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Dissolved oxygen and suspended particles regulate the benthic flux of iron from continental margins

Abstract:

We present ex situ sediment incubation results from the California and Oregon shelves and compare the calculated benthic flux of dissolved Fe with those from in situ incubations and pore water concentration profiles. We also examine the influence of oxygen depletion and sediment re-suspension on benthic Fe exchange. Ex situ incubation of the California and Oregon shelf sites yielded average benthic Fe fluxes of 3.5 and 8.3μmolm -2day -1, respe...

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Journal:
Marine Chemistry
Volume:
134-135
Pages:
59-70
Publication date:
2012-04-20
DOI:
ISSN:
0304-4203
URN:
uuid:1f99d177-237f-4e47-91dd-bb14eb1fd204
Source identifiers:
406751
Local pid:
pubs:406751

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