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Noelaerhabdaceae coccolith length (mean, 5th percentile and 95th percentile) ...
This dataset contains the data plotted in Figure 5 of the review paper Coccoliths as Recorders of Paleoceanography and Paleoclimate over the Past 66 Million Years by Bolton... -
Cadmium contents in bottom sediments and sedimentary rocks from DSDP Holes 3-...
This dataset has no description
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Chemical composition of bottom sediments from DSDP Hole 24-238
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 24-236
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 24-231
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 24-235
This dataset has no description
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(Table 2) Individual C4-C7 alkane yields of DSDP samples
This dataset has no description
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(Table 1) Total yield of C4-C7 alkanes from DSDP samples
This dataset has no description
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(Table 4) Survey of Indian Ocean DSDP sites for hiatuses PH and NH 1 through ...
This dataset has no description
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(Table 1) Uranium concentrations of basalts
Errors quoted are one standard deviation for counting statistics and do not take into account variations in total neutron fluence within the irradiation capsules, which may be... -
(Table 1) Uranium chemistry of oceanic basalt whole rock samples
This dataset has no description
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(Table 3) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
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Chemical composition of bottom sediments and rocks from DSDP Holes 3-14 throu...
Data on analyses of chemical composition of DSDP samples of bottom sediments and rocks carried out in P.P. Shirshov Institute of Oceanology are reported. Basal sediments and... -
C4-C7 alkenones in deep sea sediments
It is believed that C4 to C7 hydrocarbons in petroleum are formed by the cracking of organic matter at depths generally exceeding 1,000 m at temperatures in excess of 50 °C... -
Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
Uranium in marine basalts
The uranium content of glass from chilled margins of oceanic tholeiitic basalt flows is generally <0.1 ppm, even for old samples with highly altered crystalline interiors.... -
Uranium chemistry of oceanic basalts
Measurements of uranium concentration and the 234U/238 U activity ratio in oceanic basalts which have undergone low-temperature seafloor alteration indicate that uranium uptake... -
Magnetic properties of Cenozoic MORB and Cretaceous MORB from DSDP and ODP holes
The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been... -
(Table 10) Ranges of benthic foraminifers through the Oligocene in DSDP Hole ...
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... -
Abundances of shells of planktic foraminifera species in Upper Miocene sedime...
Locations of climatic zones at four time intervals during Miocene are reconstructed from ranges of planktic foraminifera shells in Miocene deposits of the Indian Ocean. Gradual...
