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氮添加降低了毛竹林甲烷氧化菌和产甲烷菌失衡导致的甲烷吸收。

Nitrogen addition decreases methane uptake caused by methanotroph and methanogen imbalances in a Moso bamboo forest.

机构信息

Center for Ecological Forecasting and Global Change, College of Forestry, Northwest A&F University, Yangling, 712100, China.

State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Hangzhou, 311300, China.

出版信息

Sci Rep. 2021 Mar 10;11(1):5578. doi: 10.1038/s41598-021-84422-3.

Abstract

Forest soils play an important role in controlling global warming by reducing atmospheric methane (CH) concentrations. However, little attention has been paid to how nitrogen (N) deposition may alter microorganism communities that are related to the CH cycle or CH oxidation in subtropical forest soils. We investigated the effects of N addition (0, 30, 60, or 90 kg N ha yr) on soil CH flux and methanotroph and methanogen abundance, diversity, and community structure in a Moso bamboo (Phyllostachys edulis) forest in subtropical China. N addition significantly increased methanogen abundance but reduced both methanotroph and methanogen diversity. Methanotroph and methanogen community structures under the N deposition treatments were significantly different from those of the control. In N deposition treatments, the relative abundance of Methanoculleus was significantly lower than that in the control. Soil pH was the key factor regulating the changes in methanotroph and methanogen diversity and community structure. The CH emission rate increased with N addition and was negatively correlated with both methanotroph and methanogen diversity but positively correlated with methanogen abundance. Overall, our results suggested that N deposition can suppress CH uptake by altering methanotroph and methanogen abundance, diversity, and community structure in subtropical Moso bamboo forest soils.

摘要

森林土壤通过减少大气甲烷(CH)浓度在控制全球变暖方面发挥着重要作用。然而,人们对氮(N)沉降如何改变与 CH 循环或亚热带森林土壤 CH 氧化有关的微生物群落关注甚少。我们研究了氮添加(0、30、60 或 90 kg N ha yr)对中国亚热带毛竹(Phyllostachys edulis)林土壤 CH 通量以及甲烷营养菌和产甲烷菌丰度、多样性和群落结构的影响。氮添加显著增加了产甲烷菌的丰度,但降低了甲烷营养菌和产甲烷菌的多样性。氮沉降处理下的甲烷营养菌和产甲烷菌群落结构与对照明显不同。在氮沉降处理中,甲烷杆菌属的相对丰度明显低于对照。土壤 pH 是调节甲烷营养菌和产甲烷菌多样性和群落结构变化的关键因素。CH 排放速率随氮添加而增加,与甲烷营养菌和产甲烷菌多样性呈负相关,但与产甲烷菌丰度呈正相关。总的来说,我们的结果表明,氮沉降可以通过改变亚热带毛竹林土壤中产甲烷菌和甲烷营养菌的丰度、多样性和群落结构来抑制 CH 的吸收。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/715d/7947007/4f5a418abcb5/41598_2021_84422_Fig1_HTML.jpg

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