Dispersal events of Triassic-Jurassic boundary faunas, and paleoenvironment of Tibetan Himalaya

Dispersal events of Triassic-Jurassic boundary faunas, and paleoenvironment of Tibetan Himalaya
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三叠纪-侏罗纪界线动物群的扩散事件与西藏喜马拉雅古环境

DOI:
10.1007/s11430-009-0162-4
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发表时间:
2009-12
期刊:
Science in China Series D-Earth Sciences
影响因子:
--
通讯作者:
阴家润
阴家润
中科院分区:
其他
文献类型:
--
作者:
Franz T. Fursich;阴家润

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Germig地区的末端三叠纪氨基和双壳动物群,藏族喜马拉雅山,在三叠纪 - 夏列式边界间隔中生活在热带,浅水环境中。基于氨基生物货币的高层分辨率允许追踪P
End-Triassic ammonoid and bivalve faunas of the Germig area, Tibetan Himalaya, lived in a tropical, shallow-water environment during the Triassic-Jurassic boundary interval. High stratigraphic resolution based on ammonite-biochrons allows to tracing the place of origin of several faunal elements. The bivalvesAguilerellaandCtenostreonoccurred first in the Tibetan Himalaya and migrated from there to the eastern South Pacific, exhibiting a pantropic dispersal pattern. This dispersal route is supported by the distribution pattern of the ammonitesChoristoceras,Discamphiceras, Pleuroacanthites, andPsiloceras calliphyllum. A few taxa, which went extinct everywhere else by the end of the Triassic, survived in the Tibetan Himalaya into early Early Jurassic times. They include the ammonitesChoristocerasandEopsiloceras, and the bivalvesNewaagia, Terquemia,Persia,Ryderia guangdongensis, andCultriopsis angusta. This suggests that the Tibetan Himalaya may have played a refugia role in the course of the end-Triassic mass extinction.
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