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4 Million Negative Exp

1.Introduction.Knowledge of the past wind regime over the northern indian ocean, so far, comes from the source-proximal arabian sea dust records, the isotopic composition of planktonic foraminifera, or is based on data from upwelling areas, where increased productivity is linked to intensified surface winds sirocko and sarnthein, 1989 kroon et al., 1991 clemens, 1998 gupta et al., 2003.

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