Sedimentology of the proximal portion of a large-scale, Upper Jurassic fluvial-aeolian system in Paraná Basin, southwestern Gondwana
Upper Jurassic sedimentary rocks of Guará Formation record the environmental and geotectonic changes of the early break-up stages in the southwestern portion of Gondwana. Newly-described occurrences of this formation allow the expansion of its areal distribution to the central part of the Paraná Bas...
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Published in | Journal of South American earth sciences Vol. 95; p. 102248 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
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Elsevier Ltd
01.11.2019
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Abstract | Upper Jurassic sedimentary rocks of Guará Formation record the environmental and geotectonic changes of the early break-up stages in the southwestern portion of Gondwana. Newly-described occurrences of this formation allow the expansion of its areal distribution to the central part of the Paraná Basin, Brazil. Four vertical sections are presently described in Paraná State, Brazil. Nineteen lithofacies were grouped in five facies associations, through the classical method of facies analysis. The facies analysis included Guará Formation and the adjacent portions of the underlying Pirambóia Formation and the overlying Botucatu Formation. The depositional system of Pirambóia Formation was wet aeolian fluvial-influenced and is composed by aeolian dunes, aeolian sandsheets/interdunes and ephemeral fluvial deposits facies associations. The Guará Formation is composed of multistorey fluvial facies association constituting a highly amalgamated perennial fluvial system. It is overlaid by the Botucatu Formation, characterized as a dry aeolian system formed by aeolian dune deposits. The stratigraphic units are separated by regional unconformities marked by a shift in facies and depositional systems that reflect climatic changes. The Guará Formation depositional model, established in correlation with southern sections, represents a broad fluvial system with aeolian interaction deposited in a wide basin with more than 800 km in extension. This large depositional paleoenvironment, together with other Upper Jurassic records in southwestern Gondwana, represents the early rift stage of Gondwana break-up.
•The area of Guará Formation (Upper Jurassic) is expanded to the central part of Paraná Basin.•The Guará Formation is correlated in >800 km long dip section through southern Brazil and northwestern Uruguay.•The Guará Formation records a big distributive fluvial system with aeolian influence.•The Guará Formation is the record of a wide endorheic basin related with the first tectonic efforts of Gondwana break-up. |
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AbstractList | Upper Jurassic sedimentary rocks of Guará Formation record the environmental and geotectonic changes of the early break-up stages in the southwestern portion of Gondwana. Newly-described occurrences of this formation allow the expansion of its areal distribution to the central part of the Paraná Basin, Brazil. Four vertical sections are presently described in Paraná State, Brazil. Nineteen lithofacies were grouped in five facies associations, through the classical method of facies analysis. The facies analysis included Guará Formation and the adjacent portions of the underlying Pirambóia Formation and the overlying Botucatu Formation. The depositional system of Pirambóia Formation was wet aeolian fluvial-influenced and is composed by aeolian dunes, aeolian sandsheets/interdunes and ephemeral fluvial deposits facies associations. The Guará Formation is composed of multistorey fluvial facies association constituting a highly amalgamated perennial fluvial system. It is overlaid by the Botucatu Formation, characterized as a dry aeolian system formed by aeolian dune deposits. The stratigraphic units are separated by regional unconformities marked by a shift in facies and depositional systems that reflect climatic changes. The Guará Formation depositional model, established in correlation with southern sections, represents a broad fluvial system with aeolian interaction deposited in a wide basin with more than 800 km in extension. This large depositional paleoenvironment, together with other Upper Jurassic records in southwestern Gondwana, represents the early rift stage of Gondwana break-up.
•The area of Guará Formation (Upper Jurassic) is expanded to the central part of Paraná Basin.•The Guará Formation is correlated in >800 km long dip section through southern Brazil and northwestern Uruguay.•The Guará Formation records a big distributive fluvial system with aeolian influence.•The Guará Formation is the record of a wide endorheic basin related with the first tectonic efforts of Gondwana break-up. |
ArticleNumber | 102248 |
Author | Kifumbi, Carrel Souza, Ezequiel Galvão de Amarante, Francyne Bochi do Reis, Adriano Domingos dos Scherer, Claiton Marlon dos Santos Ferronatto, João Pedro Formolo Rossetti, Marcos de Magalhães May Owen, Amanda |
Author_xml | – sequence: 1 givenname: Adriano Domingos dos orcidid: 0000-0003-1892-8459 surname: Reis fullname: Reis, Adriano Domingos dos email: a_d_reis@hotmail.com, adriano.reis@ufrgs.br organization: Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, Prédio 43137, Agronomia, 91501-970 Porto Alegre, RS, Brazil – sequence: 2 givenname: Claiton Marlon dos Santos surname: Scherer fullname: Scherer, Claiton Marlon dos Santos organization: Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Brazil – sequence: 3 givenname: Francyne Bochi do surname: Amarante fullname: Amarante, Francyne Bochi do organization: Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, Prédio 43137, Agronomia, 91501-970 Porto Alegre, RS, Brazil – sequence: 4 givenname: Marcos de Magalhães May orcidid: 0000-0002-3792-4050 surname: Rossetti fullname: Rossetti, Marcos de Magalhães May organization: Department of Geology, University of Canterbury, New Zealand – sequence: 5 givenname: Carrel surname: Kifumbi fullname: Kifumbi, Carrel organization: Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, Prédio 43137, Agronomia, 91501-970 Porto Alegre, RS, Brazil – sequence: 6 givenname: Ezequiel Galvão de surname: Souza fullname: Souza, Ezequiel Galvão de organization: Universidade Federal do Pampa, Brazil – sequence: 7 givenname: João Pedro Formolo surname: Ferronatto fullname: Ferronatto, João Pedro Formolo organization: Programa de Pós-Graduação em Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, Prédio 43137, Agronomia, 91501-970 Porto Alegre, RS, Brazil – sequence: 8 givenname: Amanda surname: Owen fullname: Owen, Amanda organization: University of Glasgow, United Kingdom |
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Keywords | Climatic changes Fluvial-aeolian interaction Upper Jurassic Southwestern Gondwana Distributive fluvial |
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Title | Sedimentology of the proximal portion of a large-scale, Upper Jurassic fluvial-aeolian system in Paraná Basin, southwestern Gondwana |
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