塔里木盆地西北缘志留系兰多维列统塔塔埃尔塔格组的遗迹化石TRACE FOSSILS FROM THE LLANDOVERY(SILURIAN)TATAAIERTAGE FORMATION IN NORTHWESTERN TARIM BASIN, XINJIANG
张小乐,季兴开,唐鹏,王怿
摘要(Abstract):
遗迹化石在古代三角洲沉积环境判定及三角洲类型区分中应用广泛。本文对塔里木盆地西北缘志留系兰多维列统塔塔埃尔塔格组进行系统的沉积学和遗迹学研究,探讨不同沉积相带的遗迹化石构成与分布特征。研究结果表明,塔塔埃尔塔格组沉积于受河流影响的浪控三角洲体系中。在不同沉积相带,影响底栖生物分布的关键环境因素不同,因而遗迹化石构成与分布也表现出规律性变化。在前三角洲沉积中,遗迹化石以贫乏的Cruziana遗迹相分子(如Cruziana isp.、Gyrolithes isp.、Lockeia siliquaria和Neoeione isp.)为特征。在三角洲前缘远端沉积中,遗迹化石丰度和分异度均较高,包括Arenicolites isp.、Cochlichnus anguineus、Diplichnites isp.、Diplocraterionparallelum、Gyrochorte comosa、Lockeia siliquaria、Neoeione isp.、Planolites montanus、Rhizocorallium commune、Skolithos linearis、Teichichnus rectus和Treptichnus pedum,指示较为典型的Cruziana遗迹相。三角洲前缘近端沉积发育少量的A renicolites curvatus、Arenicolites isp.和Skolithos linearis,以及指示机会性繁殖的Monocraterion isp.和Polykladichus irregularis,代表相对贫乏的Skolithos遗迹相。本文研究表明,相分析结合遗迹化石构成和分布研究可为古代三角洲沉积环境的划分与识别提供可靠证据。
关键词(KeyWords): 相分析;三角洲沉积;遗迹化石;兰多维列统(志留系);遗迹相
基金项目(Foundation): 中国科学院南京地质古生物研究所古生物学和地层学国家重点实验室(20192112);; 中国地质大学(武汉)生物地质与环境地质国家重点实验室(GBL22002);; 中国科学院战略性先导科技专项B类(XDB26000000);; 国家自然科学基金(42172003)共同资助
作者(Author): 张小乐,季兴开,唐鹏,王怿
DOI: 10.19839/j.cnki.dcxzz.2023.0027
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