Hot springs represent a major source of arsenic release
into the
environment. Speciation is typically reported to be dominated by arsenite,
arsenate, and inorganic thiolated arsenates. Much less is known about
the relevance and formation of methylated thioarsenates, a group with
species of high mobility and toxicity. In hot spring samples taken
from the Tengchong volcanic region in China, methylated thioarsenates
contributed up to 13% to total arsenic. Enrichment cultures were obtained
from the corresponding sediment samples and incubated to assess their
capability to convert arsenite into methylated thioarsenates over
time and in the presence of different microbial inhibitors. In contrast
to observations in other environmental systems (e.g., paddy soils),
there was no solid evidence, supporting that the sulfate-reducing
bacteria contributed to the arsenic methylation. Methanosarcina, the sole genus of methanogens detected in the enrichment cultures,
as well as Methanosarcina thermophila TM-1, a pure strain within the genus, did methylate arsenic. We
propose that methylated thioarsenates in a typical sulfide-rich hot
spring environment like Tengchong form via a combination of biotic
arsenic methylation driven by thermophilic methanogens and arsenic
thiolation with either geogenic sulfide or sulfide produced by sulfate-reducing
bacteria.