Pennsylvanian - Early Cisuralian Interglacial Macrofloristic Succession In Parana Basin Of The State Of Sao Paulo

dc.creatorCerruti Bernardes-de-Oliveira
dc.creatorMary Elizabeth; Kavali
dc.creatorPauline Sabina; Mune
dc.creatorSandra Eiko; Shivanna
dc.creatorMahesh; de Souza
dc.creatorPaulo Alves; Lannuzzi
dc.creatorRoberto; Jasper
dc.creatorAndre; Hoelzel
dc.creatorAmanda; Boardman
dc.creatorDaiana R.; Rohn
dc.creatorRosemarie; Ricardi-Branco
dc.creatorFresia
dc.date2016
dc.datedez
dc.date2017-11-13T13:57:59Z
dc.date2017-11-13T13:57:59Z
dc.date.accessioned2018-03-29T06:11:23Z
dc.date.available2018-03-29T06:11:23Z
dc.identifierJournal Of South American Earth Sciences. Pergamon-elsevier Science Ltd , v. 72, p. 351 - 374, 2016.
dc.identifier0895-9811
dc.identifierWOS:000389556100024
dc.identifier10.1016/j.jsames.2016.09.004
dc.identifierhttp://www.sciencedirect.com/science/article/pii/S0895981116301729
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/330163
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1367188
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionOne of the most completely preserved glacial sedimentary records from the Late Carboniferous to the Early Permian time corresponds to the Itarare Group, which presents a large outcropping thickness in the northeastern border of Parana Basin, especially in the State of Sao Paulo. This unit corresponds to the base of the Gondwana I Supersequence and is composed of continental to marine glacial and interglacial deposits. Based on some macrofloristic, lithostratigraphic and palynostratigraphic data, a formal scheme of the macrofloral succession is herein proposed for this interval, comprising five associations in ascending stratigraphic order namely: (1) Dwykea-Sublagenicula-Calamospora Association (recorded in Campinas Municipality), composed of lycophyte megaspores (Sublagenicula, Trileites and Calamospora sp.) and some bryophytes (Dwykea), concerning to a coastal glacial or coastal interglacial environment; (2) Eusphenopteris-Nothorhacopteris-Botrychiopsis Association (registered in Itapeva and Buri municipalities), composed of Eusphenopteris, Nothorhacopteris, Botrychiopsis, Paracalamites spp. along with Sphenophyllum, Koretrophyllites, Noeggerathiopsis and rare Cordaicarpus and Samaropsis concerning to an interglacial deltaic plain associated to coal forming swamps with cold temperate hydro-hygrophilous vegetation; (3) Paranocladus-Ginkgophyllum-Brasilodendron Association (registered in Monte Mor Municipality), composed of the first conifers of the Parana Basin (Paranocladus, Paranospermum and few Buriadia-type), lycophytes (Brasilodendron, Bumbudendron), Ginkgophyllum, Noeggerathiopsis, Samaropsis and Cordaicarpus and rare Nothorhacopteris, Botrychiopsis, Koretrophyllites and Sphenophyllum, interpreted as interglacial deltaic flood plain; (4) Dwykea-Sublagenicula-Calamospora Recurrent Association (recorded in Salto Municipality), composed of bryophytes (Dwykea) and lycopod megaspores, very similar to the first association, related to a coastal glacial or coastal interglacial depositional environment with a type-tundra vegetational cover; and (5) Gangamopteris Arberia-Stephanophyllites Association (occurring in Tiete and Cerquilho municipalities), composed of the first glossopterid leaves and fructifications of the Parana Basin (abundant Gangamopteris, Arberia, Arberiopsis and Hirsutum) and sphenophytes (Stephanophyllites and Phyllotheca), suggested as coastal prograding or alluvial environment, of an interglacial phase at the end of the sedimentary history of the Itarare Group. The first four associations are of Pennsylvanian age while the last one is of Asselian-Sakmarian age. (C) 2016 Elsevier Ltd. All rights reserved.
dc.description72
dc.description351
dc.description374
dc.descriptionFAPESP [97/03639-8]
dc.descriptionCNPq Brazil
dc.descriptionDepartment of Science and Technology of India [CNPq 490829/2007-4, DST-India RPO-24/2007]
dc.descriptionCNPq [304978/2013-2, 310727/2014-6, 309211/2013-1, 300578/2015-6, 150574/2015-0, 400972/2013-1, 461628/2014-7]
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.languageEnglish
dc.publisherPergamon-Elsevier Science LTD
dc.publisherOxford
dc.relationJournal of South American Earth Sciences
dc.rightsfechado
dc.sourceWOS
dc.subjectMacrofloral Successions
dc.subjectItarare Group
dc.subjectPermo-carboniferous
dc.subjectInterglacial Floras
dc.subjectParana Basin
dc.subjectWestern Gondwana
dc.titlePennsylvanian - Early Cisuralian Interglacial Macrofloristic Succession In Parana Basin Of The State Of Sao Paulo
dc.typeArtículos de revistas


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