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Planktic foraminifera abundance of Hole 26-253
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 26-251A
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 26-251
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 26-250
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 47-398D
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 47-398B
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 47-398A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 47-398
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Calcareous nannofossils in the Western Mediterranean during the Early-Middle ...
Taxonomic analyses of coccolithophore assemblages have been carried out on sediments from Ocean Drilling Program Site 975 in the Algero-Balearic basin (38°53.8′ N, 4°30.6′ E),... -
Calcareous nannofossil assemblage data (%) from ODP Site 202-1238
Coccoliths relative abundances (%) were analyzed spanning the last 30 ky at Site ODP 1238 (1°52.310′S, 82°46.934′W; 2203 m; 2203 m) in the EEP. -
Millennial scale coccolithophore paleoproductivity and surface water changes ...
A high resolution coccolithophore study was carried out in order to improve the understanding of the paleoceanographic evolution and changes in paleoproductivity occurring off... -
(Figure 5) Accumulation rates, total abundances of coccoliths, preservationin...
This dataset has no description
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(Table 2) Dissolution index (XDX) values and average test mass for four speci...
indicates small sample where average test mass was calculated from less than 15 tests. -
Records of biogenic carbon parameter concentrations from sediment core GeoB19...
The dataset contains concentrations of bioproductivity parameters from sediment samples from sediment core GeoB19927-3 (73°35,26' N, 58°05,66' W) located in Southern Melville... -
Stable isotopes, diversity and composition of foraminifera in sediment core G...
Sample diameter 1 cm; sample depths refer to upper limits of samples -
CT-based dissolution index of four species of planktonic foraminifera from su...
This dataset has no description
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Dissolution indices above the lysocline over the last ~40 ka measured in sedi...
We have deciphered the deep sea carbonate-ion content and associated dissolution in the central Equatorial Indian Ocean (5°N & 77°E). The marine sedimentary core was... -
(Table 16) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 85-...
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found, ! = reworked or downworked specimens -
(Table 15) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 85-...
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found, ! = reworked or downworked specimens -
(Table 14) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 41-...
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found
