All Toba tephra occurrences across peninsular India belong to the 75,000 yr BP eruption

被引:133
作者
Westgate, JA [1 ]
Shane, PAR
Pearce, NJG
Perkins, WT
Korisettar, R
Chesner, CA
Williams, MAJ
Acharyya, SK
机构
[1] Univ Toronto, Div Phys Sci, Scarborough, ON M1C 1A4, Canada
[2] Univ Auckland, Dept Geol, Auckland, New Zealand
[3] Karnatak Univ, Dept Hist & Archaeol, Dharwad 580003, Karnataka, India
[4] Eastern Illinois Univ, Dept Geol, Charleston, IL 61920 USA
[5] Univ Adelaide, Mawson Grad Ctr Environm Studies, Adelaide, SA 5005, Australia
[6] Geol Survey India, Calcutta 700016, W Bengal, India
基金
加拿大自然科学与工程研究理事会;
关键词
Toba tephra; volcanic glass; major and trace elements; fission-track age; Acheulian artifacts; India;
D O I
10.1006/qres.1998.1974
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
A controversy currently exists regarding the number of Toba eruptive events represented in the tephra occurrences across peninsular India. Some claim the presence of a single bed, the 75,000-yr-old Toba tephra; others argue that dating and archaeological evidence suggest the presence of earlier Toba tephra, Resolution of this issue was sought through detailed geochemical analyses of a comprehensive suite of samples, allowing comparison of the Indian samples to those from the Toba caldera in northern Sumatra, Malaysia, and, importantly, the sedimentary core at ODP Site 758 in the Indian Ocean-a core that contains several of the earlier Toba tephra beds. In addition, two samples of Toba tephra from western India were dated by the fission-track method. The results unequivocally demonstrate that all the presently known Toba tephra occurrences in peninsular India belong to the 75,000 yr B.P. Toba eruption. Hence, this tephra bed can be used as an effective tool in the correlation and dating of late Quaternary sedimentary sequences across India and it can no longer be used in support of a middle Pleistocene age fbr associated Acheulian artifacts. (C) 1998 University of Washington.
引用
收藏
页码:107 / 112
页数:6
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