Eastern Atlantic deep-water circulation and carbon storage inferred from neodymium and carbon isotopic compositions over the past 1.1 million years

Eastern Atlantic deep-water circulation and carbon storage inferred from neodymium and carbon isotopic compositions over the past 1.1 million years

The Mid-Pleistocene transition (MPT; 1200 to 800 thousand years, kyr) is marked by the shift from 41-kyr to 100-kyr interglacial-glacial cyclicity without substantial change in the astronomical forcing. This change in climate response relied on internal feedback processes including interaction betwe...

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Bibliographic Details
Main Authors: Bickert, T. (Author), Deschamps, P. (Author), Dubois-Dauphin, Q. (Author), Guihou, A. (Author), Pérez-Asensio, J.N (Author), Rapuc, W. (Author), Skonieczny, C. (Author), Tachikawa, K. (Author), Vidal, L. (Author), Westerhold, T. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
air-sea interaction
Atlantic meridional overturning circulations
Atlantic ocean
Atlantic Ocean
Atlantic Ocean (North)
Atlantic Ocean (South)
Benthic foraminiferal δ13C
Biological productivity
Biology
carbon cycle
Carbon isotopic composition
carbon storage
Climate change
cyclicity
deep water
Digital storage
Glacial geology
Isotopes
isotopic composition
Marine isotope stages
Meridional gradients
Mid-Pleistocene transition
Nd isotopic composition
Neodymium
neodymium isotope
Neodymium isotopic composition
Northern Hemispheres
Ocean circulation
Oceanography
Overturning circulation
Pleistocene
Seawater
Southern Ocean
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