首页> 外文期刊>Journal of the Palaeontological Society of India >LATE CRETACEOUS GONDWANATHERIAN MAMMALS OF INDIA: DISTRIBUTION, INTERRELATIONSHIPS AND BIOGEOGRAPHIC IMPLICATIONS
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LATE CRETACEOUS GONDWANATHERIAN MAMMALS OF INDIA: DISTRIBUTION, INTERRELATIONSHIPS AND BIOGEOGRAPHIC IMPLICATIONS

机译:印度晚白垩世冈第纳河哺乳动物:分布,相互关系和生物地理学意义

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摘要

Gondwanatheria is a poorly-known extinct order of the class Mammalia. It represents an enigmatic and distinctive non-tribosphenic radiation of mammals in the Southern Hemisphere with fossils documented from the Late Cretaceous and early Middle Eocene of Argentina, Late Cretaceous of Madagascar and India, ? Cretaceous of Tanzania and ? Middle Eocene of Antarctica. The Indian gondwanatherian mammals are known by two taxa (Bharattherium bonapartei Prasad et al., 2007a and Dakshina jederi Wilson et al., 2007) from the Upper Cretaceous sediments intercalated with the Deccan volcanic flows (= intertrappean beds) of peninsular India. A close examination of the type specimens of both these Indian sudamericids shows that they are morphologically similar, and given that the publication of Bharattherium pre-dates Dakshina, the latter is regarded here as a junior synonym of the former. In addition, recent fieldwork in central India has resulted in the discovery of a new sudamericid tooth in the Upper Cretaceous (Maastrichtian) intertrappean beds of Kisalpuri, District Dindori (Madhya Pradesh). Though in having two independent transverse lophs, distinct shape of the lophs, and in the absence of infundibulum, perikymata, and enamel islet this tooth differs from Bharattherium and other known sudamericid mammals from Madagascar and Argentina, it is tentatively referred to the family Sudamericidae as we are not aware of morphological variation of molariforms in different loci on the dentition of sudamericid mammals. Further, the phylogenetic and palaeobiogeographic relationships of gondwanatherian mammals are reviewed in light of recent fossil discoveries from the Late Cretaceous of India.
机译:冈瓦纳特里亚是鲜为人知的灭绝类的哺乳动物。它代表了南半球哺乳动物的一种神秘而独特的非摩擦反射性辐射,化石记录了阿根廷的晚白垩纪和始新世中期,马达加斯加的晚白垩纪和印度。坦桑尼亚的白垩纪和?南极中新世。印度冈瓦纳特哺乳动物被两个类群(Bharattherium bonapartei Prasad等人,2007a和Dakshina jederi Wilson等人,2007)从上白垩统沉积物中夹杂着,而上层白垩质沉积物夹有印度半岛的Deccan火山流(=圈内床)。对这两种印度sudamericids的类型标本进行仔细检查后发现,它们在形态上是相似的,并且考虑到Bharattherium的发布早于Dakshina,因此后者在这里被视为前者的初级同义词。此外,最近在印度中部进行的实地调查已在印多里(中央邦)基萨尔普里的上白垩统(马斯特里赫特式)圈床中发现了一种新的苏达美齿。尽管有两个独立的横头狮,它们的形态各异,并且没有漏斗,周基虫和搪瓷胰岛,但这种牙齿不同于巴拉特里姆和马达加斯加和阿根廷的其他已知的sudamericid哺乳动物,暂时将其称为Sudamericidae家族我们尚不知道苏达美类哺乳动物的牙列上不同位点的磨齿状形态变化。此外,根据印度白垩纪晚期的化石发现,回顾了冈瓦纳特哺乳动物的系统发生和古生物地理关系。

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