Evolution of the Late Ordovician Plaesiomyid Brachiopod Lineage in Laurentia

Total Page:16

File Type:pdf, Size:1020Kb

Evolution of the Late Ordovician Plaesiomyid Brachiopod Lineage in Laurentia Western University Scholarship@Western Electronic Thesis and Dissertation Repository 10-19-2012 12:00 AM Evolution of the Late Ordovician Plaesiomyid Brachiopod Lineage in Laurentia Colin D. Sproat The University of Western Ontario Supervisor Dr. Jisuo Jin The University of Western Ontario Joint Supervisor Dr. Rong-yu Li The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Colin D. Sproat 2012 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Recommended Citation Sproat, Colin D., "Evolution of the Late Ordovician Plaesiomyid Brachiopod Lineage in Laurentia" (2012). Electronic Thesis and Dissertation Repository. 913. https://ir.lib.uwo.ca/etd/913 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. EVOLUTION OF THE LATE ORDOVICIAN PLAESIOMYID BRACHIOPOD LINEAGE IN LAURENTIA (Spine title: LATE ORDOVICIAN PLAESIOMYID BRACHIOPOD LINEAGE IN LAURENTIA) Thesis format: Integrated Article by Colin Sproat Graduate Program in Geology A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science The School of Graduate and Postdoctoral Studies The University of Western Ontario London, Ontario, Canada © Colin Sproat, 2012 THE UNIVERSITY OF WESTERN ONTARIO School of Graduate and Postdoctoral Studies CERTIFICATE OF EXAMINATION Supervisors Examiners ______________________________ ______________________________ Dr. Jisuo Jin Cam Tsujita ______________________________ ______________________________ Dr. Rong-yu Li Stephen Hicock ______________________________ Renbin Zhan The thesis by Colin David Sproat entitled: Evolution of the Late Ordovician Plaesiomyid Brachiopod Lineage in Laurentia is accepted in partial fulfillment of the requirements for the degree of Master of Science in Geology ______________________ _______________________________ Date Chair of the Thesis Examination Board ii Abstract During the Late Ordovician, a transgression flooded much of Laurentia. The fauna of these intracratonic basins became differentiated from the fauna of the pericratonic shelves and platforms, typically displaying gigantism and coarser shell ornamentation. In this study, 509 specimens from 11 species of the Plaesiomyidae brachiopod family from the Katian and Hirnantian were measured, of which 198 included in principal component analysis to quantify morphological changes over this interval. Three trends were revealed: 1) increasing globosity and dorsal convexity from the early to late Katian, 2) coarser, but fewer ribs on species from the paleoequatorial intracratonic seas compared to species from the mid- to high-tropical pericratonic shelves and platforms, and 3) enlargement of the cardinal process from early to late Katian and predominance of a trilobed cardinal process in the intracratonic species versus bilobed cardinal process in pericratonic species. Two new species were assigned, and two existing species were reassigned. Key Words: brachiopod, Plaesiomyidae, Late Ordovician, Katian, Hirnantian, evolution paleoecology, faunal gradient, paleobiogeography iii Acknowledgements I would first like to thank my supervisors, Dr. Jisuo Jin and Dr. Rong-yu Li, without whom I would not have been able to reach this point. Dr. Jin's support made the last two years much easier than they may have otherwise been. I always felt welcomed by stop by for a chat in his office, whether it was paleontology related or not. His professional guidance and personal support are appreciated, and I look forward to continuing to work with him in the future. Dr. Li may not have been as readily available, but was always only an email away, and the coffee and lunches while I was back in Brandon were always appreciated. Secondly, I would like to thank all my friends I have met here in London. As someone coming from another province, I appreciated being welcomed into the department by so many kind and considerate people. Even when things were getting tough, I could always count on the support of the many friends surrounding me. A special thanks to my roommate Emrah Yenier, not only for moral support, but also for his valuable skills with spreadsheets in Microsoft Excel. Thirdly, even though they were a province away, I would not have made it through this experience without the support of all my friends from back home in Manitoba. I may not have been able to see them everyday, but when we did get together they made it count. I always enjoyed their messages of support and even simple casual conversations. Last, but certainly not least, I thank my family. Although they didn't always understand why I was still in school after all these years, they always supported me in my decisions, and were a constant source of encouragement, and for that I will never be able to thank them enough. This research was funded by a grant from the Natural Science and Engineering Research Council to Dr. Jisuo Jin. I am grateful to Ed Dobrzanski for acting as our field guide in Manitoba. Paul Mayer of the Field Museum in Chicago, Illinois, kindly provided the specimens from the Ohio-Kentucky-Indiana tri-state area. Michelle Coyne of the Geological Survey of Canada kindly provided the Plaesiomys browni type specimens for examination. iv Table of Contents Title ……………………………………………………………………………………………… i Certificate of Examination ……………………………………………………………………. ii Abstract and Keywords ……………………………………………………………………….. iii Acknowledgements …………………………………………………………………………..... iv List of Tables ……………………………………………………………………………….….. ix List of Figures …………………………………………………………...……………………... x Chapter 1 – Introduction …………………………………………………………………….… 1 1.1 – Introduction ……………………………………………………………………………...… 1 1.2 – The Great Biodiversification Event ……………………………………………………….. 2 1.2.1 – Environmental Contributors …………………………………………………...… 7 1.2.1.1 – Tectonic activity ............................................ .................... 7 1.2.1.2 – Elevated atmospheric carbon dioxide levels ................................ 8 1.2.1.3 – High sea level ......................................................... .......... 8 1.2.1.4 – Phytoplankton blooms ................................................... ..... 10 1.2.1.5 – Calcite seas ................................................................... .. 11 1.2.1.6 – Superplume? ............................................................... .... 13 1.2.2 – Changes in biodiversity ………………………………………………………… 14 1.2.2.1 – The Cambrian fauna ................................................... ....... 14 1.2.2..2 – The Paleozoic fauna .......................................................... 15 1.2.2.3 – The Modern fauna ......................................................... ... 18 1.2.3 – Radiation of articulate brachiopods ………………………………………….… 18 1.2.3.1 – Strophomenata ................................................................ 19 1.2.3.2. – Rhynchonellata ........................................................... .... 21 1.2.3.3 – α, β, and γ brachiopod diversity ............................................................ 21 1.2.3.4 – Brachiopod faunal diversity in Laurentia .................................. 22 1.2.4 – Summary …………………………………………………………………….…. 23 1.3 – Terminal Ordovician mass extinction ……………………………………………………. 24 1.3.1 – Glacial trigger …………………………………………………………….….… 25 1.3.1.1 – Productivity hypothesis ...................................................... 26 v 1.3.1.2 – Weathering hypothesis ....................................................... 27 1.3.1.3 – Carbonate deposition and weathering hypothesis ........................ 28 1.3.1.4 – Volcanism hypothesis ...................................................... .. 28 1.3.1.5 – Discussion ............................................................... ...... 29 1.3.2 – Changes in diversity ………………………………………………………….… 30 1.3.3 – Change in articulate brachiopod diversity and faunas …………………………. 34 1.3.3.1 – Survival faunas ................................................................ 33 1.4 – Ordovician Paleogeography ……………………………………………………………… 34 1.4.1 – Baltica ………………………………………………………………………….. 34 1.4.2 – Siberia ………………………………………………………………………..… 36 1.4.3 – Gondwana ……………………………………………………………………… 36 1.4.4 – Oceans and sea level …………………………………………………………… 36 1.4.5 – Laurentia ……………………………………………………………………….. 37 1.4.5.1 – Sea level and Laurentia ................................................... ... 40 1.4.5.2 – Taconic orogeny ............................................................... 40 1.5 – Objectives of Current Research and Rationale for the Project ………………………...… 41 References ……………………………………………………………………………………… 44 Chapter 2 – Geological and Stratigraphic Setting ................................................. 58 2.1 – Introduction ………………………………………………………………………………. 58 2.2 – Lake Simcoe area, Ontario ……………………………………………………………..… 58 2.2.1 – Simcoe Group ………………………………………………………………….. 58 2.2.1.1 – Shadow Lake Formation ..................................................... 60 2.2.1.2 – Gull River Formation ......................................................... 60 2.2.1.3 – Bobcaygeon Formation .................................................... ... 61 2.2.1.4 – Verulam Formation
Recommended publications
  • Early Sponge Evolution: a Review and Phylogenetic Framework
    Available online at www.sciencedirect.com ScienceDirect Palaeoworld 27 (2018) 1–29 Review Early sponge evolution: A review and phylogenetic framework a,b,∗ a Joseph P. Botting , Lucy A. Muir a Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China b Department of Natural Sciences, Amgueddfa Cymru — National Museum Wales, Cathays Park, Cardiff CF10 3LP, UK Received 27 January 2017; received in revised form 12 May 2017; accepted 5 July 2017 Available online 13 July 2017 Abstract Sponges are one of the critical groups in understanding the early evolution of animals. Traditional views of these relationships are currently being challenged by molecular data, but the debate has so far made little use of recent palaeontological advances that provide an independent perspective on deep sponge evolution. This review summarises the available information, particularly where the fossil record reveals extinct character combinations that directly impinge on our understanding of high-level relationships and evolutionary origins. An evolutionary outline is proposed that includes the major early fossil groups, combining the fossil record with molecular phylogenetics. The key points are as follows. (1) Crown-group sponge classes are difficult to recognise in the fossil record, with the exception of demosponges, the origins of which are now becoming clear. (2) Hexactine spicules were present in the stem lineages of Hexactinellida, Demospongiae, Silicea and probably also Calcarea and Porifera; this spicule type is not diagnostic of hexactinellids in the fossil record. (3) Reticulosans form the stem lineage of Silicea, and probably also Porifera. (4) At least some early-branching groups possessed biminerallic spicules of silica (with axial filament) combined with an outer layer of calcite secreted within an organic sheath.
    [Show full text]
  • Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction
    Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction by Curtis R. Congreve B.S., University of Rochester, 2006 M.S., University of Kansas, 2008 Submitted to the Department of Geology and the Faculty of the Graduate School of The University of Kansas in partial fulfillment on the requirements for the degree of Doctor of Philosophy 2012 Advisory Committee: ______________________________ Bruce Lieberman, Chair ______________________________ Paul Selden ______________________________ David Fowle ______________________________ Ed Wiley ______________________________ Xingong Li Defense Date: December 12, 2012 ii The Dissertation Committee for Curtis R. Congreve certifies that this is the approved Version of the following thesis: Evolutionary Patterns of Trilobites Across the End Ordovician Mass Extinction Advisory Committee: ______________________________ Bruce Lieberman, Chair ______________________________ Paul Selden ______________________________ David Fowle ______________________________ Ed Wiley ______________________________ Xingong Li Accepted: April 18, 2013 iii Abstract: The end Ordovician mass extinction is the second largest extinction event in the history or life and it is classically interpreted as being caused by a sudden and unstable icehouse during otherwise greenhouse conditions. The extinction occurred in two pulses, with a brief rise of a recovery fauna (Hirnantia fauna) between pulses. The extinction patterns of trilobites are studied in this thesis in order to better understand selectivity of the
    [Show full text]
  • Church 18.Pdf (1.785Mb)
    Paleontological Contributions Number 18 Efficient Ornamentation in Ordovician Anthaspidellid Sponges Stephen B. Church August 9, 2017 Lawrence, Kansas, USA ISSN 1946-0279 (online) paleo.ku.edu/contributions Ridge-and-trough ornamented outer-wall fragment of the Ordovician anthaspidellid sponge Rugocoelia eganensis Johns, 1994. Paleontological Contributions August 9, 2017 Number 18 EFFICIENT ORNAMENTATION IN ORDOVICIAN ANTHASPIDELLID SPONGES Stephen B. Church Department of Geological Sciences, Brigham Young University, Provo, Utah 84602-3300, [email protected] ABSTRACT Lithistid orchoclad sponges within the family Anthaspidellidae Ulrich in Miller, 1889 include several genera that added ornate features to their outer-wall surfaces during Early Ordovician sponge radiation. Ornamented anthaspidellid sponges commonly constructed annulated or irregularly to regularly spaced transverse ridge-and-trough features on their outer-wall surfaces without proportionately increasing the size of their internal wall or gastral surfaces. This efficient technique of modi- fying only the sponge’s outer surface without enlarging its entire skeletal frame conserved the sponge’s constructional energy while increasing outer-wall surface-to-fluid exposure for greater intake of nutrient bearing currents. Sponges with widely spaced ridge-and-trough ornament dimensions predominated in high-energy settings. Widely spaced ridges and troughs may have given the sponge hydrodynamic benefits in high wave force settings. Ornamented sponges with narrowly spaced ridge-and- trough dimensions are found in high energy paleoenvironments but also occupied moderate to low-energy settings, where their surface-to-fluid exposure per unit area exceeded that of sponges with widely spaced surface ornamentations. Keywords: lithistid sponges, Ordovician radiation, morphological variation, theoretical morphology INTRODUCTION assumed by most anthaspidellids.
    [Show full text]
  • The Paleoecology and Biogeography of Ordovician Edrioasteroids
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 8-2011 The Paleoecology and Biogeography of Ordovician Edrioasteroids Rene Anne Lewis University of Tennessee - Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Paleontology Commons Recommended Citation Lewis, Rene Anne, "The Paleoecology and Biogeography of Ordovician Edrioasteroids. " PhD diss., University of Tennessee, 2011. https://trace.tennessee.edu/utk_graddiss/1094 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 Rene Anne Lewis entitled "The Paleoecology and Biogeography of Ordovician Edrioasteroids." 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 requirements for the degree of Doctor of Philosophy, with a major in Geology. Michael L. McKinney, Major Professor We have read this dissertation and recommend its acceptance: Colin D. Sumrall, Linda C. Kah, Arthur C. Echternacht Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) THE PALEOECOLOGY AND BIOGEOGRAPHY OF ORDOVICIAN EDRIOASTEROIDS A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville René Anne Lewis August 2011 Copyright © 2011 by René Anne Lewis All rights reserved.
    [Show full text]
  • Rare Middle and Upper Devonian Dalmanelloid (Orthida) of the Cantabrian Mountains, N Spain
    SPANISH JOURNAL OF PALAEONTOLOGY Rare Middle and Upper Devonian dalmanelloid (Orthida) of the Cantabrian Mountains, N Spain Jenaro L. GARCÍA-ALCALDE Departamento de Geología, Universidad de Oviedo, c/ Jesús Arias de Velasco s/n, 33005 Oviedo, Spain; [email protected] García-Alcalde, J.L. 2018. Rare Middle and Upper Devonian dalmanelloid (Orthida) of the Cantabrian Mountains, N Spain. [Formas raras de dalmaneloideos (Orthida) del Devónico Medio y Superior de la Cordillera Cantábrica, N España]. Spanish Journal of Palaeontology, 33 (1), 57-82. Manuscript received 3 October 2017 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 6 March 2018 ABSTRACT RESUMEN Rare Cantabrian Dalmanellidae (Costisorthis lisae nov. sp.), Se describen y fi guran por primera vez en España braquiópodos Dicoelosiidae (Teichertina cf. peregrina, T. cf. fi tzroyensis), órtidos inusuales de las familias Dalmanellidae (Costisorthis and Mystrophoridae (Mystrophora sp., Biernatium sucoi nov. lisae n. sp), Dicoelosiidae (Teichertina cf. peregrina y sp., and Biernatium sp. 2) are described and fi gured for the fi rst Teichertina cf. fi tzroyensis) y Mystrophoridae (Mystrophora time in Spain. Most of them are scarce forms that occur only in sp., Biernatium sucoi nov. sp. y Biernatium sp. 2). La mayoría certain localities. All the species but one came from the lower de ellos son escasos y aparecen en localidades puntuales. part of the Portilla (province of León) and Candás (province Todas las especies menos una proceden de la parte baja de of Asturias) formations, Faunal Interval 21, Polygnathus las formaciones Portilla (en León) y Candás (en Asturias), rhenanus/P. varcus conodont zone, middle Givetian. The Intervalo Faunístico 21, Biozona de Polygnathus rhenanus/P.
    [Show full text]
  • Chapter 2 Paleozoic Stratigraphy of the Grand Canyon
    CHAPTER 2 PALEOZOIC STRATIGRAPHY OF THE GRAND CANYON PAIGE KERCHER INTRODUCTION The Paleozoic Era of the Phanerozoic Eon is defined as the time between 542 and 251 million years before the present (ICS 2010). The Paleozoic Era began with the evolution of most major animal phyla present today, sparked by the novel adaptation of skeletal hard parts. Organisms continued to diversify throughout the Paleozoic into increasingly adaptive and complex life forms, including the first vertebrates, terrestrial plants and animals, forests and seed plants, reptiles, and flying insects. Vast coal swamps covered much of mid- to low-latitude continental environments in the late Paleozoic as the supercontinent Pangaea began to amalgamate. The hardiest taxa survived the multiple global glaciations and mass extinctions that have come to define major time boundaries of this era. Paleozoic North America existed primarily at mid to low latitudes and experienced multiple major orogenies and continental collisions. For much of the Paleozoic, North America’s southwestern margin ran through Nevada and Arizona – California did not yet exist (Appendix B). The flat-lying Paleozoic rocks of the Grand Canyon, though incomplete, form a record of a continental margin repeatedly inundated and vacated by shallow seas (Appendix A). IMPORTANT STRATIGRAPHIC PRINCIPLES AND CONCEPTS • Principle of Original Horizontality – In most cases, depositional processes produce flat-lying sedimentary layers. Notable exceptions include blanketing ash sheets, and cross-stratification developed on sloped surfaces. • Principle of Superposition – In an undisturbed sequence, older strata lie below younger strata; a package of sedimentary layers youngs upward. • Principle of Lateral Continuity – A layer of sediment extends laterally in all directions until it naturally pinches out or abuts the walls of its confining basin.
    [Show full text]
  • 59319647.Pdf
    Article "Stratigraphic and Structural Framework of Upper Middle Ordovician Rocks in the Head Lake- Burleigh Falls Area of South-Central Ontario" Bruce V. Sanford Géographie physique et Quaternaire, vol. 47, n° 3, 1993, p. 253-268. Pour citer cet article, utiliser l'information suivante : URI: http://id.erudit.org/iderudit/032956ar DOI: 10.7202/032956ar Note : les règles d'écriture des références bibliographiques peuvent varier selon les différents domaines du savoir. Ce document est protégé par la loi sur le droit d'auteur. L'utilisation des services d'Érudit (y compris la reproduction) est assujettie à sa politique d'utilisation que vous pouvez consulter à l'URI https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Érudit est un consortium interuniversitaire sans but lucratif composé de l'Université de Montréal, l'Université Laval et l'Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. Érudit offre des services d'édition numérique de documents scientifiques depuis 1998. Pour communiquer avec les responsables d'Érudit : [email protected] Document téléchargé le 12 février 2017 07:14 Géographie physique et Quaternaire, 1993, vol. 47, n° 3, p. 253-268, 15 fig. STRATIGRAPHIC AND STRUCTURAL FRAMEWORK OF UPPER MIDDLE ORDOVICIAN ROCKS IN THE HEAD LAKE- BURLEIGH FALLS AREA OF SOUTH- CENTRAL ONTARIO Bruce V. SANFORD, Independent Exploration Geologist,17 Meadowglade Gardens, Nepean, Ontario K2G 5J4. ABSTRACT Field investigations in the RÉSUMÉ Cadre stratigraphique et structu­ ZUSAM M EN FASSU NG Stratigraphischer Head Lake-Burleigh Falls area of south- ral des roches de l'Ordovicien moyen supé­ und struktureller Rahmen der Felsen aus central Ontario, that focused mainly on the rieur dans la région de Head Lake-Burleigh dem oberen mittleren Ordovizium in der Covey Hill(?), Shadow Lake, Gull River and Falls, au centre-sud de l'Ontario.
    [Show full text]
  • Save Hi-Res Pdf (0.76
    Paleobiology, 45(2), 2019, pp. 221–234 DOI: 10.1017/pab.2019.4 Dissecting the paleocontinental and paleoenvironmental dynamics of the great Ordovician biodiversification Franziska Franeck and Lee Hsiang Liow Abstract.—The Ordovician was a time of drastic biological and geological change. Previous work has suggested that there was a dramatic increase in global diversity during this time, but also has indicated that regional dynamics and dynamics in specific environments might have been different. Here, we contrast two paleocontinents that have different geological histories through the Ordovician, namely Laurentia and Baltica. The first was situated close to the equator throughout the whole Ordovician, while the latter has traversed tens of latitudes during the same time. We predict that Baltica, which was under long-term environmental change, would show greater average and interval-to-interval origination and extinction rates than Laurentia. In addition, we are interested in the role of the environment in which taxa originated, specifically, the patterns of onshore–offshore dynamics of diversification, where onshore and offshore areas represent high-energy and low-energy environments, respectively. Here, we predict that high-energy environments might be more conducive for originations. Our new analyses show that the global Ordovician spike in genus richness from the Dapingian to the Darriwilian Stage resulted from a very high origination rate at the Dapingian/Darriwilian boundary, while the extinction rate remained low. We found substantial interval-to-interval variation in the origin- ation and extinction rates in Baltica and Laurentia, but the probabilities of origination and extinction are somewhat higher in Baltica than Laurentia. Onshore and offshore areas have largely indistinguishable origination and extinction rates, in contradiction to our predictions.
    [Show full text]
  • The Great Ordovician Radiation of Marine Life: Examples from South China
    Available online at www.sciencedirect.com Progress in Natural Science 18 (2008) 1–12 Review The great Ordovician radiation of marine life: Examples from South China Renbin Zhan a,*, Jisuo Jin b, Yuandong Zhang a, Wenwei Yuan a a State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China b Department of Earth Sciences, University of Western Ontario, London Ont., Canada N6A 5B7 Received 14 March 2007; received in revised form 23 July 2007; accepted 27 July 2007 Abstract The Ordovician radiation is the earliest and most important biodiversification event in the evolution of the Paleozoic Evolutionary Fauna (PEF), when the basic framework of PEF was established. The radiation underwent a gradual, protracted process spanning more than 40 million years and was marked by several diversity maxima of the PEF. Case studies conducted on the Upper Yangtze Platform (South China Palaeoplate) showed that the Ordovician radiation was characterized by drastic increases in a- and b-diversity in various groups of organisms. During the radiation, brachiopods, trilobites, and graptolites of the PEF became more diverse to dominate over the Cambrian Evolutionary Fauna (CEF) in all marine environments. At either global or regional scales, however, the Ordovician radiation was highly heterogeneous in time and space, and the rate and pattern of radiation exhibited by different major fossil groups were also variable. Ó 2007 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved. Keywords: Ordovician radiation; Paleozoic Evolutionary Fauna; a-diversity; b-diversity; Upper Yangtze Platform 1.
    [Show full text]
  • The Eoorthid Brachiopod Apheoorthina in the Lower Ordovician of NW Argentina and the Dispersal Pathways Along Western Gondwana
    The eoorthid brachiopod Apheoorthina in the Lower Ordovician of NW Argentina and the dispersal pathways along western Gondwana DIEGO F. MUÑOZ and JUAN L. BENEDETTO Muñoz, D.F. and Benedetto, J.L. 2016. The eoorthid brachiopod Apheoorthina in the Lower Ordovician of NW Argentina and the dispersal pathways along western Gondwana. Acta Palaeontologica Polonica 61 (3): 633–644. The eoorthid brachiopod Apheoorthina is reported for the first time from the Lower Ordovician of NW Argentina. It is represented by a species similar to A. ferrigena from the Tremadocian of the Prague Basin, increasing the faunal af- finities between the Central Andean Basin and the South European microcontinents, in particular the Bohemian region (Perunica). Nine out of the fourteen brachiopod genera reported from the Tremadocian of the Central Andean Basin (~64%) are shared with the Mediterranean region, four of which (~28%) have been recorded in the Prague Basin, and two (Kvania and Apheoorthina) are restricted to the Central Andes and Perunica. Dispersal pathways around Gondwana are analyzed in the light of major factors affecting large-scale distribution of brachiopods (environment, larval capacity for dispersal, oceanic currents). The presence in Apheoorthina aff. ferrigena of a well-preserved larval protegulum measuring 420 μm in width and 210 μm in length strongly suggests that this species had planktotrophic larvae capable of long-distance dispersal. According to recent ocean-atmosphere general circulation models for the Ordovician Period, the Central Andean margin was dominated by the cold-water Antarctica Current. Despite the complex non-zonal pattern produced by current deflections around the peri-Gondwanan microcontinents, the general westward circulation sense favoured larval dispersal from the Andean region to North Africa, Avalonia, the Armorican Terrane Assemblage, and Perunica.
    [Show full text]
  • Combined Analysis of Extant Rhynchonellida (Brachiopoda) Using Morphological and Molecular Data
    Syst. Biol. 67(1):32–48, 2018 © The Author(s) 2017. Published by Oxford University Press, on behalf of the Society of Systematic Biologists. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. DOI:10.1093/sysbio/syx049 Advance Access publication May 8, 2017 Combined Analysis of Extant Rhynchonellida (Brachiopoda) using Morphological and Molecular Data ,∗ , DAV I D W. BAPST1 ,HOLLY A. SCHREIBER1 2, AND SANDRA J. CARLSON1 1Department of Earth and Planetary Sciences, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA; and 2Penn Dixie Fossil Park and Nature Reserve, 3556 Lakeshore Rd, Ste. 210 Blasdell, NY 14219, USA ∗ Correspondence to be sent to: Department of Earth and Planetary Sciences, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA; E-mail: [email protected]. Received 5 August 2016; reviews returned 14 October 2016; accepted 28 April 2017 Associate Editor: Ken Halanych Abstract.—Independent molecular and morphological phylogenetic analyses have often produced discordant results for certain groups which, for fossil-rich groups, raises the possibility that morphological data might mislead in those groups for which we depend upon morphology the most. Rhynchonellide brachiopods, with more than 500 extinct genera but only 19 extant genera represented today, provide an opportunity to explore the factors that produce contentious phylogenetic signal across datasets, as previous phylogenetic hypotheses generated from molecular sequence data bear little agreement with those constructed using morphological characters.
    [Show full text]
  • 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).
    [Show full text]