Adaptive Radiation
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New Late Campanian Ammonites from the Gschliefgraben
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 1999 Band/Volume: 24 Autor(en)/Author(s): Kennedy William James, Summesberger Herbert Artikel/Article: New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria) 23-39 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont. 24:23-39, Wien 1999 New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria) by William J. K ennedy 1 & Herbert Summesberger 1 2 Kennedy , WJ. & S ummesberger , H., 1999. New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria). - Beitr. Palaont., 24:23-39, 1 Text-fig., 3 Plates, Wien. Contents [in:] Tr Oger et al., 1999, this volume). The first note on the ammonite fauna of the Gschliefgraben was pub Abstract, Zusammenfassung.................................... 23 lished by M ojsisovics & Schl Onbach (1868, p. 213: Introduction.............................................................. 23 „Baculites, Hamites, Scaphites, Ammonites“). B rink Systematic Palaeontology 24 mann (1935) noted five ammonite taxa. Twenty-five Sedimentology 31 Stratigraphic conclusions..................................... 31 taxa were described by K ennedy & S ummesberger Palaeobiogeography................................................31 (1984). The geologic situation of the Gschliefgraben References .................................................................31 -
SI Appendix for Hopkins, Melanie J, and Smith, Andrew B
Hopkins and Smith, SI Appendix SI Appendix for Hopkins, Melanie J, and Smith, Andrew B. Dynamic evolutionary change in post-Paleozoic echinoids and the importance of scale when interpreting changes in rates of evolution. Corrections to character matrix Before running any analyses, we corrected a few errors in the published character matrix of Kroh and Smith (1). Specifically, we removed the three duplicate records of Oligopygus, Haimea, and Conoclypus, and removed characters C51 and C59, which had been excluded from the phylogenetic analysis but mistakenly remain in the matrix that was published in Appendix 2 of (1). We also excluded Anisocidaris, Paurocidaris, Pseudocidaris, Glyphopneustes, Enichaster, and Tiarechinus from the character matrix because these taxa were excluded from the strict consensus tree (1). This left 164 taxa and 303 characters for calculations of rates of evolution and for the principal coordinates analysis. Other tree scaling methods The most basic method for scaling a tree using first appearances of taxa is to make each internal node the age of its oldest descendent ("stand") (2), but this often results in many zero-length branches which are both theoretically questionable and in some cases methodologically problematic (3). Several methods exist for modifying zero-length branches. In the case of the results shown in Figure 1, we assigned a positive length to each zero-length branch by having it share time equally with a preceding, non-zero-length branch (“equal”) (4). However, we compared the results from this method of scaling to several other methods. First, we compared this with rates estimated from trees scaled such that zero-length branches share time proportionally to the amount of character change along the branches (“prop”) (5), a variation which gave almost identical results as the method used for the “equal” method (Fig. -
Fossil Spatangoid Echinoids of Cuba
SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 55 Fossil Spatangoid Echinoids of Cuba Porter M. Kier SMITHSONIAN INSTITUTION PRESS City of Washington 1984 ABSTRACT Kier, Porter M. Fossil Spatangoid Echinoids of Cuba. Smithsonian Contributions to Paleobiology, number 55, 336 pages, frontispiece, 45 figures, 90 plates, 6 tables, 1984.—The fossil spatangoid echinoids of Cuba are described based for the most part on specimens in the Sanchez Roig Collection. Seventy-nine species are recognized including 10 from the Late Cretaceous, 36 from the Eocene, 20 from the Oligocene-Miocene, 11 from the Miocene, and 2 of uncertain age. Three of the Eocene species are new: Schizas ter forme III, Linthia monteroae, and Antillaster albeari. A new genus of schizasterid is described, Caribbaster, with the Eocene Prenaster loveni Cotteau as the type-species. A new Asterostoma, A. pawsoni, is described from the Eocene of Jamaica. The Eocene age of the Cuban echinoid-bearing localities is confirmed by the presence outside Cuba of many ofthe same species in beds dated on other fossils. Some evidence supports the Miocene determinations, but the echinoids are of little assistance in resolving the question whether the Cuban beds attributed to the Oligocene are Oligocene or Miocene. Cuban, and in general, the Caribbean Tertiary echinoid faunas are distinct from those in Europe and the Mediterranean. Many genera are confined to the Caribbean. The Cuban fauna is also different from that found nearby in Florida. This difference may be due to a suggested greater depth of water in Cuba. Se describen los equinoideos espatangoideos de Cuba, incluyendo los es- pecimenes de la Coleccion Sanchez Roig. -
The Barremian Heteromorph Ammonite Dissimilites from Northern Italy: Taxonomy and Evolutionary Implications
The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxonomy and evolutionary implications ALEXANDER LUKENEDER and SUSANNE LUKENEDER Lukeneder, A. and Lukeneder, S. 2014. The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxon- omy and evolutionary implications. Acta Palaeontologica Polonica 59 (3): 663–680. A new acrioceratid ammonite, Dissimilites intermedius sp. nov., from the Barremian (Lower Cretaceous) of the Puez area (Dolomites, northern Italy) is described. Dissimilites intermedius sp. nov. is an intermediate form between D. dissimilis and D. trinodosum. The new species combines the ribbing style of D. dissimilis (bifurcating with intercalating single ribs) with the tuberculation style of D. trinodosum (trituberculation on entire shell). The shallow-helical spire, entirely comprising single ribs intercalated by trituberculated main ribs, is similar to the one of the assumed ancestor Acrioceras, whereas the increasing curvation of the younger forms resembles similar patterns observed in the descendant Toxoc- eratoides. These characters support the hypothesis of a direct evolutionary lineage from Acrioceras via Dissimilites to Toxoceratoides. D. intermedius sp. nov. ranges from the upper Lower Barremian (Moutoniceras moutonianum Zone) to the lower Upper Barremian (Toxancyloceras vandenheckii Zone). The new species allows to better understand the evolu- tion of the genus Dissimilites. The genus appears within the Nicklesia pulchella Zone represented by D. duboise, which most likely evolved into D. dissimilis. In the Kotetishvilia compressissima Zone, two morphological forms developed: smaller forms very similar to Acrioceras and forms with very long shaft and juvenile spire like in D. intermedius sp. nov. The latter most likely gave rise to D. subalternatus and D. trinodosum in the M. -
Revision of Hamites Wernickei Wollemann, 1902 (Cephalopoda, Ancyloceratina) from the Classic Lüneburg Section (Upper Cretaceous, Northern Germany)
Acta Geologica Polonica, Vol. 66 (2016), No. 4, pp. 627–644 DOI: 10.1515/agp-2016-0033 Revision of Hamites wernickei Wollemann, 1902 (Cephalopoda, Ancyloceratina) from the classic Lüneburg section (Upper Cretaceous, northern Germany) BIRGIT NIEBUHR1 and JOHN W.M. JAGT2 1 Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie (MMG), Sektion Paläozoologie, Königsbrücker Landstraße 159, 01109 Dresden, Germany. E-mail: [email protected] 2 Natuurhistorisch Museum Maastricht, de Bosquetplein 6–7, 6211 KJ Maastricht, the Netherlands. E-mail: [email protected] ABSTRACT: Niebuhr, B. and Jagt, J.W.M. 2016. Revision of Hamites wernickei Wollemann, 1902 (Cephalopoda, Ancylocera- tina) from the classic Lüneburg section (Upper Cretaceous, northern Germany). Acta Geologica Polonica, 66 (4), 627–644. Warszawa. A re-examination of heteromorph ammonites of late Campanian age from the Zeltberg section at Lüneburg has demonstrated that the type series of Hamites wernickei in fact comprises two different species that are here assigned to the nostoceratid Nostoceras Hyatt, 1894 and the polyptychoceratid Oxybeloceras Hyatt, 1900. Nostoceras (Didy- moceras) wernickei (Wollemann, 1902) comb. nov., to which three of the four specimens that were described and illustrated by Wollemann (1902) belong, has irregularities of ribbing and tuberculation and changes its direction of growth at the transition from the helicoidal whorls to the hook, which is a typical feature of members of the sub- family Nostoceratinae. Torsion of body chambers is not developed in hairpin-shaped ammonite species, which means that the species name wernickei is no longer available for such polyptychoceratine diplomoceratids. Consequently, the fourth specimen figured and assigned to Hamites wernickei by Wollemann (1902) is here transferred to Oxy- beloceras and considered conspecific to material from the Hannover area (Lehrte West Syncline) as O. -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Relative Biodiversity Trends of the Cenozoic Caribbean Region
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 12-2003 Relative biodiversity trends of the Cenozoic Caribbean Region : investigations of possible causes and issues of scale using a biostratigraphic database of corals, echinoids, bivalves, and gastropods William Gray Dean Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Recommended Citation Dean, William Gray, "Relative biodiversity trends of the Cenozoic Caribbean Region : investigations of possible causes and issues of scale using a biostratigraphic database of corals, echinoids, bivalves, and gastropods. " PhD diss., University of Tennessee, 2003. https://trace.tennessee.edu/utk_graddiss/5124 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by William Gray Dean entitled "Relative biodiversity trends of the Cenozoic Caribbean Region : investigations of possible causes and issues of scale using a biostratigraphic database of corals, echinoids, bivalves, and gastropods." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for -
Paleontología Mexicana ISSN (Revista Impresa): 0185-478X ISSN (Revista Electrónica): 2007-5189 Número De Certificado De Licitud De Título: No
DATOS Paleontología Mexicana • Año 3 • Número 65 (versión impresa) • Volumen 4 (versión electrónica) • Febrero 2015 Título: Paleontología Mexicana ISSN (revista impresa): 0185-478X ISSN (revista electrónica): 2007-5189 Número de certificado de licitud de título: No. 04-2012-081311041800-203 Número de reserva de derechos al uso exclusivo del título: No. 04-2012-081311041800-203 Tipo de publicación: Periódica Periodicidad: Semestral Número de publicación: Volumen 65 Número 1 Fecha de publicación: Febrero 2015 Año de inicio de la publicación: 1956 Editada por: Universidad Nacional Autónoma de México, Ciudad Universitaria Domicilio: Instituto de Geología, UNAM, Ciudad Universitaria, Circuito de la Investigación Científica, Copilco El Alto, Coyoacán, 04360 México, D.F. Paleontología Mexicana, Año 3, Número 65 impreso, Volumen 4 electrónica, febrero 2015, es una publicación semestral editada por la Universidad Nacional Autónoma de México, Ciudad Universitaria, Delegación Coyoacán, C.P. 04510, México D. F., a través del Instituto de Geología, Circuito de la Investigación Científica, Copilco, El Alto, Coyoacán, 04510 México D.F., tel. 52 55 56224312 ext 178, http://www.geologia.unam.mx/igl/, [email protected]. Editor responsable Sergio R.S. Cevallos Ferriz. Reserva de derechos al uso exclusivo No. 04- 2012-081311041800-203, ISSN: 2007-5189. Responsable de la última actualización de este número, Instituto de Geología, UNAM, Denise Viridiana Hernández Villalva, Circuito de la Investigación Científica, Copilco El Alto, Coyoacan, 04510 México D.F., fecha de última modificación, 27 de febrero del 2015. Paleontología Mexicana • Año 3 • Número 65 (versión impresa) • Volumen 4 (versión electrónica) • Febrero 2015 Crinoides del Misisípico de la región de El Bísani, 2 noroeste del Estado de Sonora, México Blanca E. -
T Arrantites, a New Heteromorph Ammonite Genus from the Albian Of
Tarrantites, a new heteromorph ammonite genus from the Albian of Texas and Pakistan Herbert Christian Klinger Natural History Collections Department, lziko South African Museum, P 0 Box 61, Cape Town, 8000 South Africa and Department of Geological Sciences, University of Cape Town, Private Bag, Rondebosch, 7701 South Africa E-mail hklinger@iziko org za William James Kennedy Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, UK E-mail jim kennedy@oum oxac uk & Keith P. Minor Texas Research Institute, Austin, 415 Crystal Creek Drive, Austin TX78746, U.SA E-mail kminor@tri-austin com (with 6 figures) Received 12 March 201 0. Accepted 30 March 201 0 A new heteromorphammonite genus, Tarrantites, is proposed for Hamites adkinsi Scott, 1928. The description of the new genus is based mainly on a near<omplete specimen from the Middle Albian part of the G:1odland Limestone of Tarrant County, Texas, the holotype, and on an abraded mould on a pebble from the bed of a stream in Hill County, Texas. In addition, we record the presence of the genus in the Albian of Pakistan. Tarrantites shows a remarkable resemblance to the labeceratine genera Labeceras Spath, 1925 and Myloeeras Spath, 1925: in coiling and size to the former, and in ornamentation to the latter, but is excluded from the subfamily Labeceratinae Spath, 1925, because it has a distinct bifid adventive (A) lobe. This latterfeature, and the ornamentation, rather suggest affinities of Tarrantites with the family Anisoceratidae Hyatt, 1900. Key words: Albian, heteromorph ammonite, Tarrantites, Anisoceratidae,labeceratine homoeomorph, Texas, Pakistan. CONTENTS Abstract · · · · · · · · · · · · · · · · · · 91 Family ?Aniaoc:eratidae · · · · · 91 Discussion · · · · · · · · · · · · · · · 92 Repository of specimens·· · · 91 Genus Tarrantites gen. -
Adec Preview Generated PDF File
Records of the Western Australian Museum 21: 157-165 (2002). The asterostomatid echinoid Antillaster from the Paradash Group (Middle Eocene) of the Nakhichevan Region of Azerbaijan Kenneth J. McNamaral and Oktay H. Melikov2 I Department of Earth and Planetary Sciences, Western Australian Museum, Francis Street, Perth, Western Australia 6000, Australia 2 Azerbaijan State Oil Academy, 370102 Azadlik pr. 20, Baku, Azerbaijan Abstract - The asterostomatid echinoid Antillaster has previously been recorded only from the Caribbean region and northeastern South America. Here we report the first occurrence of this genus from outside the Americas, in the Lesser Caucasus, where it has been found in Middle Eocene sediments of the Paradash Group in the Nakhichevan region of Azerbaijan. The material is described as Antillaster bagmanovi sp. novo It is the earliest known occurrence of the genus. Its presence in the Paratethys, in a region far removed from previous known occurrences, has significant palaeobiogeographic implications. Its disappearance from the Lesser Caucasus, but persistence in the Caribbean, may be linked to the contraction of the Tethys during the Cenozoic. INTRODUCTION from Eocene to Miocene sediments in Venezuela, Eocene sediments in the Nakhichevan region of Cuba, Jamaica, Bonaire, Antigua, Puerto Rico and Azerbaijan have long attracted the attention of Mexico (ICier 1984). Here we report the first record many investigators, due to their good exposure and of this genus from outside the Caribbean region, in extensive foraminiferal and molluscan fauna. The Middle Eocene sediments of the Lesser Caucasus dating of the predominantly clay-sand facies as region in Azerbaijan. This provides the earliest being Eocene is based on this rich foraminiferal and record of asterostomatid echinoids in the Paratethys molluscan fauna (Azizbekov 1961; Bagmanov 1966, region. -
(Campanian and Maestrichtian) Ammonites from Southern Alaska
Upper Cretaceous (Campanian and Maestrichtian) Ammonites From Southern Alaska GEOLOGICAL SURVEY PI SSIONAL PAPER 432 Upper Cretaceous (Campanian and Maestrichtian) Ammonites From Southern Alaska By DAVID L. JONES GEOLOGICAL SURVEY PROFESSIONAL PAPER 432 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows: Jones, David Lawrence, 1930- Upper Cretaceous (Campanian and Maestrichtian) am monites from southern Alaska. Washington, U.S. Govt. Print. Off., 1963. iv, 53 p. illus., maps, diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 432) Part of illustrative matter folded in pocket. 1. Amnionoidea. 2. Paleontology-Cretaceous. 3. Paleontology- Alaska. I. Title. (Series) Bibliography: p. 47-^9. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract-__________________________ 1 Comparison with other areas Continued Introduction. ______________________ 1 Vancouver Island, British Columbia.. 13 Stratigraphic summary ______________ 2 California. ______________--_____--- 14 Matanuska Valley-Nelchina area. 2 Western interior of North America. __ 14 Chignik Bay area._____._-._____ 6 Gulf coast area___________-_-_--_-- 15 Herendeen Bay area____________ 8 Madagascar. ______________________ 15 Cape Douglas area______________ 9 Antarctica ________________________ 15 Deposition and ecologic conditions___. 11 Geographic distribution ________________ 16 Age and correlation ________________ 12 Systematic descriptions.________________ 22 Comparison with other areas _ _______ 13 Selected references._________--_---__-__ 47 Japan _________________________ 13 Index._____-______-_----_-------_---- 51 ILLUSTRATIONS [Plates 1-5 in pocket; 6-41 follow index] PLATES 1-3. -
Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda.