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1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing. -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Trace Fossils from the Baltoscandian Erratic Boulders in Sw Poland
Annales Societatis Geologorum Poloniae (2017), vol. 87: 229–257 doi: https://doi.org/10.14241/asgp.2017.014 TRACE FOSSILS FROM THE BALTOSCANDIAN ERRATIC BOULDERS IN SW POLAND Alina CHRZĄSTEK & Kamil PLUTA Institute of Geological Sciences, Wrocław University; Maksa Borna 9, 50-204 Wrocław, Poland e-mails: [email protected], [email protected] Chrząstek, A. & Pluta, K, 2017. Trace fossils from the Baltoscandian erratic boulders in SW Poland. Annales Societatis Geologorum Poloniae, 87: 229–257. Abstract: Many well preserved trace fossils were found in erratic boulders and the fossils preserved in them, occurring in the Pleistocene glacial deposits of the Fore-Sudetic Block (Mokrzeszów Quarry, Świebodzice outcrop). They include burrows (Arachnostega gastrochaenae, Balanoglossites isp., ?Balanoglossites isp., ?Chondrites isp., Diplocraterion isp., Phycodes isp., Planolites isp., ?Rosselia isp., Skolithos linearis, Thalassinoides isp., root traces) and borings ?Gastrochaenolites isp., Maeandropolydora isp., Oichnus isp., Osprioneides kamp- to, ?Palaeosabella isp., Talpina isp., Teredolites isp., Trypanites weisei, Trypanites isp., ?Trypanites isp., and an unidentified polychaete boring in corals. The boulders, Cambrian to Neogene (Miocene) in age, mainly came from Scandinavia and the Baltic region. The majority of the trace fossils come from the Ordovician Orthoceratite Limestone, which is exposed mainly in southern and central Sweden, western Russia and Estonia, and also in Norway (Oslo Region). The most interesting discovery in these deposits is the occurrence of Arachnostega gastrochaenae in the Ordovician trilobites (?Megistaspis sp. and Asaphus sp.), cephalopods and hyolithids. This is the first report ofArachnostega on a trilobite (?Megistaspis) from Sweden. So far, this ichnotaxon was described on trilobites from Baltoscandia only from the St. -
Mcabee Fossil Site Assessment
1 McAbee Fossil Site Assessment Final Report July 30, 2007 Revised August 5, 2007 Further revised October 24, 2008 Contract CCLAL08009 by Mark V. H. Wilson, Ph.D. Edmonton, Alberta, Canada Phone 780 435 6501; email [email protected] 2 Table of Contents Executive Summary ..............................................................................................................................................................3 McAbee Fossil Site Assessment ..........................................................................................................................................4 Introduction .......................................................................................................................................................................4 Geological Context ...........................................................................................................................................................8 Claim Use and Impact ....................................................................................................................................................10 Quality, Abundance, and Importance of the Fossils from McAbee ............................................................................11 Sale and Private Use of Fossils from McAbee..............................................................................................................12 Educational Use of Fossils from McAbee.....................................................................................................................13 -
The Mesozoic Corals. Bibliography 1758-1993
June, 1, 2017 The Mesozoic Corals. Bibliography 1758-1993. Supplement 22 ( -2016) Compiled by Hannes Löser1 Summary This supplement to the bibliography (published in the Coral Research Bulletin 1, 1994) contains 18 additional references to literary material on the taxonomy, palaeoecology and palaeogeography of Mesozoic corals (Triassic - Cretaceous; Scleractinia, Octocorallia). The bibliography is available in the form of a data bank with a menu-driven search program for Windows-compatible computers. Updates are available through the Internet (www.cp-v.de). Key words: Scleractinia, Octocorallia, corals, bibliography, Triassic, Jurassic, Cretaceous, data bank Résumé Le supplément à la bibliographie (publiée dans Coral Research Bulletin 1, 1994) contient 18 autres références au sujet de la taxinomie, paléoécologie et paléogéographie des coraux mesozoïques (Trias - Crétacé; Scleractinia, Octocorallia). Par le service de mise à jour (www.cp-v.de), la bibliographie peut être livrée sur la base des données avec un programme de recherche contrôlée par menu avec un ordinateur Windows-compatible. Mots-clés: Scleractinia, Octocorallia, coraux, bibliographie, Trias, Jurassique, Crétacé, base des données Zusammenfassung Die Ergänzung zur Bibliographie (erschienen im Coral Research Bulletin 1, 1994) enthält 18 weitere Literaturzitate zur Taxonomie und Systematik, Paläoökologie und Paläogeographie der mesozoischen Korallen (Trias-Kreide; Scleractinia, Octocorallia). Die Daten sind als Datenbank zusammen mit einem menügeführten Rechercheprogramm für Windows-kompatible Computer im Rahmen eines Ände- rungsdienstes im Internet (www.cp-v.de) verfügbar. Schlüsselworte: Scleractinia, Octocorallia, Korallen, Bibliographie, Trias, Jura, Kreide, Datenbank 1 Estación Regional del Noroeste, Instituto de Geología, Universidad Nacional Autónoma de México, Hermosillo, Sonora, México; [email protected] © CPESS VERLAG 2017 • http://www.cp-v.de/crb • [email protected] 3 extremely rare. -
Late Jurassic Reef Bioerosion – the Dawning of a New Era
Late Jurassic reef bioerosion – the dawning of a new era MARKUS BERTLING Bertling, M.: Late Jurassic reef bioerosion - the dawning of a new era. Bulletin of the Geological Society of Denmark, Vol. 45, pp. 173–176. Copenhagen 1999– 01–30. Coral reefs of the Late Jurassic (Oxfordian) in northern Germany and France have a style of bioerosion that is closer to that of Late Triassic reefs than of modern ones. Boring sponges played minor roles here but gradually became more important in more southerly regions during the Tithonian. This is likely to be linked to a falling sea-level whose increased nutrient input triggered microbial growth in shallow water. With sponges feeding on microbes, the Late Jurassic was the time of a change to modern borer associations in reefs. Key words: Bioerosion, reefs, Jurassic, nutrients, sponges. M. Bertling [[email protected]], Geologisch-Paläontologisches Museum, Pferdegasse 3, D - 48143 Münster, Germany. 1 September 1998. The bioerosion of modern reefs is characterised by vironment has been documented before (Bertling the prevalent action of grazing sea urchins and fishes; 1993; Bertling & Insalaco 1998). The study sites (Fig. clionid sponges generally are the most important 1) are similar in depth (0–20 m) as well as climatic, macroborers, with lithophagine bivalves and micro- nutrient and salinity conditions but represent various polychaetes being locally abundant (e.g. Hutchings environments regarding water energy and sedimenta- 1986). Neither Lithophaginae nor sponges of the fam- tion (including turbidity): a high-energy coral-micro- ily Clionidae (or related forms) have been reported bial reef (Novion-Porcien NP), an occurrence within from reefs older than Late Triassic age (own observa- permanently turbulent water with slight intermittent tions); and grazing reef fish families only originated (storm) sedimentation (Luchsholklippe LU), a deep- in the Eocene (Bellwood 1996). -
Paleoecology ...Of ... Reefs from the Late Jurassic
Project: Le “Vergleichende Palokologie und Faziesentwicklung oberjurassischer Riffstrukturen des westlichen Tethys-Nordrandes * und des Lusitanischen Beckens (Zentraiportugal)/E, Project Leader: R. Leinfelder (Stuttgart) . Paleoecology, Growth Parameters and Dynamics of Coral, Sponge and Microbolite Reefs from the Late Jurassic Reinhold R. Werner, Martin Nose, Dieter U. Schmid, Laternser, Martin Takacs & Dorothea Area of Study: Portugal, Spain, Southern Germany, France, Poland Environment: Shallow to deep carbonate platforms Stratigraphy: Late Jurassic Organisms: Corals, siliceous sponges, microbes, microen- crusters Depositional Setting: Brackish-lagoonal to deep ramp set- tings Constructive Processes: Frame-building, baffling and binding (depending on reef type and type of reef- building organisms) Destructive Processes: Borings by bivalves and sponges; wave action Preservation: Mostly well preserved Research Topic: Comparative facies analysis and paleo- ecology of Upper Jurassic reefs, reef organisms and communities Spongiolitic facies Fig. I: Distribution of Upper Jurassic reefs studied in detail. Abstract framework and pronounced relief whenever microbolite crusts provided stabilization. Reefs in steepened slope set- Reefs from the Late Jurassic comprise various types of tings are generally rich in microbolites because of bypass coral reefs, siliceous sponge reefs and microbolite reefs. possibilities for allochthonous sediment. Reef rimmed shal- Upper Jurassic corals had a higher ratio of heterotrophic low-water platforms did occur but only developed on pre- versus autotrophic energy uptake than modern ones, which existing uplifts. Upper Jurassic sponge-microbolite mud explains their frequent occurrence in terrigenous settings. mounds grew in subhorizontal mid to outer ramp settings Coral communities changed along a bathymetric gradient and reflect a delicate equilibrium of massive and peloidal but sedimentation exerted a stronger control on diversities microbolite precipitation and accumulation of allochthonous than bathymetry. -
Newsletter Number 86
The Palaeontology Newsletter Contents 86 Editorial 2 Association Business 3 Outreach and Education Grants 27 Association Meetings 28 From our correspondents Darwin’s diffidence 33 R for palaeontologists: Introduction 2 40 Future meetings of other bodies 48 Meeting Reports 55 Obituary Dolf Seilacher 64 Sylvester-Bradley reports 67 Outside the Box: independence 80 Publicity Officer: old seas, new fossils 83 Book Reviews 86 Books available to review 90 Palaeontology vol 57 parts 3 & 4 91–92 Special Papers in Palaeontology 91 93 Reminder: The deadline for copy for Issue no 87 is 13th October 2014. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 86 2 Editorial You know you are getting pedantic when you find yourself reading the Constitution of the Palaeontological Association, but the third article does serve as a significant guide to the programme of activities the Association undertakes. The aim of the Association is to promote research in Palaeontology and its allied sciences by (a) holding public meetings for the reading of original papers and the delivery of lectures, (b) demonstration and publication, and (c) by such other means as the Council may determine. Council has taken a significant step under categories (b) and (c) above, by committing significant funds, relative to spending on research and travel, to Outreach and Education projects (see p. 27 for more details). This is a chance for the membership of the Association to explore a range of ways of widening public awareness and participation in palaeontology that is led by palaeontologists. Not by universities, not by research councils or other funding bodies with broader portfolios. -
A Review of Paleobotanical Studies of the Early Eocene Okanagan (Okanogan) Highlands Floras of British Columbia, Canada and Washington, USA
Canadian Journal of Earth Sciences A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) Highlands floras of British Columbia, Canada and Washington, USA. Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2015-0177.R1 Manuscript Type: Review Date Submitted by the Author: 02-Feb-2016 Complete List of Authors: Greenwood, David R.; Brandon University, Dept. of Biology Pigg, KathleenDraft B.; School of Life Sciences, Basinger, James F.; Dept of Geological Sciences DeVore, Melanie L.; Dept of Biological and Environmental Science, Keyword: Eocene, paleobotany, Okanagan Highlands, history, palynology https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 70 Canadian Journal of Earth Sciences 1 A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) 2 Highlands floras of British Columbia, Canada and Washington, USA. 3 4 David R. Greenwood, Kathleen B. Pigg, James F. Basinger, and Melanie L. DeVore 5 6 7 8 9 10 11 Draft 12 David R. Greenwood , Department of Biology, Brandon University, J.R. Brodie Science 13 Centre, 270-18th Street, Brandon, MB R7A 6A9, Canada; 14 Kathleen B. Pigg , School of Life Sciences, Arizona State University, PO Box 874501, 15 Tempe, AZ 85287-4501, USA [email protected]; 16 James F. Basinger , Department of Geological Sciences, University of Saskatchewan, 17 Saskatoon, SK S7N 5E2, Canada; 18 Melanie L. DeVore , Department of Biological & Environmental Sciences, Georgia 19 College & State University, 135 Herty Hall, Milledgeville, GA 31061 USA 20 21 22 23 Corresponding author: David R. Greenwood (email: [email protected]) 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 70 24 A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) 25 Highlands floras of British Columbia, Canada and Washington, USA. -
World Catalog of Fossil Cantharidae
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/317166287 World catalog of fossil Cantharidae Article · May 2017 CITATIONS READS 2 362 1 author: Fabrizio Fanti 36 PUBLICATIONS 86 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Studies of the world fossil Soldier Beetles (Cantharidae) View project All content following this page was uploaded by Fabrizio Fanti on 26 May 2017. The user has requested enhancement of the downloaded file. Gruppo Umbro Mineralogico Paleontogico Special Issue World catalog of fossil Cantharidae N° 2/2017 Fossils & minerals index World Catalog of foSSIl CantharIdaE Fabrizio FANTI Pag 1 Cover: Cantharidae. Amber. Photo courtesy of Artur R. Michalski Editorial Boarding Chief: Boccali Roldano Balocchi Pamela Calzolari Prospero Famiani Federico Giorgi Maria Pia Nessi Enrico Partenzi Chiara Sensi Claudio Tassi Luca Scientific commitee: Bogni Giorgio Venturi Federico Biagini Publio Carlini Rossano Tipography : Tipolito Properzio Adresse : Via dei Carrettieri, 12 - 06081 Località: Santa Maria degli Angeli - ASSISI - PERUGIA Italia Authorization No. 17 of 2 November 2016 - Court of Perugia Fossils & minerals World Catalog of foSSIl CantharIdaE Fabrizio FANTI [email protected] abstract acknowledgements A catalogue and bibliography of the world fossil Cantharidae are I am grateful to: Susana Adamonis and Cecilia Soledad given. Rhagonycha germari (Heer, 1847) n. comb., Rhagonycha Cataldo (Buenos Aires University), Vitalii I. Alekseev, Clive tertiaria (Heer, 1847) n. comb. and Rhagonycha hesperus A. Auton, Gabriel Biffi (Brazil), Albertas Bitinas (Klaipėda (Wickham, 1914) n. comb. are transferred from Telephorus University - Lithuania), Guido Bonamie (Merendree - Belgium), Schaeffer, 1766 = Cantharis Linnaeus, 1758 to Rhagonycha Jan Bosselaers, Christopher J. -
A New Coral Fauna from the Campanian of Northern Spain (Torallola Village, Prov
Geol. Paläont. Mitt. Innsbruck, ISSN 0378-6870, Band 23, S. 127-191, 1998 A NEW CORAL FAUNA FROM THE CAMPANIAN OF NORTHERN SPAIN (TORALLOLA VILLAGE, PROV. LLEIDA) Rosemarie C. Baron-Szabo With 4 figures, 5 tables and 12 plates Abstract: A new coral fauna is described from the Puimanyons Olisthostrome Member of the Vallcarga Formation (Campanian) in the Torallola area, north Spain. Taxonomic diversity is emphasized by the appearance of 36 genera belonging to 2 orders and 9 suborders. Four species are new: Placophyllia bandeli n. sp., Barysmilia iberica n. sp., Latohelia circularia n. sp., and Gyrodendron leptonema n. sp.. Within the European Province the coral fauna from Torallola represents one of its most complex Campanian coral communities. Zusammenfassung: Vom Puimayons Olisthostrom Member der Vallcarga Formation (Campan), bei Torallola, Nordspanien, wird erstmalig eine Korallenfauna beschrieben. Ihre taxonomische Diversität wird durch das Auftreten von 36 Gattungen, welche 2 Ordnungen und 9 Unterordnungen entstammen, aufgezeigt. Vier Arten werden neu beschrieben: Placophyllia bandeli n. sp., Barysmilia iberica n. sp., Latohelia circularia n. sp. und Gyrodendron leptonema n. sp.. Innerhalb der europäischen Provinz stellt die Korallenfauna von Torallola eine der komplexesten Korallenvergesellschaftungen des Campan dar. 1. Introduction Cretaceous have been reported, mainly of Turon- ian to Santonian or Maastrichtian age (e.g. BA- In the European Province (BARON-SZABO, TALLER, 1936, 1937; ROSELL, 1967; PONS, 1973; 1997) during the Late Cretaceous coral assem- VIDAL, 1980; REIGORIOL, 1989,1992). blages became more and more restricted to local- This paper presents data complementary to that ities in central and southern regions (e.g. TURNSEK, of the working group of K. -
Evolutionary Trends in the Epithecate Scleractinian Corals
Evolutionary trends in the epithecate scleractinian corals EWA RONIEWICZ and JAROSEAW STOLARSKI Roniewicz, E. & Stolarski, J. 1999. Evolutionary trends in the epithecate scleractinian corals. -Acta Palaeontologica Polonica 44,2, 131-166. Adult stages of wall ontogeny of fossil and Recent scleractinians show that epitheca was the prevailing type of wall in Triassic and Jurassic corals. Since the Late Cretaceous the fre- quency of epithecal walls during adult stages has decreased. In the ontogeny of Recent epithecate corals, epitheca either persists from the protocorallite to the adult stage, or is re- placed in post-initial stages by trabecular walls that are often accompanied by extra- -calicular skeletal elements. The former condition means that the polyp initially lacks the edge zone, the latter condition means that the edge zone develops later in coral ontogeny. Five principal patterns in wall ontogeny of fossil and Recent Scleractinia are distinguished and provide the framework for discrimination of the four main stages (grades) of evolu- tionary development of the edge-zone. The trend of increasing the edge-zone and reduction of the epitheca is particularly well represented in the history of caryophylliine corals. We suggest that development of the edge-zone is an evolutionary response to changing envi- ronment, mainly to increasing bioerosion in the Mesozoic shallow-water environments. A glossary is given of microstructural and skeletal terms used in this paper. Key words : Scleractinia, microstructure, thecal structures, epitheca, phylogeny. Ewa Roniewicz [[email protected]]and Jarostaw Stolarski [[email protected]], Instytut Paleobiologii PAN, ul. Twarda 51/55, PL-00-818 Warszawa, Poland. In Memory of Gabriel A.