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排水沼泽中的产甲烷菌群落:灰分施肥的影响。

Methanogen communities in a drained bog: effect of ash fertilization.

作者信息

Galand P E, Juottonen H, Fritze H, Yrjälä K

机构信息

Department of Biological and Environmental Sciences, Division of General Microbiology, University of Helsinki, P.O. Box 56, 00014 Helsinki, Finland.

出版信息

Microb Ecol. 2005 Feb;49(2):209-17. doi: 10.1007/s00248-003-0229-2. Epub 2005 Jun 17.

Abstract

Forestry practises such has drainage have been shown to decrease emissions of the greenhouse gas methane (CH(4)) from peatlands. The aim of the study was to examine the methanogen populations in a drained bog in northern Finland, and to assess the possible effect of ash fertilization on potential methane production and methanogen communities. Peat samples were collected from control and ash fertilized (15,000 kg/ha) plots 5 years after ash application, and potential CH(4) production was measured. The methanogen community structure was studied by DNA isolation, PCR amplification of the methyl coenzyme-M reductase (mcr) gene, denaturing gradient gel electrophoresis (DGGE), and restriction fragment length polymorphism (RFLP) analysis. The drained peatland showed low potential methane production and methanogen diversity in both control and ash-fertilized plots. Samples from both upper and deeper layers of peat were dominated by three groups of sequences related to Rice cluster-I hydrogenotroph methanogens. Even though pH was marginally greater in the ash-treated site, the occurrence of those sequences was not affected by ash fertilization. Interestingly, a less common group of sequences, related to the Fen cluster, were found only in the fertilized plots. The study confirmed the depth related change of methanogen populations in peatland.

摘要

诸如排水等林业实践已被证明可减少泥炭地温室气体甲烷(CH₄)的排放。本研究的目的是调查芬兰北部一个排水后的沼泽地中的产甲烷菌种群,并评估灰分施肥对潜在甲烷产生和产甲烷菌群落的可能影响。在施用灰分5年后,从对照地块和灰分施肥地块(15,000千克/公顷)采集泥炭样本,并测量潜在的CH₄产生量。通过DNA分离、甲基辅酶-M还原酶(mcr)基因的PCR扩增、变性梯度凝胶电泳(DGGE)和限制性片段长度多态性(RFLP)分析来研究产甲烷菌群落结构。在对照地块和灰分施肥地块中,排水后的泥炭地均显示出较低的潜在甲烷产生量和产甲烷菌多样性。泥炭上层和深层的样本均以与水稻菌群-I氢营养型产甲烷菌相关的三组序列为主。尽管灰分处理地块的pH值略高,但这些序列的出现不受灰分施肥的影响。有趣的是,仅在施肥地块中发现了一组与芬菌群相关的不太常见的序列。该研究证实了泥炭地产甲烷菌种群与深度相关的变化。

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