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New dinosaur species from the Upper Triassic Upper Maleri and Lower Dharmaram formations of Central India

机译:印度中部上三叠统上马累和下达玛拉姆组的新恐龙种

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The beginning of dinosaur evolution is currently known based on a handful of highly informative Gondwanan outcrops of Ischigualastian age (late Carnian–early Norian). The richest Triassic dinosaur records of the southern continents are those of South America and South Africa, with taxonomically diverse faunas, whereas faunas from India and central Africa are more poorly known. Here, the known diversity of Gondwanan Triassic dinosaurs is increased with new specimens from central India, which allow a more comprehensive characterisation of these dinosaur assemblages. Five dinosauriform specimens are reported from the probable late Norian–earliest Rhaetian Upper Maleri Formation, including two new sauropodomorph species, the nonplateosaurian Nambalia roychowdhurii and the plateosaurian Jaklapallisaurus asymmetrica, a guaibasaurid and two basal dinosauriforms. The Lower Dharmaram Formation, probably latest Norian–Rhaetian in age, includes basal sauropodomorph and neotheropod remains, providing the second record of a Triassic Gondwanan neotheropod. The currently available evidence suggests that the oldest known Gondwanan dinosaur assemblages (Ischigualastian) were not homogeneous, but more diverse in South America than in India. In addition, the Upper Maleri and Lower Dharmaram dinosaur assemblages resemble purported coeval South American and European beds in the presence of basal sauropodomorphs. Accordingly, the current available evidence of the Triassic beds of the Pranhita–Godavari Basin suggests that dinosaurs increased in diversity and abundance during the late Norian to Rhaetian in this region of Gondwana.
机译:目前,恐龙进化的开始是基于少数具有高度信息量的Ischigualastian年代(Carnian – Norian早期)的冈瓦南露头而闻名的。南部大陆最丰富的三叠纪恐龙记录是南美和南非的记录,其动物学具有不同的分类,而印度和中部非洲的动物则鲜为人知。在这里,来自印度中部的新标本增加了冈瓦南三叠纪恐龙的已知多样性,这使这些恐龙组合的特征更加全面。据报道,可能来自诺里安晚期至最早的雷蒂亚上马里构造的五个恐龙龙标本,包括两个新的蜥脚类目物种,非板龙Nambalia roychowdhurii和板龙不对称的Jaklapallisaurus,一个鳄龙和两个基底龙。下达玛拉姆组,可能是年龄最晚的诺里安-拉提安时代,包括基底蜥脚类动物和新兽脚类动物遗骸,提供了三叠纪冈瓦南新兽脚类动物的第二份记录。目前可用的证据表明,已知最古老的冈瓦南恐龙组合(伊斯基瓜拉斯蒂安)不是同质的,但在南美比印度更多样化。此外,在基部蜥脚类目动物存在的情况下,上马列里恐龙和下达玛拉姆恐龙组合类似于据说的南美和欧洲古代床。因此,Pranhita-Godavari盆地三叠纪河床的现有证据表明,在冈瓦纳地区从Norian到Rhaetian晚期,恐龙的多样性和丰度增加了。

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