(Table 11-2) Values of dark carbon dioxide assimilation in supra bottom water and surface layer sediments of the Kara Sea along the section from the Yamal Peninsula to the Novaya Zemlya in September 2007
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...
Main Authors: | , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA - Data Publisher for Earth & Environmental Science
2012
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.785611 https://doi.pangaea.de/10.1594/PANGAEA.785611 |
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. |
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