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Journal of Paleontology 91(4):672–684
Chains, Zamora (2010); the rhombiferan Vizcainoia Zamora and Smith, 2012 from the Coulouma Formation [global Cambrian Series 3, lower Drumian], Montagne Noire [France], Zamora and Smith (2012)). The Jbel Warwmast Formation, the Murero Formation, and the Coulouma Formation consist of upper offshore fine siliciclastic sediments (siltstone to clay- stone) deposited under low or moderately low energy conditions in a temperate mixed platform (Liñan and Mergl, 2001; Landing et al., 2006; Álvaro et al., 2008). The closely related and con- temporaneous lepidocystoids occur in obrution deposits in the Impure Carbonate Facies in the Emigsville Member of the Kinzers Formation (global Cambrian Series 2, Stage 4) in the Conestoga Valley (southern Pennsylvania), interpreted as an offshore environment with active bottom currents in a mixed platform (Skinner, 2005). An undetermined lepidocystoid was mentioned in the transgressive claystone-dominated Issafen Formation [global Cambrian Series 2, Stage 4] in the Central Anti-Atlas (Morocco) (Smith et al., 2013). The (par)auto- chthonous occurrences of the felbabkacystids and lepidocystoids in the deeper facies in the Paradoxides (P.) paradoxissimus gracilis Zone [global Cambrian Series 3, mid-Drumian] suggest that the morphological innovation of the overgrown vaulted oral area might have occurred in an offshore and quiet environment. All occurrences of lepidocystoids, felbabkacystids, and Medi- terranean eocrinids-lichenoids are related to relatively deep (up to mid offshore) lithofacies in transgressive and/or drowning plat- form contexts (Skinner, 2005; Landing et al., 2006; Fatka and Szabad, 2014). The echinoderm plasticity and geographic dis- tribution, even at low taxonomic levels, might be controlled by environmental changes such as the water energy, the water depth, and the substrate consistency (Guensburg and Sprinkle, 1992; Sprinkle and Guensburg, 1995; Álvaro et al., 2013; Smith et al., 2013). The morphological innovation and the high diversity in offshore environments during the early mid-Cambrian times seem to dispute the onshore-offshore pattern for the early echinoderm diversification (Jablonski et al., 1983; Sepkoski, 1991; Smith et al., 2013).
Acknowledgments
All authors contributed to this study. This study was supported by MSM 0021620855 and the Czech Science Foundation through the PRVOUK P44 of the Ministry of Education, Youth and Sports of Czech Republic. It is a contribution to the group “Lithosphère-Océan-Atmosphère” of the UMR CNRS5563/ IRD234/UPS/CNES GET (EN), to the SYNTHESYS projects SE-TAF-2924 (EN) and CZ-TAF-6049 (BL), and to the UMR CNRS 5276 LGLTPE (BL). The authors are particularly grate- ful to T. E. Guensburg and R. L. Parsley for their very helpful comments, and to S. Zamora, C. D. Sumrall, and J. Sprinkle for their constructive remarks, which greatly helped to improve the manuscript.
Accessibility of supplemental data
Data available from the Dryad Digital Repository:
http://dx.doi. org/10.5061/
dryad.sg931
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