Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China

	Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China
	Ehiro, Masayuki 1; Shen, Shuzhong (沈树忠)2
	2008-09-01
发表期刊	PALEONTOLOGICAL RESEARCH
ISSN	1342-8144
卷号	12 期号:3 页码:255-259
摘要	Two Permian ammonoid specimens belonging to the genus Kufengoceras are described from the topmost bed of the Laibin Limestone, Guangxi, South China. The ammonoid horizon is just above the Global Stratotype Section and Point for the Guadalupian/Lopingian Boundary. Kufengoceras is a typical Middle Permian ammonoid, and its occurrence above the GSSP supports the previous opinion that the ammonoid faunal changeover took place slightly after the beginning of the Lopingian.
关键词	Permian Ammonoid Kufengoceras Guadalupian/lopingian Boundary Faunal Changeover South China
语种	英语
WOS研究方向	Paleontology
WOS类目	Paleontology
WOS记录号	WOS:000259982700004
出版者	PALAEONTOLOGICAL SOC JAPAN
文献类型	期刊论文
条目标识符	http://ir.nigpas.ac.cn/handle/332004/181
专题	中国科学院南京地质古生物研究所其他
通讯作者	Ehiro, Masayuki
作者单位	1.Tohoku Univ Museum, Sendai, Miyagi 9808578, Japan 2.Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
推荐引用方式 GB/T 7714	Ehiro, Masayuki,Shen, Shuzhong . Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China[J]. PALEONTOLOGICAL RESEARCH,2008,12(3):255-259.
APA	Ehiro, Masayuki,&Shen, Shuzhong .(2008).Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China.PALEONTOLOGICAL RESEARCH,12(3),255-259.
MLA	Ehiro, Masayuki,et al."Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China".PALEONTOLOGICAL RESEARCH 12.3(2008):255-259.