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    Late Quaternary Faunal Change in Coastal Arabian sea Sediments

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    Quat_Res_18_236.pdf (293Kb)
    Date
    1982
    Author
    Borole, D.V.
    Rao, K.K.
    Krishnamurthy, R.V.
    Somayajulu, B.L.K.
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    Abstract
    Carbonate content and faunal composition of two gravity cores from the coastal Arabian Sea provide evidence of a major environmental change in surface ocean waters about 13,000 yr B.P. Radiocarbon dating indicates that deposition rates ranged from 1.8 to 9.8 cm/103 yr, with a major change in rate occurring in one core at about 7500 yr B.P.
    URI
    http://drs.nio.org/drs/handle/2264/6628
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