2015
DOI: 10.4072/rbp.2015.1.09
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Palinomorfos de afinidad incierta en la perforación DI.NA.MI.GE. 254 “Paso de las Toscas” (Pérmico Inferior), Cuenca Paraná, Uruguay

Abstract: Un rasgo importante que presentan las asociaciones palinológicas del Neopaleozoico en las cuencas Paraná (tanto en Brasil como en Uruguay) y Chacoparaná (Argentina) es la presencia de palinomorfos del Silúrico-Devónico retrabajados

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Cited by 9 publications
(3 citation statements)
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“…As previously mentioned, the shallow lacustrine successions of the La Veteada Formation were initially deposited in Sierra de Narváez, where the palynological associations are consistent with a Guadalupian age for that section (Gutiérrez et al, 2011). In contrast, the Central Famatina deposition of this unit begins with paleosols of undefined age (b5 m), underlying a lacustrine succession deposited during the Lopingian (Zavattieri and Gutiérrez, 2012;Gutiérrez et al, 2015). The absence of records of the younger palynological association in the north may be due fact that to top of the sequence is eroded.…”
Section: Discussionmentioning
confidence: 60%
“…As previously mentioned, the shallow lacustrine successions of the La Veteada Formation were initially deposited in Sierra de Narváez, where the palynological associations are consistent with a Guadalupian age for that section (Gutiérrez et al, 2011). In contrast, the Central Famatina deposition of this unit begins with paleosols of undefined age (b5 m), underlying a lacustrine succession deposited during the Lopingian (Zavattieri and Gutiérrez, 2012;Gutiérrez et al, 2015). The absence of records of the younger palynological association in the north may be due fact that to top of the sequence is eroded.…”
Section: Discussionmentioning
confidence: 60%
“…The suprageneric classification of spores and pollen grains follows the criteria of Potonié & Kremp (1954) and subsequent modifications (Playford & Dettmann 1996). Reworked elements were identified on the basis of their poor state of preservation and their anomalous stratigraphic positions (see Gutiérrez et al 1997Gutiérrez et al , 2015. Schopf, Wilson & Bentall 1944 [OD] Calamospora fissurata sp.…”
Section: Taxonomic Inventorymentioning
confidence: 99%
“…Tetraporina) e esporos de fungo (Portalites e indeterminados). Os gêneros de alga Brazilea e Tetraporina evidenciam deposição em um ambiente de água doce (Gutiérrez & Limarino, 2001;Longhim, 2007;Guerra-Sommer et al, 2008d;Gutiérrez et al 2015) enquanto que o gênero Navifusa é considerada como parte de microplâncton marinho (Gutiérrez & Limarino, 2001;Jasper et al, 2006), e poderia ser indicativo de pequenas ingressões marinhas, uma vez que a quantidade registrada é muito baixa.…”
Section: Paleoecologiaunclassified