Simulating atmospheric CO2, 13C and the marine carbon cycle during the Last Glacial–Interglacial cycle: possible role for a deepening of the mean remineralization depth and an increase in the oceanic nutrient inventory

No abstract is available for this paper.

• Publication year

  2012

• Venue

  Quaternary Science Reviews

• Publication date

  2012-11-21

• Fields of study

  Geology, Environmental Science

• Identifiers
  DOI 10.1016/J.QUASCIREV.2012.09.012
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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  2012influential reference
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