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New Wiwaxia material from the Tsinghsutung Formation (Cambrian Series 2) of Eastern Guizhou, China

机译:来自贵州东部青松洞组(寒武系2)的新的Wiwaxia物质

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摘要

Wiwaxia is an extinct early metazoan with uncertain affinities, which is well represented in strata of Cambrian Series 2-3 age. Well-preserved representatives of Wiwaxia are known from the Burgess Shale Biota and the Kaili Biota. Here, new material of Wiwaxia corrugata (Matthew, 1899) is reported from the upper part of the Tsinghsutung. Formation (Cambrian Series 2) near Balang Village, Guizhou Province, China. These specimens have a close evolutionary relationship to Wiwaxia taijiangensis Zhao, Qian & Lee, 1994 from the overlying Kaili Formation. New Wiwaxia material from the Tsinghsutung Formation and observations of specimens with articulated individuals from the Kaili Formation suggest that Wiwaxia taijiangensis should be a junior synonym of W. corrugata. A new study indicates that W. corrugata has a wide geographic distribution, a short geological history and evolutionary uniqueness and provides new data on taphonomy of this genus.
机译:Wiwaxia是已灭绝的早期后生动物,具有不确定的亲和力,在寒武纪2-3年龄层中可以很好地表示。柏格斯页岩生物群和凯里生物群中保存完好的Wiwaxia代表。在这里,青瓦台的上部报道了Wiwaxia corrugata的新材料(Matthew,1899年)。中国贵州省巴浪村附近的地层(寒武系2系列)。这些标本与上覆的凯里组与太湖Wiwaxia Zhao,Qian&Lee,1994有密切的演化关系。来自青松洞组的新的Wiwaxia物质以及对来自Kaili组的具关节的个体的标本的观察表明,台江Wiwaxia应该是W. corrugata的初级同义词。一项新的研究表明,W。corrugata具有广泛的地理分布,短的地质历史和进化的独特性,并提供了有关该属的分类学的新数据。

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