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Detailed investigation (630 samples) of clay mineral assemblages and benthic foraminifer accumulation rates (BFAR) as a proxy for paleoproductivity has been conducted on two late Eocene-Oligocene sequences drilled at intermediate water depths of the Kerguelen Plateau and Maud Rise (Southern Ocean). Distinct changes in clay assemblages and BFAR - that are in general a factor two higher on the Maud...
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