Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu

Detalhes bibliográficos
Autor(a) principal: Frana, Vitor André
Data de Publicação: 2011
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Biblioteca Digital de Teses e Dissertações do UNIOESTE
Texto Completo: http://tede.unioeste.br/handle/tede/5484
Resumo: Spatial gradients in aquatic environments reflect gradual changes in physical, chemical and biological features along of the longitudinal, transverse and vertical axis, which are of relevance for understanding the mechanisms that operate in reservoirs. This work aims to verify if assemblage abundance of fish of Foz do Areia reservoir presents distinct longitudinal gradients, forming fluvial, transitional and lacustrine zones, and if this assemblage is differentiated in bottom, surface and margin regions. It was also valuated the longitudinal gradients formation in physical and chemical variables in surface and if these variables present concordance with assemblage abundance. For this, fish samples were collected quarterly between January 2004 and October 2007, in bottom, surface and margin regions, in three zones, near the dam (LAC), transition (TRA) and up-stream (FLU). The abundances were expressed as catch per unit effort (CPUE), summarized by Detrended Correspondence Analysis (DCA) and spatially compared with the Multi-Response Permutation Procedure (MRPP). Additionally, the indicator species analysis (indval) was performed aims to elucidate preferential zone and regions of each species. The degree of congruence between the physical and chemical water variables and assemblage fish matrices in surface was evaluated with Protest after summarized them with Nonmetric Multidimensional Scaling (NMS). Therefore, it was verified that assemblage structure distinguished for the zone (LAC, TRA and FLU), and more sharply between in bottom, surface and margin regions. Additionally, it was identified that there was longitudinal gradient of fishes assemblage abundance, and it gradient was different in bottom, surface and margin. Furthermore, the longitudinal gradients of physical and chemical variables were observed and they were consistent with the fish assemblage structure in surface. Thus, the Foz de Areia reservoir had spatial gradients, both, in the fish’s assemblage and in the physical and chemical variables, which are concordant. Moreover, dependencies between the longitudinal axis, vertical and horizontal were evident in assemblage.
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spelling Baumgartner, Gilmarhttp://lattes.cnpq.br/4429292734049977Piana, Pitágoras Augustohttp://lattes.cnpq.br/4575333508754234Gubiani, Éder Andréhttp://lattes.cnpq.br/9034190459322164Piana, Pitágoras Augustohttp://lattes.cnpq.br/4575333508754234Gomes, Luiz Carloshttp://lattes.cnpq.br/8293391668117402http://lattes.cnpq.br/9521775348476015Frana, Vitor André2021-07-21T18:21:18Z2011-08-12FRANA, Vitor André. Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu. 2011. 27 f. Dissertação (Mestrado em Recursos Pesqueiros e Engenharia de Pesca) - Universidade Estadual do Oeste do Paraná, Toledo, 2011.http://tede.unioeste.br/handle/tede/5484Spatial gradients in aquatic environments reflect gradual changes in physical, chemical and biological features along of the longitudinal, transverse and vertical axis, which are of relevance for understanding the mechanisms that operate in reservoirs. This work aims to verify if assemblage abundance of fish of Foz do Areia reservoir presents distinct longitudinal gradients, forming fluvial, transitional and lacustrine zones, and if this assemblage is differentiated in bottom, surface and margin regions. It was also valuated the longitudinal gradients formation in physical and chemical variables in surface and if these variables present concordance with assemblage abundance. For this, fish samples were collected quarterly between January 2004 and October 2007, in bottom, surface and margin regions, in three zones, near the dam (LAC), transition (TRA) and up-stream (FLU). The abundances were expressed as catch per unit effort (CPUE), summarized by Detrended Correspondence Analysis (DCA) and spatially compared with the Multi-Response Permutation Procedure (MRPP). Additionally, the indicator species analysis (indval) was performed aims to elucidate preferential zone and regions of each species. The degree of congruence between the physical and chemical water variables and assemblage fish matrices in surface was evaluated with Protest after summarized them with Nonmetric Multidimensional Scaling (NMS). Therefore, it was verified that assemblage structure distinguished for the zone (LAC, TRA and FLU), and more sharply between in bottom, surface and margin regions. Additionally, it was identified that there was longitudinal gradient of fishes assemblage abundance, and it gradient was different in bottom, surface and margin. Furthermore, the longitudinal gradients of physical and chemical variables were observed and they were consistent with the fish assemblage structure in surface. Thus, the Foz de Areia reservoir had spatial gradients, both, in the fish’s assemblage and in the physical and chemical variables, which are concordant. Moreover, dependencies between the longitudinal axis, vertical and horizontal were evident in assemblage.Gradientes espaciais em ambientes aquáticos refletem mudanças gradativas nas características físicas, químicas e biológicas ao longo de eixos longitudinais, transversais e verticais, sendo estas de relevância para o entendimento dos mecanismos que operam nos reservatórios. Assim, o objetivo desse trabalho foi verificar se a abundância da assembleia de peixes do reservatório de Foz do Areia apresenta distintos gradientes longitudinais, formando zonas fluvial, transição e lacustre, bem como se a mesma é diferenciada em relação aos estratos de fundo, superfície e margem. Verificou-se também a formação de gradientes longitudinais em variáveis físicas e químicas da superfície e se essas variáveis apresentaram concordância com a abundância da assembleia. Para tanto, coletas de peixes foram realizadas trimestralmente, entre janeiro de 2004 e outubro de 2007, nos estratos de fundo, superfície e margem, das zonas Lacustre (LAC), Transição (TRA) e Fluvial (FLU). As abundâncias foram expressas em captura por unidade de esforço (CPUE), sumarizadas pela análise de correspondência com remoção do efeito de arco (DCA) e comparadas espacialmente com o procedimento permutacional de multi-resposta (MRPP). Adicionalmente, a análise de espécie indicadora (INVAL) foi realizada com o intuito de elucidar os estratos e as zonas preferenciais de cada espécie. O grau de congruência entre as matrizes das variáveis físicas e químicas da água e da assembleia de peixes do estrato superficial foi avaliado com o Protest, após sumarizá-las com a técnica de escalonamento muldimensional não-paramétrico (NMS). Com isto, foi verificado que a estrutura da assembleia distinguiu-se em relação as zonas LAC, TRA e FLU, e de forma mais acentuada, entre os estratos de fundo, margem e superfície. Adicionalmente, foi identificado que o gradiente longitudinal apresentado pela abundância da assembleia foi diferenciado nos estratos de fundo, superfície e margem. Além disto, as variáveis físicas e químicas também formaram gradientes longitudinais e foram concordantes com a estrutura da assembleia de peixes na superfície. Desta forma, o reservatório de Foz de Areia apresentou gradientes espaciais tanto na assembleia de peixes, quanto das variáveis físicas e químicas, sendo estas concordantes. Além disso, dependências entre os eixos longitudinais, verticais e transversais ficaram evidentes na assembleia.Submitted by Marilene Donadel (marilene.donadel@unioeste.br) on 2021-07-21T18:21:18Z No. of bitstreams: 1 Vitor_Frana_2011.pdf: 1025465 bytes, checksum: aaef113de0251ef5f884955c833f49bf (MD5)Made available in DSpace on 2021-07-21T18:21:18Z (GMT). No. of bitstreams: 1 Vitor_Frana_2011.pdf: 1025465 bytes, checksum: aaef113de0251ef5f884955c833f49bf (MD5) Previous issue date: 2011-08-12Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESapplication/pdfpor-2624803687637593200500Universidade Estadual do Oeste do ParanáToledoPrograma de Pós-Graduação em Recursos Pesqueiros e Engenharia de PescaUNIOESTEBrasilCentro de Engenharias e Ciências ExatasGradientes longitudinaisGradientes verticaisIctiofaunaVariáveis abióticasLongitudinal gradientsVertical gradientsFish faunaAbiotic variablesCIENCIAS AGRARIAS::RECURSOS PESQUEIROS E ENGENHARIA DE PESCAGradientes espaciais no reservatório de Foz do Areia - Rio IguaçuSpatial gradients in Foz do Areia reservoir - Iguazu Riverinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesis634168548598223434600600600600-7734402124082146922-61317501987095198112075167498588264571info:eu-repo/semantics/openAccessreponame:Biblioteca Digital de Teses e Dissertações do UNIOESTEinstname:Universidade Estadual do Oeste do Paraná (UNIOESTE)instacron:UNIOESTEORIGINALVitor_Frana_2011.pdfVitor_Frana_2011.pdfapplication/pdf1025465http://tede.unioeste.br:8080/tede/bitstream/tede/5484/2/Vitor_Frana_2011.pdfaaef113de0251ef5f884955c833f49bfMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-82165http://tede.unioeste.br:8080/tede/bitstream/tede/5484/1/license.txtbd3efa91386c1718a7f26a329fdcb468MD51tede/54842021-07-21 15:21:18.968oai:tede.unioeste.br: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Biblioteca Digital de Teses e Dissertaçõeshttp://tede.unioeste.br/PUBhttp://tede.unioeste.br/oai/requestbiblioteca.repositorio@unioeste.bropendoar:2021-07-21T18:21:18Biblioteca Digital de Teses e Dissertações do UNIOESTE - Universidade Estadual do Oeste do Paraná (UNIOESTE)false
dc.title.por.fl_str_mv Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
dc.title.alternative.eng.fl_str_mv Spatial gradients in Foz do Areia reservoir - Iguazu River
title Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
spellingShingle Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
Frana, Vitor André
Gradientes longitudinais
Gradientes verticais
Ictiofauna
Variáveis abióticas
Longitudinal gradients
Vertical gradients
Fish fauna
Abiotic variables
CIENCIAS AGRARIAS::RECURSOS PESQUEIROS E ENGENHARIA DE PESCA
title_short Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
title_full Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
title_fullStr Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
title_full_unstemmed Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
title_sort Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu
author Frana, Vitor André
author_facet Frana, Vitor André
author_role author
dc.contributor.advisor1.fl_str_mv Baumgartner, Gilmar
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/4429292734049977
dc.contributor.advisor-co1.fl_str_mv Piana, Pitágoras Augusto
dc.contributor.advisor-co1Lattes.fl_str_mv http://lattes.cnpq.br/4575333508754234
dc.contributor.referee1.fl_str_mv Gubiani, Éder André
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/9034190459322164
dc.contributor.referee2.fl_str_mv Piana, Pitágoras Augusto
dc.contributor.referee2Lattes.fl_str_mv http://lattes.cnpq.br/4575333508754234
dc.contributor.referee3.fl_str_mv Gomes, Luiz Carlos
dc.contributor.referee3Lattes.fl_str_mv http://lattes.cnpq.br/8293391668117402
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/9521775348476015
dc.contributor.author.fl_str_mv Frana, Vitor André
contributor_str_mv Baumgartner, Gilmar
Piana, Pitágoras Augusto
Gubiani, Éder André
Piana, Pitágoras Augusto
Gomes, Luiz Carlos
dc.subject.por.fl_str_mv Gradientes longitudinais
Gradientes verticais
Ictiofauna
Variáveis abióticas
topic Gradientes longitudinais
Gradientes verticais
Ictiofauna
Variáveis abióticas
Longitudinal gradients
Vertical gradients
Fish fauna
Abiotic variables
CIENCIAS AGRARIAS::RECURSOS PESQUEIROS E ENGENHARIA DE PESCA
dc.subject.eng.fl_str_mv Longitudinal gradients
Vertical gradients
Fish fauna
Abiotic variables
dc.subject.cnpq.fl_str_mv CIENCIAS AGRARIAS::RECURSOS PESQUEIROS E ENGENHARIA DE PESCA
description Spatial gradients in aquatic environments reflect gradual changes in physical, chemical and biological features along of the longitudinal, transverse and vertical axis, which are of relevance for understanding the mechanisms that operate in reservoirs. This work aims to verify if assemblage abundance of fish of Foz do Areia reservoir presents distinct longitudinal gradients, forming fluvial, transitional and lacustrine zones, and if this assemblage is differentiated in bottom, surface and margin regions. It was also valuated the longitudinal gradients formation in physical and chemical variables in surface and if these variables present concordance with assemblage abundance. For this, fish samples were collected quarterly between January 2004 and October 2007, in bottom, surface and margin regions, in three zones, near the dam (LAC), transition (TRA) and up-stream (FLU). The abundances were expressed as catch per unit effort (CPUE), summarized by Detrended Correspondence Analysis (DCA) and spatially compared with the Multi-Response Permutation Procedure (MRPP). Additionally, the indicator species analysis (indval) was performed aims to elucidate preferential zone and regions of each species. The degree of congruence between the physical and chemical water variables and assemblage fish matrices in surface was evaluated with Protest after summarized them with Nonmetric Multidimensional Scaling (NMS). Therefore, it was verified that assemblage structure distinguished for the zone (LAC, TRA and FLU), and more sharply between in bottom, surface and margin regions. Additionally, it was identified that there was longitudinal gradient of fishes assemblage abundance, and it gradient was different in bottom, surface and margin. Furthermore, the longitudinal gradients of physical and chemical variables were observed and they were consistent with the fish assemblage structure in surface. Thus, the Foz de Areia reservoir had spatial gradients, both, in the fish’s assemblage and in the physical and chemical variables, which are concordant. Moreover, dependencies between the longitudinal axis, vertical and horizontal were evident in assemblage.
publishDate 2011
dc.date.issued.fl_str_mv 2011-08-12
dc.date.accessioned.fl_str_mv 2021-07-21T18:21:18Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.identifier.citation.fl_str_mv FRANA, Vitor André. Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu. 2011. 27 f. Dissertação (Mestrado em Recursos Pesqueiros e Engenharia de Pesca) - Universidade Estadual do Oeste do Paraná, Toledo, 2011.
dc.identifier.uri.fl_str_mv http://tede.unioeste.br/handle/tede/5484
identifier_str_mv FRANA, Vitor André. Gradientes espaciais no reservatório de Foz do Areia - Rio Iguaçu. 2011. 27 f. Dissertação (Mestrado em Recursos Pesqueiros e Engenharia de Pesca) - Universidade Estadual do Oeste do Paraná, Toledo, 2011.
url http://tede.unioeste.br/handle/tede/5484
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dc.publisher.none.fl_str_mv Universidade Estadual do Oeste do Paraná
Toledo
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Recursos Pesqueiros e Engenharia de Pesca
dc.publisher.initials.fl_str_mv UNIOESTE
dc.publisher.country.fl_str_mv Brasil
dc.publisher.department.fl_str_mv Centro de Engenharias e Ciências Exatas
publisher.none.fl_str_mv Universidade Estadual do Oeste do Paraná
Toledo
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