Iron plays an important role in oceanic biogeochemistry and is known to lim
it biological activity in certain ocean regions. Such regions have a replet
e complement of major nutrients but low primary production of phytoplankton
due to low ambient iron concentrations. The determination of iron in seawa
ter is a major challenge, although much progress has been made during the l
ast two decades. Techniques for total dissolved iron and iron speciation ha
ve been developed in order to rationalise its biogeochemical cycling and be
tter understand its role in limiting phytoplankton growth. In this paper, a
critical review of historical and current analytical methods for the deter
mination of iron in seawater is presented and their capabilities evaluated.
The need for standard protocols for the clean sampling and storage of low-
level (<1 nM) iron seawater in order to maintain sample integrity is emphas
ised. The importance of laboratory and shipboard intercomparison exercises
to distinguish between environmental variability and operationally measured
fractions is also considered. (C) 2001 Elsevier Science B.V. All rights re
served.