Impact Studies
DOI: 10.1007/3-540-25736-5_9
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Unravelling the Cretaceous-Paleogene (KT) Turnover, Evidence from Flora, Fauna and Geology

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Cited by 14 publications
(12 citation statements)
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“…8) is shortly after the Cretaceous/ Tertiary (K/T) boundary approximately 65 million years ago (Pope et al, 1998). Evidence suggests that the massive extinctions at the K/T boundary were the result of a meteorite impact causing a global cloud of dust that blocked sunlight and caused a freezing blackout (Alvarez et al, 1980), and had the long-term ecological effect of an overall drying in North and Central America (Ocampo et al, 2006). Specific morphological traits are not readily apparent as potential key innovations that contributed to the great disparity in diversification between these two main clades of Croton.…”
Section: Character Evolutionmentioning
confidence: 99%
“…8) is shortly after the Cretaceous/ Tertiary (K/T) boundary approximately 65 million years ago (Pope et al, 1998). Evidence suggests that the massive extinctions at the K/T boundary were the result of a meteorite impact causing a global cloud of dust that blocked sunlight and caused a freezing blackout (Alvarez et al, 1980), and had the long-term ecological effect of an overall drying in North and Central America (Ocampo et al, 2006). Specific morphological traits are not readily apparent as potential key innovations that contributed to the great disparity in diversification between these two main clades of Croton.…”
Section: Character Evolutionmentioning
confidence: 99%
“…Gierliński & Ahlberg 1994;Meyer et al 2001;Turner et al 2009;Niedźwiedzki 2011;Thulborn 2013). The extinction of non-avian dinosaurs at the CretaceousPaleogene boundary has been the subject of intense debate (Ocampo et al 2006;Wigforss-Lange et al 2007;Schulte et al 2010a,b), but relatively little attention has been given to the dinosaurian response to environmental changes during the endTriassic extinction event (Brusatte et al 2010). Interestingly, Olsen et al (2002) noted that non-dinosaurian footprint diversity drops at the Tr -J boundary, whereas dinosaurian ichnogeneric diversity increases to a maximum in the overlying Jurassic sediments of the Newark Basin, USA.…”
Section: Introductionmentioning
confidence: 99%
“…The nonavian dinosaur fauna present in the Hell Creek Formation disappears at the CretaceousePaleogene boundary (e.g. Lyson et al, 2012 and references therein) reflecting the global extinction of species connected to this event where global food webs were disrupted (Vajda et al, 2001(Vajda et al, , 2004Ocampo et al, 2006: Chin et al, 2013.…”
Section: Introductionmentioning
confidence: 99%