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    华南二叠纪生物成礁模式探讨

    Reef-building model for the Permian organic reefs in South China

    • 摘要: 二叠纪生物礁广泛发育于我国南方碳酸盐岩地区。鉴于许多研究者从成礁的外部环境因素来探讨生物礁的发育模式,笔者从我国南方二叠纪生物礁的内部成礁因素分析,即从主要造礁生物——钙质海绵和钙质藻类等的生物学和生态学特征、埋藏和保存特点方面进行分析,继而提出了华南二叠纪海绵礁的成礁模式。此模式不同于其它地质历史时期生物礁的成礁模式。

       

      Abstract: The Permian organic reefs are widely developed in the carbonate areas of South China. Unlike the previous reef-buildng models grounded on the external reef-buildng environmental factors by many researchers,the model presented in this study is employed to study the internal reef-building factors,with the emphasis on biological and ecological characteristics, burial and preservation of the main reef-building organisms such as calcareous sponge and algae,resulting in the presentation of the reef-building model for the Permian sponge reefs in South China. This model is also distinct from the other reef-building models for the organic reefs in geologic records.

       

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