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, uncert...

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Vydané v:	Nature communications Ročník 8; číslo 1; s. 15425 - 9
Hlavní autori:	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
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	London Nature Publishing Group UK 09.06.2017 Nature Publishing Group Nature Portfolio
Predmet:	45/23 704/106/413 704/47/4112 Archives & records Bioavailability Carbon dioxide fixation Drainage Drawdown Dust Earth Sciences Environmental Sciences Geothermal power Humanities and Social Sciences Hydrology Ice sheets Marine sediments multidisciplinary Productivity Science Science (multidisciplinary) Sciences of the Universe Surface water New Zealand Ross Sea Australia France Southern Ocean
ISSN:	2041-1723, 2041-1723
On-line prístup:	Získať plný text
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