The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum

Marine sediment records suggest that episodes of major atmospheric CO(2) drawdown during the last glacial period were linked to iron (Fe) fertilization of subantarctic surface waters. The principal source of this Fe is thought to be dust transported from southern mid-latitude deserts. However, uncer...

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Bibliografske podrobnosti
izdano v:Nat Commun
Main Authors: Frisia, Silvia, Weyrich, Laura S., Hellstrom, John, Borsato, Andrea, Golledge, Nicholas R., Anesio, Alexandre M., Bajo, Petra, Drysdale, Russell N., Augustinus, Paul C., Rivard, Camille, Cooper, Alan
Format: Artigo
Jezik:Inglês
Izdano: Nature Publishing Group 2017
Teme:
Article
Online dostop:https://ncbi.nlm.nih.gov/pmc/articles/PMC5472753/
https://ncbi.nlm.nih.gov/pubmed/28598412
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15425
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