carbon dioxide
; cold water
; isotope
; neodymium
; unclassified drug
; water
; Article
; climate change
; controlled study
; geographic and geological phenomena
; Holocene
; Middle Holocene
; Pacific Deep Water
; priority journal
; Southern Hemisphere
; Southern Hemisphere westerly wind
; Southern Ocean
; Upper Circumpolar Deep Water
; water and water related phenomena
; water mass
; wind
Struve, T., Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, United Kingdom, Grantham Institute for Climate Change and the Environment, Imperial College London, London, SW7 2AZ, United Kingdom; Wilson, D.J., Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, United Kingdom, Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, London, WC1E 6BT, United Kingdom; van de Flierdt, T., Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, United Kingdom; Pratt, N., Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, United Kingdom; Crocket, K.C., School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FE, United Kingdom
Recommended Citation:
Struve T.,Wilson D.J.,van de Flierdt T.,et al. Middle Holocene expansion of Pacific Deep Water into the Southern Ocean[J]. Proceedings of the National Academy of Sciences of the United States of America,2020-01-01,117(2)