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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/76717
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dc.contributor.authorStevaux, José C.-
dc.contributor.authorCorradini, Fabrício A.-
dc.contributor.authorAquino, Samia-
dc.date.accessioned2014-05-27T11:30:47Z-
dc.date.accessioned2016-10-25T18:54:38Z-
dc.date.available2014-05-27T11:30:47Z-
dc.date.available2016-10-25T18:54:38Z-
dc.date.issued2013-10-01-
dc.identifierhttp://dx.doi.org/10.1016/j.jsames.2011.12.007-
dc.identifier.citationJournal of South American Earth Sciences, v. 46, p. 113-121.-
dc.identifier.issn0895-9811-
dc.identifier.urihttp://hdl.handle.net/11449/76717-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/76717-
dc.description.abstractIn fluvial systems, the relationship between a dominant variable (e.g. flood pulse) and its dependent ones (e.g. riparian vegetation) is called connectivity. This paper analyzes the connectivity elements and processes controlling riparian vegetation for a reach of the upper Paraná River (Brazil) and estimates the future changes in channel-vegetation relationship as a consequence of the managing of a large dam. The studied reach is situated 30km downstream from the Porto Primavera Dam (construction finished in 1999). Through aerial photography (1:25,000, 1996), RGB-CBERS satellite imagery and a previous field botany survey it was possible to elaborate a map with the five major morpho-vegetation units: 1) Tree-dominated natural levee, 2) Shrubby upper floodplain, 3) Shrub-herbaceous mid floodplain, 4) Grass-herbaceous lower floodplain and 5) Shrub-herbaceous flood runoff channel units. By use of a detailed topographic survey and statistical tools each morpho-vegetation type was analyzed according to its connectivity parameters (frequency, recurrence, permanence, seasonality, potamophase, limnophase and FCQ index) in the pre- and post-dam closure periods of the historical series. Data showed that most of the morpho-vegetation units were predicted to present changes in connectivity parameters values after dam closing and the new regime could affect, in different intensity, the river ecology and particularly the riparian vegetation. The methods used in this study can be useful for dam impact studies in other South American tropical rivers. © 2012 Elsevier Ltd.en
dc.format.extent113-121-
dc.language.isoeng-
dc.sourceScopus-
dc.subjectConnectivity processes-
dc.subjectFloods-
dc.subjectParaná river-
dc.subjectRegulated river-
dc.subjectRiparian vegetation-
dc.subjectaerial photography-
dc.subjectconnectivity-
dc.subjectdam-
dc.subjectflood-
dc.subjectfloodplain-
dc.subjectriparian vegetation-
dc.subjectriver channel-
dc.subjectsatellite imagery-
dc.subjecttopographic mapping-
dc.subjectBrazil-
dc.subjectParana River-
dc.subjectPorto Primavera Dam-
dc.subjectSao Paulo [Brazil]-
dc.titleConnectivity processes and riparian vegetation of the upper Paraná River, Brazilen
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual de Maringá (UEM)-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.contributor.institutionUniversidade Federal do Pará (UFPA)-
dc.contributor.institutionUniversity of Texas at Austin - Department of Geography and Environment-
dc.description.affiliationUniversidade Estadual de Maringá/GEMA, 87020-900 Maringá, PR-
dc.description.affiliationUNESP Insituto de Geciências e Ciências Exatas, Rio Claro-
dc.description.affiliationUniversidade Federal do Pará - UFPA Faculdade de Geografia Geografia Física, Rua Folha 31, CEP 68501-970 Marabá, PA-
dc.description.affiliationUniversity of Texas at Austin - Department of Geography and Environment, 1 University Station, A3100, Austin, 78712 TX-
dc.description.affiliationUnespUNESP Insituto de Geciências e Ciências Exatas, Rio Claro-
dc.identifier.doi10.1016/j.jsames.2011.12.007-
dc.identifier.wosWOS:000324455500010-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofJournal of South American Earth Sciences-
dc.identifier.scopus2-s2.0-84882870571-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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