Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.

We have measured the radiocarbon contents of individual, solvent-extractable, short-chain (C (sub 14) , C (sub 16) , and C (sub 18) ) fatty acids isolated from Ross Sea surface sediments. The corresponding (super 14) C ages are equivalent to that of the post-bomb dissolved inorganic carbon (DIC) res...

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Main Authors: Ohkouchi, Naohiko, Eglinton, Timothy I, Hayes, John M
Format: Article in Journal/Newspaper
Language:English
Published: Radiocarbon 2003
Subjects:
Online Access:https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155
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spelling ftunivarizonaojs:oai:journals.uair.arizona.edu:article/4155 2023-05-15T14:02:46+02:00 Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies. Ohkouchi, Naohiko Eglinton, Timothy I Hayes, John M 2003-01-01 application/pdf https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155 eng eng Radiocarbon https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155/3580 https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155 Radiocarbon; Vol 45, No 1 (2003); 17-24 0033-8222 Ross Sea;Southern Ocean;fatty acids;marine sedimentation;Antarctica;inorganic materials;sedimentation;sedimentation rates;marine sediments;organic acids;Holocene;upper Holocene;organic compounds;sediments;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;absolute age info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 2003 ftunivarizonaojs 2020-11-14T17:53:01Z We have measured the radiocarbon contents of individual, solvent-extractable, short-chain (C (sub 14) , C (sub 16) , and C (sub 18) ) fatty acids isolated from Ross Sea surface sediments. The corresponding (super 14) C ages are equivalent to that of the post-bomb dissolved inorganic carbon (DIC) reservoir. Moreover, molecular (super 14) C variations in surficial (upper 15 cm) sediments indicate that these compounds may prove useful for reconstructing chronologies of Antarctic margin sediments containing uncertain (and potentially variable) quantities of relict organic carbon. A preliminary molecular (super 14) C chronology suggests that the accumulation rate of relict organic matter has not changed during the last 500 (super 14) C yr. The focus of this study is to determine the validity of compound-specific (super 14) C analysis as a technique for reconstructing chronologies of Antarctic margin sediments. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ross Sea Southern Ocean Journals at the University of Arizona Antarctic Ross Sea Southern Ocean
institution Open Polar
collection Journals at the University of Arizona
op_collection_id ftunivarizonaojs
language English
topic Ross Sea;Southern Ocean;fatty acids;marine sedimentation;Antarctica;inorganic materials;sedimentation;sedimentation rates;marine sediments;organic acids;Holocene;upper Holocene;organic compounds;sediments;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;absolute age
spellingShingle Ross Sea;Southern Ocean;fatty acids;marine sedimentation;Antarctica;inorganic materials;sedimentation;sedimentation rates;marine sediments;organic acids;Holocene;upper Holocene;organic compounds;sediments;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;absolute age
Ohkouchi, Naohiko
Eglinton, Timothy I
Hayes, John M
Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
topic_facet Ross Sea;Southern Ocean;fatty acids;marine sedimentation;Antarctica;inorganic materials;sedimentation;sedimentation rates;marine sediments;organic acids;Holocene;upper Holocene;organic compounds;sediments;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;absolute age
description We have measured the radiocarbon contents of individual, solvent-extractable, short-chain (C (sub 14) , C (sub 16) , and C (sub 18) ) fatty acids isolated from Ross Sea surface sediments. The corresponding (super 14) C ages are equivalent to that of the post-bomb dissolved inorganic carbon (DIC) reservoir. Moreover, molecular (super 14) C variations in surficial (upper 15 cm) sediments indicate that these compounds may prove useful for reconstructing chronologies of Antarctic margin sediments containing uncertain (and potentially variable) quantities of relict organic carbon. A preliminary molecular (super 14) C chronology suggests that the accumulation rate of relict organic matter has not changed during the last 500 (super 14) C yr. The focus of this study is to determine the validity of compound-specific (super 14) C analysis as a technique for reconstructing chronologies of Antarctic margin sediments.
format Article in Journal/Newspaper
author Ohkouchi, Naohiko
Eglinton, Timothy I
Hayes, John M
author_facet Ohkouchi, Naohiko
Eglinton, Timothy I
Hayes, John M
author_sort Ohkouchi, Naohiko
title Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
title_short Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
title_full Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
title_fullStr Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
title_full_unstemmed Radiocarbon dating of individual fatty acids as a tool for refining Antarctic margin sediment chronologies.
title_sort radiocarbon dating of individual fatty acids as a tool for refining antarctic margin sediment chronologies.
publisher Radiocarbon
publishDate 2003
url https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155
geographic Antarctic
Ross Sea
Southern Ocean
geographic_facet Antarctic
Ross Sea
Southern Ocean
genre Antarc*
Antarctic
Antarctica
Ross Sea
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
Ross Sea
Southern Ocean
op_source Radiocarbon; Vol 45, No 1 (2003); 17-24
0033-8222
op_relation https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155/3580
https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/4155
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