A Middle-Upper Devonian Boundary Section in the Open Platform, Platform Margin Facies of Guilin, South China

被引:4
作者
Li Hua [1 ]
Ma Xueping [1 ]
Wei Longming [2 ]
机构
[1] Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[2] Guilin Univ Technol, Dept Resource & Environm, Guangxi 541004, Peoples R China
基金
中国国家自然科学基金;
关键词
conodont; biostratigraphy; Givetian-Frasnian boundary; Devonian; Caiziyan; Guangxi; ANTI-ATLAS; PERTURBATION; MOROCCO;
D O I
10.1111/j.1755-6724.2009.00048.x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Caiziyan Middle and Upper Devonian boundary section is located approximately 30 km northeast of Guilin. It hosts relatively abundant benthic and common-rare pelagic fossils, including brachiopods, corals, tentaculites, and conodonts, which may serve as a better suitable section for pelagic and neritic stratigraphic correlation. In this section, 10 "standard" conodont zones are recognized across the Givetian-Frasnian boundary, including, in descending order, the Lower hassi Zone, punctata Zone, transitans Zone, the Upper falsiovalis Zone, the Lower falsiovalis Zone, disparilis Zone, the Upper hermanni-cristatus Zone, the Lower hermanni-cristatus Zone, the Upper varcus Zone, and the Middle varcus Zone, all of which are defined by the first occurrence of their defining conodont species. The Middle-Upper Devonian (Givetian-Frasnian) boundary is defined by the first occurrence of Ancyrodella pristina in accordance with the Global Stratotype Section and Point (GSSP), which is assigned at 6.2m above the base of bed 19 in the Caiziyan section.
引用
收藏
页码:524 / 534
页数:11
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