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Jess F. Adkins The role of deep ocean circulation in setting glacial climates Paleoceanography 28

Article first published online: 19 SEP 2013 | DOI: 10.1002/palo.20046

Key Points

  • There is a lot of information about the past deep ocean
  • Tracers can be used to constrain the past circulation
  • Cooling NADW is a mechanism for entering glacials

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