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Sediment reflectance of gravity core LV28-34-2
Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of... -
Benthic stable isotopes, biogenic silica and sediment geochemistry of gravity...
Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of... -
Radiocarbon datings of planktic foraminifer samples from gravity core LV28-34-2
Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of... -
Organic carbon and calcium carbonate concentrations in bulk sediment of gravi...
Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of... -
(Appendix 3) Stable oxygen isotope ratios of benthic foraminifera in sediment...
Measured on 2-3 species of the endobenthic foraminiferal species Uvigerina auberiana and Uvigerina aktiaensis (Uvigerina peregrina of authors) from the 250-500 um size fraction. -
(Appendix 6) Stable oxygen isotope ratios of benthic foraminifera from sedime...
Measured on 2-3 species of the endobenthic foraminiferal species Uvigerina auberiana and Uvigerina aktiaensis (Uvigerina peregrina of authors) from the 250-500 um size fraction. -
Documentation of sediment core LV28-34-2
This dataset has no description
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Physical properties of sediment core LV28-34-2
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Grain size distribution in sediment core LV28-34-2
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Coarse fraction analysis of sediment core LV28-34-2
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Geochemistry and documentation of water and sediment profiles from KOMEX I ex...
Documentation and geochemical measurements of water and sediment profiles from KOMEX I expedition. -
Oceanographic investiations from the Sea of Ochotsk
The Sea of Okhotsk is a marginal sea of the Pacific Ocean, which is characterized by strong variations in the productivity and sediment supply due to sea ice transport and river... -
(Table 5) Chemical composition of grains of sulfides, oxides, and native meta...
This dataset has no description
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(Table 4) Chemical composition of grains of intermetallic compounds of nonfer...
This dataset has no description
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(Table 3) Chemical composition of precious metal grains from ferromanganese c...
Due to extremely small sizes of grains surrounding particles were often included in the microprobe analysis. -
(Table 2) Chemical composition of matrix of ferromanganese crusts from the ce...
Since most of ore crusts are loose, microprobe analyses often yield sum of elements less than 100%. -
(Table 1) Chemical composition of ferromanganese formations from the central ...
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Geochemical conditions on sediment profile LV28-44-4
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Geochemical conditions on sediment profile LV28-37-1
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Geochemical conditions on sediment profile LV28-30-4
data from single multi-corer tube(s)
