2012
DOI: 10.1016/j.cretres.2011.09.006
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An Early Cretaceous flora from Cusano Mutri, Benevento, southern Italy

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Cited by 20 publications
(7 citation statements)
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“…Comparison with other fossil taxa. -The plant megafossil that is most similar to Pseudoasterophyllites cretaceus is Montsechia vidalii (Zeiller) Teixeira from much older (Early Cretaceous, Barremian) lacustrine deposits at El Montsec and Las Hoyas in Spain (Gomez & al., 2015) and the late Aptian of Italy (Bartiromo & al., 2012). This similarity was recognized by Zeiller (1902), who originally assigned M. vidalii to Pseudoasterophyllites.…”
Section: Version Of Recordmentioning
confidence: 99%
“…Comparison with other fossil taxa. -The plant megafossil that is most similar to Pseudoasterophyllites cretaceus is Montsechia vidalii (Zeiller) Teixeira from much older (Early Cretaceous, Barremian) lacustrine deposits at El Montsec and Las Hoyas in Spain (Gomez & al., 2015) and the late Aptian of Italy (Bartiromo & al., 2012). This similarity was recognized by Zeiller (1902), who originally assigned M. vidalii to Pseudoasterophyllites.…”
Section: Version Of Recordmentioning
confidence: 99%
“…Two main groups of Cheirolepidiaceae are generally recognized based on differences in their shoot morphology: the so-called frenelopsids and nonfrenelopsids. Frenelopsids have predominantly a whorled phyllotaxis and the representative genera (e.g., Frenelopsis and Pseudofrenelopsis) are found mainly in Laurasia (Alvin et al, 1981;Alvin, 1982;Francis, 1983;Watson, 1988;Clement-Westerhof and van Konijnenburg-van Cittert, 1991;Zhou, 1995;Guignard et al, 1998;Watson and Alvin, 1999;Daviero et al, 2001;Gomez et al, 2002b;Axsmith, 2006;Yang et al, 2006;Mendes et al, 2010;Bartiromo et al, 2012), but a few are also known from Gondwana (Watson, 1983;Kunzmann et al, 2006;Sucerquia et al, 2008). The non-frenelopsids have leaves borne in a spiral arrangement and include representatives of genera such as Brachyphyllum (Watson, 1988;Du et al, 2013) and Watsoniocladus (Srinivasan, 1995) from Laurasia, and Tomaxellia and Tarphyderma (Archangelsky, 1963(Archangelsky, , 1966(Archangelsky, , 1968Taylor, 1986, 1991;Villar de Seoane, 1998;Kunzmann et al, 2006) from Gondwana.…”
Section: Introductionmentioning
confidence: 99%
“…with local development of bauxite and lacustrine or saltmarsh to evaporite deposits, depending on major shifts in hydroclimatic conditions (Mindszenty et al, 1995;Carannante et al, 2007;Simone et al, 2012;Graziano & Raspini, 2015;Graziano et al, 2016;Bartiromo et al, 2019). Distinct fossil Lagerst€ atten, 0.5 to 1.5 m thick on average, were therefore formed as major stratigraphic key markers during the longest sea-level lowstands in the Aptian-Cenomanian (Bravi et al, 2004;Bartiromo et al, 2012Bartiromo et al, , 2019Graziano et al, 2016). Figure 2 reports the resulting continental and paralic fossiliferous Lagerst€ atten in the upper Aptian-lower Albian of the ApCP in the south-east Matese Mountains which is being increasingly referred to as a crucial area for understanding the high-frequency mid-Cretaceous palaeoclimatic dynamics in a supra-regional perspective (Graziano et al, 2016).…”
Section: Geological Framework and Synthetic Stratigraphy Of The Pietr...mentioning
confidence: 99%