dc.contributorInstituto Nacional de Pesquisas da Amazônia
dc.contributorThe University of Texas at Austin
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniversidade Estadual de Maringá (UEM)
dc.creatorFeitosa, Yuri Oliveira
dc.creatorAbsy, Maria Lucia
dc.creatorLatrubesse, Edgardo Manuel [UNESP]
dc.creatorStevaux, José Candido [UNESP]
dc.date2015-10-22T06:22:17Z
dc.date2015-10-22T06:22:17Z
dc.date2015-01-01
dc.date.accessioned2023-09-12T07:00:23Z
dc.date.available2023-09-12T07:00:23Z
dc.identifierhttp://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-33062015000100120&lng=en&nrm=iso&tlng=en
dc.identifierActa Botanica Brasilica. Sao Paulo Sp: Soc Botanica Brasil, v. 29, n. 1, p. 120-128, 2015.
dc.identifier0102-3306
dc.identifierhttp://hdl.handle.net/11449/129644
dc.identifier10.1590/0102-33062014abb3711
dc.identifierS0102-33062015000100120
dc.identifierWOS:000351140400014
dc.identifierS0102-33062015000100120.pdf
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8778981
dc.descriptionThe present study reconstructs the paleovegetation of a varzea (seasonally flooded) forest in the central parts of the Madeira River floodplain in Brazil using palynological data. Forty-nine cut-bank sediment samples from the Madeira River were processed in the study; from these, ten samples contained pollen: two contained pollen from the Middle Pleniglacial age, one contained pollen from the Tardiglacial age, six contained pollen from the Holocene, and one contained more recently deposited pollen. The Middle Pleniglacial pollen belonged to a primary succession varzea forest, while the Tardiglacial pollen represented a late succession varzea forest. On the other hand, the three Holocene samples showed the characteristic composition of chavascal (water-logged forest) or lacustrine varzea forest, and three samples belonged to a late succession varzea forest. The most recent pollen deposit represented a secondary succession varzea forest. This paleovegetation showed a typical mosaic distribution, which may be explained by the fluvial dynamics, high species richness and diversity in the varzea forest, and the presence of dominant species.
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.descriptionInstituto Nacional de Pesquisas da Amazônia, Coordenação de Biodiversidade, Laboratório de Palinologia
dc.descriptionThe University of Texas at Austin, Department of Geography and Environment
dc.descriptionUniversidade Estadual Paulista, Departamento de Geologia, Instituto de Geociências e Ciências Exatas de Rio Claro
dc.descriptionCNPq: 477127/2011-8
dc.format120-128
dc.languageeng
dc.publisherSoc Botanica Brasil
dc.relationActa Botanica Brasilica
dc.relation0.817
dc.relation0,325
dc.rightsAcesso aberto
dc.sourceWeb of Science
dc.subjectCut-bank sediment
dc.subjectLate Pleistocene-Holocene
dc.subjectPalynology
dc.subjectSouthern Amazonian tributary
dc.subjectVarzea
dc.titleLate Quaternary vegetation dynamics from central parts of the Madeira River in Brazil
dc.typeArtigo


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