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Physical oceanography during Morskoy Geophysik cruise MG1973 to the North Sea
This dataset has no description
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Abundance of diatom cells in sediments from the Okhotsk and Bering Seas and t...
The present investigation was targeted at diatom composition studies in the surface sediments (0-1 cm) sampled in the Sea of Okhotsk and the northwest Pacific in the depth range... -
(Table 5) Chemical composition of Holocene siliceous sediments from the Sea o...
This dataset has no description
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(Table 4) Chemical composition of bottom sediments from the Sea of Okhotsk
This dataset has no description
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(Table 3) Mineral composition of clay fraction from bottom sediments of the S...
0 = traces; + = kaolinite is inferred from resolution of reflection doublets of chlorite (004) and kaolinite (002) in diffractograms; empty digital cells = questionable data. -
(Table 2) Physical properties of Holocene and Upper Pleistocene bottom sedime...
This dataset has no description
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(Table 1) Sedimentation rates and accumulation rates of Upper Pleistocene and...
This dataset has no description
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(Table 2) Average sedimentation and accumulation rates of Sea of Okhotsk bott...
This dataset has no description
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(Table 1) Manganese contents in sediment cores and in the upper reduced sedim...
This dataset has no description
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Ages of sediments from Core MG34-89211, northern shelf of the Sea of Okhotsk
The combined micropaleontological (spores and pollen, diatoms, benthic foraminifers), lithologic, and isotopic-geochemical analysis of sediments from the northern shelf of the... -
Physical properties, mineral and chemical compositions, and accumulation rate...
Mineral and chemical compositions and physical properties of diatomaceous clayey-siliceous sediments from the Sea of Okhotsk are studied. Accumulation rates of silica are... -
Manganese contents and accumulation rates in reduced bottom sediments of the ...
Manganese contents in reduced sediments and accumulation rates were investigated. Their values in sediments of most of cores are background (0.03-0.07 %).Anomalous...
