Dc. Smith et al., BACTERIAL MEDIATION OF CARBON FLUXES DURING A DIATOM BLOOM IN A MESOCOSM, Deep-sea research. Part 2. Topical studies in oceanography, 42(1), 1995, pp. 75-97
Bacteria-diatom interactions were studied during a diatom bloom produc
ed in a mesocosm, in the absence of metazoan grazers, in order to exam
ine the significance of bacterial hydrolytic ectoenzymes in mediating
carbon fluxes and influencing diatom aggregation. The abundances of ba
cteria and protozoa, the production rates and hydrolytic ectoenzyme ac
tivities (protease alpha and beta glucosidase and chitobiase) of attac
hed and free bacteria, were followed as well as the dynamics of the di
ssolved organic carbon (DOC) pool. An intense diatom bloom occurred wi
th chlorophyll a (chl a) concentrations reaching 132 mu g liter(-1) pr
ior to aggregation. The diatoms were colonized by bacteria early on in
the bloom and remained colonized throughout the bloom, yet they grew
rapidly (>1 day(-1)). Attached bacteria were numerically a small fract
ion of the total, but they also grew very rapidly (mu = 4-16 day(-1))
and were generally responsible for the majority of bacterial carbon de
mand, BCD, (46-92%) and hydrolytic enzyme activities (41-99%). BCD acc
ounted for an estimated 40-60% of the total carbon fixed during the bl
oom; thus, roughly one-half of the primary production was channeled, v
ia the DOC pool, into bacteria. The high ectohydrolase activities of b
acteria attached to the surface of diatoms suggests that the hydrolysi
s of diatom surface mucus could be responsible for a major flux into t
he DOC pool making it a significant, but previously unrecognized, mech
anism of DOM production. Enzymatic hydrolysis of surface mucus may als
o have inhibited diatom aggregation. Addition of purified glucosidase
and protease to samples from the mesocosm inhibited diatom aggregation
in experiments designed to induce aggregation. It is hypothesized tha
t the action of bacterial ectoenzyme on diatom surfaces inhibited diat
om aggregation by reducing stickiness, thus prolonging the bloom and a
llowing the accumulation of extremely high chl a levels prior to aggre
gation. Future studies should consider bacterial hydrolytic ectoenzyme
s as a potentially important variable influencing carbon flux pathways
, particle aggregation, and the size and duration of diatom blooms in
the ocean.