Late Holocene Development Of A Mangrove Ecosystem In Southeastern Brazil (itanhaém, State Of São Paulo)

dc.creatordo Amaral P.G.C.
dc.creatorLedru M.-P.
dc.creatorBranco F.R.
dc.creatorGiannini P.C.F.
dc.date2006
dc.date2015-06-30T18:05:24Z
dc.date2015-11-26T14:22:46Z
dc.date2015-06-30T18:05:24Z
dc.date2015-11-26T14:22:46Z
dc.date.accessioned2018-03-28T21:24:41Z
dc.date.available2018-03-28T21:24:41Z
dc.identifier
dc.identifierPalaeogeography, Palaeoclimatology, Palaeoecology. , v. 241, n. 03/04/15, p. 608 - 620, 2006.
dc.identifier310182
dc.identifier10.1016/j.palaeo.2006.04.010
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-33751051180&partnerID=40&md5=98f96b775177e7c36664e8661d2003c8
dc.identifierhttp://www.repositorio.unicamp.br/handle/REPOSIP/103038
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/103038
dc.identifier2-s2.0-33751051180
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1244921
dc.descriptionMost palynological studies of mangroves have been carried out in the Indo-Pacific region, but few have investigated these ecosystems along the southern Atlantic coast. This paper provides information on the palynology of a mangrove at Itanhaém, state of São Paulo, on the southeastern Brazilian coast. This mangrove occurs on microtidal flats adjacent to a fluvial-tidal channel mouth (Itanhaém River), part of an estuarine lagoon system established in the mid-Holocene. Pollen samples were collected from the surface and from bromeliad water in order to define the composition of modern pollen rain in the study area. The results show a strong presence of rain forest taxa in the mangrove pollen spectra, which differ from those obtained from northern Brazilian mangroves, which are characterized by higher percentages of the mangrove taxa Rhizophora and Avicennia. Based on palynological and 14C chronological analysis of a shallow core measuring 135 cm in depth, the Itanhaém mangrove already existed by 1300 years BP and began expanding about 1000 years BP, reaching its present extent sometime after 300 years BP. Its evolution is related to the sedimentary filling of the estuarine-lagoonal depositional system. Two factors may have controlled the development of this mangrove: the relative increase of intertidal areas due to this sedimentary filling and the decrease in wave action and increase in pelitic deposition in the intertidal zone related to the partial closing of the estuarine-lagoonal inlets. These processes were favored by the advance of bayhead deltas and by the development of sand spits as a part of the regression of the Holocene strandplain. © 2006 Elsevier B.V. All rights reserved.
dc.description241
dc.description03/04/15
dc.description608
dc.description620
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dc.languageen
dc.publisher
dc.relationPalaeogeography, Palaeoclimatology, Palaeoecology
dc.rightsfechado
dc.sourceScopus
dc.titleLate Holocene Development Of A Mangrove Ecosystem In Southeastern Brazil (itanhaém, State Of São Paulo)
dc.typeArtículos de revistas


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