(Table 10-2) Parameters of the water column in the Kara Sea along the section ftom 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...

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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 - Data Publisher for Earth & Environmental Science 2012
Subjects:
Event label
Latitude of event
Longitude of event
Elevation of event
Date/Time of event
DEPTH, water
Salinity
Suspended particulate matter
Microorganisms, abundance
Carbon dioxide dark assimilation rate
δ13C, particulate organic carbon
Multiple investigations
CTD, Neil Brown
Filtration
Counting
14C uptake
Mass spectrometry
AMK54
Akademik Mstislav Keldysh
Archive of Ocean Data ARCOD
Kara Sea
Yamal Peninsula
Novaya Zemlya
Online Access:https://dx.doi.org/10.1594/pangaea.785609
https://doi.pangaea.de/10.1594/PANGAEA.785609
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.

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