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首页> 外文期刊>Indian Minerals >Ichthyofauna of the Lower Triassic Panchet Formation, Damodar valley basin, West Bengal, and its implications
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Ichthyofauna of the Lower Triassic Panchet Formation, Damodar valley basin, West Bengal, and its implications

机译:西孟加拉邦达莫达尔河谷盆地下三叠世潘切特组的鱼腥藻属植物及其意义

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摘要

A diverse and abundant freshwater ichthyofauna has been recorded from the Lower Triassic Panchet Formation of Damodar valley basin, West Bengal. It is represented by numerous scales, teeth and tooth plates assigned to actinopterygian and dipnoi fishes and chondrichthyan shark, the latter being an important addition to the known global record of freshwater shark in the Lower Triassic. Some of the actinopterygian fish scales are comparable with those of the Arcadia Formation of Australia which is considered as older than the Lower Burgersdrop Formation of South Africa. This substantiates correlation of the Panchet Formation with the globally recognised Lootsbergian Land Vertebrate Faunachron. The new finds from the Panchet Formation refute the contention that the Lower Triassic freshwater actinopterygian fishes were endemic and support the view that the Gondwana landmasses were connected during the Lower Triassic.
机译:西孟加拉邦Damodar谷盆地的下三叠世Panchet组已经记录到多种多样的丰富淡水鱼科鱼类。它由分配给放线y和and鱼和软骨鱼类的众多鳞片,牙齿和齿板代表,后者是已知的下三叠纪淡水鲨鱼全球记录的重要补充。一些放线翅目鱼鳞与澳大利亚的阿卡迪亚组相当,后者被认为比南非的下伯格斯drop组更老。这证实了Panchet组与全球公认的Lootsbergian陆生脊椎动物Faunachron的相关性。潘切特组的新发现驳斥了下三叠纪淡水放线翅目鱼类是地方性的论点,并支持了冈瓦纳陆块在下三叠纪发生联系的观点。

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