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将亚马逊雨林转变为农业用地会改变甲烷循环生物的群落特征。

Conversion of Amazon rainforest to agriculture alters community traits of methane-cycling organisms.

作者信息

Meyer Kyle M, Klein Ann M, Rodrigues Jorge L M, Nüsslein Klaus, Tringe Susannah G, Mirza Babur S, Tiedje James M, Bohannan Brendan J M

机构信息

Institute of Ecology and Evolution, Department of Biology, University of Oregon, Eugene, OR, USA.

Department of Land, Air and Water Resources, University of California, Davis, CA, USA.

出版信息

Mol Ecol. 2017 Mar;26(6):1547-1556. doi: 10.1111/mec.14011. Epub 2017 Feb 10.

Abstract

Land use change is one of the greatest environmental impacts worldwide, especially to tropical forests. The Amazon rainforest has been subject to particularly high rates of land use change, primarily to cattle pasture. A commonly observed response to cattle pasture establishment in the Amazon is the conversion of soil from a methane sink in rainforest, to a methane source in pasture. However, it is not known how the microorganisms that mediate methane flux are altered by land use change. Here, we use the deepest metagenomic sequencing of Amazonian soil to date to investigate differences in methane-cycling microorganisms and their traits across rainforest and cattle pasture soils. We found that methane-cycling microorganisms responded to land use change, with the strongest responses exhibited by methane-consuming, rather than methane-producing, microorganisms. These responses included a reduction in the relative abundance of methanotrophs and a significant decrease in the abundance of genes encoding particulate methane monooxygenase. We also observed compositional changes to methanotroph and methanogen communities as well as changes to methanotroph life history strategies. Our observations suggest that methane-cycling microorganisms are vulnerable to land use change, and this vulnerability may underlie the response of methane flux to land use change in Amazon soils.

摘要

土地利用变化是全球范围内最大的环境影响之一,对热带森林的影响尤为显著。亚马孙雨林的土地利用变化率特别高,主要转变为牧场。在亚马孙地区,人们普遍观察到,随着牧场的建立,土壤从雨林中的甲烷汇转变为牧场中的甲烷源。然而,尚不清楚介导甲烷通量的微生物如何因土地利用变化而改变。在此,我们利用迄今为止对亚马孙土壤进行的深度宏基因组测序,来研究雨林土壤和牧场土壤中甲烷循环微生物及其特征的差异。我们发现,甲烷循环微生物对土地利用变化有响应,其中消耗甲烷而非产生甲烷的微生物表现出最强的响应。这些响应包括甲烷营养菌相对丰度的降低以及编码颗粒状甲烷单加氧酶的基因丰度的显著下降。我们还观察到甲烷营养菌和产甲烷菌群落的组成变化以及甲烷营养菌生活史策略的变化。我们的观察结果表明,甲烷循环微生物易受土地利用变化的影响,这种脆弱性可能是亚马孙土壤中甲烷通量对土地利用变化作出响应的基础。

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