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Applied and Environmental Microbiology, June 1999, p. 2402-2408, Vol. 65, No. 6
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.

Vertical Distribution of Methanogens in the Anoxic Sediment of Rotsee (Switzerland)

K. Zepp Falz,1,* C. Holliger,1 R. Großkopf,2 W. Liesack,2 A. N. Nozhevnikova,1 B. Müller,1 B. Wehrli,1 and D. Hahn3,4

Limnological Research Center, Swiss Federal Institute for Environmental Science and Technology (EAWAG), CH-6047 Kastanienbaum, Switzerland1; Max-Planck-Institut für Terrestrische Mikrobiologie, D-35043 Marburg/Lahn, Germany2; Department of Chemical Engineering, Chemistry and Environmental Sciences, New Jersey Institute of Technology, Newark, New Jersey 071023; and Department of Biological Sciences, Rutgers University, Newark, New Jersey 07102-18114

Received 14 December 1998/Accepted 31 March 1999

Anoxic sediments from Rotsee (Switzerland) were analyzed for the presence and diversity of methanogens by using molecular tools and for methanogenic activity by using radiotracer techniques, in addition to the measurement of chemical profiles. After PCR-assisted sequence retrieval of the 16S rRNA genes (16S rDNA) from the anoxic sediment of Rotsee, cloning, and sequencing, a phylogenetic analysis identified two clusters of sequences and four separated clones. The sequences in cluster 1 grouped with those of Methanosaeta spp., whereas the sequences in cluster 2 comprised the methanogenic endosymbiont of Plagiopyla nasuta. Discriminative oligonucleotide probes were constructed against both clusters and two of the separated clones. These probes were used subsequently for the analysis of indigenous methanogens in a core of the sediment, in addition to domain-specific probes against members of the domains Bacteria and Archaea and the fluorescent stain 4',6-diamidino-2-phenylindole (DAPI), by fluorescent in situ hybridization. After DAPI staining, the highest microbial density was obtained in the upper sediment layer; this density decreased with depth from (1.01 ± 0.25) × 1010 to (2.62 ± 0.58) × 1010 cells per g of sediment (dry weight). This zone corresponded to that of highest metabolic activity, as indicated by the ammonia, alkalinity, and pH profiles, whereas the methane profile was constant. Probes Eub338 and Arch915 detected on average 16 and 6% of the DAPI-stained cells as members of the domains Bacteria and Archaea, respectively. Probe Rotcl1 identified on average 4% of the DAPI-stained cells as Methanosaeta spp., which were present throughout the whole core. In contrast, probe Rotcl2 identified only 0.7% of the DAPI-stained cells as relatives of the methanogenic endosymbiont of P. nasuta, which was present exclusively in the upper 2 cm of the sediment. Probes Rotp13 and Rotp17 did not detect any cells. The spatial distribution of the two methanogenic populations corresponded well to the methane production rates determined by incubation with either [14C]acetate or [14C]bicarbonate. Methanogenesis from acetate accounted for almost all of the total methane production, which concurs with the predominance of acetoclastic Methanosaeta spp. that represented on average 91% of the archaeal population. Significant hydrogenotrophic methanogenesis was found only in the organically enriched upper 2 cm of the sediment, where the probably hydrogenotrophic relatives of the methanogenic endosymbiont of P. nasuta, accounting on average for 7% of the archaeal population, were also detected.


* Corresponding author. Mailing address: Swiss Federal Institute for Environmental Science and Technology (EAWAG), Limnological Research Center, Seestrasse 79, CH-6047 Kastanienbaum, Switzerland. Phone: 41-41-349 2153. Fax: 41-41-349 2168. E-mail: kornelia.zepp{at}eawag.ch.


Applied and Environmental Microbiology, June 1999, p. 2402-2408, Vol. 65, No. 6
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.



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