The chemical composition and degradation of dissolved amino acids and gluco
se by bacteria were investigated in the northern Sargasso Sea. Multiple poo
ls of amino acids were discerned based on microbial reactivity. Concentrati
ons of dissolved free amino acid (DFAA) were highest in the surface waters,
where rapid utilization of DFAA accounted for <20% of the measured bacteri
al growth requirements for C and N. Dissolved combined amino acid (DCAA) an
d protein (using the BCA assay) concentrations were 10- to 25-fold higher t
han that of DFAA. In surface waters, DCAA was largely identifiable as prote
in (similar to 100%), but most of the DCAA at depth (>100 m) did not respon
d to the protein assay (<50%). In surface waters, protein was the dominant
form of organic nitrogen used to support bacterial growth, supporting 20 to
65% of the calculated bacterial N demand. In deeper waters, utilization of
a modified form of protein (glucosylated protein) accounted for the highes
t portion of the bacterial growth demands. Free and combined amino acids di
d not meet the full bacterial N demand at depth, and other, unmeasured nitr
ogen sources were required. Similar to trends in utilization, maximum uptak
e rate (V-max) for protein was highest in surfaces waters. Modified protein
had higher V-max in deep waters, consistent with the longer turnover time
of this pool of DCAA and the likelihood that it is produced in the surface
and transported to depth each winter during mixing events.