Influence of surface ocean density on planktonic foraminifera calcification

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  • who: Stergios D. Zarkogiannis from the Dissolution assessmentThe dissolution degree of the ODP , specimens that were used in buoyancy calculations (Table, ), for which XMCT scans exist, was assessed by applying the XDX, an empirical dissolution index that evaluates the appearance of dissolution features in the tomographs30. The XMCT appearance of their internal structure resembles that of almost intact specimens implying in most of the cases less than, % of calcite loss31. In the absence of XMCT scans for the rest of the record, the carbonate preservation state of samples from ODP Site , for the first , My was examined . . .

     

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