Active North Atlantic deepwater formation during Heinrich Stadial 1

Active North Atlantic deepwater formation during Heinrich Stadial 1

Deepwater circulation significantly changed during the last deglaciation from a shallow to a deep-reaching overturning cell. This change went along with a drawdown of isotopically light waters into the abyss and a deep ocean warming that changed deep ocean stratification from a salinity-to a tempera...

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Bibliographic Details
Main Authors: Bauch, H.A (Author), Cartapanis, O. (Author), Haug, G.H (Author), Lisiecki, L. (Author), Muglia, J. (Author), Mulitza, S. (Author), Rand, D. (Author), Repschläger, J. (Author), Schiebel, R. (Author), Schmittner, A. (Author), Zhao, N. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
Atlantic Ocean
Atlantic Ocean (North)
carbon isotope
Data compilation
Data compilation stable isotope
Data compilation stable isotopes
Deep ocean
deep water
Deepwater
Deep-water formation
drawdown
Iceland Basin
last deglaciation
North Atlantic
Oceanography
oxygen isotope
Paleoceanography
Quaternary
Stable isotopes
stratification
warming
Water levels
water mass
Water mass
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