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The marine δ18O record overestimates continental ice volume during Marine Isotope Stage 3

Daltona AS, Pico T, Gowan EJ, Clague JJ, Forman SL, McMartin I, Sarala P and Helmenskl KF
Global and Planetary Change
212
2022
https://doi.org/10.1016/j.gloplacha.2022.103814
Fig. 1 Dalton et al. May 2022

The authors acknowledge PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), which in turn received support from the Swiss Academy of Sciences and the Chinese Academy of Sciences. 

 

Category:
Journal articles