A variety of metallic elements, particularly Fe and Zn, are considered esse
ntial for biological processes in a variety of natural ecosystems, but are
generally present only in trace amounts. Although their essential nature in
terrestrial ecosystems has been known for many decades, it is only in rece
nt years that scientific methodology has improved to the point that the bio
geochemical behaviour of trace metals can be adequately studied in aquatic
ecosystems such as the ocean. This paper reviews some of the recent scienti
fic progress and demonstrates how conventional thinking about the biogeoche
mical role of trace metals in the ocean has been advanced by the findings o
f this research. In particular, it is now clear that the availability of se
veral trace elements is a factor that controls phytoplankton growth in the
ocean.