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Applied and Environmental Microbiology, August 2006, p. 5648-5652, Vol. 72, No. 8
0099-2240/06/$08.00+0 doi:10.1128/AEM.00727-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
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Peter Claus,1
Peter Casper,2 and
Ralf Conrad1*
Max Planck Institute for Terrestrial Microbiology, Karl-von-Frisch Str., 35043 Marburg, Germany,1 Leibniz Institute of Freshwater Ecology and Inland Fisheries, Department of Limnology of Stratified Lakes, 16775 Stechlin, Germany2
Received 29 March 2006/ Accepted 31 May 2006
The isotope enrichment factors (
) in Methanosaeta concilii and in a lake sediment, where acetate was consumed only by Methanosaeta spp., were clearly less negative than the
usually observed for Methanosarcina spp. The fraction of methane produced from acetate in the sediment, as determined by using stable isotope signatures, was 10 to 15% lower when the appropriate
of Methanosaeta spp. was used.
Present address: Institute of Groundwater Ecology, GSF-National Research Center for Environment and Health, 85764 Neuherberg, Germany.
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