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(Table 2) Stable carbon ond oxygen isotope ratios of planktonic foraminifera ...
Depth is composite depth (mcd) -
(Table 3) Stable oxagen isotope record of planktonic foraminifera from Centra...
Above the Walvis Ridge, in the SE Atlantic Ocean, we collected living plantkic foraminifera from the upper water column using depth stratified plantkon tows. The oxygen isotope... -
Sample locations, stratigraphic information and listing of carbon and oxygen ...
We explored the potential to use the stable isotopic compositions of planktonic foraminifera as a proxy for the position of the Brazil-Malvinas Confluence (BMC) in the Argentine... -
(Table 17) Distribution of planktonic foraminifers in ODP Hole 108-668B
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 16) Distribution of planktonic foraminifers in ODP Hole 108-667A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 15) Distribution of planktonic foraminifers in ODP Hole 108-666A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 14) Distribution of planktonic foraminifers in ODP Hole 108-665A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 12) Distribution of planktonic foraminifers in ODP Hole 108-664D
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 11) Distribution of planktonic foraminifers in ODP Hole 108-657A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 10) Distribution of planktonic foraminifers in ODP Hole 108-662A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 8) Distribution of planktonic foraminifers in ODP Hole 108-661A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 7) Distribution of planktonic foraminifers in ODP Hole 108-660A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 5) Distribution of planktonic foraminifers in ODP Hole 108-659A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 4) Distribution of planktonic foraminifers in ODP Hole 108-658A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
(Table 3) Distribution of planktonic foraminifers in ODP Hole 108-657A
Species abundance: A = abundant (>30%), C = common, (15-30%), F = few (3-15%), R = rare (<3%), X = present, but no abundance estimated, - = absent. -
Planktic foraminifera abundance of Hole 29-284
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 29-282
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera fauna from sediment core SS0206-GC15
This dataset has no description
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Planktic foraminifera fauna from sediment core MD03-2611G
This dataset has no description
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Planktonic foraminiferal assemblages from sediment core ODP-161-976A
This dataset provides planktonic foraminiferal assemblage data from the marine sediment core: ODP-161-976A (Alboran Sea). Planktonic foraminiferal species are presented in...
