广西中—晚泥盆世拉利和四红山剖面的碳酸盐岩微相和牙形石生物地层格架THE MIDDLE–LATE DEVONIAN SEDIMENTARY MICROFACIES AND CONODONT BIOSTRATIGRAPHY IN THE SIHONGSHAN AND LALI SECTIONS, GUANGXI
安晏庆,张欣松,杜伟东
摘要(Abstract):
华南中—上泥盆统碳酸盐岩高度发育,但却缺乏系统碳酸盐岩微相研究。广西都安四红山剖面和宜州拉利剖面的中—上泥盆统连续发育,是华南泥盆系重要的参考剖面。中—晚泥盆世,四红山剖面为斜坡—盆地相,而拉利剖面为台地—盆地相。本文重建了这两条剖面中—上泥盆统牙形石生物地层,在此基础上结合碳酸盐岩微相沉积学研究,恢复了它们同时期沉积环境演变过程,为不同地层单元的区域对比提供了可靠依据。在吉维特期和弗拉期FZ1~FZ4期,四红山剖面主要为分水岭组硅质灰岩及“榴江组”钙质泥岩,拉利剖面主要为老爷坟组礁灰岩。而在弗拉期牙形石带FZ5~FZ8期间,两条剖面均因海侵事件造成台地淹没形成五指山组,主要特征为大化石稀少的微晶/瘤状/泥质条带灰岩,本次海侵可以与全球Middlesex事件相对应。此外中—晚泥盆世一系列生物环境事件,如F-F事件可通过牙形类的种群更替得以识别。
关键词(KeyWords): 吉维特阶;弗拉阶;广西;泥盆纪;沉积微相;牙形类
基金项目(Foundation): 国家自然科学基金(42002017)资助
作者(Author): 安晏庆,张欣松,杜伟东
DOI: 10.19839/j.cnki.dcxzz.2024.0011
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