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Registro Completo |
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Biblioteca(s): |
Embrapa Tabuleiros Costeiros. |
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Data corrente: |
02/08/1996 |
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Data da última atualização: |
02/08/1996 |
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Autoria: |
LEAO, A. C.; MELO, A. A. O. de. |
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Título: |
Morfologia, mineralogia e caracteristicas fisico-quimicas dos principais solos de cacau da Bahia, Brasil. |
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Ano de publicação: |
1988 |
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Fonte/Imprenta: |
Revista Theobroma, Ilheus, v.18, n.1, p.1-18, jan./mar. 1988. |
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Idioma: |
Português |
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Conteúdo: |
O Estado da Bahia produz aproximadamente 90% do cacau brasileiro. A area cultivada situa-se no Sudeste do Estado, onde existe uma grande variedade de solos. Dados obtidos a partir de "(perfis) descritos e analisados permitiram caracterizar os solos tradicionais de cacau sob os aspectos morfologico, fisico, quimico e mineralogico e classifica-los segundo o Soil taxonomy (SSS-USDA) e Sistema Brasileiro (SNLCS/EMBRAPA). As principais unidades identificadas sao as seguintes: Cepec (Tropudalf ou Podzolico Vermelho Amarelo eutrofico Ta A moderado textura argilosa fase floresta perenifolia relevo suave ondulado e ondulado): Itabuna (Tropudalf ou Podzolico Vermelho Amarelo eutrofico Ta A moderado textura media/argilosa fase floresta perenifolia relevo ondulado); Morro Redondo (Tropodult ou Podzolico Vermelho Amarelo Tb A moderado textura argilosa/muito argilosa fase floresta perenifolia relevo ondulado, forte ondulado e montanhoso); Agua sumida Umbriorthox ou Latossolo Vermelho Amarelo distrofico textura argilosa fase floresta perenifolia relevo forte ondulado e montanhoso. |
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Palavras-Chave: |
Morfologia; Morphology; Solos; Tableland; Tabuleiros. |
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Thesagro: |
Mineralogia; Podzólico Vermelho Amarelo. |
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Thesaurus Nal: |
mineralogy; soil. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 01753naa a2200241 a 4500
001 1355020
005 1996-08-02
008 1988 bl uuuu u00u1 u #d
100 1 $aLEAO, A. C.
245 $aMorfologia, mineralogia e caracteristicas fisico-quimicas dos principais solos de cacau da Bahia, Brasil.
260 $c1988
520 $aO Estado da Bahia produz aproximadamente 90% do cacau brasileiro. A area cultivada situa-se no Sudeste do Estado, onde existe uma grande variedade de solos. Dados obtidos a partir de "(perfis) descritos e analisados permitiram caracterizar os solos tradicionais de cacau sob os aspectos morfologico, fisico, quimico e mineralogico e classifica-los segundo o Soil taxonomy (SSS-USDA) e Sistema Brasileiro (SNLCS/EMBRAPA). As principais unidades identificadas sao as seguintes: Cepec (Tropudalf ou Podzolico Vermelho Amarelo eutrofico Ta A moderado textura argilosa fase floresta perenifolia relevo suave ondulado e ondulado): Itabuna (Tropudalf ou Podzolico Vermelho Amarelo eutrofico Ta A moderado textura media/argilosa fase floresta perenifolia relevo ondulado); Morro Redondo (Tropodult ou Podzolico Vermelho Amarelo Tb A moderado textura argilosa/muito argilosa fase floresta perenifolia relevo ondulado, forte ondulado e montanhoso); Agua sumida Umbriorthox ou Latossolo Vermelho Amarelo distrofico textura argilosa fase floresta perenifolia relevo forte ondulado e montanhoso.
650 $amineralogy
650 $asoil
650 $aMineralogia
650 $aPodzólico Vermelho Amarelo
653 $aMorfologia
653 $aMorphology
653 $aSolos
653 $aTableland
653 $aTabuleiros
700 1 $aMELO, A. A. O. de
773 $tRevista Theobroma, Ilheus$gv.18, n.1, p.1-18, jan./mar. 1988.
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Embrapa Tabuleiros Costeiros (CPATC) |
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Registro Completo
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Biblioteca(s): |
Embrapa Cerrados; Embrapa Florestas. |
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Data corrente: |
18/04/2022 |
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Data da última atualização: |
11/07/2022 |
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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: |
LAVELLE, P.; MATHIEU, J.; SPAIN. A.; BROWN, G. G.; FRAGOSO, C.; LAPIED, E.; AQUINO, A. de; BAROIS, I.; BARRIOS, E.; BARROS, M. E.; BEDANO, J. C.; BLANCHART, E.; CAULFIELD, M.; CHAGUEZA, Y.; DAI, J.; DECAËNS, T.; DOMINGUEZ, A.; DOMINGUEZ, Y.; FEIJOO, A.; FOLGARAIT, P.; FONTE, S. J.; GOROSITO, N.; HUERTA, E.; JIMENEZ, J. J.; KELLY, C.; LORANGER, G.; MARCHAO, R. L.; MARICHAL, R.; PRAXEDES, C.; RODRIGUEZ, L.; ROUSSEAU, G.; ROUSSEAU, L.; RUIZ, N.; SANABRIA, C.; SUAREZ, J. C.; TONDOH, J. E.; VALENÇA, A. de; VANEK, S. J.; VASQUEZ, J.; VELASQUEZ, E.; WEBSTER, E.; ZHANG, C. |
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Afiliação: |
PATRICK LAVELLE, Université Paris-Sorbonne Nouvelle; JÉRÔME MATHIEU, Université Paris-Sorbonne Nouvelle; ALISTER SPAIN; GEORGE GARDNER BROWN, CNPF; CARLOS FRAGOSO, Red Biodiversidad y Sistemática, Instituto de Ecologia A.C., Xalapa; EMMANUEL LAPIED, Taxonomia Biodiversity Fund.; ADRIANA DE AQUINO; ISABELLE BAROIS, Red Ecología Funcional, Instituto de Ecologia A.C., Xalapa; EDMUNDO BARRIOS, FAO; MARIA ELEUSA BARROS, Université Paris-Sorbonne Nouvelle; JOSÉ CAMILO BEDANO, Universidad Nacional de Rio Cuarto; ERIC BLANCHART, Eco& Sols, Université de Montpellier, IRD, CIRAD, INRAe, Institut Agro; MARK CAULFIELD, Eco& Sols, Université de Montpellier, IRD, CIRAD, INRAe, Institut Agro; Wageningen University; YAMILETH CHAGUEZA, Universidad Nacional de Colombia; JUN DAI, South China Agricultural University; THIBAUD DECAËNS, Centre d'Ecologie Fonctionnelle et Evolutive; ANAHI DOMINGUEZ, Universidad Nacional de Rio Cuarto; YAMILETH DOMINGUEZ, Universidad del Atlántico; ALEXANDER FEIJOO, Universidad Tecnológica de Pereira; PATRICIA FOLGARAIT, Universidad Nacional de Quilmes; STEVEN J. FONTE, Colorado State University; NORMA GOROSITO, Universidad Nacional de Quilmes; ESPERANZA HUERTA, HUERTA; Wageningen University and Research; JUAN JOSE JIMENEZ, Pyrenean Institute of Ecology; COURTLAND KELLY, Colorado State University; GLADYS LORANGER, Université des Antilles; ROBELIO LEANDRO MARCHAO, CPAC; RAPHAEL MARICHAL, CIRAD; CATARINA PRAXEDES, Museu Paraense Emilio Goeldi; LEONARDO RODRIGUEZ, Universidad de la Amazonia; GUILLAUME ROUSSEAU, Maranhão State University; LAURENT ROUSSEAU, Université Paris-Sorbonne Nouvelle; NURIA RUIZ, French National Research Agency; CATALINA SANABRIA, UNIVALLE; JUAN CARLOS SUAREZ, Universidad de la Amazonia; JERÔME EBAGNERIN TONDOH, Université Nagui Abrogoua; ANNE DE VALENÇA, Wageningen University; STEVEN J. VANEK, Colorado State University; JOEL VASQUEZ, Instituto de Investigaciones de la Amazonia Peruana; Universidad Nacional de la Amazonia Peruana; ELENA VELASQUEZ, Universidad Nacional de Colombia; EMILY WEBSTER, University of California; CHI ZHANG, South China Agricultural University. |
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Título: |
Soil macroinvertebrate communities: a world-wide assessment. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Global Ecology and Biogeography, v. 31, n. 7, p. 1261-1276, 2022. |
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DOI: |
https://doi.org/10.1111/geb.13492 |
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Idioma: |
Inglês
Português |
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Conteúdo: |
AIM. Macroinvertebrates comprise a highly diverse set of taxa with great potential as indicators of soil quality. Communities were sampled at 3,694 sites distributed world-wide. We aimed to analyse the patterns of abundance, composition and network characteristics and their relationships to latitude, mean annual temperature and rainfall, land cover, soil texture and agricultural practices.
LOCATION. Sites are distributed in 41 countries, ranging from 55° S to 57° N latitude, from 0 to 4,000 m in elevation, with annual rainfall ranging from 500 to >3,000 mm and mean temperatures of 5?32°C.
TIME PERIOD. 1980-2018.
MAJOR TAXA STUDIED.
All soil macroinvertebrates: Haplotaxida; Coleoptera; Formicidae; Arachnida; Chilopoda; Diplopoda; Diptera; Isoptera; Isopoda; Homoptera; Hemiptera; Gastropoda; Blattaria; Orthoptera; Lepidoptera; Dermaptera; and ?others?.
METHODS.
Standard ISO 23611-5 sampling protocol was applied at all sites. Data treatment used a set of multivariate analyses, principal components analysis (PCA) on macrofauna data transformed by Hellinger?s method, multiple correspondence analysis for environmental data (latitude, elevation, temperature and average annual rainfall, type of vegetation cover) transformed into discrete classes, coinertia analysis to compare these two data sets, and bias-corrected and accelerated bootstrap tests to evaluate the part of the variance of the macrofauna data attributable to each of the environmental factors. Network analysis was performed. Each pairwise association of taxonomic units was tested against a null model considering local and regional scales, in order to avoid spurious correlations.
RESULTS
Communities were separated into five clusters reflecting their densities and taxonomic richness. They were significantly influenced by climatic conditions, soil texture and vegetation cover. Abundance and diversity, highest in tropical forests (1,895 ± 234 individuals/m2) and savannahs (1,796 ± 72 individuals/m2), progressively decreased in tropical cropping systems (tree-associated crops, 1,358 ± 120 individuals/m2; pastures, 1,178 ± 154 individuals/m2; and annual crops, 867 ± 62 individuals/m2), temperate grasslands (529 ± 60 individuals/m2), forests (232 ± 20 individuals/m2) and annual crops (231 ± 24 individuals/m2) and temperate dry forests and shrubs (195 ± 11 individuals/m2). Agricultural management decreased overall abundance by ≤54% in tropical areas and 64% in temperate areas. Connectivity varied with taxa, with dominant positive connections in litter transformers and negative connections with ecosystem engineers and Arachnida. Connectivity and modularity were higher in communities with low abundance and taxonomic richness.
MAIN CONCLUSIONS.
Soil macroinvertebrate communities respond to climatic, soil and land-cover conditions. All taxa, except termites, are found everywhere, and communities from the five clusters cover a wide range of geographical and environmental conditions. Agricultural practices significantly decrease abundance, although the presence of tree components alleviates this effect. MenosAIM. Macroinvertebrates comprise a highly diverse set of taxa with great potential as indicators of soil quality. Communities were sampled at 3,694 sites distributed world-wide. We aimed to analyse the patterns of abundance, composition and network characteristics and their relationships to latitude, mean annual temperature and rainfall, land cover, soil texture and agricultural practices.
LOCATION. Sites are distributed in 41 countries, ranging from 55° S to 57° N latitude, from 0 to 4,000 m in elevation, with annual rainfall ranging from 500 to >3,000 mm and mean temperatures of 5?32°C.
TIME PERIOD. 1980-2018.
MAJOR TAXA STUDIED.
All soil macroinvertebrates: Haplotaxida; Coleoptera; Formicidae; Arachnida; Chilopoda; Diplopoda; Diptera; Isoptera; Isopoda; Homoptera; Hemiptera; Gastropoda; Blattaria; Orthoptera; Lepidoptera; Dermaptera; and ?others?.
METHODS.
Standard ISO 23611-5 sampling protocol was applied at all sites. Data treatment used a set of multivariate analyses, principal components analysis (PCA) on macrofauna data transformed by Hellinger?s method, multiple correspondence analysis for environmental data (latitude, elevation, temperature and average annual rainfall, type of vegetation cover) transformed into discrete classes, coinertia analysis to compare these two data sets, and bias-corrected and accelerated bootstrap tests to evaluate the part of the variance of the macrofauna data attributable to each of the environmental factors. Network analysis was perf... Mostrar Tudo |
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Palavras-Chave: |
Banco de dados; Cobertura da terra; Communities; Ecologia do solo; Macrofauna; Macrofauna database; Macroinvertebrados; Network analysis; Soil macroinvertebrates. |
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Thesaurus NAL: |
Land cover; Soil ecology. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 05077naa a2200757 a 4500
001 2142258
005 2022-07-11
008 2022 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1111/geb.13492$2DOI
100 1 $aLAVELLE, P.
245 $aSoil macroinvertebrate communities$ba world-wide assessment.$h[electronic resource]
260 $c2022
520 $aAIM. Macroinvertebrates comprise a highly diverse set of taxa with great potential as indicators of soil quality. Communities were sampled at 3,694 sites distributed world-wide. We aimed to analyse the patterns of abundance, composition and network characteristics and their relationships to latitude, mean annual temperature and rainfall, land cover, soil texture and agricultural practices. LOCATION. Sites are distributed in 41 countries, ranging from 55° S to 57° N latitude, from 0 to 4,000 m in elevation, with annual rainfall ranging from 500 to >3,000 mm and mean temperatures of 5?32°C. TIME PERIOD. 1980-2018. MAJOR TAXA STUDIED. All soil macroinvertebrates: Haplotaxida; Coleoptera; Formicidae; Arachnida; Chilopoda; Diplopoda; Diptera; Isoptera; Isopoda; Homoptera; Hemiptera; Gastropoda; Blattaria; Orthoptera; Lepidoptera; Dermaptera; and ?others?. METHODS. Standard ISO 23611-5 sampling protocol was applied at all sites. Data treatment used a set of multivariate analyses, principal components analysis (PCA) on macrofauna data transformed by Hellinger?s method, multiple correspondence analysis for environmental data (latitude, elevation, temperature and average annual rainfall, type of vegetation cover) transformed into discrete classes, coinertia analysis to compare these two data sets, and bias-corrected and accelerated bootstrap tests to evaluate the part of the variance of the macrofauna data attributable to each of the environmental factors. Network analysis was performed. Each pairwise association of taxonomic units was tested against a null model considering local and regional scales, in order to avoid spurious correlations. RESULTS Communities were separated into five clusters reflecting their densities and taxonomic richness. They were significantly influenced by climatic conditions, soil texture and vegetation cover. Abundance and diversity, highest in tropical forests (1,895 ± 234 individuals/m2) and savannahs (1,796 ± 72 individuals/m2), progressively decreased in tropical cropping systems (tree-associated crops, 1,358 ± 120 individuals/m2; pastures, 1,178 ± 154 individuals/m2; and annual crops, 867 ± 62 individuals/m2), temperate grasslands (529 ± 60 individuals/m2), forests (232 ± 20 individuals/m2) and annual crops (231 ± 24 individuals/m2) and temperate dry forests and shrubs (195 ± 11 individuals/m2). Agricultural management decreased overall abundance by ≤54% in tropical areas and 64% in temperate areas. Connectivity varied with taxa, with dominant positive connections in litter transformers and negative connections with ecosystem engineers and Arachnida. Connectivity and modularity were higher in communities with low abundance and taxonomic richness. MAIN CONCLUSIONS. Soil macroinvertebrate communities respond to climatic, soil and land-cover conditions. All taxa, except termites, are found everywhere, and communities from the five clusters cover a wide range of geographical and environmental conditions. Agricultural practices significantly decrease abundance, although the presence of tree components alleviates this effect.
650 $aLand cover
650 $aSoil ecology
653 $aBanco de dados
653 $aCobertura da terra
653 $aCommunities
653 $aEcologia do solo
653 $aMacrofauna
653 $aMacrofauna database
653 $aMacroinvertebrados
653 $aNetwork analysis
653 $aSoil macroinvertebrates
700 1 $aMATHIEU, J.
700 1 $aSPAIN. A.
700 1 $aBROWN, G. G.
700 1 $aFRAGOSO, C.
700 1 $aLAPIED, E.
700 1 $aAQUINO, A. de
700 1 $aBAROIS, I.
700 1 $aBARRIOS, E.
700 1 $aBARROS, M. E.
700 1 $aBEDANO, J. C.
700 1 $aBLANCHART, E.
700 1 $aCAULFIELD, M.
700 1 $aCHAGUEZA, Y.
700 1 $aDAI, J.
700 1 $aDECAËNS, T.
700 1 $aDOMINGUEZ, A.
700 1 $aDOMINGUEZ, Y.
700 1 $aFEIJOO, A.
700 1 $aFOLGARAIT, P.
700 1 $aFONTE, S. J.
700 1 $aGOROSITO, N.
700 1 $aHUERTA, E.
700 1 $aJIMENEZ, J. J.
700 1 $aKELLY, C.
700 1 $aLORANGER, G.
700 1 $aMARCHAO, R. L.
700 1 $aMARICHAL, R.
700 1 $aPRAXEDES, C.
700 1 $aRODRIGUEZ, L.
700 1 $aROUSSEAU, G.
700 1 $aROUSSEAU, L.
700 1 $aRUIZ, N.
700 1 $aSANABRIA, C.
700 1 $aSUAREZ, J. C.
700 1 $aTONDOH, J. E.
700 1 $aVALENÇA, A. de
700 1 $aVANEK, S. J.
700 1 $aVASQUEZ, J.
700 1 $aVELASQUEZ, E.
700 1 $aWEBSTER, E.
700 1 $aZHANG, C.
773 $tGlobal Ecology and Biogeography$gv. 31, n. 7, p. 1261-1276, 2022.
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