A comprehensive study of the key ammonium-assimilating enzyme, glutarnine synthetase (GS), was made in a variety of marine phytoplankton. GS activity was detected in 13 out of the 15 species examined comprising 6 algal classes. Both the biosynthetic GS reaction as well as the transferase reaction were measured with phytoplankton extracts for comparative purposes. In evaluating the differences between the 2 assays it was found that the biosynthetic assay was more sensitive than the transferase assay in terms of final product formed/assay. The transferase assay yielded a more stable final product but the reaction is not specific for GS (Meister, 1974). A series of kinetic studies on the GS enzyme were carried out on a number of marine species. These studies included the determination of the pH optimum, linearity of the reaction with time, apparent energies of activation (E,) and apparent Y, values for the substrates: NH,', glutamate and ATP. In addition, the optimum requirement for the divalent cation, Mgf + was ascertained. The most significant finding of these studies was the broad distribution of GS activity in marine phytoplankton. The apparent K, values for ammonium were in the micromolar range. This is in marked contrast to earlier observations of the requirement of glutamate dehydrogenase (GDH), an alternate ammonium-assimilating enzyme, which has been shown to have a K, for ammonium ions in the millimolar range. These data support the view that GS is the primary ammonium-assimilating enzyme in phytoplankton found in areas of intermittent nitrogen supply.