2020
DOI: 10.1080/02724634.2020.1828438
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To be or not to be: The Hidden Side ofCargninia Enigmaticaand Other Puzzling Remains of Lepidosauromorpha from the Upper Triassic of Brazil

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Cited by 9 publications
(3 citation statements)
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“…Located in the municipality of Faxinal do Soturno, State of Rio Grande do Sul, this site has revealed an astonishing quantity and diversity of Norian vertebrates (Bonaparte, Schultz, & Martinelli, 2010; Schultz et al, 2020). After its discovery at the end of the 1990s, this site yielded hundreds of tetrapod remains that stand out for their exceptional preservation, including several cranial and postcranial materials of non‐mammaliaform cynodonts (Bonaparte et al, 2001, 2003, 2005; Bonaparte, Schultz, & Martinelli, 2010; Guignard et al, 2019a, 2019b; Martinelli et al, 2005; Martinelli & Soares, 2016; Oliveira et al, 2011; Soares et al, 2011), one partial skeleton of the saurischian dinosaur Guaibasaurus candelariensis (Agnolín & Martinelli, 2012; Bonaparte et al, 2007), remains of a putative pterosaur (Bonaparte, Schultz, & Soares, 2010; but see Soares et al, 2013; Dalla Vecchia, 2014), skulls and postcranial elements of procolophonoids (Cisneros & Schultz, 2003), sphenodontians (Arantes et al, 2009; Bonaparte & Sues, 2006; Ferigolo, 2000; Hsiou et al, 2015; Romo de Vivar, Martinelli, Hsiou, & Soares, 2020; Romo de Vivar & Soares, 2015), and skull remains of non‐rhynchocephalian lepidosauromorphs (Bonaparte, Schultz, & Martinelli, 2010; Romo de Vivar, Martinelli, Fonseca, & Soares, 2020). In addition, fish remains, insects, conchostracans, invertebrate ichnofossils, dinosaur footprints, and gymnosperms have been recovered at the site (Barboni & Dutra, 2013; Rohn et al, 2014; Silva et al, 2012), although from overlaying levels.…”
Section: Introductionmentioning
confidence: 99%
“…Located in the municipality of Faxinal do Soturno, State of Rio Grande do Sul, this site has revealed an astonishing quantity and diversity of Norian vertebrates (Bonaparte, Schultz, & Martinelli, 2010; Schultz et al, 2020). After its discovery at the end of the 1990s, this site yielded hundreds of tetrapod remains that stand out for their exceptional preservation, including several cranial and postcranial materials of non‐mammaliaform cynodonts (Bonaparte et al, 2001, 2003, 2005; Bonaparte, Schultz, & Martinelli, 2010; Guignard et al, 2019a, 2019b; Martinelli et al, 2005; Martinelli & Soares, 2016; Oliveira et al, 2011; Soares et al, 2011), one partial skeleton of the saurischian dinosaur Guaibasaurus candelariensis (Agnolín & Martinelli, 2012; Bonaparte et al, 2007), remains of a putative pterosaur (Bonaparte, Schultz, & Soares, 2010; but see Soares et al, 2013; Dalla Vecchia, 2014), skulls and postcranial elements of procolophonoids (Cisneros & Schultz, 2003), sphenodontians (Arantes et al, 2009; Bonaparte & Sues, 2006; Ferigolo, 2000; Hsiou et al, 2015; Romo de Vivar, Martinelli, Hsiou, & Soares, 2020; Romo de Vivar & Soares, 2015), and skull remains of non‐rhynchocephalian lepidosauromorphs (Bonaparte, Schultz, & Martinelli, 2010; Romo de Vivar, Martinelli, Fonseca, & Soares, 2020). In addition, fish remains, insects, conchostracans, invertebrate ichnofossils, dinosaur footprints, and gymnosperms have been recovered at the site (Barboni & Dutra, 2013; Rohn et al, 2014; Silva et al, 2012), although from overlaying levels.…”
Section: Introductionmentioning
confidence: 99%
“…Known from an isolated but largely complete lower jaw, it appears to suffice for setting up a minimum age for Iguania at the Campanian/Maastrichtian boundary (72.1 ± 0.2 Ma: ICS), which I round to 72 Ma. I should mention, however, that a reviewer doubts the phylogenetic position of Gueragama for unstated reasons, and that Romo de Vivar et al (2020) found that most or all of the similarities between Gueragama and Acrodonta are shared with the Triassic pan-lepidosaur Cargninia , likely indicating that these features are evolutionarily correlated with each other and prone to convergence. Meanwhile, Alifanov (2020) called Gueragama an isodontosaurid (see above) without stating a reason.…”
Section: Methodsmentioning
confidence: 98%
“…As indicated by previous authors (e.g., Evans, 2003;Benson et al, 2013;Cleary et al, 2018), the main obstacle for understanding the early evolution and origins of different squamate lizard clades is probably the poorly documented fossil record in the Southern Hemisphere. Despite the paucity of this record, the growing fossil record of lepidosaurian taxa highlights a hidden history of the group in Gondwana (e.g., Bonaparte et al, 2010;Simões et al, 2015a, b;Bittencourt et al, 2020;Romo de Vivar et al, 2020).…”
Section: Paleochelco Occultato and Its Implications On The Fossil Record Of Lizardsmentioning
confidence: 99%