2020
DOI: 10.1016/j.geobios.2020.04.002
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New plant fossil records and biostratigraphic analysis from the Uspallata Group (Late Triassic) at Cacheuta Hill, Cuyo Basin, west-central Argentina

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Cited by 16 publications
(9 citation statements)
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“…The presence of Scytophyllum is the first mention of these structures for the Agua de los Pajaritos depocenter. The discovery of materials assignable to Rissikianthus extends its distribution because previously, similar elements had only been mentioned in the Cañadón Largo Formation of the El Tranquilo Group (Gnaedinger and Herbst, 2008;Gnaedinger, 2010) and in the Cacheuta Formation (Bodnar et al, 2020).The presence of Acevedoa cf. rastroensis expanded the distribution of this genus, which had previously been described only in the Los Rastros Formation in the Ischigualasto-Villa Unión Basin Lutz, 2010, 2014).…”
Section: Discussionmentioning
confidence: 76%
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“…The presence of Scytophyllum is the first mention of these structures for the Agua de los Pajaritos depocenter. The discovery of materials assignable to Rissikianthus extends its distribution because previously, similar elements had only been mentioned in the Cañadón Largo Formation of the El Tranquilo Group (Gnaedinger and Herbst, 2008;Gnaedinger, 2010) and in the Cacheuta Formation (Bodnar et al, 2020).The presence of Acevedoa cf. rastroensis expanded the distribution of this genus, which had previously been described only in the Los Rastros Formation in the Ischigualasto-Villa Unión Basin Lutz, 2010, 2014).…”
Section: Discussionmentioning
confidence: 76%
“…The importance of discovering strobiliform structures assigned to the genus Rissikianthus corresponds to the first record of this genus in the San Juan Province. In addition, it expands the biostratigraphic distribution of the genus because materials assignable to Rissikianthus have been mentioned in the Cañadón Largo Formation of the El Tranquilo Group (Gnaedinger, 2010;Gnaedinger and Herbst, 2008) andthe Cacheuta Formation of the Uspallata Group (Bodnar et al, 2020), both from the Upper Triassic. The presence of permineralized wood assignable to the genus Protocircoporoxylon also extends the paleobiogeographic distribution of the genus to the Cuyana Basin.…”
Section: Paleogeographic and Biostratigraphic Considerationsmentioning
confidence: 95%
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“…However, the Cretaceous voltzialean conifers, which are members of the family Krassiloviaceae, produced peltate OCs with multiple spines at their distal area. Moreover, while some Paleozoic Voltziales have a leaf morphology comparable to that of the Patagonian remains (e.g., Stewart & Rothwell, 1993; Hernandez‐Castillo et al, 2009), Mesozoic Voltziales are characterized by expanded, multiveined leaves (Escapa et al, 2010; Morel et al, 2011; Bomfleur et al, 2013; Bodnar et al, 2020; Herrera et al, 2020).…”
Section: Discussionmentioning
confidence: 99%
“…Umkomasia has been affiliated with the microsporangium Pteruchus and Dicroidium leaves (Thomas, 1933;Petriella, 1977Petriella, , 1980Petriella, , 1981Anderson & Anderson, 2003;Anderson et al, 2019). In Argentina specimens assigned to Umkomasia have been reported in the Potrerillos, Cortaderita, and Paso Flores formations (Cuyana Basin) (Artabe et al, 2001;Gnaedinger & Zavattieri, 2017;Bodnar et al, 2020).…”
Section: Systematic Paleontologymentioning
confidence: 99%