Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea

Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea

Phases of high bottom water temperature in the northwestern Barents Sea caused repeated destabilization of methane gas hydrates since the last glacial, according to a foraminifera Mg/Ca bottom water temperature record and hydrate stability modelling

Bibliographic Details
Main Authors: Naima El bani Altuna, Tine Lander Rasmussen, Mohamed Mahmoud Ezat, Sunil Vadakkepuliyambatta, Jeroen Groeneveld, Mervyn Greaves
Format: Article
Language:English
Published: Nature 2021-09-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-021-00264-x
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spelling doaj-7eb4c37c851c401aa62be2d48c9a44cf2021-09-12T11:13:13ZengNatureCommunications Earth & Environment2662-44352021-09-01211910.1038/s43247-021-00264-xDeglacial bottom water warming intensified Arctic methane seepage in the NW Barents SeaNaima El bani Altuna0Tine Lander Rasmussen1Mohamed Mahmoud Ezat2Sunil Vadakkepuliyambatta3Jeroen Groeneveld4Mervyn Greaves5CAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of NorwayCAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of NorwayCAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of NorwayCAGE-Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of NorwayAlfred Wegener Institute, Helmholtz Center for Polar and Marine ResearchGodwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of CambridgePhases of high bottom water temperature in the northwestern Barents Sea caused repeated destabilization of methane gas hydrates since the last glacial, according to a foraminifera Mg/Ca bottom water temperature record and hydrate stability modellinghttps://doi.org/10.1038/s43247-021-00264-x
collection DOAJ
language English
format Article
sources DOAJ
author Naima El bani Altuna
Tine Lander Rasmussen
Mohamed Mahmoud Ezat
Sunil Vadakkepuliyambatta
Jeroen Groeneveld
Mervyn Greaves
spellingShingle Naima El bani Altuna
Tine Lander Rasmussen
Mohamed Mahmoud Ezat
Sunil Vadakkepuliyambatta
Jeroen Groeneveld
Mervyn Greaves
Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
Communications Earth & Environment
author_facet Naima El bani Altuna
Tine Lander Rasmussen
Mohamed Mahmoud Ezat
Sunil Vadakkepuliyambatta
Jeroen Groeneveld
Mervyn Greaves
author_sort Naima El bani Altuna
title Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
title_short Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
title_full Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
title_fullStr Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
title_full_unstemmed Deglacial bottom water warming intensified Arctic methane seepage in the NW Barents Sea
title_sort deglacial bottom water warming intensified arctic methane seepage in the nw barents sea
publisher Nature
series Communications Earth & Environment
issn 2662-4435
publishDate 2021-09-01
description Phases of high bottom water temperature in the northwestern Barents Sea caused repeated destabilization of methane gas hydrates since the last glacial, according to a foraminifera Mg/Ca bottom water temperature record and hydrate stability modelling
url https://doi.org/10.1038/s43247-021-00264-x
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