2006
DOI: 10.1671/0272-4634(2006)26[471:atdsaf]2.0.co;2
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A titanosauriform (Dinosauria: Sauropoda) axis from the Lameta Formation (Upper Cretaceous: Maastrichtian) of Nand, central India

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Cited by 66 publications
(97 citation statements)
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“…Among theropod dinosaurs known from other Gondwanan continents, none compare favourably with DUGF/52. Abelisauroids, including small noasaurids such as those previously described from India and Madagascar 15,[43][44][45] , could be considered the most likely possibility, but they are markedly different from DUGF/52 in dental morphology, most obviously in denticle size and crown height. The only other Gondwanan maniraptorans identified at present are dromaeosaurids, known mainly from Argentina 46 , as well as from India's close Cretaceous neighbour Madagascar 47,48 .…”
Section: Discussionmentioning
confidence: 99%
“…Among theropod dinosaurs known from other Gondwanan continents, none compare favourably with DUGF/52. Abelisauroids, including small noasaurids such as those previously described from India and Madagascar 15,[43][44][45] , could be considered the most likely possibility, but they are markedly different from DUGF/52 in dental morphology, most obviously in denticle size and crown height. The only other Gondwanan maniraptorans identified at present are dromaeosaurids, known mainly from Argentina 46 , as well as from India's close Cretaceous neighbour Madagascar 47,48 .…”
Section: Discussionmentioning
confidence: 99%
“…The supracetabular crest continues posteriorly and connects with the brevis-shelf, a morphology observed in most abelisauroids (e.g. Masiakasaurus Carrano et al, 2011;Majungasaurus Carrano, 2007;Eoabelisaurus Pol & Rauhut, 2012; although not in Rajasaurus Wilson et al, 2003). This contrasts to the condition in most theropods, in which there is a gap between the crest and the lateral margin of the brevis fossa (Carrano & Sampson, 2008).…”
Section: Introductionmentioning
confidence: 93%
“…The palaeobiogeographic significance of the biotic assemblages of the infra-and intertrappean beds has recently been discussed in detail by Khosla and Verma (2014). It is now well understood from the diverse fossil assemblages that, despite its northward drift as an isolated landmass, India supported widely dispersed biota from both Laurasia (Sahni and Khosla 1994a;Prasad et al 2010;Fernández and Khosla 2014;Khosla and Verma 2014) and Gondwana (Wilson et al 2003;Prasad et al 2010;Verma et al 2012;Fernández and Khosla 2014) in addition to endemic species Whatley 2012;Bajpai et al 2013;Khosla and Verma 2014) during the Late Cretaceous. Apart from charophyte and ostracod assemblages the infra-and intertrappean beds also contain vertebrate faunas of Laurasian affinity, though recently doubt has been cast on such relationships Prasad et al 2010).…”
Section: Palaeobiogeographical Implicationsmentioning
confidence: 99%