Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?

A new reconstruction of past atmospheric Δ14C (Δ14Catm) based on Polish lake varved sediments has suggested that previous Δ14Catm values (e.g. from the Cariaco basin record) for the beginning of the Younger Dryas cold event (YD) are overestimates and that the Δ14Catm rise at the YD onset could only...

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Published in:Earth and Planetary Science Letters
Main Authors: Marchal, Olivier, Stocker, Thomas F., Muscheler, Raimund
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2001
Subjects:
Online Access:https://boris.unibe.ch/158539/1/marchal01epsl.pdf
https://boris.unibe.ch/158539/
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spelling ftunivbern:oai:boris.unibe.ch:158539 2023-08-20T04:06:57+02:00 Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both? Marchal, Olivier Stocker, Thomas F. Muscheler, Raimund 2001 application/pdf https://boris.unibe.ch/158539/1/marchal01epsl.pdf https://boris.unibe.ch/158539/ eng eng Elsevier https://boris.unibe.ch/158539/ info:eu-repo/semantics/restrictedAccess Marchal, Olivier; Stocker, Thomas F.; Muscheler, Raimund (2001). Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both? Earth and planetary science letters, 185(3-4), pp. 383-395. Elsevier 10.1016/S0012-821X(00)00383-6 <http://dx.doi.org/10.1016/S0012-821X(00)00383-6> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2001 ftunivbern https://doi.org/10.1016/S0012-821X(00)00383-6 2023-07-31T22:08:11Z A new reconstruction of past atmospheric Δ14C (Δ14Catm) based on Polish lake varved sediments has suggested that previous Δ14Catm values (e.g. from the Cariaco basin record) for the beginning of the Younger Dryas cold event (YD) are overestimates and that the Δ14Catm rise at the YD onset could only be due to changes in atmospheric 14C production (PC-14). This result would have profound climatic implications, for the YD is a paradigm example of abrupt climate change which is usually thought to have been triggered by a reduction in the northward heat flux by the Atlantic thermohaline circulation. Here we examine results from a large number of simulations (300) based on a zonally averaged ocean circulation model, to constrain the effect on Δ14Catm of PC-14 changes during the YD as reconstructed from a Greenland ice core record of 10Be flux. Our results suggest that the scatter in the lake data set is too large to exclude the probable change in deep ocean ventilation at the onset of the YD. By contrast, the model fit to the higher Δ14Catm levels throughout the YD detected in the marine record is generally better when a substantial decrease in deep ocean ventilation is simulated. The early Δ14Catm drawdown that initiated during the first half of the YD, however, could entirely be due to production changes. If this was the case, the drawdown would not reflect an increasing formation of North Atlantic Intermediate Water or Southern Ocean water, as previously suggested. The rapid Δ14Catm rise at the YD onset documented in the marine record, however, remains unexplained. Article in Journal/Newspaper Greenland Greenland ice core ice core North Atlantic Southern Ocean BORIS (Bern Open Repository and Information System, University of Bern) Greenland Southern Ocean Earth and Planetary Science Letters 185 3-4 383 395
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Marchal, Olivier
Stocker, Thomas F.
Muscheler, Raimund
Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
topic_facet 530 Physics
description A new reconstruction of past atmospheric Δ14C (Δ14Catm) based on Polish lake varved sediments has suggested that previous Δ14Catm values (e.g. from the Cariaco basin record) for the beginning of the Younger Dryas cold event (YD) are overestimates and that the Δ14Catm rise at the YD onset could only be due to changes in atmospheric 14C production (PC-14). This result would have profound climatic implications, for the YD is a paradigm example of abrupt climate change which is usually thought to have been triggered by a reduction in the northward heat flux by the Atlantic thermohaline circulation. Here we examine results from a large number of simulations (300) based on a zonally averaged ocean circulation model, to constrain the effect on Δ14Catm of PC-14 changes during the YD as reconstructed from a Greenland ice core record of 10Be flux. Our results suggest that the scatter in the lake data set is too large to exclude the probable change in deep ocean ventilation at the onset of the YD. By contrast, the model fit to the higher Δ14Catm levels throughout the YD detected in the marine record is generally better when a substantial decrease in deep ocean ventilation is simulated. The early Δ14Catm drawdown that initiated during the first half of the YD, however, could entirely be due to production changes. If this was the case, the drawdown would not reflect an increasing formation of North Atlantic Intermediate Water or Southern Ocean water, as previously suggested. The rapid Δ14Catm rise at the YD onset documented in the marine record, however, remains unexplained.
format Article in Journal/Newspaper
author Marchal, Olivier
Stocker, Thomas F.
Muscheler, Raimund
author_facet Marchal, Olivier
Stocker, Thomas F.
Muscheler, Raimund
author_sort Marchal, Olivier
title Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
title_short Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
title_full Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
title_fullStr Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
title_full_unstemmed Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both?
title_sort atmospheric radiocarbon during the younger dryas: production, ventilation, or both?
publisher Elsevier
publishDate 2001
url https://boris.unibe.ch/158539/1/marchal01epsl.pdf
https://boris.unibe.ch/158539/
geographic Greenland
Southern Ocean
geographic_facet Greenland
Southern Ocean
genre Greenland
Greenland ice core
ice core
North Atlantic
Southern Ocean
genre_facet Greenland
Greenland ice core
ice core
North Atlantic
Southern Ocean
op_source Marchal, Olivier; Stocker, Thomas F.; Muscheler, Raimund (2001). Atmospheric radiocarbon during the Younger Dryas: production, ventilation, or both? Earth and planetary science letters, 185(3-4), pp. 383-395. Elsevier 10.1016/S0012-821X(00)00383-6 <http://dx.doi.org/10.1016/S0012-821X(00)00383-6>
op_relation https://boris.unibe.ch/158539/
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/S0012-821X(00)00383-6
container_title Earth and Planetary Science Letters
container_volume 185
container_issue 3-4
container_start_page 383
op_container_end_page 395
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