Tf. Thingstad et al., PHOSPHORUS CYCLING AND ALGAL-BACTERIAL COMPETITION IN SANDSFJORD, WESTERN NORWAY, Marine ecology. Progress series, 99(3), 1993, pp. 239-259
Microbial phosphorus-cycling, with particular emphasis on algal/bacter
ial competition, was studied in depth profiles through the halocline s
eparating a brackish top layer, rich in nitrate and poor in phosphate,
from the underlying coastal water, poor in both nitrate and phosphate
, in the Sandsfjord area, western Norway. At 2 stations along the axis
of natural freshwater outflow, physiological P-deficiency of algae an
d bacteria in the brackish layer was inferred from rapid luxury consum
ption of added PO43- by organisms in size fractions > 1 mum and 1-0.2
mum, respectively. In a branch of the fjord without natural freshwater
outlets, luxury consumption in the brackish layer was less, and witho
ut a clear difference between the 2 water layers. High luxury consumpt
ion coincided with short (< 30 min) turnover times for PO43- and stron
g bacterial dominance of (PO43-)-P-32-uptake, suggesting bacterial sup
eriority as competitors during P-limiting conditions. Estimation of P-
specific maximum uptake rate and affinity for PO43--uptake from isotop
e dilution experiments indicated bacterial superiority at low and alga
l superiority at high concentrations. Although most of the P-32 hydrol
yzed from added (gamma-ATP)-P-32 was initially liberated as free (PO4)
-P-32 partitioning of incorporated P-32 between size fractions > 1 mum
and 1-0.2 mum was found to depend on whether label was added as (gamm
a-AVP)-P-32 or as (PO43-)-P-32, indicating that coupling of uptake to
hydrolysis by cell-bound enzymes could modify the outcome of algal-bac
terial phosphorus competition. Disappearance rate of P-32 from the 1-0
.2 mum size fraction following initial labeling and a subsequent cold
chase with PO43- was used to estimate the flow-rate of phosphorus thro
ugh the microbial food web. Combined with measured kinetic constants f
or PO43- uptake, alkaline phosphatases and 5'nucleotidases, a coherent
flow-scheme could only be obtained assuming very low (< 1 nmol l-1) c
oncentrations of PO43- and nucleotides. Chemically measured concentrat
ions of dissolved organic phosphorus (DOP) more than 2 orders of magni
tude above the estimated nucleotide level and with an estimated turnov
er time of ca 500 h, are consistent with the view that this large P-re
servoir consists mainly of slowly hydrolyzable polymers.