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Jennifer Fehrenbacher and Pamela Martin Western equatorial Pacific deep water carbonate chemistry during the Last Glacial Maximum and deglaciation: Using planktic foraminiferal Mg/Ca to reconstruct sea surface temperature and seafloor dissolution Paleoceanography 26

Version of Record online: 30 JUN 2011 | DOI: 10.1029/2010PA002035

Key Points

  • Deep Pacific carbonate chemistry was lower during the LGM compared to the Modern
  • Changes in preservation and circulation have occurred over the last 25 kyr
  • Preservation was enhanced in this region during the deglaciation

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