Towards a global highly reactive iron cycle

The global fluxes of iron oxy(hydr)oxides into the oceans from rivers, glaciers, atmospheric dust, hydrothermal activity, coastal erosion and diagenetic recycling have been quantified. The main sources to the shelf are from rivers, atmospheric dust and diagenetic recycling, and the main sources to t...

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Bibliographic Details
Published in:Journal of geochemical exploration 2006-01, Vol.88 (1), p.436-439
Main Author: Raiswell, R.
Format: Article
Language:English
Subjects:
Bioavailability
Global cycles
Iron oxy(hydr)oxides
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Summary:The global fluxes of iron oxy(hydr)oxides into the oceans from rivers, glaciers, atmospheric dust, hydrothermal activity, coastal erosion and diagenetic recycling have been quantified. The main sources to the shelf are from rivers, atmospheric dust and diagenetic recycling, and the main sources to the deep sea originate from glaciers or are exported from the shelf.
ISSN:0375-6742
1879-1689
DOI:10.1016/j.gexplo.2005.08.098