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Multiple sources of atmospheric CO2 activated by AMOC recovery at the onset of interglacial MIS 9 Proceedings of the National Academy of Sciences of the United States of America, 2025 (Ref: 17321)
Authors:
Krauss F.Baggenstos D.Schmitt J.Tuzon B.Menking J.A.Mächler L.Silva L.Grimmer M.Capron E.Stocker T.F.Bauska T.K.Fischer H.
Category 1: Peer-reviewed literature

Using high-precision ice core measurements of CO2, ?13C-CO2, CH4, and N2O, this study provides carbon isotope constraints on a sizeable, centennial-scale CO2 jump at the onset of Marine Isotope Stage 9 (MIS 9). The very end of the Heinrich stadial (HS) characterizing Termination IV (T-IV, ca.

AMOC Modulates Ocean Heat Content During Deglaciations Geophysical Research Letters, 2025 (Ref: 17241)
Authors:
Grimmer M.Baggenstos D.Schmitt J.Krauss F.Shackleton S.Severinghaus J.P.Fischer H.
Category 1: Peer-reviewed literature

During deglaciations, Earth takes up vast amounts of energy, about half of which heats the global ocean. Thus, ocean heat content (OHC) is a key metric to assess Earth's energy budget.

The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature Geophysical Research Letters, 2023 (Ref: 16752)
Authors:
Poppelmeier F.Baggenstos D.Grimmer M.Liu Z.Schmitt J.Fischer H.Stocker T.F.
Category 1: Peer-reviewed literature

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