Dataset - B2FIND

Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 fo...

Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 of those five species modeled by PLAFOM, i.e., N. pachyderma, N. incompta, G. bulloides, G. ruber...

(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 1) Contents and composition of n-alkanes in bottom sediments of the No...

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(Table 1) n-Alkanes in bottom sediments of the West European Basin (area of t...

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(Table 1) Contents and molecular composition of n-alkanes in bottom sediments...

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(Table 3) Relative content of n-alkane groups in samples from hydrothermal fi...

Optimum conditions were selected for chromatographic separation of model mixtures of C12-C40 n-alkanes. For one of samples of hydrothermal deposits extraction conditions of...

(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 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...