He. Kolm et al., SPATIAL-DISTRIBUTION AND TEMPORAL VARIABILITY OF HETEROTROPHIC BACTERIA IN THE SEDIMENTS OF PARANAGUA AND ANTONINA BAYS, PARANA, BRAZIL, Revista de Microbiologia, 28(4), 1997, pp. 230-238
The temporal and spatial variability of heterotrophic bacteria was ana
lyzed in sandy, sandy-silt and silty sediments of Paranagua and Antoni
na Bays (SE Brazil). Samples were taken from seven stations along a sa
linity gradient, from the Paranagua Bay access to Corisco Island in An
tonina Bay, between November 1985 and November 1986. The results were
compared with deep-water salinity, pH, temperature, dissolved oxygen a
nd rainfall. ZoBell 2216E, at the salinities 0 parts per thousand and
32 parts per thousand, was used as culture media. Principal component
analysis showed that the concentration of heterotrophic bacteria was c
onsistently lower in sandy sediments near the entrance of the Paranagu
a Bay. Otherwise, the silty sediments did not differ significantly fro
m the other sediments. Highest halophilic levels were recorded at the
mouth of Maciel tidal creek. These results suggest that the amount of
bacteria, in the region, is not related to sediment grain size but to
currents speed which may benefit or not the organic matter deposition.
Non halophile and halotolerant bacteria can be limited by high salini
ty. Contrary to observations in the water column, high pluviosity did
not influence the heterotrophic bacteria number in the sediment from t
he studied area.