Effects of an iron-light co-limitation on the elemental composition (Si, C, N) of the marine diatoms <i>Thalassiosira oceanica</i> and <i>Ditylum brightwellii</i>
Abstract. We examined the effect of iron (Fe) and Fe-light (Fe-L) co-limitation on cellular silica (BSi), carbon (C) and nitrogen (N) in two marine diatom species, Thalassiosira oceanica and Ditylum brightwellii. We showed that C and N per cell tend to decrease with increasing Fe and Fe-L co-limitation (i.e. decreasing growth rate). We observed an increase (T. oceanica, Fe-L co-limitation), no change (T. oceanica, Fe limitation) and a decrease (D. brightwellii, Fe and Fe-L limitations) in BSi per cell with increasing degree of limitation. When comparing our results to literature data, we noted that the trend in C and N per cell for other Fe limited diatoms was similar to ours. However there was no global trend in BSi, which suggests interspecific differences. The relative variations in C:N, Si:C and Si:N versus the relative variation in specific growth rate (i.e. μ:μmax) followed the same patterns for both species under Fe and Fe-L co-limitation. The variations of C:N under Fe limitation reported in the literature for other diatoms are contrasted, which may thus be more related to growth conditions than to interspecific differences. Si:C and Si:N ratios increased by more than 2-fold between 100% and 40% of μmax. Under more severe limitation (Fe or Fe-L), these ratios tend to decrease. To asses the field significance of our results, we compared them to those of artificial Fe fertilisation experiments. This comparison showed that Si:N increased between 100% and ~40% of μmax, but decreased between 40% and 20% of μmax, and increased again below 20% of μmax. Between ~15% and 30% of μmax, Si:N was even lower than under non limiting conditions. These results may have important biogeochemical implications on the understanding and the modeling of the oceanic biogeochemical cycles, e.g. carbon export.