Use este identificador para citar ou linkar para este item: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1166076
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dc.contributor.authorPRIMO, A. A.
dc.contributor.authorLUSTOSA FILHO, J. F.
dc.contributor.authorMAROTA, H. B.
dc.contributor.authorTONUCCI, R. G.
dc.contributor.authorSILVA, I. R. da
dc.contributor.authorOLIVEIRA, T. S. de
dc.date.accessioned2024-07-30T18:05:57Z-
dc.date.available2024-07-30T18:05:57Z-
dc.date.created2024-07-30
dc.date.issued2024
dc.identifier.citationPedobiologia - Journal of Soil Ecology, v. 106, 150985, 2024.
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1166076-
dc.descriptionSoil organic matter (SOM) is the main pathway of carbon (C) input to the soil with the decomposition of shoot residues, roots and their exudates. The objective was to evaluate the contribution of different vegetal composition and plant parts of Caatinga species and the effects of introducing a grass in the soil microbial community structure and biochemical composition of SOM. A trial was conducted under controlled conditions (120 days) using, separately, the shoot and roots residues of native species from the herbaceous (HERB) and shrub-arboreal (ARB) strata and a grass (GRASS). Megathyrsus maximum, which is native from Africa, but well adapted to the semi-arid conditions of Brazil, was used. Combinations of these species in different proportions were also evaluated: (i) 55 % shrub and trees + 45 % grass (MIX1) and (ii) 75 % shrub and trees + 25 % grass (MIX2). At the end of incubation, soil samples were collected to evaluate the microbial community structure through the phospholipid fatty acids (PLFA). Physical fractioning of SOM into particulate organic matter (POM) and mineralassociated organic matter (MAOM) was also performed, followed by biochemical characterization of these fractions by thermochemolysis analysis. The ARB shoot residue resulted in a 181.5 % increase (p < 0.05) in total PLFA biomass in the soil. A significant increase (p < 0.05) in the abundance of fungi and bacteria was observed with the incorporation of shoot residues. MAOM was characterized by a higher abundance of aliphatic (31.6 ± 5.0 %) and nitrogen-bearing compounds (21.0 ± 2.0 %), while higher lignin derivatives were observed in POM (18.0 ± 0.6 %). The ground cover provided a diversity of compounds in the SOM, thus regulating the structure of the microbial community. These results highlight the importance of conserving biodiversity, both in natural ecosystems and in agroecosystems in the semi-arid environment.
dc.language.isoeng
dc.rightsopenAccess
dc.subjectThermochemolysis
dc.subjectPOM
dc.subjectMAOM
dc.subjectComunidade microbiana
dc.titleDifferent composition of plant residues as a driver of microbial community structure and soil organic matter composition: a microcosm study.
dc.typeArtigo de periódico
dc.subject.thesagroCaatinga
dc.subject.thesagroMatéria Orgânica
dc.subject.thesagroSolo
riaa.ainfo.id1166076
riaa.ainfo.lastupdate2024-07-30
dc.identifier.doihttps://doi.org/10.1016/j.pedobi.2024.150985
dc.contributor.institutionANACLAUDIA ALVES PRIMO, UNIVERSIDADE FEDERAL DO CEARÁ; JOSE FERREIRA LUSTOSA FILHO; HELEN BOTELHO MAROTA, UNIVERSIDADE FEDERAL DE VIÇOSA; RAFAEL GONCALVES TONUCCI, CNPGL; IVO RIBEIRO DA SILVA, UNIVERSIDADE FEDERAL DE VIÇOSA; TEOGENES SENNA DE OLIVEIRA, UNIVERSIDADE FEDERAL DE VIÇOSA.
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