First record of ostracods from the Upper Ordovician red-coloured marine sandstones of the Tierekeawati Formation in Tarim Basin, NW China: implications on palaeoenvironment and palaeobiogeography

First record of ostracods from the Upper Ordovician red-coloured marine sandstones of the Tierekeawati Formation in Tarim Basin, NW China: implications on palaeoenvironment and palaeobiogeography
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塔里木盆地铁热克瓦提组上奥陶统红色海相砂岩中介形类的首次记录:对古环境和古生物地理学的意义

DOI:
10.1186/s42501-020-00064-y
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发表时间:
2020-05
期刊:
Journal of Palaeogeography
影响因子:
--
通讯作者:
Zheng-Jiang Luo
Zheng-Jiang Luo
中科院分区:
其他
文献类型:
--
作者:
Jun-Jun Song;Yi-Xin Shen;Peng Tang;Xiao-Le Zhang;Qi-Jian Li;Zheng-Jiang Luo

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在新疆塔里木盆地西北部柯坪地区上奥陶统铁热克瓦提组阿里苏剖面(阿里苏红层)红色海相砂岩中首次发现介形类。记述并绘制了13属22种。介形类动物群表明,这些岩层可能属于沙边-卡田时代。介形类动物群的古生态组合反映了塔里木盆地铁热克瓦提组阿里苏红层沉积时的近岸-近海环境。在阿里苏红层的介形类动物群中发现了许多世界性属和省级属,暗示了晚奥陶世塔里木、西藏和南中国板块以及欧洲和北美大陆之间可能的生物地理关系。介形类在晚奥陶世经历了劳伦斯和塔里木板块之间的动物群交换。
Ostracods are described for the first time from the red-coloured marine sandstones of Arisu section (Arisu red beds) of the Upper Ordovician Tierekeawati Formation in Kalpin area of northwestern Tarim Basin, Xinjiang Uygur Autonomous Region (Xinjiang), Northwest China. Twenty-two species belonging to thirteen genera are described and figured. The ostracod fauna suggests a probable Sandbian–Katian age for these beds. The palaeoecological assemblage of ostracod fauna implies the deposition in a nearshore-offshore environment during a regression when the Arisu red beds of the Tierekeawati Formation were laid down in the Tarim Basin. Many cosmopolitan and provincial genera were present in diversified ostracod fauna of the Arisu red beds, suggesting the possible biogeographic relationships among the Tarim, Tibet, and South China plates, as well as Europe and North America continents during the Late Ordovician. Ostracods experienced faunal exchanges between Laurentia and the Tarim Plate during the Late Ordovician Period.
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