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Raw data files of X-ray diffraction analysis of the clay fraction from 13 sed...
Clay fraction less than 2 micron was quantitatively separated by Atterberg method (settling tube), washed, dried and milled. Clay was resuspended and texturized on sample holder... -
Fig. 2. Stable isotope analysis on C. wuellerstorfi from sediment core GeoB17...
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Table A5. Benthic foraminifera counts, accumulation rates, and statistical an...
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Surface sediment data
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Table A1. Age model of sediment core GeoB1710-3
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Table A7. Statistical analysis of late Quaternary benthic foraminiferal assem...
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Kaolinite/chlorite ratios measured on sediment core GeoB1710-3
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Kaolinite/chlorite ratios measured on sediment core GeoB1712-4
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X-ray fluorescence (XRF) scanner Ca/Fe ratio of sediment core GeoB1711-4
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Tie-points and sedimentation rate of sediment core GeoB1711-4
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(Table 1) Sampling locations, water depth, and physical and chemical properti...
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(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
Collection of X-ray micro computed tomography images of shells of planktic fo...
Calcite shells of planktic foraminifera (Protista, Rhizaria) constitute a large portion of deep-sea sediments. The shells are constructed by sequential addition of partly... -
Distribution of coccoliths in surface sediments of the south-eastern South At...
Recent coccoliths from 52 surface sediment samples recovered from the south-eastern South Atlantic were examined qualitatively and quantitatively in order to assess the... -
Phytoplanktonic microfossil groups of sediments from the South and Equatorial...
Individual planktonic microfossil species, or assemblage groups of different species, are often used to, qualitatively and/or quantitatively, reconstruct past (sub)surface-water... -
Coccolith carbonate mass of sediment core GeoB1710-3
coccolith mass (m) = 2.7 * ks l*3, where 2.7 = calcite density; ks = shape factor; l = coccolith length after Young and Ziveri (2000), Young, J.R., Ziveri, P., 2000. Calculation... -
Coccolith accumulation rate, diversity and CEX´ of sediment core GeoB1710-3
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Dinoflagellate assemblage in surface sediments of the South Atlantic
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Dinoflagellates (organic) in surface sediments of the South Atlantic
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Total coccolith abundance, coccolith carbonat and CEX´ of surface sediment sa...
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