Estudio palinologico de la Formacion Piedra Pintada, Jurasico inferior da la Cuenca Neuquina (Argentina)

dc.creatorArguijo, M
dc.creatorVolkheimer, W
dc.creatorRosenfeld, U
dc.date1982-12-01
dc.date.accessioned2022-12-15T19:36:08Z
dc.date.available2022-12-15T19:36:08Z
dc.identifierhttps://ppegeo.igc.usp.br/index.php/bigusp/article/view/2694
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5357951
dc.descriptionThis is a study of four microfloristic assemblages, in which the terrestrial species (43) are prevailing. The genera present are Deltoidospora, Alsophilidites, Dictyophyllidites, Lygodiumsporites, Concavisporites, Verrucosisporites, Leptolepidites, Foveosporites, Granulat isporit es, Baculatisporites, Lycopodiumsporites, Gleicheniidites, Antulsporites, Interulobites, Nevesisporites, Taurocusporites, Peromonolites, Vitreisporites, Alisporites, Podocarpidites, Phrixipollenites, Microcachryidites, Inaperturopollenites, Araucariacites, Perinopollenites, Classopollis, Cycadopites and Monosulcites, and the marine genera Pleurozonaria and Leiosphaeridia. The age indicated by the microflora (Nevesiporites vallatus-Assemblage, previous to the income of Callialasporites spp.), is the pre-upper Toarcian Lower Jurassic.en-US
dc.formatapplication/pdf
dc.languagespa
dc.publisherUniversidade de São Paulo, Instituto de Geociênciaspt-BR
dc.relationhttps://ppegeo.igc.usp.br/index.php/bigusp/article/view/2694/2278
dc.rightsDireitos autorais 1982 Boletim IGpt-BR
dc.sourceBoletim IG; v. 13 (1982); 100-107pt-BR
dc.source2316-8978
dc.source0100-3879
dc.titleEstudio palinologico de la Formacion Piedra Pintada, Jurasico inferior da la Cuenca Neuquina (Argentina)es-ES
dc.titleEstudio palinologico de la Formacion Piedra Pintada, Jurasico inferior da la Cuenca Neuquina (Argentina)pt-BR
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typept-BR


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