Revision of Saurorhynchus (Actinopterygii: Saurichthyidae) from the Early Jurassic of England and Germany
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Liste Ambulante Pflegedienste Im Landkreis Göppingen
Ambulante Pflegedienste im Landkreis Göppingen Stand Mai 2021/ Angaben ohne Gewähr Gemeinde Pflegedienst Kontakt Einzugsgebiet Bad Boll Diakoniestation Raum Bad Boll Telefon: Aichelberg, Bad Boll, Dürnau, Gammelshausen, Blumhardtweg 30 07164/2041 Hattenhofen, Zell unter Aichelberg. 73087 Bad Boll www.diakoniestation-badboll.de E-Mail: [email protected] Bad Überkingen Pflegedienst Mirjam Care GmbH & Co. Telefon: Bad Ditzenbach und Teilorte, Bad Überkingen KG 07331/951520 und Teilorte, Deggingen mit Reichenbach, Amtswiese 2 Drackenstein, Geislingen und Teilorte, 73337 Bad Überkingen E-Mail: Gruibingen, Hohenstadt, Kuchen, Mühlhausen, www.mirjam-care.de [email protected] Wiesensteig Böhmenkirch Pflegedienst Mirjam Care Böhmenkirch Telefon: Böhmenkirch und Teilorte, Donzdorf und GmbH 07332/9247203 Teilorte, Geislingen und Teilorte, Lauterstein Buchenstraße 44 89558 Böhmenkirch E-Mail: www.mirjam-care-boehmenkirch.de info@mirjam-care- boehmenkirch.de 1 Gemeinde Pflegedienst Kontakt Einzugsgebiet Deggingen Sozialstation Oberes Filstal Telefon: Bad Ditzenbach und Teilorte, Deggingen mit Am Park 9 07334/8989 Reichenbach, Drackenstein, Gruibingen, 73326 Deggingen Hohenstadt, Mühlhausen, Wiesensteig www.sozialstation-deggingen.de E-Mail: sozialstation-deggingen@t- online.de Donzdorf Sozialstation St. Martinus Telefon: Böhmenkirch und Teilorte, Donzdorf und Hauptstraße 60 07162/912230 Teilorte, Lauterstein 73072 Donzdorf www.sozialstation-donzdorf.de E-Mail: [email protected] Ebersbach Dienste für Menschen gGmbH Telefon: -
Geology of the Yorkshire Coast 4. Staithes
05/03/2013 Geology of the Yorkshire Coast Dr Liam Herringshaw - [email protected] 4. Staithes – of Sand and Iron Early Jurassic Staithes Sandstone Formation Cleveland Ironstone Formation 1 05/03/2013 Staithes to Old Nab Simplified cliff section Rocks get younger towards south and east: RMF-SSF-CIF-WMF 2 05/03/2013 Staithes Sandstone Formation •Early Jurassic: Middle Pliensbachian Key features Sandstones with cross-stratification Burrowed siltstones 3 05/03/2013 Hummocky cross-stratification Fine-grained storm deposits 4 05/03/2013 Burrowed siltstones •After each storm, organic-rich silts deposited in quieter conditions Cleveland Ironstone Formation Transition from SSF to CIF, Penny Nab 5 05/03/2013 Oolitic ironstones Cleveland Ironstone Formation Modern oolites Warm, wave-agitated waters 6 05/03/2013 Stratigraphy Fossils 7 05/03/2013 Old Nab Ironstone burrows 8 05/03/2013 Siderite – iron carbonate Grows in sediment Needs low oxygen, low-sulphide conditions with iron and calcium Normally grey; turns red when oxidized Cleveland ironstone environment Fossils = marine conditions Ooids = high energy environment Primary iron-rich ooids = iron-rich waters Burrow scratches = firm sediments Shallow sea, wave-agitated, lots of runoff from land (with iron-rich soils?) 9 05/03/2013 Jet-powered Whitby Early Jurassic Whitby Mudstone Formation Grey Shales Black Shales Alum Shales Whitby Mudstone Formation 10 05/03/2013 Whitby Mudstone Formation Late Early Jurassic – Toarcian 5 subdivisions, mostly muddy Common features - sediments Finely laminated, -
Annual Report 2020 Group Operating Result
DREES & SOMMER GROUP ANNUAL REPORT 2020 GROUP OPERATING RESULT PROFIT & LOSS STATEMENT BALANCE SHEET 2020 (in euros) ASSETS (in euros) LIABILITIES (in euros) 517.2 1. Revenues 485,394,084 A. Fixed assets A. Equity MILLION EUROS 2. Change in work in progress 26,084,016 I. Intangible assets 21,963,398 I. Subscribed capital 13,222,286 SALES 3. Other operating income 5,713,136 517,191,236 1. EDP software, licenses 8,091,787 less nominal value of treasury shares 0 4. Expenditure for purchased services 64,276,703 2. Good will resulting from capital consolidation 13,871,611 II. Capital reserves 25,710,034 5. Personnel expenses 306,846,208 II. Tangible assets 43,515,000 III. Revenue reserves 3,350,289 a) Wages and salaries 268,398,526 1. Land, rights equivalent to real property rights, and buildings 8,764,115 IV. Net income 49,570,262 57.2 b) Social security costs and pension fund 38,447,682 2. Other assets, operating equipment, fixtures and fittings 16,728,916 V. Change in equity due to exchange rate difference 50,439 MILLION EUROS 6. Depreciation 10,305,895 3. Payments on account and tangible assets under construction 18,021,969 VI. Minority interests 1,556,308 OPERATING 7. Other operating expenses 77,021,617 458,450,424 III. Financial assets 1,705,305 93,459,618 RESULT 8. Income from shareholdings –929,754 1. Shareholdings 192,305 9. Income from other securities and from long-term loans 695,872 2. Other securities lending 1,512,999 B. -
Ambush Predator’ Guild – Are There Developmental Rules Underlying Body Shape Evolution in Ray-Finned Fishes? Erin E Maxwell1* and Laura AB Wilson2
Maxwell and Wilson BMC Evolutionary Biology 2013, 13:265 http://www.biomedcentral.com/1471-2148/13/265 RESEARCH ARTICLE Open Access Regionalization of the axial skeleton in the ‘ambush predator’ guild – are there developmental rules underlying body shape evolution in ray-finned fishes? Erin E Maxwell1* and Laura AB Wilson2 Abstract Background: A long, slender body plan characterized by an elongate antorbital region and posterior displacement of the unpaired fins has evolved multiple times within ray-finned fishes, and is associated with ambush predation. The axial skeleton of ray-finned fishes is divided into abdominal and caudal regions, considered to be evolutionary modules. In this study, we test whether the convergent evolution of the ambush predator body plan is associated with predictable, regional changes in the axial skeleton, specifically whether the abdominal region is preferentially lengthened relative to the caudal region through the addition of vertebrae. We test this hypothesis in seven clades showing convergent evolution of this body plan, examining abdominal and caudal vertebral counts in over 300 living and fossil species. In four of these clades, we also examined the relationship between the fineness ratio and vertebral regionalization using phylogenetic independent contrasts. Results: We report that in five of the clades surveyed, Lepisosteidae, Esocidae, Belonidae, Sphyraenidae and Fistulariidae, vertebrae are added preferentially to the abdominal region. In Lepisosteidae, Esocidae, and Belonidae, increasing abdominal vertebral count was also significantly related to increasing fineness ratio, a measure of elongation. Two clades did not preferentially add abdominal vertebrae: Saurichthyidae and Aulostomidae. Both of these groups show the development of a novel caudal region anterior to the insertion of the anal fin, morphologically differentiated from more posterior caudal vertebrae. -
Osteichthyes, Actinopterygii) from the Early Triassic of Northwestern Madagascar
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 123(2): 219-242. July 2017 REDESCRIPTION OF ‘PERLEIDUS’ (OSTEICHTHYES, ACTINOPTERYGII) FROM THE EARLY TRIASSIC OF NORTHWESTERN MADAGASCAR GIUSEPPE MARRAMÀ1*, CRISTINA LOMBARDO2, ANDREA TINTORI2 & GIORGIO CARNEVALE3 1*Corresponding author. Department of Paleontology, University of Vienna, Geozentrum, Althanstrasse 14, 1090 Vienna, Austria. E-mail: [email protected] 2Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Mangiagalli 34, I-20133 Milano, Italy. E-mail: cristina.lombardo@ unimi.it; [email protected] 3Dipartimento di Scienze della Terra, Università degli Studi di Torino, Via Valperga Caluso 35, I-10125 Torino, Italy. E-mail: giorgio.carnevale@ unito.it To cite this article: Marramà G., Lombardo C., Tintori A. & Carnevale G. (2017) - Redescription of ‘Perleidus’ (Osteichthyes, Actinopterygii) from the Early Triassic of northwestern Madagascar . Riv. It. Paleontol. Strat., 123(2): 219-242. Keywords: Teffichthys gen. n.; TEFF; Ankitokazo basin; geometric morphometrics; intraspecific variation; basal actinopterygians. Abstract. The revision of the material from the Lower Triassic fossil-bearing-nodule levels from northwe- stern Madagascar supports the assumption that the genus Perleidus De Alessandri, 1910 is not present in the Early Triassic. In the past, the presence of this genus has been reported in the Early Triassic of Angola, Canada, China, Greenland, Madagascar and Spitsbergen. More recently, it has been pointed out that these taxa may not be ascri- bed to Perleidus owing to several anatomical differences. The morphometric, meristic and morphological analyses revealed a remarkable ontogenetic and individual intraspecific variation among dozens of specimens from the lower Triassic of Ankitokazo basin, northwestern Madagascar and allowed to consider the two Malagasyan species P. -
Gesetzblatt Für Baden-Württemberg
237 GESETZBLATT FÜR BADEN-WÜRTTEMBERG 1979 Ausgegeben Stuttgart, Freitag, 13. Juli 1979 NI" 10 Tag INHALT Seite 26.6.79 Gesetz zur Änderung des Vermessungsgesetzcs .................................................... 237 26. 6. 79 Gesetz zur Änderung des Gesetzes über die Prüfung der Landtagswahlen ....... .. 238 26. 6. 79 Gesetz zur Änderung des Landesgesetzcs über die freiwillige Gerichtsbarkeit . .. 238 15.5.79 Verordnung der Landesregierung über die Zulassung zu den Vorbereitungsdiensten für die Lehrämter an Gymnasien, beruflichen Schulen, Realschulen und Sonderschulen . .. 238 15.5.79 Verordnung der Landesregierung zur Festsetzung der Zulassungszahlen und der Quoten für die Vergabe der Ausbildungsplätze für die im September 1979 und im Februar 1980 beginnenden Vorbereitungsdienste für die Lehrämter an Gymnasien, beruflichen Schulen, Realschulen und Sonderschulen. .. .. 241 15.5.79 Verordnung des Innenministeriums über die Zuständigkeit zur Zuweisung von Asylbewerbern (AsyIZuVO) 244 2.7.79 Verordnung des Ministeriums für Wissenschaft und Kunst über die Festsetzung von Zulassungszahlen an den Universitäten im Wintersemester 1979/80 und Sommersemester 1980 (Zulassungszahlenv~ordnung). 244 4.7.79 Verordnung des Ministeriums für Wissenschaft und Kunst über die Festsetzung von Zulassungszahlen an den Pädagogischen Hochschulen im Wintersemester 1979/80 und im Sommersemester 1980 (Zulassungs- zahlenverordnung - PH) ...................................................................... 251 15.6.79 Dreizehnte V~rordnung des Innenministeriums -
Mary Anning: Princess of Palaeontology and Geological Lioness
The Compass: Earth Science Journal of Sigma Gamma Epsilon Volume 84 Issue 1 Article 8 1-6-2012 Mary Anning: Princess of Palaeontology and Geological Lioness Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/compass Part of the Paleontology Commons Recommended Citation Davis, Larry E. (2012) "Mary Anning: Princess of Palaeontology and Geological Lioness," The Compass: Earth Science Journal of Sigma Gamma Epsilon: Vol. 84: Iss. 1, Article 8. Available at: https://digitalcommons.csbsju.edu/compass/vol84/iss1/8 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in The Compass: Earth Science Journal of Sigma Gamma Epsilon by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. Figure. 1. Portrait of Mary Anning, in oils, probably painted by William Gray in February, 1842, for exhibition at the Royal Academy, but rejected. The portrait includes the fossil cliffs of Lyme Bay in the background. Mary is pointing at an ammonite, with her companion Tray dutifully curled beside the ammonite protecting the find. The portrait eventually became the property of Joseph, Mary‟s brother, and in 1935, was presented to the Geology Department, British Museum, by Mary‟s great-great niece Annette Anning (1876-1938). The portrait is now in the Earth Sciences Library, British Museum of Natural History. A similar portrait in pastels by B.J.M. Donne, hangs in the entry hall of the Geological Society of London. -
Back Matter (PDF)
Index Note: Page numbers in italic denote figures. Page numbers in bold denote tables. Abel, Othenio (1875–1946) Ashmolean Museum, Oxford, Robert Plot 7 arboreal theory 244 Astrodon 363, 365 Geschichte und Methode der Rekonstruktion... Atlantosaurus 365, 366 (1925) 328–329, 330 Augusta, Josef (1903–1968) 222–223, 331 Action comic 343 Aulocetus sammarinensis 80 Actualism, work of Capellini 82, 87 Azara, Don Felix de (1746–1821) 34, 40–41 Aepisaurus 363 Azhdarchidae 318, 319 Agassiz, Louis (1807–1873) 80, 81 Azhdarcho 319 Agustinia 380 Alexander, Annie Montague (1867–1950) 142–143, 143, Bakker, Robert. T. 145, 146 ‘dinosaur renaissance’ 375–376, 377 Alf, Karen (1954–2000), illustrator 139–140 Dinosaurian monophyly 93, 246 Algoasaurus 365 influence on graphic art 335, 343, 350 Allosaurus, digits 267, 271, 273 Bara Simla, dinosaur discoveries 164, 166–169 Allosaurus fragilis 85 Baryonyx walkeri Altispinax, pneumaticity 230–231 relation to Spinosaurus 175, 177–178, 178, 181, 183 Alum Shale Member, Parapsicephalus purdoni 195 work of Charig 94, 95, 102, 103 Amargasaurus 380 Beasley, Henry Charles (1836–1919) Amphicoelias 365, 366, 368, 370 Chirotherium 214–215, 219 amphisbaenians, work of Charig 95 environment 219–220 anatomy, comparative 23 Beaux, E. Cecilia (1855–1942), illustrator 138, 139, 146 Andrews, Roy Chapman (1884–1960) 69, 122 Becklespinax altispinax, pneumaticity 230–231, Andrews, Yvette 122 232, 363 Anning, Joseph (1796–1849) 14 belemnites, Oxford Clay Formation, Peterborough Anning, Mary (1799–1847) 24, 25, 113–116, 114, brick pits 53 145, 146, 147, 288 Benett, Etheldred (1776–1845) 117, 146 Dimorphodon macronyx 14, 115, 294 Bhattacharji, Durgansankar 166 Hawker’s ‘Crocodile’ 14 Birch, Lt. -
“Geochemical Characterisation of the Pliensbachian-Toarcian Boundary During the Onset of the Toarcian Oceanic Anoxic Event
“Geochemical characterisation of the Pliensbachian-Toarcian boundary during the onset of the Toarcian Oceanic Anoxic Event. North Yorkshire, UK” Najm-Eddin Salem A thesis submitted to Newcastle University In partial fulfilment of the requirements for the degree of Doctor of Philosophy in the Faculty of Science and Agriculture School of Civil Engineering and Geosciences, Newcastle University, UK. February 2013 I ABSTRACT The lower Whitby Mudstone Formation of the Cleveland Basin in North Yorkshire (UK) is a world renowned location for the Early Toarcian (T-OAE). Detailed climate records of the event have been reported from this location that shed new light on the forcing and timing of climate perturbations and associated development of ocean anoxia. Despite this extensive previous work, few studies have explored the well-preserved sediments below the event that document different phases finally leading to large-scale (global) anoxia, which is the focus of this project. We resampled the underlying Grey Shale Member at cm-scale resolution and conducted a detailed multi-proxy geochemical approach to reconstruct the redox history prior to the Toarcian OAE. The lower Whitby Mudstone Formation, subdivided into the Grey Shale Member overlain by the Jet Rock (T-OAE), is a cyclic transgressive succession that evolved from the relatively shallow water sediments of the Cleveland Ironstone Formation. The Grey Shale Member is characterised by three distinct layers of organic rich shales (~10-60 cm thick), locally named as the ‘sulphur bands’. Directly above and below these conspicuous beds, the sediments represent more normal marine mudstones. Further upwards the sequence sediments become increasingly laminated and organic carbon rich (up to 14 wt %) representing a period of maximum flooding that culminated in the deposition of the Jet Rock (T-OAE). -
Local Geodiversity Action Plan for Oxfordshire’S Lower and Middle Jurassic
Local Geodiversity Action Plan for Oxfordshire’s Lower and Middle Jurassic Supported by Oxfordshire’s Lower and Middle Jurassic Geodiversity Action Plan has been produced by Oxfordshire Geology Trust with funding from the ALSF Partnership Grants Scheme through Defra’s Aggregates Levy Sustainability Fund. Oxfordshire Geology Trust The Geological Records Centre The Corn Exchange Faringdon SN7 7JA 01367 243 260 www.oxfordshiregt.org [email protected] © Oxfordshire Geology Trust, June 2006 Lower and Middle Jurassic Local Geodiversity Action Plan, Edition 1 Page 1 of 25 © Oxfordshire Geology Trust March 2007 Contents Introduction 3 What is Geodiversity? 4 The Conservation of our Geodiversity National Geoconservation Initiatives 5 Geoconservation in Oxfordshire 6 Local Geodiversity Action plans – Purpose and Process The Purpose of LGAPs 7 The Geographical Boundary 7 Preparing the Plan 8 Geodiversity Audit 8 Oxfordshire’s Lower and Middle Jurassic Geodiversity Resource Lower Lias 10 Middle Lias 11 Upper Lias 12 Inferior Oolite 12 Great Oolite 12 Oxford Clay 16 Fossils 16 Geomorphological Features 17 Building Stone 18 Museum Collections 18 History of Geological Research 19 Implementation Relationships with other Management Plans 21 Future of the LGAP 22 The Action Plan 23 Lower and Middle Jurassic Local Geodiversity Action Plan, Edition 1 Page 2 of 25 © Oxfordshire Geology Trust March 2007 Introduction Oxfordshire’s geology has long been admired by geologists and utilised by industry. In fact, it was a driving force for the industrialization of the nation through the exploitation of ironstone. Our geodiversity however, extends beyond our exposures of rocks and fossils to include landscape and geomorphology, building stones, museums collections and soils. -
Copyrighted Material
06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago).