2021
DOI: 10.1111/let.12398
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Moulting in the Cambrian oryctocephalid trilobiteArthricocephalites xinzhaiheensisfrom Guizhou Province, South China

Abstract: It is important to understand moulting behaviours in trilobites through different growth stages. Most studies have focused on patterns of moulting in trilobites based on a few exuviae. The present study is based on 177 disarticulated specimens of Arthricocephalites xinzhaiheensis from the Balang Formation (Cambrian Series 2, Stage 4, Guizhou Province, South China). The abundance of disarticulated assemblages allows the distinction between carcasses and exuviae to be made with confidence and enables a detailed … Show more

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Cited by 6 publications
(24 citation statements)
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“…No isotopic dating is available for the Balang Formation, therefore its age is regarded as Stage 4 according to a series of trilobite-based correlations of Cambrian strata between South China and other continents (Zhou et al, 1979, 1980; Zhou and Yuan, 1980; Peng and Babcock, 2001; Yuan et al, 2001, 2006, 2011; Qin et al, 2010; Yan et al, 2014; Yuan and Ng, 2014; Shen et al, 2016; Y.F. Wang et al, 2020), corresponding to the Qiandongian early Duyunian of the Cambrian chronostratigraphic system of China in slope facies (Peng and Babcock, 2001).
Figure 1.( 1 ) Map showing the distribution of the Balang Formation (gray areas) in Guizhou Province, the location of the fossil locality (star); and ( 2 ) the lithological column of the Lazizhai section.
…”
Section: Geological Settingmentioning
confidence: 99%
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“…No isotopic dating is available for the Balang Formation, therefore its age is regarded as Stage 4 according to a series of trilobite-based correlations of Cambrian strata between South China and other continents (Zhou et al, 1979, 1980; Zhou and Yuan, 1980; Peng and Babcock, 2001; Yuan et al, 2001, 2006, 2011; Qin et al, 2010; Yan et al, 2014; Yuan and Ng, 2014; Shen et al, 2016; Y.F. Wang et al, 2020), corresponding to the Qiandongian early Duyunian of the Cambrian chronostratigraphic system of China in slope facies (Peng and Babcock, 2001).
Figure 1.( 1 ) Map showing the distribution of the Balang Formation (gray areas) in Guizhou Province, the location of the fossil locality (star); and ( 2 ) the lithological column of the Lazizhai section.
…”
Section: Geological Settingmentioning
confidence: 99%
“…Many fossil assemblages have been discovered from the middle to upper part of the Balang Formation at various localities (Peng et al, 2005, 2012a, b; Peng, 2009; Da et al, 2011; Ma et al, 2011; Liu and Lei, 2013; Zhao et al, 2015; Y.F. Wang et al, 2020), and the Balang Biota comprises at least 80 species of 63 genera (Zhao et al, 2007; Peng et al, 2010a, 2012c, 2016; Sun et al, 2015, 2017; Liu, 2018; Liu et al, 2018a; Wen, 2019; Wen et al, 2019). In Guizhou, collections were conducted mainly in three localities: Xiangshuidong Village in Songtao County; Tongren City and Jiaobang and Lazizhai villages in Jianhe County; and Kaili City.…”
Section: Geological Settingmentioning
confidence: 99%
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“…In a recent paper we studied mouting in Ar. xinzhaiheensis and found two kinds of moult configurations (Wang et al, 2020). A concentration of well-preserved disarticulated configurations of the early Cambrian oryctocephalid trilobite Ar.…”
Section: Introductionmentioning
confidence: 97%
“…A concentration of well-preserved disarticulated configurations of the early Cambrian oryctocephalid trilobite Ar. xinzhaiheensis provides an unparalleled opportunity to allow the distinction between carcasses and exuviae to be made with confidence (Wang et al, 2020), and then explore moulting behavior during development.…”
Section: Introductionmentioning
confidence: 99%