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Orgainic iron (III) speciation in surface transects across a frontal zone: the Chatham Rise, New Zealand

Tian, Feng; Frew, R; Sander, S; Hunter, K; Ellwood, Michael


Iron (Fe) is a critical nutrient in marine systems and the organic complexation of Fe is a central factor of the marine biogeochemistry of Fe. In the present study, total dissolved Fe and its organic speciation were measured in filtered seawater samples (<0.2 ?m) collected along three surface transects across the subtropical (ST) front, east of New Zealand, in austral spring (October 2000). Total dissolved Fe concentrations were low (∼0.1 nm) in the subantarctic (SA) waters. The highest Fe...[Show more]

CollectionsANU Research Publications
Date published: 2006
Type: Journal article
Source: Marine and Freshwater Research
DOI: 10.1071/MF05209


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