Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx

We present the first study which directly compares carbonate radiocarbon ( 14 C) dates with the Ramped PyrOx (RP) radiocarbon dating technique within a single sediment core, and we confirm the utility for the latter constructing chronologies of high latitude, Holocene marine margin sediment successi...

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Published in:The Holocene
Main Authors: Subt, Cristina, Fangman, Kimberly A, Wellner, Julia S, Rosenheim, Brad E
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2015
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683615608688
http://journals.sagepub.com/doi/pdf/10.1177/0959683615608688
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spelling crsagepubl:10.1177/0959683615608688 2024-06-23T07:47:49+00:00 Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx Subt, Cristina Fangman, Kimberly A Wellner, Julia S Rosenheim, Brad E 2015 http://dx.doi.org/10.1177/0959683615608688 http://journals.sagepub.com/doi/pdf/10.1177/0959683615608688 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615608688 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 26, issue 2, page 265-273 ISSN 0959-6836 1477-0911 journal-article 2015 crsagepubl https://doi.org/10.1177/0959683615608688 2024-06-04T06:28:17Z We present the first study which directly compares carbonate radiocarbon ( 14 C) dates with the Ramped PyrOx (RP) radiocarbon dating technique within a single sediment core, and we confirm the utility for the latter constructing chronologies of high latitude, Holocene marine margin sediment successions. Historically, the heavily detrital nature of Antarctic margin sedimentary organic material and lack of carbonate preservation have made these sediments difficult to date accurately. Here, we use archived cores with existing foraminiferal ages to compare with RP dates at equal or similar depth intervals. The lowest temperature RP splits were integrated over narrower intervals than in previous studies to reduce the amount of mixing with older, more thermochemically stable end-members during pyrolytic decomposition. Ages of the low-temperature RP splits coincide with their corresponding carbonate counterparts, suggesting that the RP 14 C dating method is a reliable alternative to carbonate dates in sediments where carbonates are absent or not sufficiently preserved for 14 C dating. The rarity of calcareous material in most Antarctic sediments often obligates the use of the bulk acid insoluble organic (AIO) fraction of the sediment, which can be problematic because of contamination by older carbon. The bulk AIO 14 C ages, which are calculated using the weighted arithmetic mean of all RP splits of individual samples, show that age reversals and biases can occur using bulk AIO dates for age models because of variable proportions of pre-aged organic matter down-core. The application of the RP dating method can reduce these effects to produce a more reliable chronology that is statistically identical to the foraminiferal dating chronology. Article in Journal/Newspaper Antarc* Antarctic SAGE Publications Antarctic The Holocene 26 2 265 273
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
description We present the first study which directly compares carbonate radiocarbon ( 14 C) dates with the Ramped PyrOx (RP) radiocarbon dating technique within a single sediment core, and we confirm the utility for the latter constructing chronologies of high latitude, Holocene marine margin sediment successions. Historically, the heavily detrital nature of Antarctic margin sedimentary organic material and lack of carbonate preservation have made these sediments difficult to date accurately. Here, we use archived cores with existing foraminiferal ages to compare with RP dates at equal or similar depth intervals. The lowest temperature RP splits were integrated over narrower intervals than in previous studies to reduce the amount of mixing with older, more thermochemically stable end-members during pyrolytic decomposition. Ages of the low-temperature RP splits coincide with their corresponding carbonate counterparts, suggesting that the RP 14 C dating method is a reliable alternative to carbonate dates in sediments where carbonates are absent or not sufficiently preserved for 14 C dating. The rarity of calcareous material in most Antarctic sediments often obligates the use of the bulk acid insoluble organic (AIO) fraction of the sediment, which can be problematic because of contamination by older carbon. The bulk AIO 14 C ages, which are calculated using the weighted arithmetic mean of all RP splits of individual samples, show that age reversals and biases can occur using bulk AIO dates for age models because of variable proportions of pre-aged organic matter down-core. The application of the RP dating method can reduce these effects to produce a more reliable chronology that is statistically identical to the foraminiferal dating chronology.
format Article in Journal/Newspaper
author Subt, Cristina
Fangman, Kimberly A
Wellner, Julia S
Rosenheim, Brad E
spellingShingle Subt, Cristina
Fangman, Kimberly A
Wellner, Julia S
Rosenheim, Brad E
Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
author_facet Subt, Cristina
Fangman, Kimberly A
Wellner, Julia S
Rosenheim, Brad E
author_sort Subt, Cristina
title Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
title_short Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
title_full Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
title_fullStr Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
title_full_unstemmed Sediment chronology in Antarctic deglacial sediments: Reconciling organic carbon 14 C ages to carbonate 14 C ages using Ramped PyrOx
title_sort sediment chronology in antarctic deglacial sediments: reconciling organic carbon 14 c ages to carbonate 14 c ages using ramped pyrox
publisher SAGE Publications
publishDate 2015
url http://dx.doi.org/10.1177/0959683615608688
http://journals.sagepub.com/doi/pdf/10.1177/0959683615608688
http://journals.sagepub.com/doi/full-xml/10.1177/0959683615608688
geographic Antarctic
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op_source The Holocene
volume 26, issue 2, page 265-273
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0959683615608688
container_title The Holocene
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