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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
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ユング・ドリアス期における深水形成の変化は,10Beと14Cの記録から推論された

R Muscheler1, J Beer, G Wagner

  • 1Department of Surface Waters, EAWAG, Dübendorf, Switzerland. muscheler@eawag.ch

Nature
|December 16, 2000
PubMed
まとめ

若干乾期における大気中の放射性炭素 (14C) の変動は,主に炭素循環だけでなく,生産率の変動によって引き起こされた. ベリリウム-10 (10Be) のデータを用いた分析は,深水形成の変化が14Cレベルにも影響したことを示しています.

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