Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG

Detalhes bibliográficos
Ano de defesa: 2007
Autor(a) principal: Neri, Andreza Viana
Orientador(a): Meira Neto, João Augusto Alves lattes
Banca de defesa: Carmo, Flávia Maria da Silva lattes, Gato, Otília da Conceição Alves Correia Vale de
Tipo de documento: Tese
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Viçosa
Programa de Pós-Graduação: Doutorado em Botânica
Departamento: Botânica estrutural; Ecologia e Sistemática
País: BR
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: http://locus.ufv.br/handle/123456789/345
Resumo: The Cerrado physiognomic and structural mosaic is determined greatly by the soil fertility gradient, as well as by the irregularity of fire occurrence. The factors have an influence on the structure and floristic composition of the vegetation. Therefore, this work aims to classify the Paraopeba National Forest soils in Minas Gerais and to study the community and vegetation population variation according to the soils physical and chemical characteristics. Samples were collected with an auger and morphological observations were made for soil description in five different profile locations. For the routine chemical and granulometric analysis soil samples were collected every ten cm until the depth of 30cm, and from then on every 20cm until 150cm, with a total of nine samples per profile. The color, detailed morphological characteristics and P content were determined only for the 0-20cm and 0-40cm depth samples. Floristic composition and structure analysis were determined from a phytosociological sample of the woody vegetation, using the plot method. For sampling, five 20 x 100m plots were set out, totalizing 1 ha, where only the individuals with a soil height circumference (CAS) ≥ 10 cm were included. The floristic variation analysis was verified by floristic similarity in between the five plots and the structural variation through the analysis of the dissimilarity in which absolute density and dominance were used. Four soil classes were sampled, Red Latosoil, Red-yellow Latosoil, Yellow Latosoil and Cambisoil. The total FLONA richness was of 132 species distributed in 47 families. Of the species sampled, 111 were identified to species level, 12 to genus level, four to family level and five remained undetermined. The families that presented greatest richness were Fabaceae (18 species), Myrtaceae (9), Vochysiaceae (8), Bignoniaceae (7), Malpighiaceae (6), Rubiaceae (6), Anacardiaceae, Annonaceae, Erythroxylaceae e Melastomataceae (4). The five studied areas proved to be floristically and structurally distinct. A structural variation exists along the Paraopeba FLONA, even within the areas with equal phytophysiognomies as in the Cerrado s.s. over CXb and the Cerrado s.s. over LA. The variation of the Cerrado vegetation in the Paraopeba FLONA relates to the pedological variations encountered. Richness is positively correlated to fertility and negatively correlated to the aluminum content. The floristic similarity doesn t relate to the gradients, being influenced before that by the proximity of samples. The structural variation is less related to fertility than to aluminum. Some species showed a preference to certain environments as for example, Miconia albicans, that presented large densities where the aluminum content was high. Dilodendron bipinnatum was present only where the aluminum content was low, but with high Ca2+ content. Alibertia edulis and Myrcia tomentosa occurred together associated to lower aluminum content and larger basal areas, which is being interpreted as less tolerance to aluminum and more tolerance to shading. Xylopia aromatica occurred associated to larger aluminum content and larger basal areas, which is being interpreted as larger tolerance to aluminum and shading. The pedological factors, especially aluminum, have a strong influence on physiognomy, floristic composition and the structure of the Cerrado in the Paraopeba FLONA.
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spelling Neri, Andreza Vianahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4777187T2Schaefer, Carlos Ernesto Gonçalves Reynaudhttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4723204Y8Souza, Agostinho Lopes dehttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4787807J6Meira Neto, João Augusto Alveshttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4728376H9Carmo, Flávia Maria da Silvahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4727338J9Gato, Otília da Conceição Alves Correia Vale de2015-03-26T12:19:16Z2008-03-052015-03-26T12:19:16Z2007-03-23NERI, Andreza Viana. Pedological-vegetation gradient of Cerrado in Paraopeba, MG. 2007. 141 f. Tese (Doutorado em Botânica estrutural; Ecologia e Sistemática) - Universidade Federal de Viçosa, Viçosa, 2007.http://locus.ufv.br/handle/123456789/345The Cerrado physiognomic and structural mosaic is determined greatly by the soil fertility gradient, as well as by the irregularity of fire occurrence. The factors have an influence on the structure and floristic composition of the vegetation. Therefore, this work aims to classify the Paraopeba National Forest soils in Minas Gerais and to study the community and vegetation population variation according to the soils physical and chemical characteristics. Samples were collected with an auger and morphological observations were made for soil description in five different profile locations. For the routine chemical and granulometric analysis soil samples were collected every ten cm until the depth of 30cm, and from then on every 20cm until 150cm, with a total of nine samples per profile. The color, detailed morphological characteristics and P content were determined only for the 0-20cm and 0-40cm depth samples. Floristic composition and structure analysis were determined from a phytosociological sample of the woody vegetation, using the plot method. For sampling, five 20 x 100m plots were set out, totalizing 1 ha, where only the individuals with a soil height circumference (CAS) ≥ 10 cm were included. The floristic variation analysis was verified by floristic similarity in between the five plots and the structural variation through the analysis of the dissimilarity in which absolute density and dominance were used. Four soil classes were sampled, Red Latosoil, Red-yellow Latosoil, Yellow Latosoil and Cambisoil. The total FLONA richness was of 132 species distributed in 47 families. Of the species sampled, 111 were identified to species level, 12 to genus level, four to family level and five remained undetermined. The families that presented greatest richness were Fabaceae (18 species), Myrtaceae (9), Vochysiaceae (8), Bignoniaceae (7), Malpighiaceae (6), Rubiaceae (6), Anacardiaceae, Annonaceae, Erythroxylaceae e Melastomataceae (4). The five studied areas proved to be floristically and structurally distinct. A structural variation exists along the Paraopeba FLONA, even within the areas with equal phytophysiognomies as in the Cerrado s.s. over CXb and the Cerrado s.s. over LA. The variation of the Cerrado vegetation in the Paraopeba FLONA relates to the pedological variations encountered. Richness is positively correlated to fertility and negatively correlated to the aluminum content. The floristic similarity doesn t relate to the gradients, being influenced before that by the proximity of samples. The structural variation is less related to fertility than to aluminum. Some species showed a preference to certain environments as for example, Miconia albicans, that presented large densities where the aluminum content was high. Dilodendron bipinnatum was present only where the aluminum content was low, but with high Ca2+ content. Alibertia edulis and Myrcia tomentosa occurred together associated to lower aluminum content and larger basal areas, which is being interpreted as less tolerance to aluminum and more tolerance to shading. Xylopia aromatica occurred associated to larger aluminum content and larger basal areas, which is being interpreted as larger tolerance to aluminum and shading. The pedological factors, especially aluminum, have a strong influence on physiognomy, floristic composition and the structure of the Cerrado in the Paraopeba FLONA.O mosaico fisionômico e estrutural do Cerrado é determinado em grande parte por manchas de solos com fertilidade variável, bem como pela irregularidade da ação do fogo. Esses fatores exercem influência conjunta sobre a estrutura e sobre a composição florística da vegetação. O presente trabalho teve como objetivo identificar os solos da Floresta Nacional de Paraopeba, MG e estudar variações na comunidade e nas populações da vegetação lenhosa em função das características químicas e físicas do solo. Para a descrição dos solos foram feitas tradagens e foram abertos cinco perfis em áreas representativas. Para análise química e granulométrica de rotina foram coletadas amostras de dez em dez cm, até a profundidade de 30cm, e a partir daí de 20 em 20cm até 150cm, totalizando nove amostras por perfil. A cor, as características morfológicas detalhadas e os teores de fósforo total, foram determinados apenas nas amostras de 0- 20cm e de 40-60cm de profundidade. Para estudos quantitativos, a composição florística e a análise de estrutura foram determinadas a partir de uma amostra fitossociológica da vegetação lenhosa, utilizando o método de parcelas. Para amostragem foram alocadas cinco parcelas de 20 x 100m, totalizando 1 ha, onde apenas os indivíduos com circunferência à altura do solo (CAS) ≥ 10 cm foram incluídos. A análise de variação florística foi verificada por meio da similaridade florística entre as cinco parcelas e a variação estrutural através da análise de dissimilaridade utilizando os parâmetros: densidade e dominância absolutas. Foram identificadas quatro classes de solos: Latossolo Vermelho (LV), Latossolo Vermelho Amarelo (LVA), Latossolo Amarelo (LA) e Cambissolo (CXb). A riqueza total na FLONA foi de 132 espécies distribuídas em 47 famílias. Das espécies amostradas 111 foram identificadas em nível de espécie, 12 em gênero, quatro em família e cinco permaneceram indeterminadas. As famílias que apresentaram maiores riquezas foram Fabaceae (18 espécies), Myrtaceae (9), Vochysiaceae (8), Bignoniaceae (7), Malpighiaceae (6), Rubiaceae (6), Anacardiaceae, Annonaceae, Erythroxylaceae e Melastomataceae (4). As cinco áreas estudadas mostraram ser distintas tanto floristicamente quanto estruturalmente. Ao longo da FLONA de Paraopeba existe uma variação estrutural mesmo entre as áreas de mesma fitofisionomia, como é o caso do cerrado stricto sensu sobre CXb e o cerrado s.s. sobre LA. A variação na vegetação de Cerrado da FLONA de Paraopeba se relaciona com as mudanças pedológicas encontradas. A riqueza florística correlacionou-se positivamente a fertilidade e negativamente aos teores de alumínio. A similaridade florística entre as áreas estudadas não se relaciona aos gradientes pedológicos sendo antes influenciada pela proximidade entre as amostras. A variação estrutural está menos relacionada à fertilidade do que ao alumínio. Algumas espécies mostraram preferência por determinados ambientes, como por exemplo, Miconia albicans, apresentando grandes densidades onde os teores de alumínio eram maiores. Dilodendron bipinnatum esteve presente apenas onde o teor de alumínio foi baixo, mas com altos teores de Ca2+. Alibertia edulis e Myrcia tomentosa ocorreram de maneira associada a menores teores de alumínio e maiores áreas basais, sendo assim interpretado como menor tolerância ao alumínio e maior tolerância ao sombreamento. Xylopia aromatica ocorreu de maneira associada a maiores teores de alumínio e maiores áreas basais, sendo considerada mais tolerante a alumínio e ao sombreamento. Com este estudo é possível concluir que os fatores pedológicos, especialmente o alumínio, exercem forte influência na fisionomia, na composição florística e na estrutura do Cerrado na FLONA de Paraopeba.Universidade Federal de Viçosaapplication/pdfporUniversidade Federal de ViçosaDoutorado em BotânicaUFVBRBotânica estrutural; Ecologia e SistemáticaCerradoRelação solo/plantaEstruturaFlorísticaCerradoSoil/plant relationshipStructureFloristicCNPQ::CIENCIAS BIOLOGICAS::BOTANICAGradiente pedológico-vegetacional de Cerrado em Paraopeba, MGPedological-vegetation gradient of Cerrado in Paraopeba, MGinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/openAccessreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINALtexto completo.pdfapplication/pdf1552821https://locus.ufv.br//bitstream/123456789/345/1/texto%20completo.pdfd1625dc1801ff6cf8ede980da0027e19MD51TEXTtexto completo.pdf.txttexto completo.pdf.txtExtracted texttext/plain265125https://locus.ufv.br//bitstream/123456789/345/2/texto%20completo.pdf.txta93c2abdb6aacd2b180c235da6d2416bMD52THUMBNAILtexto completo.pdf.jpgtexto completo.pdf.jpgIM Thumbnailimage/jpeg3731https://locus.ufv.br//bitstream/123456789/345/3/texto%20completo.pdf.jpg1459fce80c5f467d341e279d46112ea3MD53123456789/3452016-04-06 23:01:44.109oai:locus.ufv.br:123456789/345Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452016-04-07T02:01:44LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.por.fl_str_mv Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
dc.title.alternative.eng.fl_str_mv Pedological-vegetation gradient of Cerrado in Paraopeba, MG
title Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
spellingShingle Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
Neri, Andreza Viana
Cerrado
Relação solo/planta
Estrutura
Florística
Cerrado
Soil/plant relationship
Structure
Floristic
CNPQ::CIENCIAS BIOLOGICAS::BOTANICA
title_short Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
title_full Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
title_fullStr Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
title_full_unstemmed Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
title_sort Gradiente pedológico-vegetacional de Cerrado em Paraopeba, MG
author Neri, Andreza Viana
author_facet Neri, Andreza Viana
author_role author
dc.contributor.authorLattes.por.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4777187T2
dc.contributor.author.fl_str_mv Neri, Andreza Viana
dc.contributor.advisor-co1.fl_str_mv Schaefer, Carlos Ernesto Gonçalves Reynaud
dc.contributor.advisor-co1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4723204Y8
dc.contributor.advisor-co2.fl_str_mv Souza, Agostinho Lopes de
dc.contributor.advisor-co2Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4787807J6
dc.contributor.advisor1.fl_str_mv Meira Neto, João Augusto Alves
dc.contributor.advisor1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4728376H9
dc.contributor.referee1.fl_str_mv Carmo, Flávia Maria da Silva
dc.contributor.referee1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4727338J9
dc.contributor.referee2.fl_str_mv Gato, Otília da Conceição Alves Correia Vale de
contributor_str_mv Schaefer, Carlos Ernesto Gonçalves Reynaud
Souza, Agostinho Lopes de
Meira Neto, João Augusto Alves
Carmo, Flávia Maria da Silva
Gato, Otília da Conceição Alves Correia Vale de
dc.subject.por.fl_str_mv Cerrado
Relação solo/planta
Estrutura
Florística
topic Cerrado
Relação solo/planta
Estrutura
Florística
Cerrado
Soil/plant relationship
Structure
Floristic
CNPQ::CIENCIAS BIOLOGICAS::BOTANICA
dc.subject.eng.fl_str_mv Cerrado
Soil/plant relationship
Structure
Floristic
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS BIOLOGICAS::BOTANICA
description The Cerrado physiognomic and structural mosaic is determined greatly by the soil fertility gradient, as well as by the irregularity of fire occurrence. The factors have an influence on the structure and floristic composition of the vegetation. Therefore, this work aims to classify the Paraopeba National Forest soils in Minas Gerais and to study the community and vegetation population variation according to the soils physical and chemical characteristics. Samples were collected with an auger and morphological observations were made for soil description in five different profile locations. For the routine chemical and granulometric analysis soil samples were collected every ten cm until the depth of 30cm, and from then on every 20cm until 150cm, with a total of nine samples per profile. The color, detailed morphological characteristics and P content were determined only for the 0-20cm and 0-40cm depth samples. Floristic composition and structure analysis were determined from a phytosociological sample of the woody vegetation, using the plot method. For sampling, five 20 x 100m plots were set out, totalizing 1 ha, where only the individuals with a soil height circumference (CAS) ≥ 10 cm were included. The floristic variation analysis was verified by floristic similarity in between the five plots and the structural variation through the analysis of the dissimilarity in which absolute density and dominance were used. Four soil classes were sampled, Red Latosoil, Red-yellow Latosoil, Yellow Latosoil and Cambisoil. The total FLONA richness was of 132 species distributed in 47 families. Of the species sampled, 111 were identified to species level, 12 to genus level, four to family level and five remained undetermined. The families that presented greatest richness were Fabaceae (18 species), Myrtaceae (9), Vochysiaceae (8), Bignoniaceae (7), Malpighiaceae (6), Rubiaceae (6), Anacardiaceae, Annonaceae, Erythroxylaceae e Melastomataceae (4). The five studied areas proved to be floristically and structurally distinct. A structural variation exists along the Paraopeba FLONA, even within the areas with equal phytophysiognomies as in the Cerrado s.s. over CXb and the Cerrado s.s. over LA. The variation of the Cerrado vegetation in the Paraopeba FLONA relates to the pedological variations encountered. Richness is positively correlated to fertility and negatively correlated to the aluminum content. The floristic similarity doesn t relate to the gradients, being influenced before that by the proximity of samples. The structural variation is less related to fertility than to aluminum. Some species showed a preference to certain environments as for example, Miconia albicans, that presented large densities where the aluminum content was high. Dilodendron bipinnatum was present only where the aluminum content was low, but with high Ca2+ content. Alibertia edulis and Myrcia tomentosa occurred together associated to lower aluminum content and larger basal areas, which is being interpreted as less tolerance to aluminum and more tolerance to shading. Xylopia aromatica occurred associated to larger aluminum content and larger basal areas, which is being interpreted as larger tolerance to aluminum and shading. The pedological factors, especially aluminum, have a strong influence on physiognomy, floristic composition and the structure of the Cerrado in the Paraopeba FLONA.
publishDate 2007
dc.date.issued.fl_str_mv 2007-03-23
dc.date.available.fl_str_mv 2008-03-05
2015-03-26T12:19:16Z
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dc.identifier.citation.fl_str_mv NERI, Andreza Viana. Pedological-vegetation gradient of Cerrado in Paraopeba, MG. 2007. 141 f. Tese (Doutorado em Botânica estrutural; Ecologia e Sistemática) - Universidade Federal de Viçosa, Viçosa, 2007.
dc.identifier.uri.fl_str_mv http://locus.ufv.br/handle/123456789/345
identifier_str_mv NERI, Andreza Viana. Pedological-vegetation gradient of Cerrado in Paraopeba, MG. 2007. 141 f. Tese (Doutorado em Botânica estrutural; Ecologia e Sistemática) - Universidade Federal de Viçosa, Viçosa, 2007.
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dc.publisher.department.fl_str_mv Botânica estrutural; Ecologia e Sistemática
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