The biological degradation of arginine and glutamic acid in seawater in relation to the growth of phytoplankton

The responses of natural summer coastal plankton communities to low-level additions (10^-5 to 10^-7 M) of arginine and glutamic acid has been followed by in vivo measurement of chlorophyll fluorescence. This technique is capable of detecting a response to a 10^-6 M enrichment under most conditions. The time sequence of the response varied with the amino acid used and with the enantiomeric form of the amino acid. Ammonia and carbon dioxide were liberated before the increase in chlorophyll fluorescence occurred. Liberation of ammonia in a dark bottle from L-arginine was from 75 to 85% of the theoretical yield. Microautoradiography using ¹⁴C L-arginine or L-glutamic acid at 10^-7 M showed heavy labeling associated with fecal pellets and detrital aggregates. Phytoplankton cells were not appreciably labeled. The evidence suggests that bacteria are important in the cycling of these compunds.