Determination of Microbial Production
219
carbon. The biovolume of bacterioplankton is estimated with the aid of
epiftuorescence microbial count at black Nucleopore filters (see Sect. 6.2).
Parallel estimations of bacterial production by the dark 14C02 uptake and
the radiophosphorus methods in surface waters of the eastern Pacific revealed
a quite reasonable correlation between values thus obtained (Fig. 4.15).
8
of..
. .
6
4
..
+
+
. .
2
o
o
2
4
6
8
Fig. 4.15. Correlation between the values of bacterioplankton production (mg Cm- 3
day-I) as measured by the 14C - dark uptake e 4 C) and by the 33P04_P uptake method
C 3 P) in the Peruvian region during the El Nino period
219
carbon. The biovolume of bacterioplankton is estimated with the aid of
epiftuorescence microbial count at black Nucleopore filters (see Sect. 6.2).
Parallel estimations of bacterial production by the dark 14C02 uptake and
the radiophosphorus methods in surface waters of the eastern Pacific revealed
a quite reasonable correlation between values thus obtained (Fig. 4.15).
8
of..
. .
6
4
..
+
+
. .
2
o
o
2
4
6
8
Fig. 4.15. Correlation between the values of bacterioplankton production (mg Cm- 3
day-I) as measured by the 14C - dark uptake e 4 C) and by the 33P04_P uptake method
C 3 P) in the Peruvian region during the El Nino period
