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(Table 18) Ranges of benthic foraminifers through the Neogene in DSDP Hole 23...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 5) Occurrence chart of Paleogene diatom species in DSDP holes 23-219 a...
species abundance: S = singel (<0.1%), R = rare (0.1%-1.0%), F = frequent (1%-10%), C = common (10%-30%), A = abundant (30%-50%), D = dominant (>50%), - = absent -
(Table 2) Diatom abundance and nannofossil and diatom zonation of DSDP Hole 2...
This dataset has no description
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(Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP...
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(Table 2) Analyses of anhydrite samples from DSDP Hole 23-228
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(Table 2) Analyses of anhydrite samples from DSDP Hole 23-227
Halite abundance is abundant -
(Table 2) Analyses of anhydrite samples from DSDP Hole 23-225
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(Table 1) Analyses of halite samples from DSDP Hole 23-227
Sample 23-227-45-1,75-80: Rb content is 0.00013 weight-% per total sample or 0.0014 weight-% Rb per pure polyhalite -
(Table 1) Analyses of halite samples from DSDP Hole 23-225
Sample 23-225-29-3,40-45: Rb content is 0.00037 weight-% per total sample or 0.0014 weight-% Rb per pure polyhalite -
(Table 3) Chemical composition of sediments from DSDP Site 223 recalculated o...
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(Table 2) Chemical composition of bulk sediment samples from DSDP Site 223
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(Table 3, part b) Trace element contents in chert and associated host sedimen...
This dataset has no description
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(Table 2, part a) Rare earth element contents in chert and associated host se...
This dataset has no description
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(Table 1, part b) Major element contents in chert and associated host sedimen...
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(Table III) Stable oxygen and carbon isotope ratios of Late Cretaceous to Ear...
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(Table 3) Sulfur and oxygen isotopic composition of cold water soluble sulfat...
The origin of three Red Sea submarine brine pools was investigated by analysis of the S and O isotope ratios of dissolved sulfate and Sr isotope ratios of dissolved Sr in the... -
Relative abundances of twenty-eight dominant benthic foraminifera species of ...
Tropical climate is variable on astronomical time scale, driving changes in surface and deep-sea fauna during the Pliocene-Pleistocene. To understand these changes in the... -
(Table 2) Pb isotope composition of K-feldspars from sediments of the Bengal Fan
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(Table 1) Nd isotope composition of fine-grained clay minerals from sediments...
This dataset has no description