(Table 8) Isotopic composition of organic carbon in suspended matter and percentage of newly formed organic carbon in total organic carbon content in the fluffy layer of the Dvina Bay, White Sea in July 2010 ...

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 mil); i¡ is d13C-Corg in suspended matter of the surface water layer x is percentage of newly formed Corg in total Corg...

Full description

Bibliographic Details
Main Authors: Lein, Alla Yu, Kravchishina, Marina D, Politova, Nadezhda V, Savvichev, Alexander S, Veslopolova, E F, Mitskevich, Irina N, Ul'yanova, Nina V, Shevchenko, Vladimir P, Ivanov, Mikhail V
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Event label
Latitude of event
Longitude of event
Elevation of event
δ13C, particulate organic carbon
Percentage
Multiple investigations
Mass spectrometry
Calculated
Archive of Ocean Data ARCOD
White Sea
dvina
Dvina Bay
Online Access:https://dx.doi.org/10.1594/pangaea.785605
https://doi.pangaea.de/10.1594/PANGAEA.785605
Description
Summary: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 mil); i¡ is d13C-Corg in suspended matter of the surface water layer x is percentage of newly formed Corg in total Corg content in the fluffy layer. ...

Similar Items