Nd isotope data for ODP Leg 208 holes ...
The flow of deep-water masses is a key component of heat transport in the modern climate system, yet the role of deep-ocean heat transport during periods of extreme warmth is poorly understood. The present mode of meridional overturning circulation is characterized by deep-water formation in both th...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2006
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.724682 https://doi.pangaea.de/10.1594/PANGAEA.724682 |
_version_ | 1821634643647004672 |
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author | Via, Rachael K Thomas, Deborah J |
author_facet | Via, Rachael K Thomas, Deborah J |
author_sort | Via, Rachael K |
collection | DataCite |
description | The flow of deep-water masses is a key component of heat transport in the modern climate system, yet the role of deep-ocean heat transport during periods of extreme warmth is poorly understood. The present mode of meridional overturning circulation is characterized by deep-water formation in both the North Atlantic and the Southern Ocean. However, a different mode of meridional overturning circulation operated during the extreme greenhouse warmth of the early Cenozoic, during which time the Southern Ocean was the dominant region of deep-water formation. The combination of general global cooling and tectonic evolution of the Atlantic basins over the past ~55 m.y. ultimately led to the development of a mode of overturning circulation characterized by both Southern Ocean and North Atlantic deep-water sources. The change in deep-water circulation mode may, in turn, have affected global climate; however, unraveling the causes and consequences of this transition requires a better understanding of the timing of the ... : Supplement to: Via, Rachael K; Thomas, Deborah J (2006): Evolution of Atlantic thermohaline circulation: Early Oligocene onset of deep-water production in the North Atlantic. Geology 2006, 34(6), 441-444 ... |
format | Article in Journal/Newspaper |
genre | North Atlantic Deep Water North Atlantic Southern Ocean |
genre_facet | North Atlantic Deep Water North Atlantic Southern Ocean |
geographic | Southern Ocean |
geographic_facet | Southern Ocean |
id | ftdatacite:10.1594/pangaea.724682 |
institution | Open Polar |
language | English |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.1594/pangaea.72468210.1130/g22545.1 |
op_relation | ftp://rock.geosociety.org/pub/reposit/2006/2006087.pdf https://dx.doi.org/10.1130/g22545.1 ftp://rock.geosociety.org/pub/reposit/2006/2006087.pdf |
op_rights | Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
publishDate | 2006 |
publisher | PANGAEA |
record_format | openpolar |
spelling | ftdatacite:10.1594/pangaea.724682 2025-01-16T23:29:17+00:00 Nd isotope data for ODP Leg 208 holes ... Via, Rachael K Thomas, Deborah J 2006 application/zip https://dx.doi.org/10.1594/pangaea.724682 https://doi.pangaea.de/10.1594/PANGAEA.724682 en eng PANGAEA ftp://rock.geosociety.org/pub/reposit/2006/2006087.pdf https://dx.doi.org/10.1130/g22545.1 ftp://rock.geosociety.org/pub/reposit/2006/2006087.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg208 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2006 ftdatacite https://doi.org/10.1594/pangaea.72468210.1130/g22545.1 2024-08-01T10:50:04Z The flow of deep-water masses is a key component of heat transport in the modern climate system, yet the role of deep-ocean heat transport during periods of extreme warmth is poorly understood. The present mode of meridional overturning circulation is characterized by deep-water formation in both the North Atlantic and the Southern Ocean. However, a different mode of meridional overturning circulation operated during the extreme greenhouse warmth of the early Cenozoic, during which time the Southern Ocean was the dominant region of deep-water formation. The combination of general global cooling and tectonic evolution of the Atlantic basins over the past ~55 m.y. ultimately led to the development of a mode of overturning circulation characterized by both Southern Ocean and North Atlantic deep-water sources. The change in deep-water circulation mode may, in turn, have affected global climate; however, unraveling the causes and consequences of this transition requires a better understanding of the timing of the ... : Supplement to: Via, Rachael K; Thomas, Deborah J (2006): Evolution of Atlantic thermohaline circulation: Early Oligocene onset of deep-water production in the North Atlantic. Geology 2006, 34(6), 441-444 ... Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Southern Ocean DataCite Southern Ocean |
spellingShingle | Drilling/drill rig Leg208 Joides Resolution Ocean Drilling Program ODP Via, Rachael K Thomas, Deborah J Nd isotope data for ODP Leg 208 holes ... |
title | Nd isotope data for ODP Leg 208 holes ... |
title_full | Nd isotope data for ODP Leg 208 holes ... |
title_fullStr | Nd isotope data for ODP Leg 208 holes ... |
title_full_unstemmed | Nd isotope data for ODP Leg 208 holes ... |
title_short | Nd isotope data for ODP Leg 208 holes ... |
title_sort | nd isotope data for odp leg 208 holes ... |
topic | Drilling/drill rig Leg208 Joides Resolution Ocean Drilling Program ODP |
topic_facet | Drilling/drill rig Leg208 Joides Resolution Ocean Drilling Program ODP |
url | https://dx.doi.org/10.1594/pangaea.724682 https://doi.pangaea.de/10.1594/PANGAEA.724682 |