Vertical distribution of structure and function of the methanogenic archaeal community in Lake Dagow sediment

被引:125
作者
Chan, OC
Claus, P
Casper, P
Ulrich, A
Lueders, T
Conrad, R
机构
[1] Max Planck Inst Terr Microbiol, D-35043 Marburg, Germany
[2] Leibniz Inst Freshwater Ecol & Inland Fisheries, Dept Limnol Stratified Lakes, D-16675 Stechlin, Germany
[3] Leibniz Ctr Agr Landscape & Land Use Res, ZALF, Inst Primary Prod & Microbial Ecol, D-15374 Muncheberg, Germany
关键词
D O I
10.1111/j.1462-2920.2005.00790.x
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
Detailed studies on the relation of structure and function of microbial communities in a sediment depth profile scarcely exist. We determined as functional aspect the vertical distribution of the acetotrophic and hydrogenotrophic CH4 production activity by measuring production rates and stable C-13/C-12-isotopic signatures of CH4 in the profundal sediment of Lake Dagow. The structural aspect was determined by the composition of the methanogenic community by quantifying the abundance of different archaeal groups using 'real-time' polymerase chain reaction and analysis of terminal restriction fragment length polymorphism (T-RFLP). Methane production rates in the surface sediment (0-3 cm depth) were higher in August than in May, but strongly decreased with depth (down to 20 cm). The delta C-13 of the produced CH4 and CO2 indicated an increase in isotopic fractionation with sediment depth. The relative contribution of hydrogenotrophic to total methanogenesis, which was calculated from the isotopic signatures, increased with depth from about 22% to 38%. Total numbers of microorganisms were higher in August than in May, but strongly decreased with depth. The increase of microorganisms from May to August mainly resulted from Bacteria. The Archaea, on the other hand, exhibited a rather constant abundance, but also decreased with depth from about 1 x 10(8) copies of the archaeal 16S rRNA gene per gram of dry sediment at the surface to 4 x 10(7) copies per gram at 15-20 cm depth. T-RFLP analysis combined with phylogenetic analysis of cloned sequences of the archaeal 16S rRNA genes showed that the methanogenic community consisted mainly of Methanomicrobiales and Methanosaetaceae. The relative abundance of Methanosaetaceae decreased with depth, whereas that of Methanomicrobiales slightly increased. Hence, the vertical distribution of the functional characteristics (CH4 production from acetate versus H-2/CO2) was reflected in the structure of the community consisting of acetotrophic (Methanosaetaceae) versus hydrogenotrophic (Methanomicrobiales) phenotypes.
引用
收藏
页码:1139 / 1149
页数:11
相关论文
共 45 条
[1]  
Billen G., 1982, SEDIMENT MICROBIOLOG, P15
[2]  
Boone David R., 1993, P35
[3]   Methane in an acidic bog lake: The influence of peat in the catchment on the biogeochemistry of methane [J].
Casper, P ;
Chan, OC ;
Furtado, ALS ;
Adams, DD .
AQUATIC SCIENCES, 2003, 65 (01) :36-46
[4]  
CASPER P, 1995, P ANN M 1994 DEUTSCH, P386
[5]  
Casper P, 1996, ARCH HYDROBIOL SPEC, V48, P253
[6]  
Chan OC, 2002, FEMS MICROBIOL ECOL, V42, P119, DOI 10.1111/j.1574-6941.2002.tb01001.x
[7]  
Chin KJ, 1999, APPL ENVIRON MICROB, V65, P2341
[8]   Contribution of hydrogen to methane production and control of hydrogen concentrations in methanogenic soils and sediments [J].
Conrad, R .
FEMS MICROBIOLOGY ECOLOGY, 1999, 28 (03) :193-202
[9]   Quantification of methanogenic pathways using stable carbon isotopic signatures: a review and a proposal [J].
Conrad, R .
ORGANIC GEOCHEMISTRY, 2005, 36 (05) :739-752
[10]  
Conrad R, 1999, FEMS MICROBIOL ECOL, V30, P47, DOI 10.1111/j.1574-6941.1999.tb00634.x