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首页> 外文期刊>Journal of Asian earth sciences >Middle Permian brachiopods from the Tumenling Formation in the Wuchang area, southern Heilongjiang, NE China, and their palaeobiogeographical implications
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Middle Permian brachiopods from the Tumenling Formation in the Wuchang area, southern Heilongjiang, NE China, and their palaeobiogeographical implications

机译:中国东北黑龙江武昌地区图们岭组的中二叠纪腕足动物及其古生物地理意义

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This paper describes nine brachiopod species in eight genera from the Tumenling Formation in the Wuchang area, southern Heilongjiang, northeast China. The Tumenling fauna is constrained to a Wordian-Capitanian (Guadalupian, Middle Permian) age, based on the correlation of the faunas, and previously published data from the same horizons in the same area. This Middle Permian brachiopod fauna is characterized by an admixture of elements of Boreal affinity (Kochiproductus sp., Yakovlevia sp., Stenoscisma margaritovi, Gypospirifer volatilis, Spiriferella keilhavii, Spiriferella lita and Alispiriferella neimongolensis), with Palaeoequatorial forms (Spinomarginlfera sp., Vediproductus sp., and Leptodus nobilis). The Wuchang fauna, as a whole, is comparable to several contemporaneous faunas described from Inner Mongolia in northern China, Jilin in Northeast China, South Primorye in eastern Russia, and the Hida Gaien Belt of Japan, in terms of its index elements and its Boreal-Palaeoequatorial mixture. During the Middle Permian these areas (or blocks) were referred to the Inner Mongolia-Japan transition zone or the northern transition zone between the Palaeoequatorial and Boreal Realms. The overwhelming majority of the Boreal elements reveal that the Wuchang area was probably situated in the northern subzone of this transitional zone, which belongs to the southern margin of the Bureya Block. These east and northeast Asian blocks acted as migratory stepping stones bridging faunal migration between the Palaeoequatorial and Boreal realms during the Middle Permian.
机译:本文介绍了黑龙江南部武昌地区土门岭组八属九种腕足动物。根据动物群的相关性以及先前在同一地区同一地域发布的数据,将图们灵动物区系限制在Wordian-Capitanian(瓜达卢普,中二叠纪)时代。该中二叠纪腕足动物区系的特征是与北方亲缘性元素(Kochiproductus sp。,Yakovlevia sp。,Snonoscisma margaritovi,Gypospirifer volatilis,Srifriferella keilhavii,Spriferella lita和Alispiriferella neimongolensis),古赤道形式(Spinomarginlfus)混合在一起。 。和Leptodus nobilis)。从总体上看,武昌动物区系在指标元素和北缘方面与中国北方的内蒙古,东北的吉林省,俄罗斯的东部滨海边疆区和日本的飞ida外苑地带描述的几种同期动物区系相当。 -古赤道混合物。在中二叠纪期间,这些地区(或街区)被称为内蒙古-日本过渡带或古赤道和北方领土之间的北部过渡带。绝大多数的北方元素表明,武昌地区可能位于该过渡带的北部子区域,该区域属于布雷亚地块的南部边缘。这些东亚和东北亚块体是过渡的垫脚石,架起了中二叠纪期间古赤道和北方地区之间动物迁徙的桥梁。

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