Phytoplankton Plunder Nutrients
The seawater levels of the major nutrients (phosphate, nitrate, silicate) are, when considered over long timescales, under biological control. Silicon, the fifth-most abundant element dissolved in river water flowing down into the sea, is, by comparison, largely absent from seawater due to intense biological removal. We can get an idea of the importance of the plankton influence over nutrient levels from the figure to the right. The lack of intense biological removal of elements like sodium and chlorine leaves them to completely dominate sea-salt despite not being the most abundant constituents of the dissolved salt in river water. In general, the biologically-utilised elements are anomalously scarce in seawater.
A better idea of the overwhelming importance of biological removal in setting nutrient concentrations in the ocean can be obtained by experimenting with the three different nutrient models. All of these experiments can be carried out with either the phosphate-only, the nitrate-phosphate, or the silicate-phosphate models. From the control panel of a model, select 'Model Parameters' and then change the (not consciously of course, but they are also an emergent property of ecological dynamics). Biological removal also explains why carbon and calcium, the two most abundant dissolved constituents of river water, are relatively so scarce in seawater (see the figure to the right). They are actively removed from seawater in biological residues that fall to the seafloor and get buried; both are removed in CaCO3, carbon also in soft organic tissues. The plankton do not sit in a medium that has been set purely by external forces. Rather it is the plankton themselves (or rather, innumerable generations of their ancestors) which have in large part determined the chemical composition of the medium they inhabit.