-
(Table 1) Concentration of dissolved organic carbon at Station Nesmeyanov-93_...
This dataset has no description
-
(Table 33) Chemical composition of Fe-Mn nodules and crusts from the West Pac...
Analyses have been carried out by S.P. Slavkina, V. Bakilina, V.V. Kovalenko, and A.I. Grigoriev. -
Data on mineral composition of volcanic glass and radiocarbon age of Upper Qu...
Lithological horizons have been distinguished in sediments cores from different parts of the Sea of Okhotsk based on primary descriptions of sediments and smear slides, and... -
Chemical and isotopic compositions of authigenic carbonates from bottom sedim...
The paper presents data on authigenic carbonate distribution in Holocene - Upper Pleistocene deposits of the Okhotsk, Japan, East China, Philippine and South China Seas.... -
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... -
Chemical composition of phosphorites, Fe-Mn nodules and crusts, and basalts f...
The monograph gives the first systematic description of ore-bearing guyots from the West Pacific. It is mostly based on data obtained in numerous expeditions of Russian vessels... -
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... -
Properties, sedimentation and accumulation rates, and chemical composition of...
Results of a study of contents and accumulation rates of Fe, Mn, and some trace elements in Upper Quaternary sediments of the Deryugin Basin are presented. Maps of average... -
Isotope compositions and mineralogy of carbonates and barites from sediments ...
Results of studies of mineralogy, geochemistry, and isotope parameters (d13C, d34S, d180, and 87Sr/86Sr) of carbonates and barites from sediments of the Deryugin Basin in the... -
Chemical and isotopic compositions of authigenic carbonates from the area of ...
Features of sedimentation of carbonate mineral associations in the northeastern shelf of Sakhalin and other regions of the Sea of Okhotsk are considered. Special attention is... -
Activity of ETS enzymes and phosphatase in the Sea of Okhotsk and Kuril regio...
An estimate of rate of transformation of organic matter and regeneration of nutrients (in particular phosphorus) was calculated for different regions of the Sea of Okhotsk. The... -
Dissolved organic carbon in waters of the Okhotsk and Bering Seas
A comparison was made of capability of two methods: photochemical oxidation and high-temperature catalytic combustion - to oxidize organic carbon in organic substances different... -
Dissolved and particulate organic carbon in the Sea of Okhotsk
Data on distribution of dissolved and particulate organic matter obtained during Cruises 21 and 24 of R/V Akademik A. Nesmeyanov in June-August 1992 and 1993 are presented. In... -
Hydrochemical Atlas of the Sea of Okhotsk 2001, International Ocean Atlas Ser...
Presented is a spatial distribution of Temperature, Salinity, Oxygen, Nitrate, Ammonia Nitrogen, Organic Nitrogen, Phosphate, Organic Phosphate, and Silicate data from the Sea... -
Hydrochemistry measured on water bottle samples during Akademik A Nesmeyanov ...
For definition of quality flags see hdl:10013/epic.31518.d001 -
Meteorological observations during AKADEMIK A NESMEYANOV cruise 90BM9316_1
This dataset has no description
-
Physical oceanography during Akademik A Nesmeyanov cruise in 1982
This dataset has no description
-
Physical oceanography during Akademik A Nesmeyanov cruise 90BM9316_1 on secti...
For definition of quality flags see hdl:10013/epic.31518.d001 -
(Table 4) Chemical composition of bottom sediments from the Sea of Okhotsk
This dataset has no description
-
(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.