四川盆地中二叠世栖霞期微生物丘及其对沉积环境的启示
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摘要
在四川盆地华蓥溪口地区首次发现了发育在二叠纪栖霞期的微生物灰泥丘,该灰泥丘以灰泥作为支撑结构;参与建筑的生物主要是菌类微生物,其次为多门类无脊椎动物,如有孔虫、腕足等,但生物物种分异度较低,丰度较高;岩石类型主要为生屑泥晶灰岩以及凝块石等;灰泥丘可划分为丘基、丘核及丘翼。根据地化分析,华蓥溪口栖霞组剖面野外样品古盐度Z值均>122,且δ~(13)C>0;δ~(18)O变化在-6.33‰~-4.22‰,向上δ~(18)O总体为正偏移,表明海平面逐渐下降。恢复的古水温在33.60~24.26℃。V/(V+Ni)比值为0.51228,U/Th比值为8.28205;指出华蓥溪口地区处于水体较深,水动力较弱,温度较高的超咸缺氧环境。这种环境有利于微生物丘的发育,并影响了造礁生物的发育和生长,是导致栖霞期没有发育骨架礁的原因之一。
A microbial mud mound was found for the first time in the Middle Permian Qixia Formation of Huayin Xikou area.This mud mound is supported by mud,the primary builder is fungi,followed by invertebrates.The species diversity is low,with high species richness.The main lithology includes bioclastic micritic limestone and thrombolite.The mud mound can be divided into mound-core,mound-flank,and mound-base.According to the results of sample analysis of the Qixia Formation,all of the paleosalinity 2 values >122,δ~(13)C > 0;δ~(18)O values are between-6.33‰ and-4.42‰,the ancient water temperature values are between 33.60℃ and 24.26℃,V/(V+Ni) ratio is 0.51228,and U/Th ratio is 8.28205,suggesting that the environment of Qixia period was characterized by relatively deep water,relatively weak hydrodynamics,higher temperature,high salinity and anoxic nature.Such an environment was conducive to the development of microbial mud mound,and affected the development and growth of reef-building organisms.This was one of the reasons leading to the lack of skeleton of the reef in Qixia Formation.
A microbial mud mound was found for the first time in the Middle Permian Qixia Formation of Huayin Xikou area.This mud mound is supported by mud,the primary builder is fungi,followed by invertebrates.The species diversity is low,with high species richness.The main lithology includes bioclastic micritic limestone and thrombolite.The mud mound can be divided into mound-core,mound-flank,and mound-base.According to the results of sample analysis of the Qixia Formation,all of the paleosalinity 2 values >122,δ~(13)C > 0;δ~(18)O values are between-6.33‰ and-4.42‰,the ancient water temperature values are between 33.60℃ and 24.26℃,V/(V+Ni) ratio is 0.51228,and U/Th ratio is 8.28205,suggesting that the environment of Qixia period was characterized by relatively deep water,relatively weak hydrodynamics,higher temperature,high salinity and anoxic nature.Such an environment was conducive to the development of microbial mud mound,and affected the development and growth of reef-building organisms.This was one of the reasons leading to the lack of skeleton of the reef in Qixia Formation.
引文
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