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dc.creatorValdez Buso, Victoria-
dc.creatorDanielski Aquino, Carolina-
dc.creatorGomes Paim, Paulo Sérgio-
dc.creatorAlves de Souza, Paulo-
dc.creatorMori, Ana Louisa-
dc.creatorFallgatter, Claus-
dc.creatorMilana, Juan Pablo-
dc.creatorKneller, Benjamin-
dc.date2018-12-04T21:12:24Z-
dc.date2018-12-04T21:12:24Z-
dc.date2017-09-06-
dc.date2018-10-22T17:28:54Z-
dc.date.accessioned2019-04-29T15:55:54Z-
dc.date.available2019-04-29T15:55:54Z-
dc.identifierValdez Buso, Victoria; Danielski Aquino, Carolina; Gomes Paim, Paulo Sérgio; Alves de Souza, Paulo; Mori, Ana Louisa; et al.; Late Palaeozoic glacial cycles and subcycles in western Gondwana: Correlation of surface and subsurface data of the Paraná Basin, Brazil; Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 6-9-2017; 1-16-
dc.identifier0031-0182-
dc.identifierhttp://hdl.handle.net/11336/65803-
dc.identifierCONICET Digital-
dc.identifierCONICET-
dc.identifier.urihttp://rodna.bn.gov.ar:8080/jspui/handle/bnmm/305619-
dc.descriptionThe Paraná Basin, the largest basin in South America, received glacially derived sediments during the Late Palaeozoic Ice Age (LPIA) of the Gondwana supercontinent. Despite the importance of this basin for understanding the continental development of the Gondwana glaciation, and the fact that ca. 95% of this basin is not exposed at the surface, few attempts have been made to connect the exposed glacial strata to the subsurface record. In this paper, exposures of glacial cycles in the Upper Itararé Group in Santa Catarina State, southern Brazil, are analyzed, locally correlated and then linked to the three major glacial cycles previously described from subsurface studies along the basin. Together study areas (Doutor Pedrinho and Vidal Ramos) record five, partially comparable shorter glacial subcycles (relative to the major glacial cycles). These series comprise coarse-grained subaqueous outwash deposits, turbidite sand sheets, marine shales, and diamictites, the latter mostly derived from delta slope failure and ensuing resedimentation. In addition to sedimentological and genetic stratigraphic description and analysis, preliminary age determination based on the palynological content is also presented. Besides, a regional correlation of the described succession to the subsurface record is proposed based on well logs and core information. All the palynomorph associations identified from the exposed successions, which represent the upper third part of the Itararé Group, are related to the Subzone Protohaploxypinus goraiensis, base of the Vittatina costabilis Zone. This zone and correlated ones along the Gondwana are considered Early Permian in age. However, a first isotopic age recently obtained for the upper Itararé Group and published elsewhere is considered within a regional stratigraphic framework once it leads to new insights in terms of the LPIA time span recorded in the Paraná Basin.-
dc.descriptionFil: Valdez Buso, Victoria. University of Aberdeen; Reino Unido-
dc.descriptionFil: Danielski Aquino, Carolina. Universidade do Vale do Rio Dos Sinos. Programa de Pós-Graduação em Geologia; Brasil-
dc.descriptionFil: Gomes Paim, Paulo Sérgio. Universidade do Vale do Rio Dos Sinos. Programa de Pós-Graduação em Geologia; Brasil-
dc.descriptionFil: Alves de Souza, Paulo. Universidade Federal do Rio Grande do Sul; Brasil-
dc.descriptionFil: Mori, Ana Louisa. Universidade Federal do Rio Grande do Sul; Brasil-
dc.descriptionFil: Fallgatter, Claus. University of Aberdeen; Reino Unido-
dc.descriptionFil: Milana, Juan Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - San Juan. Centro de Investigaciones de la Geosfera y Biosfera. Universidad Nacional de San Juan. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones de la Geosfera y Biosfera; Argentina-
dc.descriptionFil: Kneller, Benjamin. University of Aberdeen; Reino Unido-
dc.formatapplication/pdf-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherElsevier Science-
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.palaeo.2017.09.004-
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0031018217302675-
dc.rightsinfo:eu-repo/semantics/restrictedAccess-
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/-
dc.sourcereponame:CONICET Digital (CONICET)-
dc.sourceinstname:Consejo Nacional de Investigaciones Científicas y Técnicas-
dc.sourceinstacron:CONICET-
dc.subjectBIOSTRATIGRAPHY-
dc.subjectITARARÉ GROUP-
dc.subjectPALYNOLOGY-
dc.subjectSEQUENCE STRATIGRAPHY-
dc.subjectMeteorología y Ciencias Atmosféricas-
dc.subjectCiencias de la Tierra y relacionadas con el Medio Ambiente-
dc.subjectCIENCIAS NATURALES Y EXACTAS-
dc.titleLate Palaeozoic glacial cycles and subcycles in western Gondwana: Correlation of surface and subsurface data of the Paraná Basin, Brazil-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.typeinfo:ar-repo/semantics/articulo-
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