贵州台江中寒武世凯里组中分枝状宏观藻类化石
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Q914.82

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国家自然科学基金(编号40062001),贵州工业大学博士启动基金,国家攀登专项(编号95-专-01)联合资助的成果


Branching Macroalgal Fossils of the Early-Middle Cambrian Kaili Formation from Taijiang, Guizhou Province, China
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    摘要:

    本文描述了贵州中寒武世凯里组中的分枝状宏观藻类化石5属7种,即:Marpolia spissa Walcott,Marpolia aequalis Walcott,Guizhouella ramulosa Yang(gen.et sp.nov.),Doushantuophyton lineare Chen,Thamnophton formosus Yang(gen.et sp.nov.),Eoulothrix fibrillata Ding,Eoulothrix flabellophyton Yang(sp.mov.)。根据大量的藻类与凯里生物群共生特征,从藻类的生态及生物群分布受到沉积韵律控制等特征分析,认为凯里生物群生活环境的水深应该在30-60m,而埋藏和保存环境的水深是150m左右。另外,将凯里生物群中的宏观藻类化石与震旦纪陡山沱期的藻类化石进行了比较,两者在以分枝状藻类占主要组成上是相似的,从这一方面来说,晚震旦世宏观藻类与寒武纪宏观藻类没有大的演变,但寒武纪宏观藻类以出现钙质珊瑚藻类、分枝更加复杂的类型和具有锯齿状叶状体、生殖托构造的藻类为特征。

    Abstract:

    5 genera and 7 species of the branching macroalgal fossils of the Early - Middle Cambrian Kaili Formation from Taijiang County, Guizhou Province described in this paper, are Marpolia spissa Walcott, Marpolia ae-qualis Walcott, Doushantuophytan lineare Chen, Guizhouella ramulosa Yang (gen. et sp. nov. ), Thamnophton farmosus Yang (gen. et sp. nov. ), Eoulothrix fibrillata Ding, Eoulothrix flabellophyton Yang (sp. nov. ). Because abundant macroalgal fossils and abundant early metazoan always occur together in the Kaili Formation, the paleoecology and preserved environment of the Kaili fauna may be reconstructed by the macroalgal fossil assemblage. Based on the assemblage and the preservation pattern of macroalgal fossils and other fossil assem- blages, and sedimentary features in the Kaili Formation, it turns out that most fossils in the Kaili fauna were reworked, suggesting that the taphonomy of the Kaili fauna is similar to that of the Burgess Shale fauna in Canada. Moreover, a comparison between the macroalgal fossils in the Kaili fauna and the Precambrian macroalgal fossils in the Miaohe fauna and Lantian floras shows that they have some differences and similitude.The branching pattern of the Cambrian macroalgal fossils is more complex than that of the Precambian. The bifurfication is commonly 3 - 4 times in the Cambrian, or even up to 15 times, such as Guizhouella ramu-losa, Batinevia bayankolica. Moreover, a lot of these macroalgal fossils such as Thamnophyton and Marpolio., have a pattern of cluster emerge in the Cambrian.The calcareous Corallina fossil (Paraamphiroa Yang) with bif urf ication and node turn up in the Cambrian. Bigger macroalgal fossils occur in the Cambrian, such as Margaretia dorus in the Burgess fauna, up to 10 cm in length and 1. 2 cm in width.The evolutionary level of the algae in the Cambrian is higher than that of algae in the Precambrian, such as Eosargassum sawata Yang. The filament presents jagged pattern and receptacle structure.The Precambrian and Cambrian macroalgal fossils are very similar to the branching macroalgae in major compositions.

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杨瑞东 毛家仁 等.2001.贵州台江中寒武世凯里组中分枝状宏观藻类化石[J].地质学报,75(4):433-440.
YANG Ruidong, MAO Jiaren, ZHAO Yuanlong, CHEN Xiaoyuan, YANG Xinglian) Guizhou Institute of Geochemistry, Chinese Academy of Sciences, Guiyang,) Guizhou University of Technology, Guiyang,.2001. Branching Macroalgal Fossils of the Early-Middle Cambrian Kaili Formation from Taijiang, Guizhou Province, China[J]. Acta Geologica Sinica,75(4):433-440.

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  • 最后修改日期:2000-05-19
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