Vol 18, Number 1, March 2003
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Thomas Jefferson Meg Tooth
The ECPHORA The Newsletter of the Calvert Marine Museum Fossil Club Volume 30 Number 3 September 2015 Thomas Jefferson Meg Tooth Features Thomas Jefferson Meg The catalogue number Review; Walking is: ANSP 959 Whales Inside The tooth came from Ricehope Estate, Snaggletooth Shark Cooper River, Exhibit South Carolina. Tiktaalik Clavatulidae In 1806, it was Juvenile Bald Eagle originally collected or Sculpting Whale Shark owned by Dr. William Moroccan Fossils Reid. Prints in the Sahara Volunteer Outing to Miocene-Pliocene National Geographic coastal plain sediments. Dolphins in the Chesapeake Sloth Tooth Found SharkFest Shark Iconography in Pre-Columbian Panama Hippo Skulls CT- Scanned Squalus sp. Teeth Sperm Whale Teeth On a recent trip to the Academy of Natural Sciences of Drexel University (Philadelphia), Collections Manager Ned Gilmore gave John Nance and me a behind -the-scenes highlights tour. Among the fossils that belonged to Thomas☼ Jefferson (left; American Founding Father, principal author of the Declaration of Independence, and third President of the United States) was this Carcharocles megalodon tooth. Jefferson’s interests and knowledge were encyclopedic; a delight to know that they included paleontology. Hand by J. Nance. Photo by S. Godfrey. Jefferson portrait from: http://www.biography.com/people/thomas-jefferson-9353715 ☼ CALVERT MARINE MUSEUM www.calvertmarinemuseum.com 2 The Ecphora September 2015 Book Review: The Walking 41 million years ago and has worldwide distribution. It was fully aquatic, although it did have residual Whales hind limbs. In later chapters, Professor Thewissen George F. Klein discusses limb development and various genetic factors that make whales, whales. This is a The full title of this book is The Walking complicated topic, but I found these chapters very Whales — From Land to Water in Eight Million clear and readable. -
Part I. Revision of Buttsoceras. Part II. Notes on the Michelinoceratida
MEMOIR 10 PART I Revision of Buttsoceras PART II Notes on the Michelinoceratida By ROUSSEAU H. FLOWER 1 9 6 2 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ........................................ Governor of New Mexico Tom Wiley .......................................................... Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott ............................................................................................... Hobbs Holm 0. Bursum, Jr. ......................................................................................... Socorro Thomas M. Cramer ......................................................................................... Carlsbad Frank C. DiLuzio ...................................................................................... Albuquerque Eva M. Larrazolo (Mrs. Paul F.) ............................................................... Albuquerque Published October I2, 1962 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.00 Contents PART I REVISION OF BUTTSOCERAS Page ABSTRACT ....................................................................................................................... INTRODUCTION ............................................................................................................................. -
The Carboniferous Evolution of Nova Scotia
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. -
Paleontological Research, Vol
Paleontological Research, vol. 6. no. 1, pp. 67-72. April 30. 2002 Ç bj the Palaeontologica! Society of Japan Permian bivalves from the H. S. Lee Formation, Malaysia KEIJI NAKAZAWA 28-2 Koyama Shimouchikawara-cho, Kita-ku. Kyoto. 603-8132, Japan Received 2 July 2001: Revised manuscript accepted 7 December 2001 Abstract. Three bivalve species collected from the Permian H. S. Lee Formation at the H. S. Lee No. 8 Mine in Perak, Malaysia are described. They are identified as Sanguinolites ishii sp. nov., Megalodon (Megalodon) yanceyi sp. nov.. and Myalina (Myalina) cf. wyomingensis (Lea). The fossil locality is famous for the abundant occurrence of gastropods together with bivalves, cephalopods, calcareous algae and others, but is flooded and inaccessible now. The new species of Megalodon is considered to be the first record of the genus in the Permian. Key words: H. S. Lee Formation. Malaysia, Megalodon, Permian bivalves Introduction and previous research Grammatodon (Cosmetodon) obsoletiformis (Hayasaka) Grammatodon (Cosmetodon) sp. The bedrock of open-pit tin mines in the Kampar area, Shikamaia perakensis (Runnegar and Gobbett) Perak. Malaysia is mostly composed of carbonate rocks, Saikraconcha {Dereconcha) kamparensis Yancey and such as limestone, dolomitic limestone, and dolomite. The Boyd fossiliferous limestone beds occupying the uppermost inter- Saikraconcha (Dereconcha) sp. val of this sequence occur in the H. S. Lee and Nam Long Prospondylus chintongia Yancey Mines, and were named the H. S. Lee Beds by Sunthralin- Pernopecten malaysia Yancey gam (1968). The rich Permian fossils collected from the Palaeolima sp. H. S. Lee Mine (mostly No. 8 Mine, the type locality of the Lyroschizodus sp. -
Orthoceras Limestone" of Southwestern Sardinia (Middle-Upper Silurian) ( * )
Mem. Soc. Geol. /t., 20 (1979), 405-423. 9 ff., 4 tabb. PALEOECOLOGICAL REMARKS ON TUE "ORTHOCERAS LIMESTONE" OF SOUTHWESTERN SARDINIA (MIDDLE-UPPER SILURIAN) ( * ) Memoria di MAURIZIO GNOLI (**), GrAN CLEMENTE PAREA (***). FRANCO Russo(**) & ENRICO SERPAGLI (**) (presentata a Siena, nella Seduta /ematica del /8-/9 maggio 1979) CO NTE NT ricco di fauna esclusivamente pelagica nelle parti p age superiori e decisamente tossico verso il fondo. lNTRODUCTION 405 Analisi statistiche ed esperimenti di laborato l"Ìo hanno portato gli scriventi a considerare il GEOLOGICAL REMARKS 406 particolare tipo di orientamento presentato dai SEDIMENTOLOGICAL REMARKS 407 fossili come un effetto del moto ondoso. I gusci ed i loro frammenti, sparsi su un fondo di fango Geometry of the "Orthoceras lenses" 407 fine, verrebbero disposti dalle onde a bande suc The problem of Nautiloid orientation 410 cessive che rappresenterebbero l'equivalente mec Laboratory experiments 411 canico delle increspature di fondo tipiche dei fon Orientation analysis of the orthoconic di sabbiosi. Potrebbe trattarsi di un mare epicontinentale nautiloids 413 di profondità limitata tale da permettere al moto GENERAL FEATURES OF THE FAUNA 417 ondoso di agire sul fondo. Nektic organisms associated with the grap- tolites 417 Organisms possibly attached to floating ABSTRACT plants 417 A study of the fauna and of the sedimento ENVIRONMENTAL CONCLUSIONS 420 logica! characteristics of the "Orthoceras limestone" REFERENCES 422 has shown that these sediments were deposited in a normally oxygenated sea rich in an exclusively pelagic fauna in the upper parts but definitely KEY WORDS : Shelf environment, death as toxic towards the bottom. semblage, sedimentary structures, depth Statistica! analyses along with laboratory ex periments have led. -
Middle Devonian)
F-l Paleontological Problems of the Hamilton Group (Middle Devonian) H.B. Rollins, N. Eldridge, R.M. Linsley The stratigraphy of the Hamilton Group of the'Middle Devonian of New York State was most recently treated in its entirety by Cooper (1930, 1957). The Hamilton Group of the Chenango Valley (see chart 1) consists primarily of fine clastic sediments and occupies a mid position in this wedge shaped body of rock. In the east the wedge is thickest (about 1,680' in Schoharie Valley (Gruban, 1903, p. 213) and it thins to 285' at Lake Erie in the west (Cooper, 1930, p. 121). In the Chenango Valley the Hamilton Group is 1, 465' thick (op. cit. p. 121) and has a dip to the southwest of 65-75 feet per mile (op. cit. p. 119). The Hamilton Group lies unconformably on the Onondaga Limestone and is overlain unconformably by the Tully Formation. In a very crude sense the Hamilton Group of the Chenango Valley is composed of fine-grained black shales and limestones at the base (the Marcellus Formation) and more clastic units in the upper portion (Skaneateles, Ludlowville and Moscow Formations). However within each of these formations there exists considerable variation from true mud shales through siltstones and up to fine-grained sandstones. The nature of the substrate obviously had a great effect on the faunas associated with them. The black shales are typically associated with a Leiorhynchus fauna, gray shales and siltstones with a Tropidoleptus fauna and the fine-grained sandstones are dominated by bivalves. A more detailed discussion of some of these problems will follow in sections relating to each of the three stops of this trip. -
Review of the Ordovician Stratigraphy and Fauna of the Anarak Region in Central Iran
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/286025445 Review of the Ordovician stratigraphy and fauna of the Anarak Region in Central Iran ARTICLE in ACTA GEOLOGICA POLONICA · JANUARY 2015 Impact Factor: 0.84 · DOI: 10.1515/apg-2015-0022 READS 26 6 AUTHORS, INCLUDING: Leonid E. Popov Vachik Hairapetian National Museum Wales Islamic Azad University Khorasgan (Isfahan) Branch 231 PUBLICATIONS 2,239 CITATIONS 33 PUBLICATIONS 130 CITATIONS SEE PROFILE SEE PROFILE Mansoureh Ghobadi Pour Lars E Holmer Golestan University Uppsala University 69 PUBLICATIONS 365 CITATIONS 211 PUBLICATIONS 2,319 CITATIONS SEE PROFILE SEE PROFILE Available from: Leonid E. Popov Retrieved on: 11 December 2015 Acta Geologica Polonica, Vol. 65 (2015), No. 4, pp. 403–435 DOI: 10.1515/agp-2015-0022 Review of the Ordovician stratigraphy and fauna of the Anarak Region in Central Iran LEONID E. POPOV1, VACHIK HAIRAPETIAN2, DAVID H. EVANS3, MANSOUREH GHOBADI POUR4, LARS E. HOLMER5 and CHRISTIAN BAARS1 1Department of Geology, National Museum of Wales, Cardiff CF10 3NP, Wales, United Kingdom. E-mail: [email protected], [email protected] 2Department of Geology, Isfahan (Khorasgan) Branch, Islamic Azad University, PO Box 81595−158, Isfahan, Iran. E-mail: [email protected] 3Natural England, Suite D, Unex House, Bourges Boulevard, Peterborough PE1 1NG, England, United Kingdom. E-mail: [email protected] 4Department of Geology, Faculty of Sciences, Golestan University, Gorgan, Iran. E-mail: [email protected] 5Institute of Earth Sciences, Palaeobiology, Uppsala University, SE-752 36 Uppsala, Sweden. E-mail: [email protected] ABSTRACT: Popov, L.E., Hairapetian, V., Evans, D.H., Ghobadi Pour, M., Holmer, L.E. -
Ordovician Cephalopod Biofacies of South China and Its Provincialization
J ournal of China University o f Geosciences , Vol. 17 , No. 3 , p. 221 - 230 , September 2006 ISS N 1002 - 0705 Printed in China Ordovician Cephalopod Biofacies of South China and Its Provincialization Xiao Chuantao*(肖传桃) Faculty o f Earth Sciences , China University o f Geosciences , Wuhan 430074 , China ; Geosciences College , Y angtze University , J ingz hou 434023 , China Chen Zhiyong (陈志勇) Faculty o f Earth Sciences , China University o f Geosciences , Wuhan 430074 , China ; Qinghai Oil f ield Com pany , Dunhuang 736202 , China Liu Li (刘莉) He Youbin (何幼斌) Geosciences College , Y angtze University , J ingz hou 434023 , China ABSTRACT :The research on biofacies and its provincialization is of important significance not only for the increasing of precision of stratigraphic subdivision and correlation in South China, the reconstruction of ancient environment and paleogeography and even the guiding of oil and gas exploration, but also for the study of paleobiogeogrphy and sea level changes of southern China in Ordovician. On the basis of the studies of the ecological characteristics of Ordovician cephalopods from South China , eighteen cephalopod biofacies are recognized and described :(1)Open platform Proterocameroceras biofacies ;(2) Restricted platform Pseudoectenolites-Xiadongoceras biofacies; ( 3 ) Open platform Retroclitendoceras- Pararetroclitendoceras biofacies;(4)Open platform Prona jaceras-Mamagouceras biofacies;(5) Shelf slope-basin Cyclostomiceras biofacies;(6) Open platform Cameroceras-Cyrtovaginoceras biofacies ; (7) Open -
A Generic Classification of the Nearctic Sawflies (Hymenoptera, Symphyta)
THE UNIVERSITY OF ILLINOIS LIBRARY rL_L_ 5 - V. c_op- 2 CD 00 < ' sturn this book on or before the itest Date stamped below. A arge is made on all overdue oks. University of Illinois Library UL28: .952 &i;g4 1952 %Po S IQ";^ 'APR 1 1953 DFn 7 W54 '•> d ^r-. ''/./'ji. Lit]—H41 Digitized by tine Internet Arciiive in 2011 with funding from University of Illinois Urbana-Champaign http://www.archive.org/details/genericclassific15ross ILLINOIS BIOLOGICAL MONOGRAPHS Vol. XV No. 2 Published by the University of Illinois Under the Auspices of the Graduate School Ukbana, Illinois 1937 EDITORIAL COMMITTEE John Theodore Buchholz Fred Wilbur Tanner Harley Jones Van Cleave UNIVERSITY OF ILLINOIS 1000—7-37—11700 ,. PRESS A GENERIC CLASSIFICATION OF THE NEARCTIC SAWFLIES (HYMENOPTERA, SYMPHYTA) WITH SEVENTEEN PLATES BY Herbert H. Ross Contribution No. 188 from the Entomological Laboratories of the University of Illinois, in Cooperation with the Illinois State Natural History Survey CONTENTS Introduction 7 Methods 7 Materials 8 Morphology 9 Head and Appendages 9 Thorax and Appendages 22 Abdomen and Appendages 29 Phylogeny 33 The Superfamilies of Sawflies 33 Family Groupings 34 Hypothesis of Genealogy .... 35 Larval Characters 45 - Biology 46 Summary of Phylogeny 48 Taxonomy 50 Superfamily Tenthredinoidea 51 Superfamily Megalodontoidea 106 Superfamily Siricoidea 110 Superfamily Cephoidea 114 Bibliography 117 Plates 127 Index 162 ACKNOWLEDGMENT This monograph is an elaboration of a thesis sub- mitted in partial fulfillment for the degree of Doctor of Philosophy in Entomology in the Graduate School of the University of Illinois in 1933. The work was done under the direction of Dr. -
Cephalopod Faunas from Southwestern United States
ABOUT THE SKETCH ON COVE R- A simple orthocone with gas in the camerae would have an anterior center of gravity (G1) and an apical center of buoyancy (B1). Such a situation would cause the shell to occupy a vertical position, forcing the head into the mud on the sea floor—making the animal very unhappy and uncomfortable, as can be plainly seen from its expression. Weighting the apex of the shell with cameral deposits or siphonal deposits, or both (only cameral deposits are shown here), would move the center of gravity backward, from 01 to G2, and move the center of buoyancy forward, from B1 to B2, permitting the animal to swim and move in a horizontal position—making it very happy and comfortable, as can be seen from the ecstatic expression. Further growth of the shell requires further growth of the deposits, moving the center of gravity forward to midlength (from G2 to G3) and moving the center of buoyancy forward also from B2 to B3. Such an adjustment requires careful physiological skill. If the animal now has a rather smug expression, who can blame it? As indicated elsewhere (Flower, 1955, fig. 1, p. 247), balance is attained completely by siphonal filling in the Endoceratida, by a combination of siphonal and cameral deposits in the Actinoceratida, and mainly by cameral deposits in the Michelinoceratida. However, Hook and Flower (1976) subsequently found that the Michelinoceratidae and Troedssonellidae probably spring from different parts of the Baltoceratidae, in which there are both cameral and siphonal deposits (rods, linings, and annuli in varying combinations) in a siphuncle close to the venter. -
Geographical Distribution Patterns of Carcharocles Megalodon Over Time
Journal of Biogeography (J. Biogeogr.) (2016) ORIGINAL Geographical distribution patterns of ARTICLE Carcharocles megalodon over time reveal clues about extinction mechanisms Catalina Pimiento1,2,3* Bruce J. MacFadden2, Christopher F. Clements4, Sara Varela5,6, Carlos Jaramillo3, Jorge Velez-Juarbe7 and Brian R. Silliman8 1Paleontological Institute and Museum, ABSTRACT University of Zurich, CH-8006 Zurich, Aim Given its catastrophic consequences, the extinction of apex predators has Switzerland, 2Florida Museum of Natural long been of interest to modern ecology. Despite major declines, no present- History, University of Florida, Gainesville, FL 32611, USA, 3Smithsonian Tropical Research day species of marine apex predator has yet become extinct. Because of their Institute, Balboa, Panama, 4Department of vulnerability, understanding the mechanisms leading to their extinction in the Evolutionary Biology and Environmental past could provide insight into the natural factors that interact with human Studies, University of Zurich, Zurich CH-8057, threats to drive their loss. We studied the geographical distribution patterns of Switzerland, 5Departamento de Ciencias de la the extinct macro-predatory shark Carcharocles megalodon in order to elucidate Vida, Edificio de Ciencias, Campus Externo, its pathway to extinction. Universidad de Alcala, 28805 Alcalade Location World-wide from the Miocene to the Pliocene (c. 23–2.6 Ma). Henares Madrid, Spain, 6Museum fur€ Naturkunde, Leibniz Institute for Evolution Methods A meta-analysis of C. megalodon occurrence records was performed and Biodiversity Science, 10115 Berlin, using the Paleobiology Database as a platform. The data were binned into geo- Germany, 7Department of Mammalogy, logical time slices, and the circular home range around each data point was Natural History Museum of Los Angeles mapped in reconstructions made in GPlates. -
Anatomy and Evolution of the First Coleoidea in the Carboniferous
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2019 Anatomy and evolution of the first Coleoidea in the Carboniferous Klug, Christian ; Landman, Neil H ; Fuchs, Dirk ; Mapes, Royal H ; Pohle, Alexander ; Guériau, Pierre ; Reguer, Solenn ; Hoffmann, René Abstract: Coleoidea (squids and octopuses) comprise all crown group cephalopods except the Nautilida. Coleoids are characterized by internal shell (endocochleate), ink sac and arm hooks, while nautilids lack an ink sac, arm hooks, suckers, and have an external conch (ectocochleate). Differentiating between straight conical conchs (orthocones) of Palaeozoic Coleoidea and other ectocochleates is only possible when rostrum (shell covering the chambered phragmocone) and body chamber are preserved. Here, we provide information on how this internalization might have evolved. We re-examined one of the oldest coleoids, Gordoniconus beargulchensis from the Early Carboniferous of the Bear Gulch Fossil- Lagerstätte (Montana) by synchrotron, various lights and Reflectance Transformation Imaging (RTI). This revealed previously unappreciated anatomical details, on which we base evolutionary scenarios of how the internalization and other evolutionary steps in early coleoid evolution proceeded. We suggest that conch internalization happened rather suddenly including early growth stages while the ink sac evolved slightly later. DOI: https://doi.org/10.1038/s42003-019-0523-2 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-172717 Journal Article Published Version The following work is licensed under a Creative Commons: Attribution 4.0 International (CC BY 4.0) License. Originally published at: Klug, Christian; Landman, Neil H; Fuchs, Dirk; Mapes, Royal H; Pohle, Alexander; Guériau, Pierre; Reguer, Solenn; Hoffmann, René (2019).