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(Table 40-4) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-3) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-2) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 40-1) Speciations of chemical elements in bottom sediments from Core A...
Fractions of element occurrences: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic... -
(Table 38) Manganese fluxes in the upper sediment layer
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(Table 4) Molecular composition and concentration of hydrocarbons in hydrothe...
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(Table 1) Brief description, main minerals, and hydrocarbon and n-alkane cont...
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(Table 16-2) Distribution of δ¹³C-Corg in surface layer bottom sediments from...
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(Table 16-1) Distribution of δ¹³C-Corg in suspended matter from the surface a...
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(Table 13) Isotopic composition of organic carbon in surface layer bottom sed...
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(Table 11-2) Values of dark carbon dioxide assimilation in supra bottom water...
Calculations were made according to the isotope mass balance equation: 100A=Bx+(100-x)C, where A is d13C-Corg of sediment; i' is d13C-Corg of microorganism biomass (-20.0 per... -
(Table 11-1) Values of dark carbon dioxide assimilation in supra bottom water...
Calculations were made according to the isotope mass balance equation: 100A=Bx+(100-x)C, where A is d13C-Corg of sediment; i' is d13C-Corg of microorganism biomass (-20.0 per... -
(Table 10-2) Parameters of the water column in the Kara Sea along the section...
Calculations were made according to the isotope mass balance equation: 100A=Bx+(100-x)C, where A is d13C-Corg of sediment; i' is d13C-Corg of microorganism biomass (-20.0 per... -
(Table 10-1) Parameters of the water column in the Kara Sea along the section...
Calculations were made according to the isotope mass balance equation: 100A=Bx+(100-x)C, where A is d13C-Corg of sediment; i' is d13C-Corg of microorganism biomass (-20.0 per... -
(Table 5) Concentration of methane, rates of its formation and oxidation, as ...
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(Table 5) Average chemical and isotopic compositions of waters from the calde...
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(Table 4) Radiocarbon datings of the authigenic carbonate buildup from Site A...
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(Table 3) Isotopic composition of oxygen and hydrogen in seawater, interstiti...
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(Table 1) Chemical composition of carbonate bodies from the caldera of the Ha...
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(Table 51-2) Concentrations of nutrients in interstitial waters from bottom s...
This dataset has no description