Cm. Turley et al., Relationship between primary producers and bacteria in an oligotrophic sea- the Mediterranean and biogeochemical implications, MAR ECOL-PR, 193, 2000, pp. 11-18
The proverbial blue colour of the Mediterranean reflects some of the most e
xtreme oligotrophic waters in the world. Sea-surface Sea-viewing Wide Field
-of-view Sensor (SeaWiFS) satellite data show the relatively clear, pigment
poor, surface waters of the Mediterranean with a generally increasing olig
otrophy eastward, apparent even from space. Integrated over depth, however,
the east and west Mediterranean show similar amounts of phytoplankton and
bacterial biomass. By contrast, primary production and bacterial production
are 2 to 3 times lower in the eastern Mediterranean than in the west. Howe
ver, the relationship between bacterial production and primary production i
n the east and west are significantly different. While bacterial production
is directly proportional to primary production in the east, in the west it
increases as approximately the square root of primary production. This sug
gests that the bacteria in the west are relatively decoupled from local con
temporaneous primary production. In contrast, the gradient of close to 1 in
the log bacterial production versus log primary production relationship in
the east suggests less temporal decoupling and, therefore, less seasonal a
ccumulation of DOG. In addition, the constant proportionality between bacte
rial and primary production of 0.22, which, if all primary products are res
pired, gives an estimated geometric mean bacteria growth efficiency of 22 %
(95 % confidence limits of 17 and 29 %) for data in the eastern Mediterran
ean. Our data suggest that the degree of bacteria-phytoplankton coupling ha
s an important effect on apparent trends between bacterial and phytoplankto
n production in high frequency data. The combination of low primary product
ion and bacterial dominance of secondary production in the east is also of
significance as it could account for the low fisheries production, the low
vertical flux of material and low biomass of benthic organisms in the regio
n.