Four new occurrences of Paleozoic conulariids are reported. A species of Climacoconus is reported from the Ordovician of Korea. Conularia quichua Ulrich (in Steinmann & Doderlein, 1890) is reported for the first time from Chile. It occurs in the Zorritós Formation. (Devonian). A new species of Paraconularia occurs in the Woodford Shale (Devonian) of Oklahoma. Another species of Paraconularia is reported from the Carboniferous (Pennsylvanian) of the Kansas-Oklahoma border area.No embarg

Walls, Bradley J.

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New Occurrences of Ordovician, Devonian, and Carboniferous Conulariids from North America, South America, and Asia A Thesis Presented in partial fulfillment of the requirements for the degree of Bachelor of Science in Geological Sciences by Bradley J. Walls The Ohio State University June 2007 Approved by ~fL/J Dr. Loren E. Babcock TABLE OF CONTENTS Abstract. ................................................................................................ 2 Acknowledgments .................................................................................... 3 Introduction ......................................................................................................................... 4 Systematic Paleontology ............................................................................. 6 References ............................................................................................. 22 1 ABSTRACT Four new occurrences of Paleozoic conulariids are reported. A species of Climacoconus is reported from the Ordovician of Korea. Conularia quichua Ulrich (in Steinmann & Doderlein, 1890) is reported for the first time from Chile. It occurs in the Zorrit6s Formation. (Devonian). A new species of Paraconularia occurs in the Woodford Shale (Devonian) of Oklahoma. Another species of Paraconularia is reported from the Carboniferous (Pennsylvanian) of the Kansas-Oklahoma border area. 2 ACKNOWLEDGMENTS For his tireless assistance and his patience through my learning process, I would like to thank Dr. Loren Babcock. I would also like to thank Dr. Hans Niemeyer Rubilar (Universidad Cat61ica del Norte, Antofagasta, Chile), Dr. Duck Keun Choi (Seoul National University, Seoul, Korea), Royal H. Mapes (Ohio University, Athens, Ohio) and Tom Servais, for collecting some of the specimens. Adam English provided photographic assistance. Finally I would like to thank my family for supporting me financially and otherwise through college. 3 INTRODUCTION Conulariids are a group of problematic fossils whose phylogenetic affinities have been argued about for about 200 years. They have been described as mollusks, cnidarians, worms, vertebrates, and as an independent phylum. The heart of the problem lies in the fact that their morphology does not seem to fit well into any one group. Also, problems arise from the fact that few well preserved specimens have been found with soft parts intact. Soft part morphology is one of the best tools for classifying the group of organisms. The modern consensus view is that conulariids are an extinct group of cnidarians or have close affinities with cnidarians (Van Iten, l 992a, l 992b; Babcock, 1993). Conulariids secreted an elongate, four-sided pyramidal exoskeleton having a phosphatic composition and a subtle bilateral symmetry. Bilateral symmetry is indicated by different apical angles between the major (larger) and minor (smaller) faces. It is also evident in differences in the pattern of rod articulation between the major and minor faces; commonly a species is characterized by a right-superior pattern of articulation on one type of face, and a left-superior pattern of articulation on the other type of face. The weakly rectangular (almost square) outline of its exoskeleton, as viewed from the apertural end along the long axis, has given rise to the misconception that conulariids had a radial (tetrameral) symmetry (Babcock, 1993). The exoskeleton was open at the wider end, or aperture, and closed at the narrower end, or apex. The exoskeleton, which was moderately flexible, is composed of numerous, thin phosphatic laminae. It was thickened in part by transverse thickenings that have been called rods. Although made up of numerous laminae, similar to the 4 adjacent integument, the rods seem to be sufficiently thickened so as to have a different taphonomic history from the integument. Conulariids have a known stratigraphic range of Cambrian to Triassic. Conulariids apparently have affinities with In this thesis I report four new occurrences of Paleozoic conulariids. One, Conularia quichua, is from the Devonian of Chile. Previously, the species was reported from elsewhere in South America and Africa. A species of Climacoconus is from the Ordovician of Korea. A new species of Paraconularia is from the Devonian of Oklahoma. Finally, another new species of Paraconularia is from the Carboniferous of the Kansas-Oklahoma border area. 5 SYSTEMATIC PALEONTOLOGY Genus Climacoconus Sinclair, 1940 Remarks. - Climacoconus, as described by (Sinclair, 1948), is a small, narrow, conulariid characterized by unornamented ridges. It is nearly square in cross section. The genus has distinct corner grooves and rounded, or even ridged corner angles. Carinae interval to the midline are ubiquitous in species assigned to this genus.· Climacoconus new species Figure 1 Material. - Ten specimens on nine rock slabs. Specimens, collected by Duck Keun Choi, are reposited in the paleontology collection of Seoul National University (SNU 890603, 890605, 890606, 890608, 890611, 890612, 890617, 890620, 890626). Diagnosis. - A new species of Climacoconus is defined by distinctly incised corner grooves, two rows of internal carinae, and a wider apical angle ( 17-19°), as well as a closely spaced rods, 20-32/cm. Description. - Exoskeleton up to 11 mm in length, and nearly square in cross section. Apical angle 17-19 °. Ridge articulation of circular curve style apically and gothic arch style elsewhere. Ridges usually abut at the midline, ridge angle up to 14 ° (decreasing towards apex). 20-24 ridges/cm near the aperture, increasing to 28-32/cm toward the apex; nodes and spines absent. Apical wall not observed. 6 Occurrence. - Yeongheung Formation of the Joseon Supergroup (Middle Ordovician), Yeongweol area, along Route 38, Samgeori, Korea. The Yeongheung Formation consists of two major lithologies; massive thick-bedded dolostone at its base, and bluish-gray limestone in its upper part. Lithofacies represent a supratidal to subtidal environment. The formation is poorly fossiliferous, containing relatively uncommon trilobites, brachiopods, cephalopods, conulariids, stromatoporoids, and conodonts (Choi and Chough, 2005). The illustrated specimens are black in color against a gray shale matrix, preserved from the upper part of the Yeongheung Formation. Remarks. - Climacoconus n. sp. is the first Ordovician conulariid to be identified from Korea. Specimens reported here were previously noted (Choi and Jeong 1990), but not described. Aside from this species of Climacoconus, only one other conulariid species, Paraconularia geumcheonensis, has been reported from Korea (Choi, 1988). That species is from the Geumcheon Formation (Carboniferous) of the Sangdong area, Korea. Climacoconus n. sp. is similar to C quadratus (Sinclair, 1942), which has apical angles ranging from 12° to 19°. It is also similar to C clermontanus and C mollis (Sinclair, 1948) in the number of ridges/cm (20 to 40). C n. sp. is unique within the genus Climacoconus by the combination of a wide apical angle ( 17° to 19°) and closely spaced rods, as well as distinctly incised comer grooves and two rows of internal carinae. 7 Figure 1 8 Figure 1 - Climacoconus n. sp., from the Yeongheung Formation (Ordovician), Yeongweol area, along Route 38, Samgeori area, Korea; all specimens reposited in the paleontology collections of Seoul National University (Seoul, Korea). 1, external view of specimen, SNU 890606; x 7. 2, two specimens, a) internal view of specimen, b) external view of specimen, which shows two comer grooves clearly, SNU 890620; x8. 3, internal view of face, SNU 890626; x12. 4, a close-up of figure 1.1 showing ridge articulation, SNU 890606; x20. 5, external view of a broken specimen, SNU 890605; x7. 6, a close-up of figure 1.9 showing ridge articulation, SNU 890603; x20. 7, a close-up of figure 1.10 showing carinae, SNU 890617; x20. 8, external view of two faces, showing details of the midline, SNU 890611; xl 1. 9, external view of face, SNU 890603; x9. 10, oblique view of specimen showing distinctive carinae, SNU 890617; x 10. 11, external view of large specimen, SNU 890612; x9. 12, a specimen showing external and internal sides, SNU 890608; x13. 9 Genus Conularia Miller in Sowerby, 1821 Remarks. - Conularia is characterized by generally having closely spaced ridges, relatively small apical angles, and spines and nodes on the ridges (Babcock and Feldmann, 1986a, Babcock, 1993). Conularia quichua Ulrich in Steinmann and Doderlein, 1890 Figure 2 Canu/aria quichua - Ulrich in Steinmann and Doderlein, 1890, p. 343; Babcock et al., 1987, p. 205 (see for additional synonymy). Material. - Seven samples provided by Hans Niemeyer Rubilar. Occurrence. - Quartzite beds (metamorphosed fine sandstone layers) of the Zorrit6s Formation, Devonian, Cordon de Lila and Quebrada de las Zorras, (Atacama Desert), northern Chile. Remarks. - New material from Chile is within the range of variation of Canu/aria quichua, a species that is widespread in the Devonian of South America and Africa (Babcock et al., 1987 and references therein). Canu/aria quichua is characterized by having closely spaced ridges (21 to 32/cm) that are arranged in a gothic arch pattern apically and in an angulated circular curve pattern elsewhere. The ridges are slightly undulose except in the apical region. Apical angles on the major face are in the range of 13 to 24 degrees, and those on the minor face are 11 to 23 degrees. The rods abut at the midline of each face. An apical wall has been observed in some specimens. 10 This is the first report of Conularia in Chile. These specimens of C. quichua show different rates of growth through ontogeny, a characteristic of C. quichua that has been illustrated, but not specifically described before. Slower growth rates are suggested by areas of closely spaced ridges. 11 5 6 7 Figure 2 12 Figure 2 - Conularia quichua, from the Zorrit6s Formation (Devonian), Cordon de Lila and Quebrada de las Zorras, (Atacama Desert), northern Chile. 1, external view of crushed specimen within matrix; x2. 2, external view of face; x2. 3, external view of face; x2.5. 4, enlarged view of 2.1 showing spines, and slower growth rates of the ridges; x?. 5, crushed specimen showing apertural folds; xl.5. 6; external view of face; x?. 7, external view of face; x2. 13 Genus Paraconularia Sinclair, 1940 Remarks. - The genus Paraconularia is characterized by ridges that are generally widely spaced, 4-3 5 rods/cm. More than 60% of rods alternate at the midline; fewer than 40% abut. Apical angles are small, 9-28°. Nodes, adapertural spines, and adapical spines may be present; if present, they are usually widely spaced, 2-6/mm (Babcock and Feldman, 1986b ). Paraconularia new species Figure 3 Material. - Seven specimens on five slabs collected by Royal H. Mapes. Diagnosis. - A new species of Paraconularia having a high ridge angle, 25-27°, closely spaced ridges, 24-46/cm, and closely spaced nodes, 12-14/mm. Description. - Exoskeleton up to 5.5 cm in length. Apical angle 28-30°. Ridge articulation gothic arch style in apical region giving way to inflected gothic arch style. Largest specimens have inflected circular curve ridge articulation near aperture. Ridges usually abut at midline, if they alternate, pattern is left superior. Ridge angle about 26°. Ridges number 24-26/cm near the aperture, increasing to 44-46/cm toward apex (extrapolated). 12-14 nodes/mm. Spines absent. Apical wall not observed. Occurrence. Woodford Shale (Devonian) of the Ryan Quarry, Ada, Oklahoma. The illustrated specimens are compacted in dark gray shale. 14 Remarks. - Paraconularia n. sp. is unique within the genus because of the combination of closely spaced ridges, 24-46/cm, the number of nodes, 12-14/mm, and the high apical angle, 28-30 degrees. 15 4 5 Figure 3 16 Figure 3 - Paraconularia n. sp. from the Woodford Shale (Devonian), Ryan Quarry, Ada, Oklahoma; all specimens reposited in the Orton Geological Museum of The Ohio State University. 1, compacted specimen showing closely spaced rods towards the apex; xJ. 2, cluster of three specimens; x2. 3, close-up of right-most specimen in figure 3 .2 showing closely spaced nodes; x 5. 4, external view of face; x2.5, external view of face; x2, 17 Paraconularia new species Figure 4 Material. - One specimen from the Coffeeville Shale, (Carboniferous: Pennsylvanian), Caney, Kansas, collected by Tom Servais. Six specimens from the Coffeeville Shale (Carboniferous: Pennsylvanian), Copan, Oklahoma, collected by L. E. Babcock and Tom Servais. Diagnosis. - A new species of Paraconularia having a relatively low apical angle and closely spaced ridges in the apical region. Ridges usually abut and lack nodes and spmes. Description. - Exoskeleton up to 6.5 cm in length and nearly square in cross section. Apical angle 10-1 7 °. All available specimens show inflected circular curve style ridge articulation. Ridges usually abut at midline. Ridge angle about 17°. 10-12 ridges/cm near aperture, increasing to 22-26/cm toward apex (extrapolated). Nodes and spines absent. Apical wall not observed. Occurrence. - Coffeeville Shale along Highway 75 near Caney, Kansas, and Wann Shale, east and west sides of Highway 75, north of Copan, Oklahoma. Both formations are thought to be the same formation that outcrop in different states. The illustrated specimens, preserved in three dimensions with siderite infilling, were collected loose at the surface following weathering from gray shale. Remarks. - Paraconularia n. sp. is similar to P. byblis (White, 1862). Both have ridge angles varying from 12 to 18 degrees and both have similar ranges of ridges/cm 18 (I 0 to 26). P. n. sp. is distinguished from P. byblis by lacking nodes on its ridges as well as having a smaller apical angle. The maximum measured apical on P. n. sp. is 17 degrees whereas the minimum apical angle of the major face of a P. byblis is 18 degrees. 19 3 4 2 5 6 7 8 Figure 4 20 Figure 4 - Paraconularia n. sp. from the Coffeeville Shale (Carboniferous: Pennsylvanian), Caney, Kansas, and the Wann Shale (Carboniferous: Pennsylvanian), Copan, Oklahoma; all specimens reposited in the Orton Geological Museum of The Ohio State University. 1, external view of two faces; x 1. 2, external view of specimen in figure 4.1 showing ridge articulation; x 1. 3, external view of face showing closely spaced ridges in apical region; x 1.5. 4, external view of face; x2. 5, external view of specimen showing collapsed apical region; x 1.33. 6, external view of face; x2. 7, external view of specimen showing collapsed apical region; x 1.33. 8, single fragmented face; x 1. 21 REFERENCES Babcock, L. E. 1993. Exceptionally preserved conulariids from the Conularienschichten, Fossil-Lagerstatten in the Devonian of Bolivia. In Suarez-Soruco, R. (ed), Fosiles y Facies de Bolivia, Volume II - Invertebrados y Paleobotanica. Revista Tecnica de Yacimientos Petroliferos Fiscales Bolivianos, 13-14 (1-4): 77-91. Babcock, L. E. and Feldmann, R. M. 1986a. The phylum Conulariida. In Hoffman A. and Nitecki, M. H. (eds). Problematic Fossil Taxa. Oxford University Press, Oxford, New York, p. 135-147. Babcock, L. E. and Feldmann, R. M. 1986b. Devonian and Mississippian conulariids of North America. Part A. General description and Conularia. Annals of Carnegie Museum, 55: 349-410. Babcock, L. E. and Feldmann, R. M. 1986b. Devonian and Mississippian conulariids of North America. Part B. Paraconularia, Reticulaconularia, new genus, and organisms rejected from conulariida. Annals of Carnegie Museum, 55: 411-479. Babcock, L. E., R. M. Feldmann, M. T. Wilson, & M. Suarez-Riglos. 1987a. Devonian Conulariids of Bolivia. National Geographic Research, 3: 210-231 Choi, D. K., 1988. A conulariid from the Geumcheon Formation (Upper Carboniferous), Sangdong area, Korea. Journal of the Geological Society of Korea, 24: 87-92 Choi, D. K., Jeong, K. W., 1990. Discovery of Conulariid from the Yeongheung Formation (Ordovician), Korea. Journal of the Geological Society of Korea 26, 5: 497-499 Choi, D.K. and Chough, S. K., 2005 The Cambrian-Ordovician stratigraphy of the Taebaeksan Basin, Korea: a review. Geosciences Journal, 9: 187-214 Sinclair, G. W., 1940. The genotype of Conularia. Canadian Field-Naturalist, 54: 72-74. Sinclair, G. W., 1942. The Chazy Conularida and their Congeners. Carnegie Museum, 29: 219-240 Sinclair, G. W., 1948. The Biology of the Conularida. Unpublished Ph.D. thesis, McGill Universiy, Montreal, 442 p. Steinmann, G. Doderlein L. 1890. Elemente der Palaontologie. Verlag von Wilhelm Engelmann, Leipzig, 848 p. Van lten, H., 1992a. Morphology and phylogenetic significance of the corners and midlines of the conulariid test. Paleontology, 35: 335-358. 22 Van lten, H., 1992b. Microstructure and growth of the conulariid test: implications for conulariid affinities. Paleontology, 35: 359-372. White, C.A. 1862. Description of new species of fossils from the Devonian and Carboniferous rocks of the Mississippi Valley. Boston Society of Natural History, Proceedings, 9: 8-33. 23 

New occurrences of Ordovician, Devonian, and Carboniferous conulariids from North America, South America, and Asia

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New occurrences of Ordovician, Devonian, and Carboniferous conulariids from North America, South America, and Asia

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