Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps
International audience A C$_{25}$ highly branched isoprenoid (HBI) monoene hydrocarbon, designated IP$_{25}$, has been proposed previously to originate from diatoms living in Arctic sea ice, while the presence of IP25 in sediments has been suggested to be a proxy for the occurrence of former Arctic...
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Format: | Article in Journal/Newspaper |
Language: | English |
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ftuniversailles:oai:HAL:hal-03192517v1 2023-07-30T03:59:57+02:00 Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps Belt, Simon Massé, Guillaume Vare, Lindsay Rowland, Steven Poulin, Michel Sicre, Marie-Alexandrine Sampei, Makoto Fortier, Louis School of Geography, Earth and Environmental Sciences Plymouth (SoGEES) Plymouth University Canadian Museum of Nature (CANADA) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Paléocéanographie (PALEOCEAN) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Université Laval Québec (ULaval) 2008 https://hal.science/hal-03192517 https://hal.science/hal-03192517/document https://hal.science/hal-03192517/file/Arctic%20HBI%20isotopes%20SB%20revised.pdf https://doi.org/10.1016/j.marchem.2008.09.002 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marchem.2008.09.002 hal-03192517 https://hal.science/hal-03192517 https://hal.science/hal-03192517/document https://hal.science/hal-03192517/file/Arctic%20HBI%20isotopes%20SB%20revised.pdf doi:10.1016/j.marchem.2008.09.002 info:eu-repo/semantics/OpenAccess ISSN: 0304-4203 Marine Chemistry https://hal.science/hal-03192517 Marine Chemistry, 2008, 112 (3-4), pp.158-167. ⟨10.1016/j.marchem.2008.09.002⟩ https://www.sciencedirect.com/science/article/pii/S0304420308001473 Arctic Isotopes Biomarker IP$_{25}$ δ$^{13}$C Sea ice Sediment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2008 ftuniversailles https://doi.org/10.1016/j.marchem.2008.09.002 2023-07-16T20:23:58Z International audience A C$_{25}$ highly branched isoprenoid (HBI) monoene hydrocarbon, designated IP$_{25}$, has been proposed previously to originate from diatoms living in Arctic sea ice, while the presence of IP25 in sediments has been suggested to be a proxy for the occurrence of former Arctic sea ice. Here, we show that the $^{13}$C isotopic composition of IP$_{25}$ in sea ice, in sediment trap material collected under sea ice, and in high latitude northern sediments, is distinctive (isotopically ‘heavy’) and distinguishable from that of organic matter of planktonic or terrigenous origin. Mean δ$^{13}$C values for IP$_{25}$ were − 22.3 ± 0.4‰ (sea ice), − 19.6 ± 1.1‰ (sediment traps) and − 19.3 ± 2.3‰ (sediments). These measurements, therefore, support further the proposed use of IP$_{25}$ as an Arctic sea ice proxy. Article in Journal/Newspaper Arctic Arctic Sea ice Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Arctic Marine Chemistry 112 3-4 158 167 |
institution |
Open Polar |
collection |
Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ |
op_collection_id |
ftuniversailles |
language |
English |
topic |
Arctic Isotopes Biomarker IP$_{25}$ δ$^{13}$C Sea ice Sediment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
spellingShingle |
Arctic Isotopes Biomarker IP$_{25}$ δ$^{13}$C Sea ice Sediment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Belt, Simon Massé, Guillaume Vare, Lindsay Rowland, Steven Poulin, Michel Sicre, Marie-Alexandrine Sampei, Makoto Fortier, Louis Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
topic_facet |
Arctic Isotopes Biomarker IP$_{25}$ δ$^{13}$C Sea ice Sediment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience A C$_{25}$ highly branched isoprenoid (HBI) monoene hydrocarbon, designated IP$_{25}$, has been proposed previously to originate from diatoms living in Arctic sea ice, while the presence of IP25 in sediments has been suggested to be a proxy for the occurrence of former Arctic sea ice. Here, we show that the $^{13}$C isotopic composition of IP$_{25}$ in sea ice, in sediment trap material collected under sea ice, and in high latitude northern sediments, is distinctive (isotopically ‘heavy’) and distinguishable from that of organic matter of planktonic or terrigenous origin. Mean δ$^{13}$C values for IP$_{25}$ were − 22.3 ± 0.4‰ (sea ice), − 19.6 ± 1.1‰ (sediment traps) and − 19.3 ± 2.3‰ (sediments). These measurements, therefore, support further the proposed use of IP$_{25}$ as an Arctic sea ice proxy. |
author2 |
School of Geography, Earth and Environmental Sciences Plymouth (SoGEES) Plymouth University Canadian Museum of Nature (CANADA) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Paléocéanographie (PALEOCEAN) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Université Laval Québec (ULaval) |
format |
Article in Journal/Newspaper |
author |
Belt, Simon Massé, Guillaume Vare, Lindsay Rowland, Steven Poulin, Michel Sicre, Marie-Alexandrine Sampei, Makoto Fortier, Louis |
author_facet |
Belt, Simon Massé, Guillaume Vare, Lindsay Rowland, Steven Poulin, Michel Sicre, Marie-Alexandrine Sampei, Makoto Fortier, Louis |
author_sort |
Belt, Simon |
title |
Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
title_short |
Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
title_full |
Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
title_fullStr |
Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
title_full_unstemmed |
Distinctive $^{13}$C isotopic signature distinguishes a novel sea ice biomarker in Arctic sediments and sediment traps |
title_sort |
distinctive $^{13}$c isotopic signature distinguishes a novel sea ice biomarker in arctic sediments and sediment traps |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://hal.science/hal-03192517 https://hal.science/hal-03192517/document https://hal.science/hal-03192517/file/Arctic%20HBI%20isotopes%20SB%20revised.pdf https://doi.org/10.1016/j.marchem.2008.09.002 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Arctic Sea ice |
genre_facet |
Arctic Arctic Sea ice |
op_source |
ISSN: 0304-4203 Marine Chemistry https://hal.science/hal-03192517 Marine Chemistry, 2008, 112 (3-4), pp.158-167. ⟨10.1016/j.marchem.2008.09.002⟩ https://www.sciencedirect.com/science/article/pii/S0304420308001473 |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marchem.2008.09.002 hal-03192517 https://hal.science/hal-03192517 https://hal.science/hal-03192517/document https://hal.science/hal-03192517/file/Arctic%20HBI%20isotopes%20SB%20revised.pdf doi:10.1016/j.marchem.2008.09.002 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.marchem.2008.09.002 |
container_title |
Marine Chemistry |
container_volume |
112 |
container_issue |
3-4 |
container_start_page |
158 |
op_container_end_page |
167 |
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1772810642968805376 |