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Postglacial response of Arctic Ocean gas hydrates to climatic amelioration

Seafloor methane release due to the thermal dissociation of gas hydrates is pervasive across the continental margins of the Arctic Ocean. Furthermore, there is increasing awareness that shallow hydrate-related methane seeps have appeared due to enhanced warming of Arctic Ocean bottom water during th...

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Библиографические подробности
Опубликовано в: :Proc Natl Acad Sci U S A
Главные авторы: Serov, Pavel, Vadakkepuliyambatta, Sunil, Mienert, Jürgen, Patton, Henry, Portnov, Alexey, Silyakova, Anna, Panieri, Giuliana, Carroll, Michael L., Carroll, JoLynn, Andreassen, Karin, Hubbard, Alun
Формат: Artigo
Язык:Inglês
Опубликовано: National Academy of Sciences 2017
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Online-ссылка:https://ncbi.nlm.nih.gov/pmc/articles/PMC5474808/
https://ncbi.nlm.nih.gov/pubmed/28584081
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1619288114
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