2016
DOI: 10.1016/j.annpal.2016.02.001
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Trilobite fauna of basal Cambrian Series 3 (Stage 5) from the Parahio Valley (Spiti), Northwest Himalaya, India and its biostratigraphic significance

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Cited by 25 publications
(13 citation statements)
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“…These two zones have been recognized in a number of sections of the Kaili Formation in eastern Guizhou, for example, the Miaobanpo (Zhao et al, 2001a(Zhao et al, , b, 2005(Zhao et al, , 2011, the Jianshan (Zhao et al, 2008), the Fujiachong (Zhao et al, 2012a), the Sanwan (Zhao et al, 2012b) and the Pingzhai (Yuan et al, 2002;Zhao et al, 2012a) sections. The level coinciding with FAD of O. indicus may correlate to the base of the Tianpeng Formation of platform facies in Mengzi County of Yunnan Province, South China (Zhao et al, 2014), the base of Amecephalus arrojosensis Zone of Emigrant Formation in Great Basin, USA, and occurs in the Parahio Formation, Spiti area, Indian Himalaya (see Singh et al, 2016;Hughes et al, 2018), and the corresponding level in northwestern Korea (Saito, 1934).…”
Section: Polymerid Trilobite Biostratigraphymentioning
confidence: 99%
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“…These two zones have been recognized in a number of sections of the Kaili Formation in eastern Guizhou, for example, the Miaobanpo (Zhao et al, 2001a(Zhao et al, , b, 2005(Zhao et al, , 2011, the Jianshan (Zhao et al, 2008), the Fujiachong (Zhao et al, 2012a), the Sanwan (Zhao et al, 2012b) and the Pingzhai (Yuan et al, 2002;Zhao et al, 2012a) sections. The level coinciding with FAD of O. indicus may correlate to the base of the Tianpeng Formation of platform facies in Mengzi County of Yunnan Province, South China (Zhao et al, 2014), the base of Amecephalus arrojosensis Zone of Emigrant Formation in Great Basin, USA, and occurs in the Parahio Formation, Spiti area, Indian Himalaya (see Singh et al, 2016;Hughes et al, 2018), and the corresponding level in northwestern Korea (Saito, 1934).…”
Section: Polymerid Trilobite Biostratigraphymentioning
confidence: 99%
“…6(a)-(d)) has an intercontinental distribution and its first appearance has been acknowledged as one of the most favorable level for the GSSP defining the base of a global stage (e.g. Jell and Hughes, 1997;Yuan et al, 1997;Hughes and Jell, 1999;Sundberg et al, 1999Sundberg et al, , 2010Sundberg et al, , 2011Sundberg et al, , 2016Geyer and Shergold, 2000;Korovnikov, 2001Korovnikov, , 2006Peng and Babcock, 2001;Shergold andGeyer, 2001, 2003;Zhao et al, 2001aZhao et al, , b, 2004Zhao et al, , 2006Zhao et al, , 2007Zhao et al, , 2012aZhao et al, , b, c, 2014Zhao et al, , 2017Yuan et al, 2002;Peng, 2003;Sundberg and McCollum, 2003;Babcock et al, 2005Babcock et al, , 2014Sundberg, 2005, 2007;Peng et al, 2006Peng et al, , 2012bGeyer and Peel, 2011;Hughes, 2016;Singh et al, 2016;Esteve et al, 2017;Zhao et al, 2017). Besides South China, the species has been identified from northern India (Indian Himalaya) (Reed, 1910;Jell and Hughes, 1997;Peng et al, 2009b;Hughes, 2016;Singh et al, 2016), western USA (Sundberg andMcCollum, 1997, 2003), North Greenland…”
Section: Motivation For Selection Of the Boundary Level And Of The Pomentioning
confidence: 99%
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“…showing that it occurs at several horizons within about 6 metres of section in both the Parahio Valley (Singh et al, 2016) The great majority of brachiopods and small shelly fossils from the section were extracted by acid digestion of carbonate. Trace fossils occur at more levels than those illustrated in Hughes et al (2013) but, because of their limited stratigraphic use, were not studied as intensely.…”
Section: Tethyan Himalayamentioning
confidence: 99%