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Ostracoda abundance of Hole 48-403
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Ostracoda abundance of Hole 95-613
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Ostracoda abundance of Hole 95-612
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Ostracoda abundance of Hole 24-237
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 18) Distribution of ostracode species in Core PS51/154-11
Abundance of ostracodes was calculated per 100 grams of dry bulk sediment weight. -
(Table 7) Distribution of ostracode species in surface sediments of the centr...
Abundance of ostracodes was calculated per 100 grams of dry bulk sediment weight. -
Ostracoda in sediment core PS51/159-10
This dataset has no description
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Ostracoda in sediment core PS51/154-11
This dataset has no description
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Distribution of Holocene foraminifera and ostracoda of sediment core EV13-3 t...
DEPTH, sediment/rock [m] = Composite depth [m]. -
Counts of ostracode taxa from the Maastrichtian-Thanetian samples at IODP Sit...
This dataset has no description
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Ostracoda counts from the Paleocene-Eocene samples at ODP Site 865
Sediment depth is given in mcd. -
Ostracoda in sediment core BP00-07/05
This dataset has no description
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(Table 2) Quarternary ostracod abundance in sediment core CRP-1
This dataset has no description
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Deglacial-Holocene ostracods census data from marine sediment cores JM10-10GC...
This is the ostracods census data from 157 sub-samples from two marine sediment cores, JM10-10GC and JM10-12GC, from Storfjorden, Svalbard. Cores were taken in October 2010 by... -
Ostracode abundance and Simpson's index over the past 700,000 years at IODP S...
The Sea of Japan is a marginal sea, semi-enclosed by the Eurasian Continent, Korean Peninsula, Japanese archipelago, and connected to the Pacific Ocean and adjacent seas by... -
(Appendix) Ostracodes at DSDP Leg 72 Holes
From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed... -
(Appendix A) Abundance of ostracode species from DSDP Hole 48-401
Previous low resolution studies suggest that ostracodes, in contrast with deep sea foraminifera, largely survived the massive environmental changes of the Paleocene–Eocene... -
Stable oxygen and carbon isotope ratios of Globigerinoides obliquus of quanti...
Deep-water benthic ostracodes from the Pliocene-Pleistocene interval of ODP Leg 107, Hole 654A (Tyrrhenian Sea) were studied. From a total of 106 samples, 40 species considered... -
Late Cretaceous and Cainozoic bathyal Ostracoda of DSDP Site 62-463 in the Ce...
Cainozoic deep-sea ostracod assemblages from the summits of Mid-Pacific guyots point to high levels of endemism possibly as a result of their bathymetric separation from the... -
Range table from ostracoda in ODP Hole 159-960C
This dataset has no description
