Recently, it was shown that certain phytoplankton species in laborator
y culture can use cell-surface enzymes to oxidize amino acids and amin
es and take up ammonium produced during the oxidation. Previously, we
developed a fluorescent analog of the amino acid lysine (LYA-lysine) t
o act as a tracer of cell-surface oxidation processes. In the present
study, a kinetic approach demonstrated that these fluorescent probes e
ffectively compete with natural amino acids and are thus similar to th
e natural compounds. Field studies showed that naturally occurring phy
toplankton and bacteria-size organisms oxidized the fluorescent analog
, extending the discovery of this oxidation process to natural waters.
Parallel experiments measuring uptake of C-14-labeled amino acids and
oxidation of LYA-lysine showed that oxidation rates could be as much
as 40% of the total removal rate. This finding suggests that removal o
f amino acids from seawater might be significantly underestimated if u
ptake across the cell membrane were the only process considered. Howev
er, cell-surface oxidative deamination was detected only in summer, wh
en temperatures exceeded 22 degrees C.