The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage (Guadalupian, Middle Permian)

doi:10.18814/epiiugs/2022/022004

	The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage (Guadalupian, Middle Permian)
	Shen, Shu-zhong 11,12; Yuan, Dong-xun 10; Henderson, Charles M.9; Lambert, Lance L.8; Zhang, Yi-chun 6,7; Erwin, Douglas H.5; Ramezani, Jahandar 4; Wang, Xiang-dong 11,12; Zhang, Hua 6,7; Wu, Qiong 11,12
刊名	EPISODES
	2022-09-01
卷号	45 期号:3 页码:309-331
ISSN号	0705-3797
DOI	10.18814/epiiugs/2022/022004
通讯作者	Shen, Shu-zhong(szshen@nju.edu.cn)
英文摘要	The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage was proposed in 1999 and defined by the first appearance datum (FAD) of the conodont Jinogondolella postserrata within the lineage J. aserrata -> J. postserrata -> J. shannoni at Nipple Hill in West Texas, USA. Despite its widespread recognition for more than two decades, the official GSSP paper was not published, nor have its index conodont fossils been properly documented. At Nipple Hill, only the uppermost 0.5 m of the Pinery Member belongs to the Capitanian Stage. J. postserrata first appears at 19.8 m above the base of the auxiliary Frijole section. Based on U-Pb CA-ID-TIMS geochronology of ash beds from the GSSP area, the base of the Capitanian Stage has been constrained at 264.28 +/- 0.16 Ma. Magnetostratigraphy suggests that the Illawarra Reversal is located slightly below the base of the Capitanian Stage. Strontium isotope chemostratigraphy generally shows a continuous decline in the Sr-87/Sr-86 ratio throughout the Capitanian in the GSSP area, but all ratios are higher than the Capitanian minimum of similar to 0.7068. delta(13)C(carb)profile shows no distinct excursion around the Wordian/Capitanian boundary interval. Detailed correlation suggests that the middle-upper part of the fusuline-based Midian Stage correlates with the Capitanian Stage.
资助项目	international collaborative project of NSFC[41420104003] ; Strategic Priority Research Programs of the Chinese Academy of Sciences[XDB26000000] ; NSERC Discovery Grant
WOS关键词	SOUTHEASTERN NEW-MEXICO ; WEST TEXAS ; MASS EXTINCTION ; FAR-EAST ; LOPINGIAN BOUNDARY ; SR-87/SR-86 RATIO ; SOUTH PRIMORYE ; SW CHINA ; END ; MOUNTAINS
WOS研究方向	Geology
语种	英语
出版者	GEOLOGICAL SOC KOREA
WOS记录号	WOS:000859477100001
资助机构	international collaborative project of NSFC ; Strategic Priority Research Programs of the Chinese Academy of Sciences ; NSERC Discovery Grant
内容类型	期刊论文
源URL	[http://ir.nigpas.ac.cn/handle/332004/41270]
专题	中国科学院南京地质古生物研究所
通讯作者	Shen, Shu-zhong
作者单位	1.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 3.Guadalupe Mt Natl Pk, Salt Flat, TX 79847 USA 4.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA 5.Natl Museum Nat Hist, Dept Paleobiol, MRC 121, Washington, DC 20013 USA 6.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 2100, Peoples R China 7.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 2100, Peoples R China 8.Univ Texas San Antonio, Dept Earth & Planetary Sci, One UTSA Circle, San Antonio, TX 78249 USA 9.Univ Calgary, Dept Geosci, Calgary, AB T2N 1N4, Canada 10.China Univ Min & Technol, Sch Resources & Geosci, Xuzhou 221116, Jiangsu, Peoples R China
推荐引用方式 GB/T 7714	Shen, Shu-zhong,Yuan, Dong-xun,Henderson, Charles M.,et al. The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage (Guadalupian, Middle Permian)[J]. EPISODES,2022,45(3):309-331.
APA	Shen, Shu-zhong.,Yuan, Dong-xun.,Henderson, Charles M..,Lambert, Lance L..,Zhang, Yi-chun.,...&Wardlaw, Bruce R..(2022).The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage (Guadalupian, Middle Permian).EPISODES,45(3),309-331.
MLA	Shen, Shu-zhong,et al."The Global Stratotype Section and Point (GSSP) for the base of the Capitanian Stage (Guadalupian, Middle Permian)".EPISODES 45.3(2022):309-331.