Land use change affects soil methane sink capacity of Brazilian Biomes.

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dc.contributorLEONARDO MACHADO PITOMBO, SANEAMENTO DE GOIÁS S/A; HELIO DANILO QUEVEDO, FEDERAL UNIVERSITY OF SÃO CARLOS; DIANA SIGNOR DEON, CPATSA; CLAUDIA FERNANDA ALMEIDA TEIXEIRA-GANDRA, FEDERAL UNIVERSITY OF PELOTAS; RICARDO HIDEO TANIWAKI, FEDERAL UNIVERSITY OF ABC; CIMÉLIO BAYER, FEDERAL UNIVERSITY OF RIO GRANDE DO SUL; PAUL L. E. BODELIER, NETHERLANDS INSTITUTE OF ECOLOGY; JANAINA BRAGA DO CARMO, NETHERLANDS INSTITUTE OF ECOLOGY.
dc.creatorPITOMBO, L. M.
dc.creatorQUEVEDO, H. D.
dc.creatorSIGNOR, D.
dc.creatorGANDRA, C. F. A. T.
dc.creatorTANIWAKI, R. H.
dc.creatorBAYER, C.
dc.creatorBODELIER, P. L. E.
dc.creatorCARMO, J. B. do
dc.date2026-03-04T13:52:48Z
dc.date2026-03-04T13:52:48Z
dc.date2026-03-04
dc.date2026
dc.date.accessioned2026-07-07T06:01:39Z
dc.descriptionSoils are the only biological sink for atmospheric Methane (CH4), making microbial methane consumption a dynamic component of the global carbon cycle. However, land-use change toward agriculture can inhibit this process, partly due to the application of NH₄⁺-based fertilizers. To assess whether this effect contributes to reductions in CH₄ uptake following land-use change in Brazilian biomes, we incubated soils from natural and cultivated areas across four endangered biomes: Caatinga, Cerrado, Pampas, and Atlantic Forest. Among soils exhibiting net CH₄ uptake, natural soils oxidized an average of 11.9 μg C kg⁻¹ soil day⁻¹. Ammonium sulfate addition reduced CH₄ oxidation by 33% in pristine soils, whereas soils from agricultural fields showed no detectable methane uptake. With the exception of the Caatinga biome, pristine soils consumed atmospheric CH₄ and harbored higher abundances of methanotrophic bacteria compared to managed soils. Our findings indicate that nitrogen addition, at levels typical of NH₄⁺-based fertilization, had a less pronounced effect on CH₄ uptake than land-use change itself, underscoring the importance of conserving natural ecosystems to support the CH₄ cycle. Furthermore, soil nutrient availability, particularly micronutrients, emerged as a potential regulator of methanotrophy, capable of either stimulating or inhibiting microbial methane consumption. In the context of accelerated climate change in the tropics and globally, it is imperative to rethink agricultural practices, biomass production models, and land-use and fertilization strategies to minimize potential increases in greenhouse gas emissions.
dc.identifierDiscover Soil, v. 3, 8, 2026.
dc.identifier3005-1223
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1184931
dc.identifierhttps://doi.org/10.1007/s44378-026-00164-6
dc.identifier.urihttp://hdl.handle.net/123456789/504705
dc.languageeng
dc.rightsopenAccess
dc.subjectMetano do solo
dc.subjectBiomas brasileiros
dc.subjectBioma Caatinga
dc.subjectBioma Cerrado
dc.subjectBioma Pampas
dc.subjectBioma Mata Atlântica
dc.subjectEmissao de gases
dc.subjectEmissão de gases de efeito estufa
dc.subjectMudanca do clima
dc.subjectSolo
dc.subjectUso da Terra
dc.subjectEfeito Estufa
dc.subjectMudança Climática
dc.subjectGreenhouse gases
dc.subjectSoil
dc.subjectClimate change
dc.titleLand use change affects soil methane sink capacity of Brazilian Biomes.
dc.typeArtigo de periódico

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