Mr. Mulholland et al., EXTRACELLULAR AMINO-ACID OXIDATION BY MICROPLANKTON - A CROSS-ECOSYSTEM COMPARISON, Aquatic microbial ecology, 15(2), 1998, pp. 141-152
Rates of extracellular amino acid oxidase activity in natural phytopla
nkton, cyanobacterial, and bacterial assemblages were measured using a
fluorescent analog of the amino acid lysine. Activity was measured in
a variety of ecosystems with different levels of nutrient enrichment
and diverse community composition. Sites included a station in Shinnec
ock Bay, Long Island Sound, New York (USA); the Chesapeake Bay, Maryla
nd (USA); the NW Atlantic Ocean near the Bahamas and the Caribbean Sea
; Brazilian coastal waters; and 2 estuarine mesocosms. Highest rates o
f amino acid oxidase activity (25 to 30 nM h(-1)) were found in the su
mmer mesocosm experiments when NH4+ concentrations were near the Limit
of detection, and biomass levels were indicative of an algal bloom. L
ower rates of amino acid oxidase activity were found during a bloom of
Aureococcus anophagefferens and in oligotrophic oceanic waters. High
rates of amino acid oxidase activity (up to 20 nM h(-1)) were also fou
nd in oceanic samples enriched with colonies of the diazotrophic cyano
bacteria Trichodesmium. No activity was observed in samples from oligo
trophic environments that were prefractionated through 1.0 mu m filter
s; however, when amended with glucose or an amino acid mixture, oxidat
ion rates of up to 8 nM h(-1) were observed. No activity was found dur
ing a diatom-dominated, autumnal bloom in Chesapeake Bay. Overall, ami
no acid oxidation represented a higher percentage of NH4+ uptake in th
e oligotrophic waters (up to 10%) than in the coastal waters studied.
In oligotrophic waters, where ambient inorganic nitrogen concentration
s are low and consequently uptake rates are low, this pathway appears
to represent a potentially important source of nitrogen for phytoplank
ton and the diazotrophic cyanobacteria Trichodesmium.