Glacial deep ocean deoxygenation driven by biologically-mediated air-sea disequilibrium

Deep ocean deoxygenation inferred from proxies has been used to support the hypothesis that a lower atmospheric carbon dioxide during glacial times was due to an increase in the strength of the ocean’s biological pump. This relies on the assumption that surface ocean oxygen (O2) is equilibrated with...

Бүрэн тодорхойлолт

Номзүйн дэлгэрэнгүй
Үндсэн зохиолчид: Cliff, E, Khatiwala, S, Schmittner, A
Формат: Journal article
Хэл сонгох:English
Хэвлэсэн: Nature Research 2021