-
Seawater carbonate chemistry and processes during experiments with coccolitho...
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and... -
Seawater carbonate chemistry and processes during experiments with Emiliania ...
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and... -
Concentrations and carbon isotopic composition of suspended particulate matte...
Concentrations of particulate and dissolved organic carbon from water samples collected throughout the ice-free season in the Lena River Delta, supplemented with samples from... -
Stream chemistry of the Uhlirska catchment, Czech Republic
This dataset has no description
-
Groundwater chemistry of the Uhlirska catchment, Czech Republic
This dataset has no description
-
(Table 1b) Stable isotopes and PCB concentration in seawater and particulate ...
Samples are taken from the whole water column. 0 = below limit of detection. -
(Table 1) Properties of the bottom 30 cm of level sea ice and surface water o...
This dataset has no description
-
(Table 16-2) Distribution of δ¹³C-Corg in surface layer bottom sediments from...
This dataset has no description
-
(Table 16-1) Distribution of δ¹³C-Corg in suspended matter from the surface a...
This dataset has no description
-
(Table 15-2) Distribution of dark CO2 assimilation rate and δ¹³C-Corg values ...
This dataset has no description
-
(Table 15-1) Distribution of total population of microorganisms, dark CO2 ass...
This dataset has no description
-
(Table 13) Isotopic composition of organic carbon in surface layer bottom sed...
This dataset has no description
-
(Table 12) Distribution of total population of microorganisms, CO2 assimilati...
This dataset has no description
-
(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 8) Isotopic composition of organic carbon in suspended matter and perc...
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 7) Isotopic composition of organic carbon and percentage of newly form...
Calculations were made using the isotope mass balance: 100A=Bx+(100-x)C, where A is d13C-Corg of sediments; i' is d13C-Corg in microorganism biomass (-20 per mil); i¡ is... -
(Table 6) Characteristics of suspended matter, microbial mats, and surface se...
This dataset has no description