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依据叠层石丰度(厚度)、分异度(形态类型)及其宏观形态并结合沉积学和古生物学特征,河南登封寒武系叠层石划分为寒武系第二统的小丛状叠层石组合、半球-缓波状叠层石组合,寒武系第二、第三统的微型柱状叠层石组合,寒武系第三统的半球-缓波状叠层石组合、不规则微小柱状叠层石组合、微生物岩-小柱状叠层石组合,芙蓉统的柱-细柱状叠层石组合等七个组合类型。叠层石组合的演化存在以下相关性特征:叠层石组合的分异度与其组合层的丰度呈现一定的负相关关系,叠层石的分异度与水动力变化幅度及频度存在正相关性,叠层石组合层的厚度与水动力变化幅度及频度存在负相关性。根据前寒武纪叠层石的繁盛与衰减特征结合对现代海相叠层石的生长条件分析,海平面的变化和沉积底质的分异是河南登封寒武纪叠层石分异度及其组合类型变化的重要因素,陆源物质的注入造成了叠层石的减少,后生动物的大量出现决定了叠层石的最终消亡。
According to the abundance of strata (thickness), the degree of differentiation (morphology type) and its macroscopic morphology, combined with the sedimentary and paleontological characteristics, the strata in the Cambrian strata of Dengfeng, Henan Province are divided into small clumps of the second Cambrian Layered stacks, hemispherical-slow corrugated laminated rocks, the Cambrian second and third miniature columnar monoliths, the third member of the Cambrian-slow corrugated laminated rocks, the irregular Small columnar laminated stone combination, microbial rock - small columnar laminated stone combination, Hibiscus column - thin columnar laminated stone combination of seven combinations. The evolution of the stratigraphic assemblages has the following correlations: the stratigraphic assemblages have a negative correlation with the stratigraphic assemblages, and the stratification degree and frequency of the stratigraphic rocks vary positively Correlation, the thickness of the laminated stone composite layer and hydrodynamic changes in the magnitude and frequency of negative correlation. According to the prosperous and decaying characteristics of the Precambrian stratigraphic rocks, the variation of the sea level and sediment quality in the strata of the modern marine strata are the differentiation of the strata of the Cambrian in Dengfeng, Henan And their combination of types of changes in the important factors, the introduction of terrestrial material caused by the reduction of strata, the large number of metazoan animals determines the final disappearance of strata.