Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF

Based on the CSRD obtained by AMS the contribution of fossil OC (F14C=0; [%]) used for bacterial membrane lipid synthesis (IPL-FA) was calculated using an isotope mass balance. For the estimation two endmembers were used: 1) Fossil carbon (F14C=0) – OC derived from the local bedrock 2) Recently synt...

Full description

Bibliographic Details
Main Authors: Ruben, Manuel Jannis, Hefter, Jens, Schubotz, Florence, Geibert, Walter, Butzin, Martin, Gentz, Torben, Grotheer, Hendrik, Forwick, Matthias, Szczuciński, Witold, Mollenhauer, Gesine
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Ancient carbon
arctic fjord
Carbon
organic
fraction
standard error
Carbon cycle
compound specific radiocarbon dating
Depth
bottom/max
sediment/rock
top/min
GC
Gravity corer
HH14-897-GC-MF
Hornsund
Spitsbergen
Intact polar lipids
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.946018
https://doi.org/10.1594/PANGAEA.946018
Description
Summary:Based on the CSRD obtained by AMS the contribution of fossil OC (F14C=0; [%]) used for bacterial membrane lipid synthesis (IPL-FA) was calculated using an isotope mass balance. For the estimation two endmembers were used: 1) Fossil carbon (F14C=0) – OC derived from the local bedrock 2) Recently synthesized carbon (F14C~1) – OC derived from primary production in the water column. Detailed F14C-values were taken from surface DIC age model, depending on the year of sediment deposition (based on Pb+Cs age model).

Similar Items