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

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Autores principales: Naima El bani Altuna, Tine Lander Rasmussen, Mohamed Mahmoud Ezat, Sunil Vadakkepuliyambatta, Jeroen Groeneveld, Mervyn Greaves
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/7eb4c37c851c401aa62be2d48c9a44cf
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Sumario: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