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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia)
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Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia)

机译:来自Degon Demonian Island Arc Settings(Baruunhuurai Terrane,Western Mongolia)的康顿

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摘要

Upper Devonian marine deposits of the Baruunhuurai Terrane in western Mongolia represent island arc settings, which yielded a diverse conodont assemblage of 30 taxa, including species of Ancyrognathus (as well as one new species), Icriodus, Mehlina, Polygnathus and Palmatolepis. Biodiversity analysis of Ancyrognathus, Pelekysgnathus, Mehlina and Icriodus shows that the Mongolian conodont assemblage consists of two endemic and few cosmopolitan taxa. Representatives of the otherwise globally distributed genus Pelekysgnathus are absent. An important factor influencing the regional distribution of conodont taxa seems to be the siliciclastic-dominated sedimentation of the Baruunhuurai Terrane during the early Famennian.
机译:蒙古西部Baruunhuurai Terrane的上部德文郡海洋沉积物代表了岛弧设置,它产生了多元化的30个分类群,包括AncyRognathus(以及一种新物种),Icriodus,Mehlina,Polygnathus和Palmatolepis。 女性经验分析,Pelekysgnathus,Mehlina和Icriodus的生物多样性分析表明,蒙古康诺集团组成包括两种流行和少数国际纳瓦纳。 其他全球分布的属Pelekysgnathus的代表不存在。 影响康诺克纳群岛区域分布的一个重要因素似乎是本百年初期的帕鲁努武拉伊特拉的硅砾占主导地位。

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