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A. C. Tessin and D. C. Lund Isotopically depleted carbon in the mid-depth South Atlantic during the last deglaciation Paleoceanography 28

Version of Record online: 20 JUN 2013 | DOI: 10.1002/palo.20026

Key Points

  • Mid-depth SW Atlantic had negative d13C anomalies during the last deglaciation
  • Benthic d13C anomalies are larger than the atmospheric d13C signal
  • Isotopic results cannot be easily explained with conservative mixing

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