Soil pH modulates the activity of low-affinity methane oxidation in soils from the Amazon region.

IF 3.2 3区 生物学 Q2 BIOTECHNOLOGY & APPLIED MICROBIOLOGY Journal of Applied Microbiology Pub Date : 2025-01-06 DOI:10.1093/jambio/lxae303
Leandro Fonseca de Souza, Fernanda Mancini Nakamura, Marie Kroeger, Dasiel Obregon, Moacir Tuzzin de Moraes, Mariana Gomes Vicente, Marcelo Zacharias Moreira, Vivian Helena Pellizari, Siu Mui Tsai, Klaus Nüsslein
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Abstract

Aims: In the Amazon region, pastures are the main land use subsequent to deforestation and this change can result in soil acidification and degradation. Liming is a management practice to increase soil pH, important to recover degraded lands and increase soil fertility, but its impacts on soil methane cycling in tropical soils are unknown. Here we investigate the role of soil pH on methane uptake under high concentrations of the gas, manipulating pasture and forest soils pH by liming and evaluating the active methane cycling microbial community.

Methods and results: Top layer of forest and pasture soils were subjected to liming treatment and incubated with ∼10 000 ppm of 13CH4. Soil DNA was evaluated with Stable Isotopic Probing (SIP-DNA), methanotrophic abundance was quantified (pmoA gene), and high throughput sequencing of 16S rRNA was performed. Liming increased the methane uptake in both forest (∼10%) and pasture (∼25%) soils. Methanotrophs Methylocaldum spp. (type I) and potential methanotrophs in Beijerinckiaceae (type II) were identified to actively incorporate carbon from methane in limed pasture soils. In limed forest soils, Nitrososphaeraceae were identified as 13C-enriched taxa, indicating that ammonia oxidizers can oxidize methane in these soils.

Conclusions: Liming Amazonian pasture soils not only contributes to the fertility and recovery of degraded areas but also has the potential to improve the oxidation of methane at high concentrations of this gas.

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土壤pH调节亚马逊地区土壤低亲和力甲烷氧化活性。
目的:在亚马逊地区,牧场是森林砍伐后的主要土地用途,这种变化可能导致土壤酸化和退化。石灰化是一种提高土壤pH值的管理措施,对恢复退化土地和提高土壤肥力具有重要意义,但其对热带土壤甲烷循环的影响尚不清楚。本文研究了高浓度甲烷下土壤pH值对甲烷吸收的影响,通过石灰化和评估活跃甲烷循环微生物群落来控制牧场和森林土壤pH值。方法和结果:对森林和牧场土壤表层进行石灰化处理,并用~ 10,000 ppm的13CH4孵育。采用稳定同位素探测法(SIP-DNA)评估土壤DNA,定量测定甲烷营养丰度(pmoA基因),并对16S rRNA进行高通量测序。石灰化增加了森林(~ 10%)和牧场(~ 25%)土壤的甲烷吸收量。鉴定出甲氧营养菌Methylocaldum sp. (I型)和Beijerinckiaceae潜在的甲氧营养菌(II型)在石灰化牧草土壤中积极吸收甲烷中的碳。在石灰化森林土壤中,亚硝基磷灰石科被鉴定为富含13c的类群,表明氨氧化剂可以氧化这些土壤中的甲烷。结论:对亚马逊草原土壤进行石灰化处理不仅有助于退化地区的肥力和恢复,而且具有改善高浓度甲烷氧化的潜力。
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来源期刊
Journal of Applied Microbiology
Journal of Applied Microbiology 生物-生物工程与应用微生物
CiteScore
7.30
自引率
2.50%
发文量
427
审稿时长
2.7 months
期刊介绍: Journal of & Letters in Applied Microbiology are two of the flagship research journals of the Society for Applied Microbiology (SfAM). For more than 75 years they have been publishing top quality research and reviews in the broad field of applied microbiology. The journals are provided to all SfAM members as well as having a global online readership totalling more than 500,000 downloads per year in more than 200 countries. Submitting authors can expect fast decision and publication times, averaging 33 days to first decision and 34 days from acceptance to online publication. There are no page charges.
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