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Applied and Environmental Microbiology, November 2000, p. 4790-4797, Vol. 66, No. 11
Max-Planck-Institut für Terrestrische
Mikrobiologie, D-35043 Marburg, Germany
Received 21 June 2000/Accepted 24 August 2000
Temperature is an important factor controlling CH4
production in anoxic rice soils. Soil slurries, prepared from Italian
rice field soil, were incubated anaerobically in the dark at six
temperatures of between 10 to 37°C or in a temperature gradient block
covering the same temperature range at intervals of 1°C. Methane
production reached quasi-steady state after 60 to 90 days. Steady-state
CH4 production rates increased with temperature, with an
apparent activation energy of 61 kJ mol
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Copyright © 2000, American Society for Microbiology. All rights reserved.
Effect of Temperature on Carbon and Electron Flow
and on the Archaeal Community in Methanogenic Rice Field Soil
1. Steady-state
partial pressures of the methanogenic precursor H2 also
increased with increasing temperature from <0.5 to 3.5 Pa, so that the
Gibbs free energy change of H2 plus
CO2-dependent methanogenesis was kept at
20 to
25 kJ
mol of CH4
1 over the whole temperature range.
Steady-state concentrations of the methanogenic precursor acetate, on
the other hand, increased with decreasing temperature from <5 to 50 µM. Simultaneously, the relative contribution of H2 as
methanogenic precursor decreased, as determined by the conversion of
radioactive bicarbonate to 14CH4, so that the
carbon and electron flow to CH4 was increasingly dominated
by acetate, indicating that psychrotolerant homoacetogenesis was
important. The relative composition of the archaeal community was
determined by terminal restriction fragment length polymorphism (T-RFLP) analysis of the 16S rRNA genes (16S rDNA). T-RFLP analysis differentiated the archaeal Methanobacteriaceae,
Methanomicrobiaceae, Methanosaetaceae,
Methanosarcinaceae, and Rice clusters I, III, IV, V, and
VI, which were all present in the rice field soil incubated at
different temperatures. The 16S rRNA genes of Rice cluster I and
Methanosaetaceae were the most frequent methanogenic
groups. The relative abundance of Rice cluster I decreased with
temperature. The substrates used by this microbial cluster, and thus
its function in the microbial community, are unknown. The relative
abundance of acetoclastic methanogens, on the other hand, was
consistent with their physiology and the acetate concentrations
observed at the different temperatures, i.e., the
high-acetate-requiring Methanosarcinaceae decreased and the
more modest Methanosaetaceae increased with increasing
temperature. Our results demonstrate that temperature not only affected
the activity but also changed the structure and the function (carbon
and electron flow) of a complex methanogenic system.
*
Corresponding author. Mailing address:
Max-Planck-Institut für terrestrische Mikrobiologie,
Karl-von-Frisch-Strasse, 35043 Marburg, Germany. Phone: 49 (6421)
178-801. Fax: 49 (6421) 178-809. E-mail:
conrad{at}mailer.uni-marburg.de.
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