Our basic microbiological studies of the water column and the sediment
of Golfo Dulce, Costa Rica, were focused on aerobic and denitrifying
sulfur-oxidizing bacteria and anaerobic sulfate-reducing bacteria. We
observed no increasing numbers of total bacterial counts within the wa
ter column. Although no oxygen was present hydrogen sulfide was only d
etectable close to the sediment. The highest numbers of sulfate-reduci
ng bacteria measured by Most-Probable-Number counts were found in or c
lose to the sediment. In the anoxic bottom water sulfide-oxidizing bac
teria typically containing large sulfur globules were observed microsc
opically. They were identified as free-swimming Thiovulum and Thiospir
a species. At one station large vacuolated forms of the filamentous co
lourless sulfur bacterium Beggiatoa were noted. Together with these su
lfur containing bacteria there were long free swimming rods showing no
sulfur inclusions of unknown character. The microscopic observations
showed good correlation with Most-Probable Number-counts and molecular
biological techniques for sulfate-reducing bacteria.