(Table 7) Isotopic composition of organic carbon and percentage of newly formed organic carbon in total organic carbon content in surface layer bottom sediments of the White Sea in August 2006 ...

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 d13C-Corg in suspended matter (-29 per mil); x is percentage of newly formed Corg in total i¡org in the layer 0-0.5 cm. ...

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
Date/Time of event
Area/locality
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
δ13C, particulate organic carbon
Percentage
Multiple investigations
Mass spectrometry
Calculated
PSh80
Professor Shtokman
Archive of Ocean Data ARCOD
White Sea
Online Access:https://dx.doi.org/10.1594/pangaea.785603
https://doi.pangaea.de/10.1594/PANGAEA.785603
Description
Summary: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 d13C-Corg in suspended matter (-29 per mil); x is percentage of newly formed Corg in total i¡org in the layer 0-0.5 cm. ...

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