辽南新元古代甘井子组叠层石生长机制研究:与现代叠层石对比
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东北大学资源与土木工程学院地质系

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国家自然科学基金项目(面上项目,重点项目,重大项目)


Growth mechanism of Neoproterozoic Ganjingzi Formation stromatolites in southern Liaoning: Comparison with modern stromatolites
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1.Department of Geology, School of Resources and Civil Engineering, Northeastern University;2.Department of Geology, College of Resources and Civil Engineering, Northeastern University

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    摘要:

    辽南地区新远古界甘井子组叠层石出露完好,宏观形态完整,微观构造清晰,是研究新元古代早期微生物碳酸盐岩建造的理想对象,对恢复古环境和古生态研究具有重要意义。甘井子组地层根据岩性特征自上而下分成三段,叠层石出露于下段的底部和上段的顶部,底部叠层石为透镜状,顶部叠层石呈大规模层状。下段叠层石呈现波纹状-柱状-丘状的形态组合,上段叠层石呈现波纹状-柱状-长柱状的形态组合,均反映了叠层石柱体形态随水深增加的变化趋势。通过对比现代叠层石生长机制,确定甘井子叠层石纹层的三层构造和形成顺序,分析硬质基底对于叠层石定殖和叠层石密集生长的控制,厘定环境变化从微观到宏观对于柱体形态和叠层石规模的影响,揭示甘井子组叠层石形成机制。

    Abstract:

    Objectives:The Ganjingzi Formation stromatolites in southern Liaoning Province are an ideal object for studying the construction of early Neoproterozoic microbial carbonate, which is of great significance for restoring paleoenvironment and paleoecology. Methods:Based on field investigation, the position of the outlying stromatolites in the Ganjingzi Formation, the macroscopic morphological characteristics of stromatolites, and the morphological changes of stromatolite columns and lamellar structures are identified and recorded. Through the observation of the laminae, the different growth stages of the laminae are distinguished, and the influence of the environment on the bifurcation and morphology of the stromatolite columns are analyzed. The stromatolites building process and characteristics of Neoproterozoic the Ganjingzi Formation stromatolites are reconstructed by comparing them with modern stromatolites. After comprehensive discussion, the growth mechanism of the Ganjingzi Formation stromatolites is summarized. Results:According to different lithology, the Ganjingzi Formation is divided into three sections from bottom to top in the Yuanjiagou area, southern Liaoning Province. Stromatolites appear at the bottom of the lower member and the top of the upper member of the Ganjingzi Formation. The stromatolites at the bottom produce stromatolite mound or the large-scale stromatolite biostrome at the top. The stromatolites colonize the hard substrate and grow perpendicular to the substrate at the beginning stage. Under the influence of hydrodynamic conditions and photosynthesis, stromatolites gradually grow vertically upward. The stromatolites in the stromatolite mound present a pattern combination of corrugate-columnar-cumulus, and the stromatolites in the stromatolite biostrome present a pattern combination of corrugate-columnar-long columnar, both of which reflect the changing trend of stromatolite morphology with increasing water depth. A comprehensive comparison of modern stromatolites shows that the microstructure of the Ganjingzi Formation stromatolites is similar to that of modern stromatolites, and growth and branch have certain comparability. Conclusions:The stromatolite laminae of the Ganjingzi Formation show different sequences of formation of light laminae and dark laminae. The morphological characteristics of stromatolites show that the growth and branched of stromatolites are affected by the environment to some extent. The formation of stromatolites is subject to environmental changes. The extensive growth of stromatolites requires ample space and a suitable environment. The presence of hard substrates creates favorable conditions for the growth of stromatolites. From micro to macro, the influence of biological factors on the growth and building characteristics of microbial mats gradually increased, while the influence of environmental factors gradually decreased.

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  • 收稿日期:2023-05-29
  • 最后修改日期:2023-08-03
  • 录用日期:2023-08-06
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