Abstract
The many Early Ordovician crinoid discoveries over the past 30 years signal a largely undocumented crinoid radiation. The new crinoid diversity totals more than five times the previous known Early Ordovician list as of the year 2000. Camerate, cladid, and disparid clades had emerged by the second half of the Tremadocian Series, early during this time. Many key crinoid features such as their distinctive arms and standard cup plating originated by the end of the Early Ordovician, the Floian Stage. These new finds will provide data for character analysis in phylogenetic reconstructions, particularly those aimed at identifying early branching within the crinoid tree. Early Ordovician crinoids were among the earliest-known benthic invertebrates to exploit food resources high above the substrate. Significantly, they were also among the largest known faunal elements during this time. A tentative listing of Early Ordovician crinoids and their distributions is provided; this compendium is subdivided into time slices with Laurentian and global stratigraphic units.
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REFERENCES
Ausich, W.I., Crinoids of the Al Rose Formation (Early Ordovician, Inyo County, California, U.S.A), Alcheringa, 1986, vol. 10, pp. 217–224.
Adrain, J.M., McAdams, N.E.B., and Westrop, S.R., Trilobite stratigraphy and revised bases of the Tulena and Blackhillsian Stages of the Ibexians Series, Lower Ordovician, Western United States, Memoirs of the Association of Australasian Palaeontologists, 2009, vol. 37, pp. 541–610.
Adrain, J.M., Westrop, S.R., Karim, T.S., and Landing, E., Trilobite stratigraphy of the Stairsian Stage (upper Tremadocian ) of the Ibexian Series, Lower Ordovician, Western United States, Memoirs of the Association of Australasian Palaeontologists, 2014, vol. 45, pp. 167–214.
Blakey, D., Deep Time Maps–maps of ancient Earth. https://deeptimemaps.com/. Accessed February 3, 2020.
Carpenter, P.H., Oral and apical systems of crinoids, Q. J. Microsc. Sci., 1879, vol. 8, pp. 351–383.
Church, S.B., Lower Ordovician patch reefs in Western Utah, Brigham Young Univ. Geol. Stud., 1974, vol. 21, pp. 41–62.
Dattilo, B.F., The Lower Ordovician Fillmore Formation of Western Utah; storm-dominated sedimentation on a passive margin, Brigham Young Univ. Geol. Stud., 1993, vol. 39, pp. 71–100.
David, B. and Mooi, R., Comprendre les échinodermes: la contribution du modèle extraxial-axial, Bull. Soc. Géol. Fr., 1999, vol. 170, pp. 91–101.
Donovan, S.K. and Cope, C.W., A new camerate crinoid from the Arenig of south Wales, Palaeontology, 1989, vol. 32, pp. 101–107.
Durham, J.W., Camptostroma, and Early Cambrian supposed scyphozoan referable to Echinodermata, J. Paleontol., 1966, vol. 40, pp. 1216–1220.
Edwards, C.T., Links between early Paleozoic oxygenation and the Great Ordovician Biodiversification Event (GOBE): A review, Paleoworld, 2019, vol. 28, pp. 37–50.
Gahn, F., Homological and phylogenetic implications of a disparid-like posterior interray among lower Ordovician camerate crinoids, in Progress in Echinoderm Paleobiology, Zamora, S. and Rabano, I., Eds., Instituto Geologico y Minero de Espana, Cuadermos del Museo Geominero, 2015, vol. 19, pp. 59–65.
Guensburg, T.E., Alphacrinus new genus and the origin of the disparid clade, J. Paleontol., 2010, vol. 84, pp. 1209–1216.
Guensburg, T.E., Phylogenetic implications of the oldest crinoids, J. Paleontol., 2012, vol. 86, pp. 455–461.
Guensburg, T.E. and Sprinkle, J., Rise of echinoderms in the Paleozoic Evolutionary Fauna, Geology, 1992, vol. 20, pp. 407–410.
Guensburg, T.E. and Sprinkle, J., The oldest known crinoids and a new crinoid plate homology system, Bull. Am. Paleontol., 2003, vol. 364, pp. 1–43.
Guensburg, T.E. and Sprinkle, J., Solving the mystery of crinoid ancestry: New fossil evidence of arm origin and development, J. Paleontol., 2009, vol. 83, pp. 350–364.
Guensburg, T.E. and Waisfeld, B., South America’s earliest (Ordovician, Floian) crinoids, J. Paleontol., 2015, vol. 89, pp. 622–630.
Guensburg, T.E., Sprinkle, J., Mooi, R., Lefebvre, B., David, B., Roux, M., and Derstler, K., Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution, J. Paleontol., 2019. online version: https://doi.org/10.1017/jpa.2019.87
Hicks, H.L., On the Tremadoc rocks in the neighborhood of St. David’s, south Wales, and their fossil contents, Q. J. Geol. Soc. London, 1873, vol. 29, pp. 39–52.
Jobson, L. and Paul, C.R.C., Compagicrinus fenestratus, a new Lower Ordovician inadunate crinoid from North Greenland, Rapport Geologiske Undersøgelse, 1979, vol. 91, pp. 71–81.
Kelly, S.M. and Ausich, W.I., A new Lower Ordovician (Middle Canadian) disparid crinoid from Utah, J. Paleontol., 1978, vol. 52, pp. 916–920.
Kelly, S.M. and Ausich, W.I., A new name for the Lower Ordovician crinoid Pogocrinus Kelly and Ausich, J. Paleontol., 1979, vol. 53, p. 1433.
Lefebvre, B. and Fatka, O., Palaeogeographical and palaeoecological aspects of the Cambro-Ordovician radiation of echinoderms in Gondwanan Africa and peri-Gondwanan Europe, Palaeogeogr., Palaeoclimatol., Palaeoecol., 2003, vol. 195, pp. 73–97.
Lefebvre, B., Sumrall, C.D., Shroat-Lewis, R.A., Reich, M., Webster, G.D., Hunter, A.W., Nardin, E., Rozhnov, S.V., Guensburg, T.E., Touzeau, A., Noailles, F., and Sprinkle, J., Palaeobiogeography of Ordovician echinoderms, in Early Palaeozoic Biogeography and Palaeogeography, Harper, D.A.T. and Servais, T., Eds., London, Memoirs: Geological Society, 2013, vol. 38, pp. 173–198.
Sprinkle, J. and Colins, D., Revision of Echmatocrinus from the Middle Cambrian Burgess Shale of British Columbia, Lethaia, 2011, vol. 31, pp. 261–282.
Sprinkle, J. and Guensburg, T.E., Origin of echinoderms in the Paleozoic evolutionary fauna; the role of substrates, Palaios, 1995, vol. 10, pp. 437–453.
Sprinkle, J. and Wahlman, G.P., New echinoderms from the Early Ordovician of west Texas, J. Paleontol., 1994, vol. 68, pp. 324–338.
Servais, T. and Harper, D.A.T., The Great Ordovician Biodiversification Event, Lethaia, 2018, vol. 51, pp. 151–164.
Stigall, A.I., Cole, C.T., Freeman, R.L., and Rassmussen, C.M.O., Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks, Palaeogeogr., Palaeoclimatol., Palaeoecol., 2019, vol. 530, pp. 249–270.
Strimple, H.L. and McGinnis, M., A new camerate crinoid from the Al Rose Formation, Lower Ordovician of California, J. Paleontol., 1972, vol. 46, pp. 72–74.
Ubaghs, G., Aethocrinus moorei Ubaghs, n. gen., n. sp., le plus ancien crinoïde dicyclic connu, Univ. Kans. Paleontol. Contrib., Pap., 1969, vol. 38, pp. 1–25.
Ubaghs, G., Echinodermata, Notes sur les échinodermes de l’Ordovicien inférieur de la Montagne Noire (France), in Calymenina, Echinodermata et Hyolitha de l’Ordovicien inférieur de la Montagne Noire (France méridionale), Courtessole, R., Marek, L., Pillet, J., Ubaghs, G., and Vizcaïno, D., Eds., Mémoire de la Société d‘Etudes Scientifiques de l’Aude, 33–56.
Walker, J.D., Geissman, J.W., Bowring, S.A., and Babcock, L.E., compilers, Geological Time Scale, v. 5.0: Geol. Soc. America, 2018. Accessed on February 20, 2020.https://doi.org/10.1130/2018
Wilson, M.A., Palmer, T.J., Guensburg, T.E., Finton, C.D., and Kaufman, L.E., The development of an Early Ordovician hardground community in response to rapid sea-floor calcite precipitation, Lethaia, 1992, vol. 25, pp. 19–34.
ACKNOWLEDGMENTS
We thank Sergey Rozhnov and colleagues at the Paleontological Institute, Russian Academy of Sciences, for hosting the 10th European Echinoderm Conference, and for encouraging work on this paper. We also thank Sergey Rozhnov and Ron Parsely for constructive reviews.
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Guensburg, T.E., Sprinkle, J., Mooi, R. et al. Sea Lilies in Spring: Crinoid Diversification during the Early Ordovician. Paleontol. J. 55, 985–992 (2021). https://doi.org/10.1134/S0031030121090045
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DOI: https://doi.org/10.1134/S0031030121090045