Vj. Orphan et al., Culture-dependent and culture-independent characterization of microbial assemblages associated with high-temperature petroleum reservoirs, APPL ENVIR, 66(2), 2000, pp. 700-711
Recent investigations of oil reservoirs in a variety of locales have indica
ted that these habitats may harbor active thermophilic prokaryotic assembla
ges. In this study, we used both molecular and culture-based methods to cha
racterize prokaryotic consortia associated,vith high-temperature, sulfur-ri
ch oil reservoirs in California. Enrichment cultures designed for anaerobic
thermophiles, both autotrophic and heterotrophic, were successful at tempe
ratures ranging from 60 to 90 degrees C. Heterotrophic enrichments from all
sites yielded sheathed rods (Thermotogales), pleomorphic rods resembling T
hermoanaerobacter, and Thermococcus-like isolates. The predominant autotrop
hic microorganisms recovered from inorganic enrichments using EI,, acetate,
and CO, as energy and carbon sources were methanogens, including isolates
closely related to Methanobacterium, Methanococcus, and Methanoculleus spec
ies. Two 16S rRNA gene (rDNA) libraries were generated from total community
DNA collected from production wellheads, using either archaeal or universa
l oligonucleotide primer sets. Sequence analysis of the universal library i
ndicated that a large percentage of clones were highly similar to known bac
terial and archaeal isolates recovered from similar habitats. Represented g
enera in rDNA done libraries included Thermoanaerobacter, Thermococcus, Des
ulfothiovibrio, Aminobacterium, Acidaminococcus, Pseudomonas, Halomonas, Ac
inetobacter, Sphingomonas, Methylobacterium, and Desulfomicrobium. The arch
aeal library was dominated by methanogen-like rDNAs, with a lower percentag
e of clones belonging to the Thermococcales. Our results strongly support t
he hypothesis that sulfur-utilizing and methane-producing thermophilic micr
oorganisms have a widespread distribution in oil reservoirs and the potenti
al to actively participate in the biogeochemical transformation of carbon,
hydrogen, and sulfur in situ.