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Benthic d18O records Earth's energy imbalance. Nature Geoscience, 2023
(Ref: 17088)
Category 1: Peer-reviewed literature
Oxygen isotope ratios (d18O) of foraminifera in marine sediment records have fundamentally shaped our understanding of the ice ages and global climate change. Interpretation of these records has, however, been challenging because they reflect contributions from both ocean temperature and ice volume.