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Journal of Paleontology, 91(4), 2017, p. 735–754 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2017.7


The first Ordovician cyclocystoid (Echinodermata) from Gondwana and its morphology, paleoecology, taphonomy, and paleogeography


Mike Reich,1,2,3 James Sprinkle,4 Bertrand Lefebvre,5 Gertrud E. Rössner,1,2,3 and Samuel Zamora6


1SNSB – Bavarian State Collection of Palaeontology and Geology, Richard-Wagner-Strasse 10, 80333 München, Germany ⟨m.reich@lrz.uni-muenchen.de⟩, ⟨g.roessner@lrz.uni-muenchen.de⟩ 2Department of Earth and Environmental Sciences, Division of Palaeontology and Geobiology, Ludwig-Maximilians-Universität München,


Richard-Wagner-Strasse 10, 80333 München, Germany ⟨mike.reich@lmu.de⟩ 3GeoBio-Center, Ludwig-Maximilians-Universität München, Germany 4Department of Geological Sciences, Jackson School of Geosciences, University of Texas, 1 University Station C1100, Austin, Texas


78712-0254, USA ⟨echino@jsg.utexas.edu⟩ 5UMR CNRS 5276 LGLTPE, Université Lyon 1, 2 rue Raphaël Dubois, 69622 Villeurbanne cedex, France ⟨bertrand.lefebvre@univ-lyon1.fr⟩ 6Instituto Geológico y Minero de Espana, C/Manuel Lasala 44, 9 B, 50006 Zaragoza, Spain ⟨samuel@unizar.es


Abstract.—Moroccodiscus smithi represents a new cyclocystoid genus and species based on moldic specimens from the Middle Ordovician Taddrist Formation (Darriwilian) of SE Morocco. This represents the earliest articulated mem- ber of the Cyclocystoidea and is the first complete cyclocystoid described from the Ordovician of Gondwana, as well as the first cyclocystoid ever recorded from Africa. The anatomy and morphology of this new species were studied using a combination of conventional paleontological methods and nondestructive X-ray computed tomography. Because Moroccodiscus differs from other cyclocystoids, in particular by lacking cupules attached to the marginal ossicles, it is assigned to the new family Moroccodiscidae. This new taxon illustrates the relatively poorly known early diversification of these enigmatic extinct echinoderms and sheds light on the mode of life of cyclocystoids, including injuries to plate circlets during early ontogeny and folding of these disk-like specimens at the time of death. The overall thecal shape was very similar in cyclocystoids and many domal edrioasteroids, probably because they were both sessile or attached, benthic, suspension feeders. However, many oral surface, ambulacral, and marginal ring features had become very different, indicating that these two groups had either converged because of similar life modes or were only distantly related sister groups.


Introduction


Cyclocystoids are a relatively small extinct class of circular, flattened echinoderms that have been known for more than 160 years. Twenty genera and about 40 valid species have been named (Reich and Kutscher, 2010; Sprinkle et al., 2015), from articulated and disarticulated material, ranging from the Middle Ordovician to the early Carboniferous (Heaslip, 1969; Smith and Paul, 1982; Ressmeyer and Frest, 1983; Berg-Madsen, 1987; Fluegeman and Orr, 1990; Haude and Thomas, 1994; Boczarowski, 2001; Sevastopulo, 2002). Most specimens come from Laurentia and Baltica (Lefebvre et al., 2013), but a few are known from Avalonia and Laurussia. Jell and Jell (1999) pub- lished the only report of a cyclocystoid plate from Gondwana (Upper Devonian of Australia). However, our new cyclocystoid material described here represents the second report (and first articulated Ordovician material) of this echinoderm group from Gondwana. Cyclocystoid morphology has been controversial because


well-preserved specimens that show all parts of the animal are rare (Paul, 1982), and several different interpretations of their morpho- logy and life mode have been proposed (Salter and Billings, 1858;


Foerste, 1920; Sieverts-Doreck, 1951; Kesling, 1963, 1966). In addition, despite the abundance of cyclocystoids in Ordovician strata (Table 1) in comparison to the Silurian– Carboniferous record, our understanding of their origin and phylogeny lags well behind that of many other echinoderm groups. Smith and Paul (1982) produced a comprehensive monograph of the class using a large number of well-preserved museum specimens and established six new genera. We agree with many of their conclusions involving systematics, bio- stratigraphy, morphology, diversity, phylogeny, and perhaps biogeography, but disagree with their interpretation of orienta- tion and feeding mode. The recent discovery of a new cyclocystoid (Moroccodiscus


smithi) fromthe Middle Ordovician ofMorocco shows somewhat different morphology and additional evidence about the likely living orientation of cyclocystoids. Here we describe the eight specimens of this new taxon that have been assembled by the authors, showing different morphology in comparison to all other known cyclocystoid species, genera, and families. Moroccodiscus smithi from the Middle Ordovician of Morocco represents the oldest articulated member of the Cyclocystoidea as well as the first record of this group from Africa.


735


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