Kr. Timmermans et al., Co-limitation by iron and light of Chaetoceros brevis, C-dichaeta and C-calcitrans (Bacillariophyceae), MAR ECOL-PR, 217, 2001, pp. 287-297
The interaction between iron and light limitation was investigated in 3 mar
ine diatom species: 2 Antarctic diatom isolates, Chaetoceros brevis and C.
dichaeta, and an isolate from temperate waters, C. calcitrans. In C. calcit
rans and C. brevis, grown in the laboratory using trace metal buffered medi
um, both iron and light limitation affected growth rates, cellular chloroph
yll a fluorescence, spinal index (i.e., the number and size of spines) and
cell size. Growth rates and cell size declined at lower iron concentrations
and lower light intensities. Cellular chlorophyll a fluorescence increased
with lower light, but decreased due to iron limitation, The spinal index,
based on the ratio of side scatter to forward scatter, increased in iron- a
nd light-limited cells, The large diatom C. dichaeta, grown in natural Sout
hern Ocean water (without ethelenediaminetetraace tic acid [EDTA]) showed q
ualitatively similar responses to co-limitation by iron and light. C. dicha
eta only grew under long-day light conditions, This response was further mo
dified by the availability of iron, Addition of iron resulted in higher gro
wth rates. In contrast, ambient iron concentrations did not limit the growt
h rate of the small Antarctic diatom C. brevis, However, iron limitation co
uld be induced by addition of the natural iron binding ligand desferrioxami
ne B (DFOB). Addition of iron to Fe-depleted cultures of C. dichaeta and C.
brevis reversed the effects of DFOB, as evidenced by rapid increases (with
in 24 h) in photochemical quantum efficiency (F-v/F-m) and decreases in eff
ective absorption of the cros-section of photosystem II (sigma (PSII)), the
turnover time of the photosynthetic unit (tau) and the electron transfer r
ate (1/ tau), followed by an increase in growth rates after 48 h. The inter
actions between iron and light in Antarctic diatoms are sufficient to expla
in the observation that in the Southern Ocean some species (i.e., the small
C, brevis) thrive under low iron and low light conditions, whereas other s
pecies (i.e., the large C. dichaeta) can bloom only under conditions of rel
atively high iron concentrations and favorable high light intensities or a
long-day light period. These differences in physiological responses will ha
ve consequences for primary production, the carbon cycle and biogeochemical
cycles.