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| Registros recuperados : 330 | |
| 14. |  | MARTINS, E. de S.; BRAGA, A. R. dos S. Cartografia de paisagens do bioma cerrado e funcionamento de solos representativos. In: MOSTRA DE RESULTADOS DE PESQUISA DOS PROJETOS FINALIZADOS EM 2006 E 2007, 2., 2009, Planaltina, DF. [Anais...]. Planaltina, DF: Embrapa Cerrados, 2009. p. 86-93. (Embrapa Cerrados. Documentos, 244). Editores técnicos Eduardo Cyrino de Oliveira-Filho, Fernando Antônio Macena da Silva, Maria Lucia Meirelles, Eduardo Alano Vieira, Geraldo Bueno Martha Junior, Arminda Moreira de Carvalho, José Carlos Sousa e Silva, CPAC.| Biblioteca(s): Embrapa Cerrados. |
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| Registros recuperados : 330 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Cerrados; Embrapa Unidades Centrais. |
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Data corrente: |
13/12/2022 |
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Data da última atualização: |
13/12/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
BRUAND, A.; BRAGA, A. R. dos S.; MARTINS, E. de S. |
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Afiliação: |
ARY BRUAND, INSTITUT DES SCIENCES DE LA TERRA D'ORLÉANS; ADRIANA REATTO DOS SANTOS BRAGA, GGPP; EDER DE SOUZA MARTINS, CPAC. |
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Título: |
Allochthonous material originating from saprolite as a marker of termite activity in Ferralsols. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Scientifc Reports, v. 12, e17193, 2022. |
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DOI: |
https://doi.org/10.1038/s41598-022-21613-6 |
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Idioma: |
Inglês |
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Notas: |
Na publicação: Adriana Reatto. |
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Conteúdo: |
Ferralsols, which are estimated to cover 7.5 millions km² worldwide, are deeply weathered red or yellow soils found in the humid tropics. They are considered as the end of a geochemical sequence of weathering and are dominated by low-activity clay and sesquioxides. Their physical properties are closely related to their strong submillimetric granular structure. We aimed to characterize the 2:1 clay minerals identified in many Ferralsols and to discuss them as a marker of soil-feeding termite activity in Ferralsols. We present results recorded with Brazilian Ferralsols developed under Cerrado native vegetation on a range of parent materials. It was found that the 2:1 minerals vary from weakly weathered muscovite to hydroxy-Al interlayered vermiculite, sometimes associated to a fine material with a chemical composition highly different from that of the groundmass of the surrounding submillimetric granular aggregates. Results show that both 2:1 minerals and the associated fine material have to be considered as allochthonous material originating from the saprolite and were brought to the Ferralsol by soil-feeding termite activity. This confirms the major role of termites in the properties of Ferralsols and raises questions about the possible consequences of land use change which usually deeply affects soil biodiversity. |
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Thesagro: |
Biodiversidade; Cerrado; Composição Química; Vegetação Nativa. |
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Thesaurus NAL: |
Biodiversity; Chemical composition; Ferralsols; Saprolite; Soil physical properties; Vermiculite. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1149589/1/Allochthonous-material-originating-2022.pdf
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Marc: |
LEADER 02215naa a2200289 a 4500
001 2149589
005 2022-12-13
008 2022 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1038/s41598-022-21613-6$2DOI
100 1 $aBRUAND, A.
245 $aAllochthonous material originating from saprolite as a marker of termite activity in Ferralsols.$h[electronic resource]
260 $c2022
500 $aNa publicação: Adriana Reatto.
520 $aFerralsols, which are estimated to cover 7.5 millions km² worldwide, are deeply weathered red or yellow soils found in the humid tropics. They are considered as the end of a geochemical sequence of weathering and are dominated by low-activity clay and sesquioxides. Their physical properties are closely related to their strong submillimetric granular structure. We aimed to characterize the 2:1 clay minerals identified in many Ferralsols and to discuss them as a marker of soil-feeding termite activity in Ferralsols. We present results recorded with Brazilian Ferralsols developed under Cerrado native vegetation on a range of parent materials. It was found that the 2:1 minerals vary from weakly weathered muscovite to hydroxy-Al interlayered vermiculite, sometimes associated to a fine material with a chemical composition highly different from that of the groundmass of the surrounding submillimetric granular aggregates. Results show that both 2:1 minerals and the associated fine material have to be considered as allochthonous material originating from the saprolite and were brought to the Ferralsol by soil-feeding termite activity. This confirms the major role of termites in the properties of Ferralsols and raises questions about the possible consequences of land use change which usually deeply affects soil biodiversity.
650 $aBiodiversity
650 $aChemical composition
650 $aFerralsols
650 $aSaprolite
650 $aSoil physical properties
650 $aVermiculite
650 $aBiodiversidade
650 $aCerrado
650 $aComposição Química
650 $aVegetação Nativa
700 1 $aBRAGA, A. R. dos S.
700 1 $aMARTINS, E. de S.
773 $tScientifc Reports$gv. 12, e17193, 2022.
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