Effect of growth conditions on accumulation of internal nitrate,ammonium, amino acids,and protein in three marine diatoms

The capacity of marine phytoplankton to change their cellular content of nitrate, ammonium, amino acids, and protein in response to different growth conditions was systematically investigated. Cellular concentrations of these compounds were measured in N-starved, N-deficient, and N-sufficient Skeletonema costatum (Grev.) Cleve and in N-deficient Chaetoceros debilis Cleve and Thalassiosira gravida Cleve, both before and after the addition of a pulse of nitrogen.N-sufficient Skeletonema costatum contains high concentrations of protein, large persistent pools of amino acids, and, if it is growing on nitrate, sizeable amounts of nitrate. As it becomes N-starved, the total cellular nitrogen decreases, the internal nitrate and amino acids become entirely depleted, and the protein content is drastically reduced. After nitrogen additions to N-deficient and N-starved cultures, transient pools of unassimilated nitrogen form which can account for a large fraction of newly taken up nitrogen. The size and kind of pool which accumulates is determined by the preconditioning of the cells, the nitrogen compound which is added, and the species identity. The pools which form in S. costatum indicate that nitrate reduction is the slowest step in nitrogen assimilation, the synthesis of protein from amino acids is the next slowest, and the incorporation of ammonium into amino acid is the fastest. However, the rate limiting steps may vary between diatom species.For the first time, measurements of the variation in cellular nitrogen compounds over a wide range of environmental conditions reveal the ability of some phytoplankton to buffer the effects of a changing, and sometimes growth-limiting, nitrogen supply. They accomplish this by utilizing stored internal nitrogen for growth when the external supply is low and by quickly storing unassimilated nitrogen when the external supply is suddenly increased beyond their ability to immediately assimilate it. The accumulation of large pools of unassimilated nitrogen compounds can explain the often observed difference between nitrogen uptake rates and growth rates.