Petrogenic OC used for biosynthesis of sediment core HE519_2-3

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Hauptverfasser: Ruben, Manuel Jannis, Hefter, Jens, Schubotz, Florence, Geibert, Walter, Butzin, Martin, Gentz, Torben, Grotheer, Hendrik, Forwick, Matthias, Szczuciński, Witold, Mollenhauer, Gesine
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2022
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author Ruben, Manuel Jannis
Hefter, Jens
Schubotz, Florence
Geibert, Walter
Butzin, Martin
Gentz, Torben
Grotheer, Hendrik
Forwick, Matthias
Szczuciński, Witold
Mollenhauer, Gesine
author_facet Ruben, Manuel Jannis
Hefter, Jens
Schubotz, Florence
Geibert, Walter
Butzin, Martin
Gentz, Torben
Grotheer, Hendrik
Forwick, Matthias
Szczuciński, Witold
Mollenhauer, Gesine
collection Datos científicos de ciencias marinas y ambientales
contents 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).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_946016
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Petrogenic OC used for biosynthesis of sediment core HE519_2-3
Ruben, Manuel Jannis
Hefter, Jens
Schubotz, Florence
Geibert, Walter
Butzin, Martin
Gentz, Torben
Grotheer, Hendrik
Forwick, Matthias
Szczuciński, Witold
Mollenhauer, Gesine
Ancient carbon; arctic fjord; Carbon, organic, fraction; Carbon, organic, standard error; Carbon cycle; compound specific radiocarbon dating; DEPTH, sediment/rock; HE519; HE519_2-3; Heincke; Intact polar lipids; MUC; MultiCorer
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).
title Petrogenic OC used for biosynthesis of sediment core HE519_2-3
topic Ancient carbon; arctic fjord; Carbon, organic, fraction; Carbon, organic, standard error; Carbon cycle; compound specific radiocarbon dating; DEPTH, sediment/rock; HE519; HE519_2-3; Heincke; Intact polar lipids; MUC; MultiCorer
url https://doi.org/10.1594/PANGAEA.946016