首页> 外文期刊>Historical Biology: an international journal of paleobiology >Cyprinid fishes from Eocene molasse deposits (Liyan Formation), India-Asia collision zone, Eastern Ladakh, NW Himalaya, India: implications for non-marine aquatic connections between India and Mainland Asia
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Cyprinid fishes from Eocene molasse deposits (Liyan Formation), India-Asia collision zone, Eastern Ladakh, NW Himalaya, India: implications for non-marine aquatic connections between India and Mainland Asia

机译:鲤科的鱼类从始新世磨拉石沉积(Liyan形成),India-Asia碰撞区,印度拉达克东部、西北喜马拉雅:影响对于非海相水生印度之间的连接和亚洲大陆

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摘要

The molasse deposits in the Indus Basin of India-Asia collision zone (Indus Suture Zone) of Ladakh, NW Himalaya, preserve a record of orogenic sedimentation associated with uplift and erosion of the southern margin of Asia in the course of ongoing India-Eurasia collision. Fossils from these continental deposits are scarce but hold important clues to the early history of India-Asia collision. Here we describe a small collection of dental remains of cyprinids, a family of freshwater fishes, from the Late Eocene Liyan Formation exposed in a high altitude (>5000 m) locality in the Indus Suture Zone of Eastern Ladakh. The find assumes significance since, unlike the Liyan Formation, most other molassic deposits of Ladakh rest unconformably over the Ladakh Batholith and are much younger (Late Oligocene/Early Miocene). The Liyan cyprinids, which represent the oldest record of Cyprinidae in India, suggest fluvial connections with contemporary Eocene ecosystems in Mainland Asia where this family originated in the middle Eocene or earlier. Dispersal of cyprinids from the Mainland Asia into the Indus Suture Zone of Ladakh took place from Tibet via alluvial drainage of the paleo-Indus river during floods or high runoff following the India-Asia collision.
机译:印度河流域的磨拉石沉积India-Asia碰撞区(印度河缝合带)拉达克,NW喜马拉雅,保存的记录造山与隆起和相关沉积亚洲的南部边缘的侵蚀持续的大理石的碰撞。从这些存款是大陆化石稀缺但持有重要早期的线索India-Asia碰撞的历史。一个小的集合牙科的遗体鲤科的,一个家庭的淡水鱼类,从始新世末Liyan形成暴露在高高度(> 5000)位置在印度河缝合区东部的拉达克。意义,因为与Liyan形成,其他大多数molassic存款拉达克的休息不整合在拉达克岩基更年轻(渐新世末/中新世早期)。Liyan鲤科的,代表了最古老的在印度的鲤科的记录,建议河流联系当代始新世的生态系统在这个家族起源于亚洲大陆始新世或更早。从亚洲大陆鲤科的印度河缝合带的拉达克从西藏通过冲积的排水paleo-Indus河中洪水或高India-Asia后径流碰撞。

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