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钙质碳酸盐的微生物沉淀作用从太古代开始一直在碳酸盐台地的发育中起到了至关重要的作用.微生物碳酸盐在重大的环境变化中(包括台地环境的海侵事件和生物绝灭后的复苏阶段)是碳酸盐沉积体的重要贡献者;在层序地层不同体系域中有不同的微生物形成的碳酸盐沉积.桂林晚泥盆世法门期碳酸盐台地中的生物礁和丘完全由微生物和胶结物形成,代表了弗拉-法门期生物事件后骨骼后生生物完全缺失的礁生态系中微生物为主的、独特的生物礁类型;它们与特定的古环境和古气候有关,可以用作研究环境变化和生物事件的指标.
Microbial sedimentation of calcareous carbonate has played a crucial role in the development of the carbonate platform since the beginning of the Arctic. Microbial carbonates have been widely used in major environmental changes (including transboundary events and organisms in the platform environment) The recovery phase after extinction) is an important contributor to carbonate sediments; there are different microbial depositions in different system sequences in the sequence stratigraphy. In the late Devonian carbonate platform of Guilin Reefs and mounds, formed entirely of microorganisms and cements, represent a unique reef-type of microorganisms in the reef ecosystem in which there is a complete absence of metazoan metazoans following the phlebophane event and their association with specific paleoenvironmental and Paleoclimate can be used as an indicator of environmental change and biological events.