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浙江煤山钻孔二叠-三叠系界线剖面遗迹化石的两幕式变化

, PP. 1241-1249

Keywords: 遗迹化石,扰动指数,扰动深度,二叠-三叠系界线,两幕式演化,煤山钻孔

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Abstract:

?通过对浙江长兴煤山二叠-三叠系界线全球层型剖面附近钻孔岩芯的研究,识别出遗迹化石Chondrites,Palaeophycus,Planolites,Rhizocorallium,Skolithos,Thalassinoides共6属,遗迹化石的丰度、扰动指数及扰动深度等遗迹学指标在二叠-三叠系界线上下呈现两幕式剧烈变化:第一幕发生在25~27b,在此区间,生态习性相对复杂的Chondrites,Skolithos,Rhizocorallium和Thalassinoides遗迹化石从此逐步消失,扰动指数从1~5级降低至1~3级,扰动深度从5~66cm降低至2~5cm;第二幕发生在32层与33层之间,Palaeophycus和Planolites遗迹消失,33层至41层下部未见任何遗迹和扰动现象,41层中上部遗迹再次出现,但仅见简单细小的Planolites,扰动指数再未超过3级,扰动深度小于4mm.第一幕变化较为剧烈,对应于二叠纪末生物灭绝主幕;第二幕相对较弱,对应于造迹生物在早三叠世初的灭绝尾幕;随后出现的遗迹以生态习性和结构简单的表生潜穴占绝对优势,这表明经历了二叠纪末大灭绝沉重打击后,早三叠世初残存期的底栖生态系由表生固着向表生游移转折.也就是说,二叠-三叠纪之交遗迹化石的演变与实体化石的演变有着相似的幕式变化过程与趋势.另外,二叠-三叠纪之交遗迹组构的变化与碳同位素负偏、蓝细菌泛滥之间也存在良好的对应关系.作为物理过程与生物过程相互作用的产物,遗迹化石在研究二叠-三叠纪之交的生物和环境事件及其耦合关系和演变规律方面,提供了独特的材料,具有重要的启示意义.

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