENTOLOGY, 1982, 29 (06) :797-817
[3]   Asynchronous Holocene optimum of the East Asian monsoon [J].
An, ZS ;
Porter, SC ;
Kutzbach, JE ;
Wu, XH ;
Wang, SM ;
Liu, XD ;
Li, XQ ;
Zhou, WJ .
QUATERNARY SCIENCE REVIEWS, 2000, 19 (08) :743-762
[4]  
Anderson D.D., 1990, LANG RONGRIEN ROCKSH
[5]   A Late Pleistocene and Holocene pollen and charcoal record from peat swamp forest, Lake Sentarum Wildlife Reserve, West Kalimantan, Indonesia [J].
Anshari, G ;
Kershaw, AP ;
van der Kaars, S .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2001, 171 (3-4) :213-228
[6]  
Bar-Matthews M., 1993, GEOCHIMICA COSMOCHIM, V57
[7]  
Bar-Yosef O., 2002, ORIGINS POTTERY AGR, P39
[8]  
Bathurst R.G. C., 1975, Carbonate sediments and their diagenesis
[9]   Late Paleocene Arctic Ocean shallow-marine temperatures from mollusc stable isotopes [J].
Bice, KL ;
Arthur, MA ;
Marincovich, L .
PALEOCEANOGRAPHY, 1996, 11 (03) :241-249
[10]   Stable isotopes and sclerochronology of the bivalve Mesodesma donacium:: Potential application to Peruvian paleoceanographic reconstructions [J].
Carré, M ;
Bentaleb, I ;
Blamart, D ;
Ogle, N ;
Cardenas, F ;
Zevallos, S ;
Kalin, RM ;
Ortlieb, L ;
Fontugne, M .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2005, 228 (1-2) :4-25