Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials

How deep ocean circulation is linked to changes in atmospheric CO2 concentration remains uncertain. Here, the authors show that deep equatorial Atlantic Ocean water mass provenance was similar throughout all interglacials of the past 800 kyr, despite variable interglacial atmospheric CO2 concentrati...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Jacob N. W. Howe, Alexander M. Piotrowski
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
Materias:
Q
Acceso en línea:https://doaj.org/article/fe93879064484bafb48228ad55d3bc9a
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:fe93879064484bafb48228ad55d3bc9a
record_format dspace
spelling oai:doaj.org-article:fe93879064484bafb48228ad55d3bc9a2021-12-02T14:40:48ZAtlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials10.1038/s41467-017-01939-w2041-1723https://doaj.org/article/fe93879064484bafb48228ad55d3bc9a2017-12-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-01939-whttps://doaj.org/toc/2041-1723How deep ocean circulation is linked to changes in atmospheric CO2 concentration remains uncertain. Here, the authors show that deep equatorial Atlantic Ocean water mass provenance was similar throughout all interglacials of the past 800 kyr, despite variable interglacial atmospheric CO2 concentrations.Jacob N. W. HoweAlexander M. PiotrowskiNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-7 (2017)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Jacob N. W. Howe
Alexander M. Piotrowski
Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
description How deep ocean circulation is linked to changes in atmospheric CO2 concentration remains uncertain. Here, the authors show that deep equatorial Atlantic Ocean water mass provenance was similar throughout all interglacials of the past 800 kyr, despite variable interglacial atmospheric CO2 concentrations.
format article
author Jacob N. W. Howe
Alexander M. Piotrowski
author_facet Jacob N. W. Howe
Alexander M. Piotrowski
author_sort Jacob N. W. Howe
title Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
title_short Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
title_full Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
title_fullStr Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
title_full_unstemmed Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials
title_sort atlantic deep water provenance decoupled from atmospheric co2 concentration during the lukewarm interglacials
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/fe93879064484bafb48228ad55d3bc9a
work_keys_str_mv AT jacobnwhowe atlanticdeepwaterprovenancedecoupledfromatmosphericco2concentrationduringthelukewarminterglacials
AT alexandermpiotrowski atlanticdeepwaterprovenancedecoupledfromatmosphericco2concentrationduringthelukewarminterglacials
_version_ 1718390150224936960