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Oxfordian (Jurassic) mayaitid (ammonite) dispersal in the Tibetan Himalaya as the first signal of the establishment of the Indo-Austral subrealm
作者姓名:YIN  Jiarun
作者单位:China University of Geosciences, Beijing 100083, China
基金项目:Supported by the National Natural Science Foundation of China (Grant No. 40072001) and the National Geographic Society of USA (Grant No. 5865-97)
摘    要:New fossil collections in the Lanongla area, Tibetan Himalaya enables the establishment of the Upper Jurassic ammonoid succession. Middle Oxfordian ammonite-fauna is characterized by endemic epimayaitids with a marine deepening event, suggesting a high stand of sea level in the Tibetan Himalaya. Distribution of mayaitids around the Eastern Gondwana can be regarded as the first signal of the Indo-Austral Subrealm that was progressively established during the Late Jurassic and Early Cretaceous times.

关 键 词:Jurassic    Oxfordian    ammonites    Tibetan  Himalaya    Indo-Austral  Subrealm

Oxfordian (Jurassic) mayaitid (ammonite) dispersal in the Tibetan Himalaya as the first signal of the establishment of the Indo-Austral subrealm
YIN Jiarun.Oxfordian (Jurassic) mayaitid (ammonite) dispersal in the Tibetan Himalaya as the first signal of the establishment of the Indo-Austral subrealm[J].Progress in Natural Science,2003,13(4):282-287.
Authors:YIN Jiarun
Institution:China University of Geosciences, Beijing 100083, China
Abstract:New fossil collections in the Lanongla area, Tibetan Himalaya enables the establishment of the Upper Jurassic ammonoid succession. Middle Oxfordian ammonite-fauna is characterized by endemic epimayaitids with a marine deepening event, suggesting a high stand of sea level in the Tibetan Himalaya. Distribution of mayaitids around the Eastern Gondwana can be regarded as the first signal of the Indo-Austral Subrealm that was progressively established during the Late Jurassic and Early Cretaceous times.
Keywords:Jurassic  Oxfordian  ammonites  Tibetan Himalaya  Indo-Austral Subrealm
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