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Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal

Detalhes bibliográficos
Autor(a) principal: Joly, Carlos Alfredo
Data de Publicação: 2012
Outros Autores: Assis, Marco Antonio [UNESP], Bernacci, Luis Carlos, Tamashiro, Jorge Yoshio, Rodrigues de Campos, Mariana Cruz, Mantelli Aboin Comes, Jose Ataliba, Lacerda, Maryland Sanchez, Maes dos Santos, Flavio Antonio, Pedroni, Fernando, Pereira, Larissa de Souza, Gorgulho Padgurschi, Maira de Campos, Borges Prata, Eduardo Magalhaes [UNESP], Ramos, Eliana, Torres, Roseli Buzanelli, Rochelle, Andre, Martins, Fernando Roberto, Alves, Luciana Ferreira, Vieira, Simone Aparecida, Martinelli, Luiz Antonio, de Camargo, Plinio Barbosa, Marinho Aidar, Marcos Pereira, Eisenlohr, Pedro Vasconcellos, Simoes, Eliane, Villani, Joao Paulo, Belinello, Renato
Tipo de documento: Artigo
Idioma: por
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://www.biotaneotropica.org.br/v12n1/pt/fullpaper?bn01812012012+pt
http://hdl.handle.net/11449/20331
Resumo: This paper summarizes floristic and phytossociology data of 11, out of 14 plots of 1 ha, allocated along an altitudinal gradient in the Serra do Mar, Silo Paulo, Brazil. The study was conducted at Serra do Mar State Park and the plots start at the sea level (10 m - plot of Restinga Forest that occurs at Praia da Fazenda, Picinguaba, municipality of Ubatuba) up to 1100 m above sea level (the Montane Ombrophilous Dense occurs alongside the Itamambuca Trail, municipality of Silo Luis do Paraitinga). The Restinga Forest occurs in Pleistocenic Coastal Plain where the soil is classified as a sandy Quartzipsamment (Quartzenic Neosol), while along the slopes of the Serra do Mar, the Ombrophylus Dense Forest grows on the top of a pre-Cambrian crystalline basement with granitic rocks, where the soil is a sandy-loam Dystrophic Inceptisol (Cambisol/Latosol). In all 14 plots soils are acidic (pH 3 - 4), chemically poor, with high dilution of nutrients and high saturation of aluminum. In the Restinga and at the foot of the slope the climate is Tropical/Subtropical Humid (Af/Cfa), with no dry season, an average annual rainfall over 2,200 mm and an average annual temperature of 22 degrees C. Towards the top of the Serra do Mar there is a gradual cooling along the slope, but there is no reduction in rainfall, so at 1,100 m above sea level the climate is classified as Humid Subtropical (Cfa/Cfb), with no dry season and an average annual temperature of 17 degrees C. It is important to remark that, almost daily, from 400 m above sea level up to the top of slopes the mountains are covered by a dense fog. In the 14 plots 21,733 individuals with DBH >= 4.8 cm, including trees, palms and ferns, were marked, measured and sampled. The average number of individuals sampled in each plot was 1264 ind.ha(-1)(+/- 218 SE 95%). Within the parameters considered trees prevailed (71% in the Montane ODF to 90% in the Restinga Forest), followed by palms (10% in the RF and 25% in the Montane Ombrophilous Dense Forest/ODF) and ferns (0% % in the RF and 4% in the Montane ODF). Regarding these proportions the Exploited Lowlands ODF differs from the others with only 1.8% of palm trees and striking 10% of ferns. The forest canopy is irregular with heights ranging from 7 to 9 m, rarely emergent trees reach 18 m, and due to this irregularity of the canopy the amount of light that gets through sets conditions for the development of hundreds of epiphytic species. Aside from Montana ODF, where the number of dead trees was more than 5% of individuals sampled, in the other phytophysiognomies this value was below 2.5%. In the 11 plots where the floristic study was conducted we found 562 species in 195 genera and 68 families. Only seven species - Euterpe edulis Mart. (Arecaceae), Calyptranthes lucida Mart. ex DC. and Marlierea tomentosa Cambess (both Myrtaceae), Guapira opposita (Veil.) Reitz (Nyctaginaceae), Cupania oblongifolia Mart. (Sapindaceae), Cecropia glaziovii Snethl. and Coussapoa microcarpa (Schott) Rizzini (both Urticaceae) - occurred from Restinga to Montane ODF, while 12 other species did not occur only in the Restinga Forest. Families with the greatest number of species are Myrtaceae (133 spp), Fabaceae (47 spp), Rubiaceae (49) and Lauraceae (49) throughout the gradient and Monimiaceae (21) specifically in portions Montane ODF. Only in the F plot, where logging has occurred between 1950 and 1985, the abundance of palm trees has been replaced by Cyatheaceae. The study shows a peak of diversity and richness, Shannon-Weiner index (H') ranging from 3.96 to 4.48 nats.ind(-1), in the intermediate altitudes (300 to 400 m) along the slope. Several explanations for this result are raised here, including the fact that these elevations are within the limits expansions and retractions of the different phytophysiognomies of the Atlantic ODF due to climate fluctuations during the Pleistocene. The results presented in this paper demonstrate the extraordinary richness of tree species of the Atlantic Rainforest from the northeastern coast of the State of São Paulo, reinforcing the importance of its conservation throughout the altitudinal gradient. The richness of this forest justifies a long term commitment to study its dynamics and functioning through permanent plots, and monitor the impacts of climate change in this vegetation.
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spelling Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinalFloristic and phytosociology in permanent plots of the Atlantic Rainforest along an altitudinal gradient in southeastern BrazilSerra do Mar State ParkNucleo PicinguabaNucleo Santa Virginiaspecies richnessphytophysiognomiesVegetation Classification SystemBIOTA Functional Gradient ProjectThis paper summarizes floristic and phytossociology data of 11, out of 14 plots of 1 ha, allocated along an altitudinal gradient in the Serra do Mar, Silo Paulo, Brazil. The study was conducted at Serra do Mar State Park and the plots start at the sea level (10 m - plot of Restinga Forest that occurs at Praia da Fazenda, Picinguaba, municipality of Ubatuba) up to 1100 m above sea level (the Montane Ombrophilous Dense occurs alongside the Itamambuca Trail, municipality of Silo Luis do Paraitinga). The Restinga Forest occurs in Pleistocenic Coastal Plain where the soil is classified as a sandy Quartzipsamment (Quartzenic Neosol), while along the slopes of the Serra do Mar, the Ombrophylus Dense Forest grows on the top of a pre-Cambrian crystalline basement with granitic rocks, where the soil is a sandy-loam Dystrophic Inceptisol (Cambisol/Latosol). In all 14 plots soils are acidic (pH 3 - 4), chemically poor, with high dilution of nutrients and high saturation of aluminum. In the Restinga and at the foot of the slope the climate is Tropical/Subtropical Humid (Af/Cfa), with no dry season, an average annual rainfall over 2,200 mm and an average annual temperature of 22 degrees C. Towards the top of the Serra do Mar there is a gradual cooling along the slope, but there is no reduction in rainfall, so at 1,100 m above sea level the climate is classified as Humid Subtropical (Cfa/Cfb), with no dry season and an average annual temperature of 17 degrees C. It is important to remark that, almost daily, from 400 m above sea level up to the top of slopes the mountains are covered by a dense fog. In the 14 plots 21,733 individuals with DBH >= 4.8 cm, including trees, palms and ferns, were marked, measured and sampled. The average number of individuals sampled in each plot was 1264 ind.ha(-1)(+/- 218 SE 95%). Within the parameters considered trees prevailed (71% in the Montane ODF to 90% in the Restinga Forest), followed by palms (10% in the RF and 25% in the Montane Ombrophilous Dense Forest/ODF) and ferns (0% % in the RF and 4% in the Montane ODF). Regarding these proportions the Exploited Lowlands ODF differs from the others with only 1.8% of palm trees and striking 10% of ferns. The forest canopy is irregular with heights ranging from 7 to 9 m, rarely emergent trees reach 18 m, and due to this irregularity of the canopy the amount of light that gets through sets conditions for the development of hundreds of epiphytic species. Aside from Montana ODF, where the number of dead trees was more than 5% of individuals sampled, in the other phytophysiognomies this value was below 2.5%. In the 11 plots where the floristic study was conducted we found 562 species in 195 genera and 68 families. Only seven species - Euterpe edulis Mart. (Arecaceae), Calyptranthes lucida Mart. ex DC. and Marlierea tomentosa Cambess (both Myrtaceae), Guapira opposita (Veil.) Reitz (Nyctaginaceae), Cupania oblongifolia Mart. (Sapindaceae), Cecropia glaziovii Snethl. and Coussapoa microcarpa (Schott) Rizzini (both Urticaceae) - occurred from Restinga to Montane ODF, while 12 other species did not occur only in the Restinga Forest. Families with the greatest number of species are Myrtaceae (133 spp), Fabaceae (47 spp), Rubiaceae (49) and Lauraceae (49) throughout the gradient and Monimiaceae (21) specifically in portions Montane ODF. Only in the F plot, where logging has occurred between 1950 and 1985, the abundance of palm trees has been replaced by Cyatheaceae. The study shows a peak of diversity and richness, Shannon-Weiner index (H') ranging from 3.96 to 4.48 nats.ind(-1), in the intermediate altitudes (300 to 400 m) along the slope. Several explanations for this result are raised here, including the fact that these elevations are within the limits expansions and retractions of the different phytophysiognomies of the Atlantic ODF due to climate fluctuations during the Pleistocene. The results presented in this paper demonstrate the extraordinary richness of tree species of the Atlantic Rainforest from the northeastern coast of the State of São Paulo, reinforcing the importance of its conservation throughout the altitudinal gradient. The richness of this forest justifies a long term commitment to study its dynamics and functioning through permanent plots, and monitor the impacts of climate change in this vegetation.Univ Estadual Campinas UNICAMP, IB, Dept Biol Vegetal, BR-13081970 Campinas, SP, BrazilUniv Estadual Paulista UNESP, Dept Bot, Inst Biociencias, BR-13506900 Rio Claro, SP, BrazilIAC, Nucleo Pesquisa & Desenvolvimento Jardim Bot CEC, BR-13001970 Campinas, SP, BrazilUniv Fed Mato Grosso Sul UFMS, Inst Ciencias Biol & Saude, BR-78698000 Pontal do Araguaia, MT, BrazilSecretaria Meio Ambiente Estado SMA, Inst Bot IBt, BR-04301902 São Paulo, BrazilUniv Estadual Campinas UNICAMP, Nucleo Estudos & Pesquisas Ambientais NEPAM, BR-13083867 Campinas, SP, BrazilUniv São Paulo, CENA, Lab Ecol Isotop, BR-13416903 Piracicaba, SP, BrazilSecretaria Meio Ambiente Estado SMA, Nucleo Picinguaba, BR-11680000 Ubantba, SP, BrazilSecretaria Meio Ambiente Estado SMA, Nucleo Santa Virginia, BR-12140000 Sao Luiz do Paraitinga, SP, BrazilUniv Estadual Paulista UNESP, Dept Bot, Inst Biociencias, BR-13506900 Rio Claro, SP, BrazilRevista Biota NeotropicaUniversidade Estadual de Campinas (UNICAMP)Universidade Estadual Paulista (Unesp)IACUniversidade Federal de Mato Grosso do Sul (UFMS)Secretaria Meio Ambiente Estado SMAUniversidade de São Paulo (USP)Joly, Carlos AlfredoAssis, Marco Antonio [UNESP]Bernacci, Luis CarlosTamashiro, Jorge YoshioRodrigues de Campos, Mariana CruzMantelli Aboin Comes, Jose AtalibaLacerda, Maryland SanchezMaes dos Santos, Flavio AntonioPedroni, FernandoPereira, Larissa de SouzaGorgulho Padgurschi, Maira de CamposBorges Prata, Eduardo Magalhaes [UNESP]Ramos, ElianaTorres, Roseli BuzanelliRochelle, AndreMartins, Fernando RobertoAlves, Luciana FerreiraVieira, Simone AparecidaMartinelli, Luiz Antoniode Camargo, Plinio BarbosaMarinho Aidar, Marcos PereiraEisenlohr, Pedro VasconcellosSimoes, ElianeVillani, Joao PauloBelinello, Renato2013-09-30T18:47:47Z2014-05-20T13:57:00Z2013-09-30T18:47:47Z2014-05-20T13:57:00Z2012-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article123-145application/pdfhttp://www.biotaneotropica.org.br/v12n1/pt/fullpaper?bn01812012012+ptBiota Neotropica. Campinas: Revista Biota Neotropica, v. 12, n. 1, p. 123-145, 2012.1676-0603http://hdl.handle.net/11449/20331WOS:000307196200012WOS000307196200012.pdf4830964329792347Web of Sciencereponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPporBiota Neotropica0.8420,381info:eu-repo/semantics/openAccess2024-10-18T18:00:09Zoai:repositorio.unesp.br:11449/20331Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestrepositoriounesp@unesp.bropendoar:29462025-03-28T15:26:09.981583Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
Floristic and phytosociology in permanent plots of the Atlantic Rainforest along an altitudinal gradient in southeastern Brazil
title Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
spellingShingle Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
Joly, Carlos Alfredo
Serra do Mar State Park
Nucleo Picinguaba
Nucleo Santa Virginia
species richness
phytophysiognomies
Vegetation Classification System
BIOTA Functional Gradient Project
title_short Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
title_full Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
title_fullStr Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
title_full_unstemmed Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
title_sort Florística e fitossociologia em parcelas permanentes da Mata Atlântica do sudeste do Brasil ao longo de um gradiente altitudinal
author Joly, Carlos Alfredo
author_facet Joly, Carlos Alfredo
Assis, Marco Antonio [UNESP]
Bernacci, Luis Carlos
Tamashiro, Jorge Yoshio
Rodrigues de Campos, Mariana Cruz
Mantelli Aboin Comes, Jose Ataliba
Lacerda, Maryland Sanchez
Maes dos Santos, Flavio Antonio
Pedroni, Fernando
Pereira, Larissa de Souza
Gorgulho Padgurschi, Maira de Campos
Borges Prata, Eduardo Magalhaes [UNESP]
Ramos, Eliana
Torres, Roseli Buzanelli
Rochelle, Andre
Martins, Fernando Roberto
Alves, Luciana Ferreira
Vieira, Simone Aparecida
Martinelli, Luiz Antonio
de Camargo, Plinio Barbosa
Marinho Aidar, Marcos Pereira
Eisenlohr, Pedro Vasconcellos
Simoes, Eliane
Villani, Joao Paulo
Belinello, Renato
author_role author
author2 Assis, Marco Antonio [UNESP]
Bernacci, Luis Carlos
Tamashiro, Jorge Yoshio
Rodrigues de Campos, Mariana Cruz
Mantelli Aboin Comes, Jose Ataliba
Lacerda, Maryland Sanchez
Maes dos Santos, Flavio Antonio
Pedroni, Fernando
Pereira, Larissa de Souza
Gorgulho Padgurschi, Maira de Campos
Borges Prata, Eduardo Magalhaes [UNESP]
Ramos, Eliana
Torres, Roseli Buzanelli
Rochelle, Andre
Martins, Fernando Roberto
Alves, Luciana Ferreira
Vieira, Simone Aparecida
Martinelli, Luiz Antonio
de Camargo, Plinio Barbosa
Marinho Aidar, Marcos Pereira
Eisenlohr, Pedro Vasconcellos
Simoes, Eliane
Villani, Joao Paulo
Belinello, Renato
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universidade Estadual de Campinas (UNICAMP)
Universidade Estadual Paulista (Unesp)
IAC
Universidade Federal de Mato Grosso do Sul (UFMS)
Secretaria Meio Ambiente Estado SMA
Universidade de São Paulo (USP)
dc.contributor.author.fl_str_mv Joly, Carlos Alfredo
Assis, Marco Antonio [UNESP]
Bernacci, Luis Carlos
Tamashiro, Jorge Yoshio
Rodrigues de Campos, Mariana Cruz
Mantelli Aboin Comes, Jose Ataliba
Lacerda, Maryland Sanchez
Maes dos Santos, Flavio Antonio
Pedroni, Fernando
Pereira, Larissa de Souza
Gorgulho Padgurschi, Maira de Campos
Borges Prata, Eduardo Magalhaes [UNESP]
Ramos, Eliana
Torres, Roseli Buzanelli
Rochelle, Andre
Martins, Fernando Roberto
Alves, Luciana Ferreira
Vieira, Simone Aparecida
Martinelli, Luiz Antonio
de Camargo, Plinio Barbosa
Marinho Aidar, Marcos Pereira
Eisenlohr, Pedro Vasconcellos
Simoes, Eliane
Villani, Joao Paulo
Belinello, Renato
dc.subject.por.fl_str_mv Serra do Mar State Park
Nucleo Picinguaba
Nucleo Santa Virginia
species richness
phytophysiognomies
Vegetation Classification System
BIOTA Functional Gradient Project
topic Serra do Mar State Park
Nucleo Picinguaba
Nucleo Santa Virginia
species richness
phytophysiognomies
Vegetation Classification System
BIOTA Functional Gradient Project
description This paper summarizes floristic and phytossociology data of 11, out of 14 plots of 1 ha, allocated along an altitudinal gradient in the Serra do Mar, Silo Paulo, Brazil. The study was conducted at Serra do Mar State Park and the plots start at the sea level (10 m - plot of Restinga Forest that occurs at Praia da Fazenda, Picinguaba, municipality of Ubatuba) up to 1100 m above sea level (the Montane Ombrophilous Dense occurs alongside the Itamambuca Trail, municipality of Silo Luis do Paraitinga). The Restinga Forest occurs in Pleistocenic Coastal Plain where the soil is classified as a sandy Quartzipsamment (Quartzenic Neosol), while along the slopes of the Serra do Mar, the Ombrophylus Dense Forest grows on the top of a pre-Cambrian crystalline basement with granitic rocks, where the soil is a sandy-loam Dystrophic Inceptisol (Cambisol/Latosol). In all 14 plots soils are acidic (pH 3 - 4), chemically poor, with high dilution of nutrients and high saturation of aluminum. In the Restinga and at the foot of the slope the climate is Tropical/Subtropical Humid (Af/Cfa), with no dry season, an average annual rainfall over 2,200 mm and an average annual temperature of 22 degrees C. Towards the top of the Serra do Mar there is a gradual cooling along the slope, but there is no reduction in rainfall, so at 1,100 m above sea level the climate is classified as Humid Subtropical (Cfa/Cfb), with no dry season and an average annual temperature of 17 degrees C. It is important to remark that, almost daily, from 400 m above sea level up to the top of slopes the mountains are covered by a dense fog. In the 14 plots 21,733 individuals with DBH >= 4.8 cm, including trees, palms and ferns, were marked, measured and sampled. The average number of individuals sampled in each plot was 1264 ind.ha(-1)(+/- 218 SE 95%). Within the parameters considered trees prevailed (71% in the Montane ODF to 90% in the Restinga Forest), followed by palms (10% in the RF and 25% in the Montane Ombrophilous Dense Forest/ODF) and ferns (0% % in the RF and 4% in the Montane ODF). Regarding these proportions the Exploited Lowlands ODF differs from the others with only 1.8% of palm trees and striking 10% of ferns. The forest canopy is irregular with heights ranging from 7 to 9 m, rarely emergent trees reach 18 m, and due to this irregularity of the canopy the amount of light that gets through sets conditions for the development of hundreds of epiphytic species. Aside from Montana ODF, where the number of dead trees was more than 5% of individuals sampled, in the other phytophysiognomies this value was below 2.5%. In the 11 plots where the floristic study was conducted we found 562 species in 195 genera and 68 families. Only seven species - Euterpe edulis Mart. (Arecaceae), Calyptranthes lucida Mart. ex DC. and Marlierea tomentosa Cambess (both Myrtaceae), Guapira opposita (Veil.) Reitz (Nyctaginaceae), Cupania oblongifolia Mart. (Sapindaceae), Cecropia glaziovii Snethl. and Coussapoa microcarpa (Schott) Rizzini (both Urticaceae) - occurred from Restinga to Montane ODF, while 12 other species did not occur only in the Restinga Forest. Families with the greatest number of species are Myrtaceae (133 spp), Fabaceae (47 spp), Rubiaceae (49) and Lauraceae (49) throughout the gradient and Monimiaceae (21) specifically in portions Montane ODF. Only in the F plot, where logging has occurred between 1950 and 1985, the abundance of palm trees has been replaced by Cyatheaceae. The study shows a peak of diversity and richness, Shannon-Weiner index (H') ranging from 3.96 to 4.48 nats.ind(-1), in the intermediate altitudes (300 to 400 m) along the slope. Several explanations for this result are raised here, including the fact that these elevations are within the limits expansions and retractions of the different phytophysiognomies of the Atlantic ODF due to climate fluctuations during the Pleistocene. The results presented in this paper demonstrate the extraordinary richness of tree species of the Atlantic Rainforest from the northeastern coast of the State of São Paulo, reinforcing the importance of its conservation throughout the altitudinal gradient. The richness of this forest justifies a long term commitment to study its dynamics and functioning through permanent plots, and monitor the impacts of climate change in this vegetation.
publishDate 2012
dc.date.none.fl_str_mv 2012-01-01
2013-09-30T18:47:47Z
2013-09-30T18:47:47Z
2014-05-20T13:57:00Z
2014-05-20T13:57:00Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://www.biotaneotropica.org.br/v12n1/pt/fullpaper?bn01812012012+pt
Biota Neotropica. Campinas: Revista Biota Neotropica, v. 12, n. 1, p. 123-145, 2012.
1676-0603
http://hdl.handle.net/11449/20331
WOS:000307196200012
WOS000307196200012.pdf
4830964329792347
url http://www.biotaneotropica.org.br/v12n1/pt/fullpaper?bn01812012012+pt
http://hdl.handle.net/11449/20331
identifier_str_mv Biota Neotropica. Campinas: Revista Biota Neotropica, v. 12, n. 1, p. 123-145, 2012.
1676-0603
WOS:000307196200012
WOS000307196200012.pdf
4830964329792347
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dc.relation.none.fl_str_mv Biota Neotropica
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dc.publisher.none.fl_str_mv Revista Biota Neotropica
publisher.none.fl_str_mv Revista Biota Neotropica
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