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重庆秀山下志留统龙马溪组的双菌迹及其地质意义
引用本文:黄再琴,王约.重庆秀山下志留统龙马溪组的双菌迹及其地质意义[J].贵州大学学报(自然科学版),2011,28(4):22-24.
作者姓名:黄再琴  王约
作者单位:贵州大学资源与环境工程学院,贵州贵阳,550003
基金项目:贵州省科学技术基金(J-2010-2030)
摘    要:重庆秀山地区下志留统龙马溪组上部的灰色页岩中产出有肉红色粉砂岩填充的U形浅潜穴双菌迹(Bifungites),其丰度较高,但属种十分单调,淡化潮坪相的沉积表明秀山地区早志留世龙马溪期晚期为淡化潮坪相的沉积.

关 键 词:双菌迹(Bifungites)  沉积环境  龙马溪组  志留纪  重庆秀山

Trace fossil Bifungites from the Lower Silurian Longmaxi Formation at Xiushan,Chongqing,and its Geologic Significances
HUANG Zai-qin,WANG Yue.Trace fossil Bifungites from the Lower Silurian Longmaxi Formation at Xiushan,Chongqing,and its Geologic Significances[J].Journal of Guizhou University(Natural Science),2011,28(4):22-24.
Authors:HUANG Zai-qin  WANG Yue
Institution:HUANG Zai-qin,WANG Yue (School of Resources and Environment,Guizhou University,Guiyang,550003)
Abstract:Most of trace fossils buried in suit could interpret the sedimentary environments and use in the paleogeography.A shallow U-shaped burrow filled with red siltston,Bifungites,was discovered in the gray shales of the Lower Silurian Longmaxi Formation at Xiushan,Chongqing.Abundant and monotonous Bifungites indicate that it was a desalted tidal-flat environment during the later Longmaxi period of the early Silurian in Xiushan area,Chongqing.
Keywords:trace fossil Bifungites  sedimentary environment  Longmaxi formation  Silurian  Xiushan  Chongqing  
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