上层海洋对大气的放射性碳抵消意味着快速降冰的二氧化碳释放

Kathryn A Rose1, Elisabeth L Sikes, Thomas P Guilderson

  • 1Department of Geology, University of California, Davis, California 95616, USA.

Nature
|August 27, 2010
PubMed
概括

海洋循环影响大气中的放射性碳水平. 这项研究揭示了南大洋上游在脱冰过程中释放的旧碳,影响放射性碳 (三角洲14C) 信号,并表明北太平洋碳库的贡献.

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