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Andreas Mackensen High epibenthic foraminiferal δ13C in the Recent deep Arctic Ocean: Implications for ventilation and brine release during stadials Paleoceanography 28

Version of Record online: 20 SEP 2013 | DOI: 10.1002/palo.20058

Key Points

  • Strong 13C-Suess effect lowers δ13C of Arctic surface waters
  • Reduced stadial ABW δ13C suggested due to diminished brine formation
  • Stadial benthic δ13C spikes in Nordic seas may reflect less Arctic brine

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