In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 44, No. 5 ( 2017-03-16), p. 2377-2387
Abstract:
Labile‐particulate iron has a key role in iron cycling and can increase the overall “available” iron pool by up to 55% in the OMZ A strong relationship between particles and dissolved iron indicates that L‐pFe “buffers” the elevated dFe concentrations observed Lateral shelf transport of available Fe (L‐pFe + dFe) supplied a similar magnitude of iron as atmospheric sources
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1002/2016GL072314
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13
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