We evaluated the extent to which the average metabolic activity of open oce
an bacterioplankton changed during 2 to 3 d incubations of 1 mu m filtered
seawater at in situ temperature. Indices of bacterial activity during incub
ation experiments were compared to those of in situ bacterioplankton, which
were repeatedly sampled at each oceanic site. Indices included: total and
cell-specific incorporation rates of tritiated leucine ([H-3]-Leu) and thym
idine ([H-3]-TdR), ratio of Leu to TdR incorporation, and percentage of hig
hly active cells as determined by detectable reduction of the fluorogenic d
ye, 5-cyano-2,3-ditolyl tetrazolium chloride (CTC). Patterns of change in m
etabolic activity were similar for experiments with water collected in 3 re
gions: midshelf, slope, and offshore, off the Oregon coast, USA, and incuba
ted at in situ temperatures of 9.5 to 18 degrees C. At the beginning of the
experiments, cell-specific incorporation rates of [H-3]-Leu and [H-3]-TdR
were lower compared to in situ rates, but after 19 to 28 h, incorporation r
ates of [H-3]-Leu and [H-3]-TdR increased dramatically, by more than an ord
er of magnitude, compared to in situ activity. When scaled to the abundance
of CTC positive (CTC+) cells, rates of Leu and TdR incorporation were 2.8-
to 8.1-fold higher during the incubations compared to activity of in situ
CTC+ cells. In this study, marine bacteria in 1 mu m, incubated filtrate ex
hibited a much larger Variation in metabolic activity than did in situ bact
erioplankton. In addition, the proportion of CTC+ cells was closely related
to cell-specific rates of Leu and TdR incorporation.