Intraterrestrial waters harbor microbial communities being extensively studied to understand microbial processes underlying subsurface ecosystem functioning. This paper provides the results of an investigation on the microbiomes of unique, subsurface sulfidic waters associated with Upper Jurassic, Cretaceous, and Miocene sediments. We used high-throughput 16S rDNA amplicon sequencing to reveal the structure of bacterial and archaeal communities in water samples differing in sulfide content (20–960 mg/dm
3
), salinity (1.3–3.2%), and depth of extraction (60–660 m below ground level). Composition of the bacterial communities strongly varied across the samples; however, the bacteria participating in the sulfur cycle were common in all sulfidic waters. The shallowest borehole water (60 m bgl) was dominated by sulfur-oxidizing
Epsilonproteobacteria
(
Sulfurimonas
,
Sulfurovum
). In the waters collected from greater depths (148–300 m bgl), the prevalence of
Betaproteobacteria
(
Comamonadaceae
) and sulfate/sulfur-reducing
Deltaproteobacteria
(
Desulfopila
,
Desulfomicrobium
,
MSBL7
) was observed. Sulfate reducers (members of
Clostridia
:
Candidatus Desulforudis
) were the most abundant bacteria in the deepest borehole water (660 m bgl). Out of 850 bacterial OTUs, only one, affiliated with the
Comamonadaceae
family, was found abundant (> 1% of total bacterial sequences) in all samples. Contribution of
Archaea
to the whole microbial communities was lower than 0.5%. Archaeal communities did not differ across the samples and they consisted of
Halobacteriaceae
. Out of 372 archaeal OTUs, five, belonging to the four genera
Natronomonas
,
Halorubrum
,
Halobellus
, and
Halorhabdus
, were the most numerous.
Electronic supplementary material
The online version of this article (10.1007/s00248-018-1270-5) contains supplementary material, which is available to authorized users.