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...

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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:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.946018
https://doi.org/10.1594/PANGAEA.946018
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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
author_sort Ruben, Manuel Jannis
collection PANGAEA - Data Publisher for Earth & Environmental Science
description 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
genre Arctic
Hornsund
Spitsbergen
genre_facet Arctic
Hornsund
Spitsbergen
geographic Arctic
Hornsund
geographic_facet Arctic
Hornsund
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946018
institution Open Polar
language English
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
ENVELOPE(16.405220,16.405220,76.992580,76.992580)
op_collection_id ftpangaea
op_coverage LATITUDE: 76.992580 * LONGITUDE: 16.405220 * DATE/TIME START: 2014-10-18T00:00:00 * DATE/TIME END: 2014-10-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.015 m * MAXIMUM DEPTH, sediment/rock: 1.345 m
op_doi https://doi.org/10.1594/PANGAEA.94601810.1594/PANGAEA.946019
op_relation https://doi.org/10.1594/PANGAEA.946019
https://doi.pangaea.de/10.1594/PANGAEA.946018
https://doi.org/10.1594/PANGAEA.946018
op_rights CC0: Creative Commons Zero 1.0 Universal
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
publishDate 2022
publisher PANGAEA
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946018 2025-01-16T20:34:48+00:00 Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF Ruben, Manuel Jannis Hefter, Jens Schubotz, Florence Geibert, Walter Butzin, Martin Gentz, Torben Grotheer, Hendrik Forwick, Matthias Szczuciński, Witold Mollenhauer, Gesine LATITUDE: 76.992580 * LONGITUDE: 16.405220 * DATE/TIME START: 2014-10-18T00:00:00 * DATE/TIME END: 2014-10-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.015 m * MAXIMUM DEPTH, sediment/rock: 1.345 m 2022 text/tab-separated-values, 40 data points https://doi.pangaea.de/10.1594/PANGAEA.946018 https://doi.org/10.1594/PANGAEA.946018 en eng PANGAEA https://doi.org/10.1594/PANGAEA.946019 https://doi.pangaea.de/10.1594/PANGAEA.946018 https://doi.org/10.1594/PANGAEA.946018 CC0: Creative Commons Zero 1.0 Universal Access constraints: unrestricted info:eu-repo/semantics/openAccess 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 dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94601810.1594/PANGAEA.946019 2024-07-24T02:31:43Z 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). Dataset Arctic Hornsund Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science Arctic Hornsund ENVELOPE(15.865,15.865,76.979,76.979) ENVELOPE(16.405220,16.405220,76.992580,76.992580)
spellingShingle 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
Ruben, Manuel Jannis
Hefter, Jens
Schubotz, Florence
Geibert, Walter
Butzin, Martin
Gentz, Torben
Grotheer, Hendrik
Forwick, Matthias
Szczuciński, Witold
Mollenhauer, Gesine
Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title_full Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title_fullStr Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title_full_unstemmed Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title_short Petrogenic OC used for biosynthesis of sediment core HH14-897-GC-MF
title_sort petrogenic oc used for biosynthesis of sediment core hh14-897-gc-mf
topic 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
topic_facet 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
url https://doi.pangaea.de/10.1594/PANGAEA.946018
https://doi.org/10.1594/PANGAEA.946018