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Clay Minerals in Soils as Evidence of Holocene Climatic Change, Central Indo-Gangetic Plains, North-Central India

Published online by Cambridge University Press:  20 January 2017

Pankaj Srivastava ,
Bramha Parkash  and
Dilip K. Pal
Pankaj Srivastava
Affiliation:
Department of Earth Sciences, University of Roorkee, Roorkee, 247667, India
Bramha Parkash
Affiliation:
Department of Earth Sciences, University of Roorkee, Roorkee, 247667, India
Dilip K. Pal
Affiliation:
Division of Soil Resource Studies, National Bureau of Soil Survey and Land Use Planning, Nagpur, 440010, India
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Abstract

Clay mineral assemblages of a soil chrono-association comprising five fluvial surface members (QGH1 to QGH5) of the Indo-Gangetic Plains between the Ramganga and Rapti rivers, north-central India, demonstrate that pedogenic interstratified smectite–kaolin (Sm/K) can be considered as a potential indicator for paleoclimatic changes during the Holocene from arid to humid climates. On the basis of available radiocarbon dates, thermoluminescence dates, and historical evidence, tentative ages assigned to QGH1 to QGH5 are <500 yr B.P., >500 yr B.P., >2500 yr B.P., 8000 TL yr B.P., and 13,500 TL yr B.P., respectively. During pedogenesis two major regional climatic cycles are recorded: relatively arid climates between 10,000–6500 yr B.P. and 3800–? yr B.P. were punctuated by a warm and humid climate. Biotite weathered to trioctahedral vermiculite and smectite in the soils during arid conditions, and smectite was unstable and transformed to Sm/K during the warm and humid climatic phase (7400–4150 cal yr B.P.). When the humid climate terminated, vermiculite, smectite, and Sm/K were preserved to the present day. The study suggests that during the development of soils in the Holocene in alluvium of the Indo-Gangetic Plains, climatic fluctuations appear to be more important than realized hitherto. The soils older than 2500 yr B.P. are relict paleosols, but they are polygenetic because of their subsequent alterations.

Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 3 , November 1998 , pp. 230 - 239
Copyright
University of Washington

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