Layered structure of bacterial and archaeal communities and their in situ activities in anaerobic granules.

The microbial community structure and spatial distribution of microorganisms and their in situ activities in anaerobic granules were investigated by 16S rRNA gene-based molecular techniques and microsensors for CH(4), H(2), pH, and the oxidation-reduction potential (ORP). The 16S rRNA gene-cloning analysis revealed that the clones related to the phyla Alphaproteobacteria (detection frequency, 51%), Firmicutes (20%), Chloroflexi (9%), and Betaproteobacteria (8%) dominated the bacterial clone library, and the predominant clones in the archaeal clone library were affiliated with Methanosaeta (73%). In situ hybridization with oligonucleotide probes at the phylum level revealed that these microorganisms were numerically abundant in the granule. A layered structure of microorganisms was found in the granule, where Chloroflexi and Betaproteobacteria were present in the outer shell of the granule, Firmicutes were found in the middle layer, and aceticlastic Archaea were restricted to the inner layer. Microsensor measurements for CH(4), H(2), pH, and ORP revealed that acid and H(2) production occurred in the upper part of the granule, below which H(2) consumption and CH(4) production were detected. Direct comparison of the in situ activity distribution with the spatial distribution of the microorganisms implied that Chloroflexi contributed to the degradation of complex organic compounds in the outermost layer, H(2) was produced mainly by Firmicutes in the middle layer, and Methanosaeta produced CH(4) in the inner layer. We determined the effective diffusion coefficient for H(2) in the anaerobic granules to be 2.66 x 10(-5) cm(2) s(-1), which was 57% in water.