Kr. Timmermans et al., Growth rates of large and small Southern Ocean diatoms in relation to availability of iron in natural seawater, LIMN OCEAN, 46(2), 2001, pp. 260-266
Blooms of large diatoms dominate the CO2 drawdown and silicon cycle of the
Southern Ocean in both the past and present. The growth of these Antarctic
diatoms is limited by availability of iron (and light). Here we report the
first assessment of growth rates in relation to iron availability of two tr
uly oceanic Antarctic diatom species, the large, chain-forming diatom Chaet
oceros dichaeta and the small, unicellular diatom C. brevis. In filtered na
tural, untreated Southern Ocean water, a maximum specific growth rate of 0.
62 +/- 0.09 d(-1) and a K-m, for growth of 1.12 x 10(-9) M dissolved iron w
as calculated for C. dichaeta. This response could only be seen during a lo
ng-day light period. C. brevis maintained growth rates of 0.39 +/- 0.09 d(-
1) with and without iron addition, even under short-day light conditions, a
nd could only be forced into iron limitation by adding the siderophore desf
erri-ferrioxamine B (DFB), an iron immobilizing agent. Using this approach,
the low K-m value for growth of 0.59 x 10(-12) M dissolved Fe was calculat
ed for this Species. The size-class dependent growth response to iron (and
light) confirms the key role of these parameters in structuring Southern Oc
ean ecosystems and thus the CO2 dynamics and the silicon cycle.