Frasnian-Famennian Event and its response to the sedimentation in Quanzhou of Guangxi Province
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摘要:
晚泥盆世弗拉期-法门期之交，地球环境急剧变化。广西作为中国南方泥盆纪沉积最为发育的地区，对该事件具有良好的记录。从广西全州地区东山剖面发育的一套海相碳酸盐岩为主夹细颗粒陆源碎屑岩序列的岩相、沉积微相及生物化石入手，厘定研究区内弗拉阶-法门阶界线，揭示研究区内与弗拉期-法门期事件相关的沉积记录，进而探讨当时的海平面变化情况。综合剖面重点层位的化石类型及岩石沉积微相特征，将研究区内弗拉阶-法门阶界线限定在剖面第49~50层界线处，并认为研究区在晚泥盆世弗拉期-法门期之交发生了2次紧邻的阶跃型海平面上升和阶跃型海平面下降过程，与全球多区域海平面变化趋势一致。
Abstract:At the turn of Frasnian-Famennian(F-F)in Late Devonian, the environment of earth changed rapidly. As the most developed Devonian sedimentary area in South China, Guangxi has a good record of this event. Based on the study of lithic facies, sedimentary microfacies, and fossils from a series of marine carbonate rocks, siltstone and argillaceous rocks in the Dongshan section, the boundary of F-F was confirmed, and sedimentary records related to the F-F events in this area were revealed to discuss the sea level changes at the turn of F-F. It is suggest that the boundary of F-F can be restricted to the boundary between the 49 layer and 50 layer of the section. It is assumed that two adjacent stepped sea-level rise and fall occurred at the turn of F-F, which is similar to other areas in the world.
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Key words:
- F-F event /
- lithic facies /
- sedimentary microfacies /
- fossils /
- stepped sea-level change
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图 3 广西全州东山剖面F-F界线野外露头(A)及牙形石Palmatolepis triangularis(B) 和Palmatolepis gigas(C)典型照片(据参考文献[12])
Figure 3.
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