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最後の脱氷期における南洋の炭素交換における役割

Andrea Burke1, Laura F Robinson

  • 1Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography, Woods Hole, MA 02543, USA. aburke@whoi.edu

Science (New York, N.Y.)
|December 17, 2011
PubMed
まとめ

脱氷期における南洋の炭素放出は,大気中のCO2に大きく影響した. 深海のサンゴの記録は,約14.6kaの主要な換気イベントを明らかにし,氷河期と氷河期間の二酸化炭素シフトを説明しています.

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