Phylum: Brachiopoda
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Shell Microstructures in Lopingian Brachiopods: Implications for Fabric Evolution and Calcification
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 123(3): 541-560. November 2017 SHELL MICROSTRUCTURES IN LOPINGIAN BRACHIOPODS: IMPLICATIONS FOR FABRIC EVOLUTION AND CALCIFICATION CLAUDIO GARBELLI State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, Jiangsu 210008, P.R. China. Dipartimento di Scienze della Terra A. Desio, Università di Milano, Via Mangiagalli 34, 20133 Milan, Italy. E-mail: [email protected] To cite this article: Garbelli C. (2017) - Shell microstructures in Lopingian brachiopods: implications for fabric evolution and calcification. Riv. It. Paleontol. Strat., 123(3): 541-560. Keywords: Rhynchonelliformea; Strophomenata; biomineralization; taxonomy; columnar layer. Abstract. The study of the shell microstructure of brachiopods is fundamental to understand their evolu- tionary history and their biomineralization process. Here, species of forty Lopingian brachiopods genera, represen- tative of twenty-seven different families, are investigated using the Scanning Electron Microscope. The investiga- ted specimens come from different paleogeographic localities in the Palaeotethys/Neotethys oceans. The studied brachiopods show a large variability of the shell fabric, which is mainly related to the organization of its structural units: laminae, fibers and columns, possibly crossed by pseudopunctae or punctae. For the Strophomenata, the laminar fabric of Productida is crossed by pseudopunctae with taleolae and the laminae are often organized in packages, with the blades oriented about perpendicular to each other; this feature is less evident in the laminar Or- thotetida, which bear pseudopunctae without taleoae. For the Rhynchonellata, fibrous fabrics are either impuctate in the Spiriferida, most Athyridida and Rhynchonellida, or with punctae, as observed in the Orthida, Terebratulida and in the Neoretziidae (Athyridida). -
Dimerelloid Rhynchonellide Brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland)
1661-8726/08/010203–20 Swiss J. Geosci. 101 (2008) 203–222 DOI 10.1007/s00015-008-1250-8 Birkhäuser Verlag, Basel, 2008 Dimerelloid rhynchonellide brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland) HEINZ SULSER & HEINZ FURRER * Key words: brachiopoda, Sulcirostra, Carapezzia, new species, Lower Jurassic, Austroalpine ABSTRACT ZUSAMMENFASSUNG New brachiopods (Dimerelloidea, Rhynchonellida) from Lower Jurassic Neue Brachiopoden (Dimerelloidea, Rhynchonellida) aus unterjurassischen (?lower Hettangian) hemipelagic sediments of the Swiss National Park in hemipelagischen Sedimenten (?unteres Hettangian) des Schweizerischen Na- south-eastern Engadine are described: Sulcirostra doesseggeri sp. nov. and tionalparks im südöstlichen Engadin werden als Sulcirostra doesseggeri sp. Carapezzia engadinensis sp. nov. Sulcirostra doesseggeri is externally similar to nov. und Carapezzia engadinensis sp. nov. beschrieben. Sulcirostra doesseggeri S. fuggeri (FRAUSCHER 1883), a dubious species, that could not be included in ist äusserlich S. fuggeri (FRAUSCHER 1883) ähnlich, einer zweifelhaften Spezies, a comparative study, because relevant samples no longer exist. A single speci- die nicht in eine vergleichende Untersuchung einbezogen werden konnte, weil men was tentatively assigned to Sulcirostra ?zitteli (BÖSE 1894) by comparison kein relevantes Material mehr vorhanden ist. Ein einzelnes Exemplar wird als of its external morphology with S. zitteli from the type locality. The partly Sulcirostra ?zitteli (BÖSE 1894) bezeichnet, im Vergleich mit der Aussenmor- silicified brachiopods are associated with sponge spicules, radiolarians and phologie von S. zitteli der Typuslokalität. Die teilweise silizifizierten Brachio- crinoid ossicles. Macrofossils are rare: dictyid sponges, gastropods, bivalves, poden waren mit Schwammnadeln, Radiolarien und Crinoiden-Stielgliedern crustaceans, shark teeth and scales of an actinopterygian fish. The Lower Ju- assoziiert. -
Did the Amalgamation of Continents Drive the End Ordovician Mass Extinctions?
Palaeogeography, Palaeoclimatology, Palaeoecology 311 (2011) 48–62 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Did the amalgamation of continents drive the end Ordovician mass extinctions? Christian M.Ø. Rasmussen a,b,⁎, David A.T. Harper b,c,1 a Center for Macroecology, Evolution and Climate, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark b Nordic Center for Earth Evolution (NordCEE), Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark c Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark article info abstract Article history: Global biodiversity has been punctuated throughout the Phanerozoic by extinction events that vary in their Received 27 January 2011 degree of intensity and devastation. The mass extinction event that occurred at the end of the Ordovician Received in revised form 11 July 2011 Period rapidly removed a wide range of species. Because taxonomic loss occurred during an ice age, this is Accepted 28 July 2011 believed to have initiated the extinctions and thus, these extinctions have often been viewed as a deep time Available online 5 August 2011 analogue to the loss in species diversity during the present day glacial interval. The current study, however, indicates that temperature – though arguably being a trigger – was not the sole reason for the crisis. Based on Keywords: fi Ordovician a large, bibliographic database of rhynchonelliform brachiopods that speci cally operates within very narrow Silurian time-slices where every locality has been precisely georeferenced for the Upper Ordovician–Lower Silurian Brachiopods interval, we show that the extinctions were not uniformly distributed, nor was the succeeding recovery. -
New Barremian Rhynchonellide Brachiopod from Serbia and The
New Barremian rhynchonellide brachiopod genus from Serbia and the shell microstructure of Tetrarhynchiidae BARBARA RADULOVIĆ, NEDA MOTCHUROVA−DEKOVA, and VLADAN RADULOVIĆ Radulović, B., Motchurova−Dekova, N., and Radulović, V. 2007. New Barremian rhynchonellide brachiopod from Ser− bia and the shell microstructure of Tetrarhynchiidae. Acta Palaeontologica Polonica 52 (4): 761–782. A new rhynchonellide brachiopod genus Antulanella is erected based on the examination of the external and internal morphologies and shell microstructure of “Rhynchonella pancici”, a common species in the Barremian shallow−water limestones of the Carpatho−Balkanides of eastern Serbia. The new genus is assigned to the subfamily Viarhynchiinae, family Tetrarhynchiidae. The shell of Antulanella is small to rarely medium−sized, subglobose, subcircular, fully costate, with hypothyrid rimmed foramen. The dorsal euseptoidum is much reduced. The dental plates are thin, ventrally diver− gent. The hinge plates are straight to ventrally convex. The crura possess widened distal ends, rarely raduliform or canaliform. The shell is composed of two calcitic layers. The secondary layer is fine fibrous, homogeneous built up of predominantly anisometric anvil−like fibres. Although data on the shell microstructure of post−Palaeozoic rhyncho− nellides are still incomplete, it is possible to distinguish two types of secondary layer: (i) fine fibrous typical of the superfamilies Rhynchonelloidea and Hemithiridoidea and (ii) coarse fibrous typical of the superfamilies Pugnacoidea, Wellerelloidea, and Norelloidea. The new genus Antulanella has a fine fibrous microstructure of the secondary layer, which is consistent with its allocation in the Hemithiridoidea. Antulanella pancici occurs in association with other brachi− opods showing strong Peritethyan affinity and close resemblance to the Jura fauna (= Subtethyan fauna). -
Permophiles International Commission on Stratigraphy
Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement -
New Record of Novocrania (Brachiopoda, Craniida) from Madeira, with Notes on Recent Brachiopod Occurrences in the Macaronesian Archipelagos
New record of Novocrania (Brachiopoda, Craniida) from Madeira, with notes on Recent brachiopod occurrences in the Macaronesian archipelagos ALAN LOGAN, PETER WIRTZ & FRANK SWINNEN Logan, A., P. Wirtz & F. Swinnen, 2007. New record of Novocrania (Brachiopoda, Craniida) from Madeira, with notes on Recent brachiopod occurrences in the Macaronesian archipelagos. Arquipélago. Life and Marine Sciences 24: 17-22. The inarticulated brachiopod Novocrania anomala (Müller) is recorded for the first time from Madeira Island, bringing the total of living species for that area to six. Updated comparisons of Recent brachiopod diversities between the Macaronesian archipelagos show similar values for Madeira, the Cape Verde Islands and the Azores but higher values for the Canary Islands. Comparisons are also made between shallow-water cave and crevice communities in Madeira, the Canary Islands and the Cape Verde Islands, where dense populations of one or two brachiopod species are thriving in cryptic habitats where competition for space and resources is presumably reduced. No such occurrences have yet been found in the Azores. Key words: brachiopods, cryptic habitats, Macaronesia, seamounts, check-list Alan Logan (e-mail: [email protected]), Department of Geology, University of New Brunswick, Saint John, N.B. E2L 4L5, Canada; Peter Wirtz, Centro de Ciências do Mar, Universidade do Algarve, PT-8000-117 Faro, Portugal; Frank Swinnen, Research Associate, Museu Municipal do Funchal (Madeira, Portugal) and Lutlommel 10, BE-3920 Lommel, Belgium. INTRODUCTION from 52 stations from six seamounts to the north- east of Madeira (SEAMOUNT 1) and by Zezina Logan (1993) summarized the state of knowledge (2006) from other localities, allowing an up-to- of the diversity, biogeographic affinities, date checklist to be compiled for the whole region bathymetric range and life habits of Recent (Table 1). -
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. -
The Macro-Structure of Modern and Fossil Brachiopod Archives Abstract Shells of Brachiopods Chemistry Proxy for Paleo-Environmen
The macro-structure of modern and fossil brachiopod archives Abstract Brachiopods, are not the dominant element in modern oceans, but were very common in the past. Over 12,000 species and 5,000 genera fossils have found and recognized. As high variation and longtime distribution in the Paleozoic ocean, brachiopods are very important tools for paleontology research. Moreover, owing to the unique features of shells, which may very hard withstanding post-depositional alteration, and be considered the very credible indicators of climate changes in the ancient oceans. Shells of brachiopods Brachiopods have two hard "valves" (or shells: ventral valve and dorsal valve) on the upper and lower surfaces, also be called “lamp shells” due to the curved shells of the class Terebratulida look rather like pottery oil-lamps. Based on the hinged tooth and socket arrangement between two valves, there are two major groups of brachiopods are recognized, articulate and inarticulate. From outside to inside, articulate brachiopod shells are generally composed of following representative shell layers: 1)a thin organic periostracum (rarely preserved in fossils); 2)a thin outer primary layer(rare except in extremely well-preserved fossil shells); 3)a thicker inner secondary layer(always present in fossils); 4)a tertiary layer(always absent except in specific order). (e.g., Armstrong, 1968; Williams, 1968, 1997; Grossman et al., 1993; Azmy et al., 1998, 2006) Different kinds of brachiopods will have very different fabrics and structure of the layers, especially in the secondary layer. (Williams, 1997) Detailed different kinds secondary layer have described in (Williams, 1997): 1) organophosphatic lamination; 2) calcitic fabrics; 3) calcitic fibers; 4) calcitic tabular lamination; 5) calcitic cross-bladed lamination. -
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park By Linda Sue Lassiter1, Justin S. Tweet2, Frederick A. Sundberg3, John R. Foster4, and P. J. Bergman5 1Northern Arizona University Department of Biological Sciences Flagstaff, Arizona 2National Park Service 9149 79th Street S. Cottage Grove, Minnesota 55016 3Museum of Northern Arizona Research Associate Flagstaff, Arizona 4Utah Field House of Natural History State Park Museum Vernal, Utah 5Northern Arizona University Flagstaff, Arizona Introduction As impressive as the Grand Canyon is to any observer from the rim, the river, or even from space, these cliffs and slopes are much more than an array of colors above the serpentine majesty of the Colorado River. The erosive forces of the Colorado River and feeder streams took millions of years to carve more than 290 million years of Paleozoic Era rocks. These exposures of Paleozoic Era sediments constitute 85% of the almost 5,000 km2 (1,903 mi2) of the Grand Canyon National Park (GRCA) and reveal important chronologic information on marine paleoecologies of the past. This expanse of both spatial and temporal coverage is unrivaled anywhere else on our planet. While many visitors stand on the rim and peer down into the abyss of the carved canyon depths, few realize that they are also staring at the history of life from almost 520 million years ago (Ma) where the Paleozoic rocks cover the great unconformity (Karlstrom et al. 2018) to 270 Ma at the top (Sorauf and Billingsley 1991). The Paleozoic rocks visible from the South Rim Visitors Center, are mostly from marine and some fluvial sediment deposits (Figure 5-1). -
Appendix 7.4: Functional Diversity of Marine Ecosystems After the Late Permian Mass Extinction Event
University of Plymouth PEARL https://pearl.plymouth.ac.uk 04 University of Plymouth Research Theses 01 Research Theses Main Collection 2015 Palaeoecology of the late Permian mass extinction and subsequent recovery Foster, William J. http://hdl.handle.net/10026.1/5467 Plymouth University All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Appendix 7.4: Functional diversity of marine ecosystems after the Late Permian mass extinction event Mode of Life assignments Table S1: Mode of Life assignments. In the functional columns each number corresponds to the model in Bambach et al. (S1), where for Tiering: 2 = erect; 3 = surficial; 4 = semi-infaunal; 5 = shallow infaunal; 6 = deep infaunal; for Motility: 1 = fast motile; 2 = slow motile; 3 = facultatively motile, unattached; 4 = facultatively motile, attached; 5 = stationary, unattached; 6 = stationary, attached; and for Feeding: 1 = suspension feeder; 2 = deposit feeder; 3 = miner; 4 = grazer; 5 = predator; 6 = other (i.e. chemosymbiosis). -
An Annotated Checklist
Biodiversity Data Journal 4: e8169 doi: 10.3897/BDJ.4.e8169 Taxonomic Paper Brachiopoda of Greece: an annotated checklist Vasilis Gerovasileiou‡‡, Nicolas Bailly ‡ Institute of Marine Biology, Biotechnology and Aquaculture, Hellenic Centre for Marine Research, Heraklion, Greece Corresponding author: Vasilis Gerovasileiou ([email protected]) Academic editor: Christos Arvanitidis Received: 18 Feb 2016 | Accepted: 17 Jul 2016 | Published: 01 Nov 2016 Citation: Gerovasileiou V, Bailly N (2016) Brachiopoda of Greece: an annotated checklist. Biodiversity Data Journal 4: e8169. https://doi.org/10.3897/BDJ.4.e8169 Abstract Background Until today, only scattered species records of Brachiopoda from Greece have been included in publications on the Mediterranean brachiopod fauna. These records were mostly based on material collected during marine expeditions in the eastern Mediterranean decades ago, while few recent additional records appear in ecological studies. The aim of this paper was to give the first checklist of brachiopod species of Greece, in the framework of the Greek Taxon Information System (GTIS) initiative of the LifeWatchGreece Research Infrastructure (ESFRI), by reviewing the existing literature. New information Twelve brachiopod species have been found in Greek waters so far. The nomenclature, distribution, fossil records, ecology, and literature sources are discussed for each species. Keywords Aegean Sea, Sea of Crete, Levantine Sea, Ionian Sea, Eastern Mediterranean © Gerovasileiou V, Bailly N. This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 2 Gerovasileiou V, Bailly N Introduction Until Logan’s revision of the Mediterranean Brachiopoda (Logan 1979), several records of their extant taxa from the eastern Mediterranean were scattered in old publications on molluscs and in general benthic studies (see Logan et al. -
Jméno a Příjmení Autora: Dominik Rubeš
MASARYKOVA UNIVERZITA V BRNĚ Přírodovědecká fakulta Paleontologické nálezy z lokality Hrádok Michal Seko Bakalárska práca Vedúca práce: RNDr. Nela Doláková, CSc. Brno 2009 © 2009 Michal Seko Všetky práva vyhradené Meno a priezvisko autora: Michal Seko Názov diplomovej (bakalárskej) práce: Paleontologické nálezy z lokality Hrádok Názov v angličtine: Paleontological findings from locality Hrádok Študijný program: Geológia Študijný odbor (smer), kombinácia oborov: Geológia Vedúca diplomovej (bakalárskej) práce: RNDr. Nela Doláková, CSc. Rok obhajoby: 2009 Anotácia v slovenčine V práci sú zhrnuté aktuálne poznatky o najkomplikovanejšej geologickej stavbe na Slovensku - bradlovom pásme. Zároveň obsahuje prehľad uskutočnených paleontologických výskumov vytipovaných lokalít regiónu stredného Považia s dôrazom na litostratigrafickú príbuznosť v rámci čorštynskej jednotky, ktorej súčasťou je pribrežný strednojurský krinoidový komplex - lokalita Hrádok. Následné spracovanie vlastných paleontologických nálezov z uvedenej lokality, ktoré je hlavnou témou práce priamo nadväzuje na doterajšie geologické a paleontologické výskumy a ponúka rozšírený pohľad na strednojurskú biocenózu uloženú v sedimentoch. Anotácia v angličtine Current knowledge and information on the most complicated geological formation in Slovakia – Pieniny Klippen Belt is summarized in this work. At the same time it contains an overview of the paleontological research of the selected localities of Middle Považie region, stressing the litostratigrafic affinity within the Czorsztyn