Volumes (800 ml) were added to triplicate polycarbonate bottles and spiked with an f / 50 nutrient derivative (10 µm NaNO3 −, 0.8 µm NaH2PO43 −, 10 µm Na2SiO3 and f / 50 vitamin and trace metal concentrations [27,28]-RRB- to promote
diatom growth.
However, elevated atmospheric CO2 concentrations and ocean acidification may also have an adverse impact on
diatom growth, causing a decrease in cell size and possible further changes in phytoplankton composition.
If diatom layers are a major factor, then understanding where paleoclimate conditions may have favored
diatom growth might help reveal potential mega-slide sites.
Not exact matches
Among their findings: in streams with the amphetamine addition, the
growth of biofilms was significantly suppressed, the composition of bacterial and
diatom communities changed, and aquatic insects emerged earlier.
Unlike most regions of the global ocean which do not contain sufficient nitrogen or phosphorus for sustained phytoplankton
growth,
diatoms in the remote waters of McMurdo Sound were starving from lack of iron and deficiency of vitamin B12.
Thus any process which tends to favor the
growth of organisms made from silicate, such as
diatoms, over organisms made from carbonate, such as the coccolithophorids, will tend to lower the atmospheric CO2 concentration — and vice versa — even if the total organic biomass formed in the surface layer and sinking from that layer remains constant.
The predicted continuous warming trend of the ocean surface temperature is expected to favour the
growth of smaller phytoplankton cells (picophytoplankton replacing large
diatoms) that in turn would also favour small - sized zooplankton species (Li et al. 2009).