Oriented Microwear on a Tooth of Edestus Minor (Chondrichthyes, Eugeneodontiformes): Implications for Dental Function
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Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
Introduction and Bibliography
Downloaded from http://sp.lyellcollection.org/ by guest on October 3, 2021 Introduction and bibliography MIKE SMITH*, ZERINA JOHANSON, PAUL M. BARRETT & M. RICHTER Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author (e-mail: [email protected]) Arthur Smith Woodward (1864–1944) was ac- Wegener was proposing his theory of continental knowledged as the world’s foremost authority on drift. It would be almost half a century before fossil fishes during his lifetime and made impor- his theory gained widespread acceptance. Hallam tant contributions to the entire field of vertebrate (1983, p. 135) wrote in Great Geological Contro- palaeontology. He was a dedicated public servant, versies that ‘The American palaeontologist G. G. spending his whole career at the British Museum Simpson noted in 1943 the near unanimity of (Natural History) (now the Natural History Museum, palaeontologists against Wegener’s ideas’. Smith NHM) in London. He served on the council and as Woodward certainly fell into this camp but was president of many of the important scientific socie- more inclined to note that no certainty could yet be ties and was elected a Fellow of the Royal Society attached to the palaeontological evidence (Wood- in 1901. He was knighted on retirement from the ward 1935). Scientific theories that we accept today Museum in 1924. were still controversial and intensely debated while Smith Woodward was born on 23 May 1864 in Smith Woodward was alive. Macclesfield, an industrial town in the north Mid- A book that celebrates the life and scientific lands of England. -
Pennsylvanian Vertebrate Fauna
VII PENNSYLVANIAN VERTEBRATE FAUNA By ROY LEE MOODIE THE PENNSYLVANIAN VERTEBRATE FAUNA OF KENTUCKY By ROY LEE MOODIE INTRODUCTION The vertebrates which one may expect to find in the Penn- sylvanian of Kentucky are the various types of fishes, enclosed in nodules embedded in shale, as well as in limestone and in coal; amphibians of many types, found heretofore in nodules and in cannel coal; and probably reptiles. A single incomplete skeleton found in Ohio, described below, seems to be a true reptile. Footprints and fragmentary skeletal elements found in Pennsylvania1 in Kansas2 in Oklahoma3, in Texas4 in Illinois5, and other regions, in rocks of late Pennsylvanian or early Permian age, and often spoken of as Permo- Carboniferous, indicate types of vertebrates, some of which may be reptiles. No skeletal remains or other evidences of Pennsylvanian vertebrates have so far been found in Kentucky, but there is no reason why they cannot confidently be expected to occur. A single printed reference points to such vertebrate remains6. As shown by the map, Kentucky lies immediately adjacent to regions where Pennsylvanian vertebrates have been found. That important discoveries may still be made is indicated by Carman's recent find7. Ohio where important discoveries of 1Case, E. C. Description of vertebrate fossils from the vicinity of Pittsburgh, Pa: Annals of the Carnegie Museum, IV, Nos. III-IV, pp. 234-241. pl. LIX, 1908. 2Williston, S. W. Some vertebrates from the Kansas Permian: Kansas Univ. Quart., ser. A, VI, No.1, pp. 53. fig., 1897. 3Case, E. C., On some vertebrate fossils from the Permian beds of Oklahoma. -
Issue 3 November, 2018 ______
__________The Paleontograph________ A newsletter for those interested in all aspects of Paleontology Volume 7 Issue 3 November, 2018 _________________________________________________________________ From Your Editor Welcome to our latest edition. I've decided to produce a special edition. Since the holidays are just around the corner and books make great gifts, I thought a special book review edition might be nice. Bob writes wonderful, deep reviews of the many titles he reads. Reviews usually bring a wealth of knowledge about the book topic as well as an actual review of the work. I will soon come out with a standard edition filled with articles about specific paleo related topics and news. The Paleontograph was created in 2012 to continue what was originally the newsletter of The New Jersey Paleontological Society. The Paleontograph publishes articles, book reviews, personal accounts, and anything else that relates to Paleontology and fossils. Feel free to submit both technical and non-technical work. We try to appeal to a wide range of people interested in fossils. Articles about localities, specific types of fossils, fossil preparation, shows or events, museum displays, field trips, websites are all welcome. This newsletter is meant to be one by and for the readers. Issues will come out when there is enough content to fill an issue. I encourage all to submit contributions. It will be interesting, informative and fun to read. It can become whatever the readers and contributors want it to be, so it will be a work in progress. TC, January 2012 Edited by Tom Caggiano and distributed at no charge [email protected] PALEONTOGRAPH Volume 7 Issue 3 November 2018 Page 2 Patrons of Paleontology--A Review As you might expect from the chapter titles, this is a Bob Sheridan October 14, 2017 fairly specialized book, which is tilted more toward history than science in general, and then very concerned with large illustrated publications about fossils. -
Arthur Smith Woodward's Fossil Fish Type Specimens CONTENTS Page
ARTHUR SMITH WOODWARD’S 1 Bernard & Sm ith 2016 FOSSIL FISH TYPE SPECIMENS (http://www.geolsoc.org.uk/SUP18874) Arthur Smith Woodward’s fossil fish type specimens EMMA LOUISE BERNARD* & MIKE SMITH Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK *Corresponding author (e-mail: [email protected]) CONTENTS Page REVISION HISTORY 3 INTRODUCTION 6 TYPES 7 Class Subclass: Order: Pteraspidomorphi 7 Pteraspidiformes 7 Cephalaspidomorphi 8 Anaspidiformes 8 Placodermi 9 Condrichthyes Elasmobranchii 12 Xenacanthiformes 12 Ctenacanthiformes 15 Hybodontiformes 15 Heterodontiformes 28 Hexanchiformes 29 Carcharhiniformes 31 Orectolobiformes 32 Lamniformes 34 Pristiophoriformes 37 Rajiformes 38 Squatiniformes 44 Myliobatiformes 45 Condrichthyes Holocephali 50 Edestiformes 50 Petalodontiformes 50 Chimaeriformes 52 Psammodontiformes 70 Acanthodii 70 Actinopterygii 74 Palaeonisciformes 74 Saurichthyiformes 84 Scorpaeniformes 85 ARTHUR SMITH WOODWARD’S 2 Bernard & Sm ith 2016 FOSSIL FISH TYPE SPECIMENS (http://www.geolsoc.org.uk/SUP18874) Acipenseriformes 85 Peltopleuriformes 87 Redfieldiiformes 88 Perleidiformes 89 Gonoryhnchiformes 90 Lepisosteiformes 92 Pycnodontiformes 93 Semionotiformes 107 Macrosemiiformes 120 Amiiformes 121 Pachycormiformes 131 Aspidorhynchiformes 138 Pholidophoriformes 140 Ichthyodectiformes 144 Gonorynchiformes 148 Osteoglossiformes 149 Albuliformes 150 Anguilliformes 153 Notacanthiformes 156 Ellimmichthyiformes 157 Clupeiformes 158 Characiformes 161 Cypriniformes 162 Siluriformes 163 Elopiformes -
Arthur Smith Woodward's Fossil Fish Type
ARTHUR SMITH WOODWARD’S 1 Bernard & Smith 2015 FOSSIL FISH TYPE SPECIMENS (http://www.geolsoc.org.uk/SUP18874) Arthur Smith Woodward’s fossil fish type specimens EMMA LOUISE BERNARD* & MIKE SMITH Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK *Corresponding author (e-mail: [email protected]) CONTENTS Page INTRODUCTION 3 TYPES 4 Class Subclass: Order: Pteraspidomorphi 4 Pteraspidiformes 4 Cephalaspidomorphi 5 Anaspidiformes 5 Placodermi 6 Condrichthyes Elasmobranchii 7 Xenacanthiformes 7 Ctenacanthiformes 9 Hybodontiformes 9 Heterodontiformes 21 Hexanchiformes 22 Carcharhiniformes 23 Orectolobiformes 25 Lamniformes 27 Pristiophoriformes 30 Rajiformes 31 Squatiniformes 37 Myliobatiformes 37 Condrichthyes Holocephali 42 Edestiformes 42 Petalodontiformes 42 Chimaeriformes 44 Psammodontiformes 62 Acanthodii 62 Actinopterygii 65 Palaeonisciformes 65 Saurichthyiformes 74 Scorpaeniformes 75 Acipenseriformes 75 Peltopleuriformes 77 ARTHUR SMITH WOODWARD’S 2 Bernard & Smith 2015 FOSSIL FISH TYPE SPECIMENS (http://www.geolsoc.org.uk/SUP18874) Redfieldiiforme 78 Perleidiformes 78 Gonoryhnchiformes 80 Lepisosteiformes 81 Pycnodontiformes 82 Semionotiformes 93 Macrosemiiformes 105 Amiiformes 106 Pachycormiformes 116 Aspidorhynchiformes 121 Pholidophoriformes 123 Ichthyodectiformes 127 Gonorynchiformes 131 Osteoglossiformes 132 Albuliformes 133 Anguilliformes 136 Notacanthiformes 139 Ellimmichthyiformes 140 Clupeiformes 141 Characiformes 144 Cypriniformes 145 Siluriformes 145 Elopiformes 146 Aulopiformes 154 -
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Acta Geologica Polonica, Vol. 68 (2018), No. 3, pp. 403–419 DOI: 10.1515/agp-2018-0007 A revision of Campyloprion Eastman, 1902 (Chondrichthyes, Helicoprionidae), including new occurrences from the Upper Pennsylvanian of New Mexico and Texas, USA WAYNE M. ITANO1 and SPENCER G. LUCAS2 1 Natural History Museum, University of Colorado, Boulder, Colorado 80309, USA. E-mail: [email protected] 2 New Mexico Museum of Natural History and Science, Albuquerque, New Mexico 87104, USA. E-mail: [email protected] ABSTRACT: Itano, W.M. and Lucas, S.G. 2018. A revision of Campyloprion Eastman, 1902 (Chondrichthyes, Helicoprio- nidae), including new occurrences from the Upper Pennsylvanian of New Mexico and Texas, USA. Acta Geo- logica Polonica, 68 (3), 403−419. Warszawa. Campyloprion Eastman, 1902 is a chondrichthyan having an arched symphyseal tooth whorl similar to that of Helicoprion Karpinsky, 1899, but less tightly coiled. The holotype of Campyloprion annectans Eastman, 1902, the type species of Campyloprion, is of unknown provenance, but is presumed to be from the Pennsylvanian of North America. Campyloprion ivanovi (Karpinsky, 1922) has been described from the Gzhelian of Russia. A partial symphyseal tooth whorl, designated as Campyloprion cf. C. ivanovi, is reported from the Missourian Tinajas Member of the Atrasado Formation of Socorro County, New Mexico, USA. Partial tooth whorls from the Virgilian Finis Shale and Jacksboro Limestone Members of the Graham Formation of northern Texas, USA, are designated as Campyloprion sp. Two partial tooth whorls from the Gzhelian of Russia that were previously referred to C. ivanovi are designated as Campyloprion cf. -
On Campyloprion, a New Form of Edestus-Like Dentition
148 Dr. C. Ji. Eastman—New Form of Shark's Dentition. The great inequality and difference of shape of the opposite valves ascribed to the same species are also characteristic and peculiar features. EXPLANATION OP PLATE VII. FIG. 1.—Trochoceras spurium, Salter [a 466). "Wenloek Shale: Builth Bridge. Drawn nat. size. FIG. 2.—Orthocerasfluctuation, Salter (a 611). Lower Bala (Llandeilo): Wellfield, Builth. x twice nat. size. FIG. 3.—Pterinea exasperata, Salter (a 816). Wenloek Limestone : Dudley. x H nat. size. FIG. 4.—Ditto "(a 813). FIG. 5.—Ditto (a 816), 4 ribs enlarged 4 times nat. size, to show ornamentation. FIG. 6.—Pterinea condor, Salter (« 809). Lower Ludlow Beds: Dudley. Left valve. Nat. size. FIG. 7.—Ditto, right valve [a 810), nat. size. II.—ON CAMPYLOPPIOX, A NEW FORM OF EDESTUS-IAKK DENTITION. By Dr. C. E. EASTMAN, of Cambridge, Mass., U.S.A. (PLATE VIII.) N the January number of the GEOLOGICAL MAGAZINE for 1886, an elaborate description is given by Dr. Henry Woodward of Ia peculiar ichthyic structure from the Carboniferous of Western Australia, which is referred by him provisionally to Edestus, under the specific title of E. davisii. Interesting comparisons are drawn between this and other known species of Edestus, and the hypothesis advanced that it is a pectoral fin-spine, resembling in its segmented character the Cretaceous Pelecopterus. This segmentation, which is so conspicuous a feature of Edestus, is attributed by Dr. Bashford Dean in his book on " Fishes, Living and Fossil," to a metameral origin, .and he follows Leidy, Owen, Cope, Newberry, and others in interpreting all this class of remains as dorsal fin-spines. -
SDAS 2002 Vol 81
Proceedings of the South Dakota Academy of Science Volume 81 2002 Published by the South Dakota Academy of Science Academy Founded November 22, 1915 Editor Kenneth F. Higgins Co-Editor Steven R. Chipps Terri Symens, Wildlife & Fisheries, SDSU provided secretarial assistance Tom Holmlund, Graphic Designer TABLE OF CONTENTS Consolidated Minutes of the Eighty-Seventh Annual Meeting of the South Dakota Academy of Science ........................................................................................1 Presidential Address: Reflections on Science in South Dakota and on Vitamin B12. M. Steven McDowell ..............................................................................11 Complete Senior Research Papers presented at The 87th Annual Meeting of the South Dakota Academy of Science Hydrogeology of the Homestake Mine. Perry H. Rahn and William M. Roggenthen ..............................................................................................19 Mycorrhizal Colonization as Impacted by Corn Hybrid. Marie-Laure A. Sauer, Diane H. Rickerl, Patricia K. Wieland, Courtenay Hoernemann, and W.B. Gordon........................................................................................................27 Retention and Survival Rates Associated With the Use of T-Bar Anchor Tags in Marking Yellow Perch. George D. Scholten, Daniel A. Isermann and David W. Willis ....................................................................................................35 Impact of Crop Harvest on Small Mammal Populations in Brookings County, -
Helicoprion—Spine Or Tooth?
Reviews—Kai'pimky on Helicoprion. 33 The Oi'dovician chert of Chypon's Farm, in Mullion parish, continuous with the Eadiolarian chert of Mullion Island, was examined in 1899, and yielded: Sphseroidea, 3 genera (with 3 species); Prunoidea, 3 genera (6 species); and Discoidea, 1 genus (1 species). Dr. Hinde's latest memoir on Eadiolaria has been prepared as an Appendix for the " Geology of Central Borneo," to be published by Professor Dr. G. A. F. Molengraaf, of the Dutch Exploring Expedi- tion, in 1893-4. In his Introduction Dr. Hinde describes thu outcrops and general character of the Eadiolarian rocks under notice, namely, jaspers, cherts, hornstone, and diabase tuff. Their local occurrence in the siliceous rocks and in the tuffs, and the dis- tribution of these fossil Eadiolaria in other countries, are indicated in the table at pp. 44-4G, and treated in detail in the text:— Genera. Species Beloidea 1 1 Sphceroidea ... 5 17 Prunoidea 5 12 Discoidea 6 16 Cyrtoidea 13 54 30 100 These rocks are stated to underlie strata of Cenomanian age, and they seem to belong either to the latest Jurassic or the earliest Cretaceous age, as is the case also with the Eadiolarian cherts and jaspers of the Coast Eange in California. Great services have been rendered to geology by Dr. Hinde's elucidation of the relics of some very obscure Invertebrata, in his successful studies of the Silurian Conodonts, of Sponges of every group and age, and now of Palaeozoic and other Kadiolaria. He has thus indicated how the relative age of many rocks may be deter- mined by the evidence of several kinds of microscopic fossils. -
A New Fossil-Lagerstätte from the Late Devonian of Morocco : Faunal Composition, Taphonomy and Paleoecology
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2019 A new fossil-Lagerstätte from the Late Devonian of Morocco : faunal composition, taphonomy and paleoecology Frey, Linda Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-177848 Dissertation Published Version Originally published at: Frey, Linda. A new fossil-Lagerstätte from the Late Devonian of Morocco : faunal composition, taphon- omy and paleoecology. 2019, University of Zurich, Faculty of Science. A New Fossil-Lagerstätte from the Late Devonian of Morocco: Faunal Composition, Taphonomy and Palaeoecology Dissertation zur Erlangung der naturwissenschaftlichen Doktorwürde (Dr. sc. nat.) vorgelegt der Mathematisch-naturwissenschaftlichen Fakultät der Universität Zürich von Linda Frey von St. Ursen FR Promotionskommission Prof. Dr. Christian Klug (Leitung der Dissertation) Prof. Dr. Hugo Bucher Prof. Dr. Marcelo Sánchez Prof. Dr. Michael Coates Dr. Martin Rücklin Zürich, 2019 ABSTRACT ................................................................................................................................................2 INTRODUCTION......................................................................................................................................5 CHAPTER I Late Devonian and Early Carboniferous alpha diversity, ecospace occupation, vertebrate assemblages and bio-events of southeastern Morocco ..............................27 -
SDAS 2002 Vol 81
Proceedings of the South Dakota Academy of Science,Vol. 81 (2002) 81 CHONDRICHTHYES FROM THE UPPER PART OF THE MINNELUSA FORMATION (MIDDLE PENNSYLVANIAN: DESMOINESIAN), MEADE COUNTY, SOUTH DAKOTA D.J. Cicimurri Bob Campbell Geology Museum Clemson University Clemson, SC 29634 M.D. Fahrenbach Geological Survey Program South Dakota Department of Environment and Natural Resources Rapid City, SD 57702 ABSTRACT Numerous teeth, denticles, and scales of selachians and holocephalans have been recovered from an outcropping of the upper Minnelusa Formation in Meade County, South Dakota. Specimens include the denticles Petrodus patelliformis and Listracanthus histrix, the scale Holmesella quadrata, and teeth of Caseodus aff. C. eatoni, Edestus sp., cf. "Cladodus" sp., and Janassa sp. Associated conodont elements of Idiognathodus “delicatus” and Idioprioniodus conjunctus indicate a middle Pennsylvanian (Desmoinesian) age. A similar chondrichthyan assemblage has been reported from temporally equivalent rocks of Arkansas, Kansas, Missouri, Illinois, Oklahoma, and Iowa. Keywords Minnelusa Formation, Pennsylvanian, Chondrichthyes, South Dakota INTRODUCTION The material presented in this report was obtained during field trips con- ducted by the Department of Geology and Geological Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota. Matrix was collected to recover conodont fossils, although it had been known that fossil vertebrates occurred at the locality (Elder 1993). The outcrop is located on the north side of Little Elk Creek, approximately 2.5 km west of Piedmont, and ap- proximately 30 km north of Rapid City (Fig. 1). Fossils were recovered from green and gray silty shale referred to as the Petrodus II bed by Elder (1993) (Fig. 2). This shale occurs approximately 0.7 m above the Petrodus I bed (Elder 1993) and consists of 1-2.5 cm of light green 82 Proceedings of the South Dakota Academy of Science,Vol.