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...

Full description

Bibliographic Details
Main Authors: Via, Rachael K, Thomas, Deborah J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2006
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.724682
https://doi.pangaea.de/10.1594/PANGAEA.724682
id ftdatacite:10.1594/pangaea.724682
record_format openpolar
spelling ftdatacite:10.1594/pangaea.724682 2024-09-15T18:20:42+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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg208
Joides Resolution
Ocean Drilling Program ODP
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 ...
topic_facet Drilling/drill rig
Leg208
Joides Resolution
Ocean Drilling Program ODP
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
author Via, Rachael K
Thomas, Deborah J
author_facet Via, Rachael K
Thomas, Deborah J
author_sort Via, Rachael K
title Nd isotope data for ODP Leg 208 holes ...
title_short 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_sort nd isotope data for odp leg 208 holes ...
publisher PANGAEA
publishDate 2006
url https://dx.doi.org/10.1594/pangaea.724682
https://doi.pangaea.de/10.1594/PANGAEA.724682
genre North Atlantic Deep Water
North Atlantic
Southern Ocean
genre_facet North Atlantic Deep Water
North Atlantic
Southern Ocean
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
op_doi https://doi.org/10.1594/pangaea.72468210.1130/g22545.1
_version_ 1810459092891729920