A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient
The fact that the deep-ocean benthic δ 13 C minimum shifted from the North Pacific to the South Atlantic during the Last Glacial Maximum is often interpretted as evidence of a change in deep water circulation, such as the development of deep water ventilation in the North Pacific or a decrease in So...
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ftdoajarticles:oai:doaj.org/article:3aa8fab1509946ff88a292627d4eeb32 2023-05-15T18:25:34+02:00 A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient L. E. Lisiecki 2010-05-01T00:00:00Z https://doi.org/10.5194/cp-6-305-2010 https://doaj.org/article/3aa8fab1509946ff88a292627d4eeb32 EN eng Copernicus Publications http://www.clim-past.net/6/305/2010/cp-6-305-2010.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-6-305-2010 1814-9324 1814-9332 https://doaj.org/article/3aa8fab1509946ff88a292627d4eeb32 Climate of the Past, Vol 6, Iss 3, Pp 305-314 (2010) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2010 ftdoajarticles https://doi.org/10.5194/cp-6-305-2010 2022-12-31T04:48:28Z The fact that the deep-ocean benthic δ 13 C minimum shifted from the North Pacific to the South Atlantic during the Last Glacial Maximum is often interpretted as evidence of a change in deep water circulation, such as the development of deep water ventilation in the North Pacific or a decrease in Southern Ocean overturning. This study re-evaluates the implications of changes in benthic δ 13 C gradients by comparing Pacific Deep Water (PDW) δ 13 C measurements with the values expected for the null hypothesis that PDW ventilation sources remained unchanged throughout the Late Pleistocene. The δ 13 C compositions of PDW, Northern Component Water (NCW) and Southern Component Water (SCW) are estimated from regional benthic δ 13 C stacks of 3–6 sites. Changes in PDW δ 13 C and PDW-SCW δ 13 C gradients over the past 800 kyr are found to be well described by a constant mixture of 60% NCW and 40% SCW plus a constant Pacific remineralization offset of −0.5‰. Thus, a change in PDW ventilation cannot be inferred solely on the basis of changes in the Pacific-South Atlantic benthic δ 13 C gradient. Article in Journal/Newspaper Southern Ocean Directory of Open Access Journals: DOAJ Articles Southern Ocean Pacific Climate of the Past 6 3 305 314 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
spellingShingle |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 L. E. Lisiecki A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
topic_facet |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
description |
The fact that the deep-ocean benthic δ 13 C minimum shifted from the North Pacific to the South Atlantic during the Last Glacial Maximum is often interpretted as evidence of a change in deep water circulation, such as the development of deep water ventilation in the North Pacific or a decrease in Southern Ocean overturning. This study re-evaluates the implications of changes in benthic δ 13 C gradients by comparing Pacific Deep Water (PDW) δ 13 C measurements with the values expected for the null hypothesis that PDW ventilation sources remained unchanged throughout the Late Pleistocene. The δ 13 C compositions of PDW, Northern Component Water (NCW) and Southern Component Water (SCW) are estimated from regional benthic δ 13 C stacks of 3–6 sites. Changes in PDW δ 13 C and PDW-SCW δ 13 C gradients over the past 800 kyr are found to be well described by a constant mixture of 60% NCW and 40% SCW plus a constant Pacific remineralization offset of −0.5‰. Thus, a change in PDW ventilation cannot be inferred solely on the basis of changes in the Pacific-South Atlantic benthic δ 13 C gradient. |
format |
Article in Journal/Newspaper |
author |
L. E. Lisiecki |
author_facet |
L. E. Lisiecki |
author_sort |
L. E. Lisiecki |
title |
A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
title_short |
A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
title_full |
A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
title_fullStr |
A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
title_full_unstemmed |
A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ 13 C gradient |
title_sort |
simple mixing explanation for late pleistocene changes in the pacific-south atlantic benthic δ 13 c gradient |
publisher |
Copernicus Publications |
publishDate |
2010 |
url |
https://doi.org/10.5194/cp-6-305-2010 https://doaj.org/article/3aa8fab1509946ff88a292627d4eeb32 |
geographic |
Southern Ocean Pacific |
geographic_facet |
Southern Ocean Pacific |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
Climate of the Past, Vol 6, Iss 3, Pp 305-314 (2010) |
op_relation |
http://www.clim-past.net/6/305/2010/cp-6-305-2010.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-6-305-2010 1814-9324 1814-9332 https://doaj.org/article/3aa8fab1509946ff88a292627d4eeb32 |
op_doi |
https://doi.org/10.5194/cp-6-305-2010 |
container_title |
Climate of the Past |
container_volume |
6 |
container_issue |
3 |
container_start_page |
305 |
op_container_end_page |
314 |
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1766207124816265216 |