Tf. Thingstad et al., INCORPORATION RATES AND BIOMASS CONTENT OF C AND P IN PHYTOPLANKTON AND BACTERIA IN THE BAY-OF-AARHUS (DENMARK) JUNE 1992, Journal of plankton research, 18(1), 1996, pp. 97-121
Biomass content and incorporation rates for carbon (C) and phosphorus
(P) in microbial plankton in the Bay of Aarhus were investigated durin
g a 1 week period. Samples taken daily at a fixed station, as well as
during a diel cycle, allowed comparison of the water masses above, in
and below the pycnocline, and in influxes of different water masses. T
he coupling between the activity of phytoplankton and bacteria was exa
mined by the stoichiometric composition in pools and fluxes. From micr
oscope-based estimates of bacterial C and chemical determination of ph
osphate in the size fraction 1-0.2 mu m, the mean C:P ratio (molar) fo
r bacterial biomass was 78, while the mean C:P ratio for incorporation
was 96 or 63 from thymidine- and leucine-based estimates of bacterial
C production. Thymidine-based estimates of mean bacterial generation
time varied from 2.5 to 4.1 days with a minimum in the interface betwe
en water of Baltic and Skagerrak origin. These values are in good agre
ement with P-based generation time estimates. C-14 measurements of pri
mary production and orthophosphate incorporation into the size fractio
n >1 mu m gave a mean C:P ratio of 118, similar to the Redfield ratio
(106), but about twice the estimated mean C:P of 52 in protist biomass
. The combined methodological concept can be used to examine the simul
taneous role of microorganisms in the C and P budgets.