Da. Caron et al., THE CONTRIBUTION OF MICROORGANISMS TO PARTICULATE CARBON AND NITROGENIN SURFACE WATERS OF THE SARGASSO SEA NEAR BERMUDA, Deep-sea research. Part 1. Oceanographic research papers, 42(6), 1995, pp. 943-972
Seawater samples were collected from the euphotic zone of the Sargasso
Sea near Bermuda in August of 1989 and March-April of 1990. Microbial
population abundances, chlorophyll concentration, particulate carbon
and particulate nitrogen were measured. Calculations were performed to
establish the relative and absolute importance of the various microbi
al assemblages. The choice of conversion factors (g C and N cell(-1),
or g C and N mu m(-3)) for the microbial populations dramatically affe
cted the estimation of ''living'' and ''detrital'' particulate materia
l in the samples, and the relative importance of the various microbial
groups. Averaged over all samples on either of the two cruises, micro
bial biomass constituted a greater proportion of the total particulate
carbon and nitrogen during March-April (55% and 63%, respectively), t
han during August (approximate to 24% and 30%, respectively) using ''c
onstrained'' conversion factors that were derived. Accordingly, detrit
al material constituted the bulk of the particulate material during Au
gust, but was similar to the amount of microbial biomass during March-
April. The bacterial assemblage constituted the largest single pool of
microbial carbon (35%) and nitrogen (45%) in the water, and a signifi
cant fraction of the total particulate carbon (approximate to 10-20%)
and nitrogen (approximate to 15-30%). Phototrophic nanoplankton (micro
algae 2-20 mu m in size) were second in overall biomass, and often dom
inated the microbial biomass in the deep chlorophyll maxima that were
present during both cruises. The results temper recent assertions conc
erning the overwhelming importance of bacterial biomass in the oligotr
ophic Sargasso Sea but still support a major role for these microorgan
isms in the open ocean as repositories for carbon and nutrients.