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辽东半岛震旦系甘井子组叠层石生长机制研究

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辽东半岛新元古界震旦系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.笔者等选择甘井子组地层为研究对象,根据岩性特征该组自上而下可分成3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,均为水深不断增加的结果.笔者等通过对比现代叠层石生长机制,确定甘井子组叠层石纹层的3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,揭示了甘井子组叠层石的形成机制.
Growth mechanism of stromatolites in the Ganjingzi Formation,Sinian System,in Liaodong Penisula
Objectives:The stromatolites in Ganjingzi Formation,Sinian System(Ediacaaran System),in Liaodong Penisula,are ideal object for studying the construction of Neoproterozoic microbial carbonate,which is of great significance for restoring paleoenvironment and paleoecology.Methods:Based on field investigation on the Yuanjiagou profile,Fuzhou Bay,Liaodong Penisula,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:Based on different lithology,the Ganjingzi Formation is divided into three sections from bottom to top in the Yuanjiagou profile,Fuzhou Bay,Liaodong Penisula.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.

stromatoliteSinian Systemthe Ganjingzi Formationsouthern Liaoning regionLiaodong PenisulaFormation mechanism

苑鼎成、张永利、赖冠明、巩恩普、王俊杰、李德鹏

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东北大学,沈阳,110819

叠层石 震旦系 甘井子组 辽南地区 辽东半岛 生长机制

国家自然科学基金资助项目

42272008

2024

地质论评
中国地质学会

地质论评

CSTPCD北大核心
影响因子:1.842
ISSN:0371-5736
年,卷(期):2024.70(1)
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