DOI: 10.1016/j.palaeo.2014.04.013
论文题名: The late early Cambrian microbial reefs immediately after the demise of archaeocyathan reefs, Hunan Province, South China
作者: Adachi N. ; Ezaki Y. ; Liu J.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2014
卷: 407 起始页码: 45
结束页码: 55
语种: 英语
英文关键词: Archaeocyaths
; Extinction
; Late early Cambrian
; Microbial reefs
英文摘要: The archaeocyath-bearing reefs that first appeared in South China in the Atdabanian were last seen in the lower Toyonian (e.g., in the Tianheban and Jindingshan formations). The upper Toyonian-lower Amgan Qingxudong Formation of Hunan Province examined in this study includes large-sized reefs formed solely by calcimicrobes of Epiphyton, Kordephyton, Girvanella, Hedstroemia, and Renalcis. During the middle and upper Cambrian, small-scale stromatolite reefs were formed. The Qingxudong reefs are therefore interpreted to be the most well-developed microbial reefs of the post archaeocyath-bearing reefs in the late early Cambrian. The transition from archaeocyath-bearing to purely microbial reefs was caused by a decline in the diversity of metazoans, and was accompanied by a reduction in the abundance of reefs, possibly related in part to late early Cambrian regression. The late early Cambrian reefs of South China contain a well-preserved record of reef succession, and provide important insights into the factors that led to the demise of archaeocyath-bearing reefs and the subsequent long-lasting hindrances to the development of skeletal-dominated reefs during the middle and late Cambrian. © 2014 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69310
Appears in Collections: 过去全球变化的重建
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作者单位: Department of Geosciences, Naruto University of Education, Naruto, Tokushima 772-8502, Japan; Department of Geosciences, Osaka City University, Sugimoto, Sumiyoshi-ku, Osaka 558-8585, Japan; School of Earth and Space Sciences, Peking University, Haidian, Beijing 100871, China
Recommended Citation:
Adachi N.,Ezaki Y.,Liu J.. The late early Cambrian microbial reefs immediately after the demise of archaeocyathan reefs, Hunan Province, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2014-01-01,407