Quantitative Untersuchungen an Rhaetina Gregaria (Suess) (Brachiopoda) 3-35 © Biodiversity Heritage Library

Total Page:16

File Type:pdf, Size:1020Kb

Quantitative Untersuchungen an Rhaetina Gregaria (Suess) (Brachiopoda) 3-35 © Biodiversity Heritage Library ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Zitteliana - Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Histor. Geologie Jahr/Year: 1974 Band/Volume: 3 Autor(en)/Author(s): Klören Christoph Artikel/Article: Quantitative Untersuchungen an Rhaetina gregaria (Suess) (Brachiopoda) 3-35 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 3 ZITTELIANA 3 3—35 München, 1. 10. 1974 Quantitative Untersuchungen an Rhaetina gregaria (Suess ) (Brachiopoda) Von CHRISTOPH KLÖREN1) Mit 31 Abbildungen und Tafeln 1—5 Zusammenfassung Am Beispiel einer rätisdien Terebratuliden-Fauna 5. Die Bildung von Quotienten y/x oder x/y (wenn (Bradiiopoda) werden quantitative Untersuchungs­ y = ax), bzw. nach Translation von Originaldaten techniken diskutiert und durchgeführt. die Bildung von Tangens oder Cotangens, ist dann gleichermaßen sinnvoll, wenn eine Schichtung der Methodische Ergebnisse Population nach dem relativen Alter nicht vorge­ 1 . Die für eine optimale Stichprobe geltenden Homo­ nommen wurde. Erfolgte eine Schichtung, so sind genitätskriterien können im Rahmen paläontologi- die Daten, die das relative Alter repräsentieren, im scher Stichproben nur näherungsweise erfüllt wer­ Nenner des Quotientenbruches zu führen. den, da die Inhomogenität bewirkenden Faktoren 6. Die Schätzung von Korrelationskoeffizienten für in Ausmaß und Richtung ihrer Wirksamkeit nur die ontogenetisch veränderten Merkmalspaare einer noch theoretisch, nicht aber konkret und damit eli­ Population liefert keine sinnvoll interpretierbaren minierbar zu erfassen sind. Ergebnisse. 2. Werden zum Zwecke der formalen Ausschaltung der ontogenetischen Variabilität aus den Indivi- Faunistische Ergebnisse duen-Daten (x u. y) einer paarigen Meßreihe Quo­ 1 . Die analysierten Individuen gehören den Arten tienten y/x gebildet, so sind diese vom ontogene­ Rhaetina gregaria (Suess ) und Rhaetina pyriformis tischen Zustand der Daten liefernden Individuen (Suess ) an. unabhängig, wenn das mittlere relative Wachstum der Population einer Geradegleichung der allge­ 2. Beide Populationen sind als „life assemblages“ im meinen Form y = ax folgt. Sinne Boucot ’s aufzufassen. Quotienten, die aus den Individuendaten einer Po­ 3. Die qualitative Differenzierung der beiden Popula­ pulation gebildet werden, deren relatives Wachstum tionen gelingt bei Individuen ab etwa 14 mm Län­ durch die allgemeine Gleichung y = ax + b oder ge. Eine Unterscheidung kleinerer Formen ist nur y = ax — b beschrieben werden kann, sind vom formal auf quantitativem Wege durchführbar. ontogenetischen Zustand der Daten liefernden Indi­ 4. Der Brachialapparat der Individuen von Rhaetina viduen abhängig. Solche Quotienten liefern daher gregaria (Suess ) erfährt eine Metamorphose. keine sinnvoll interpretierbaren Verteilungen. 3. Populationen, die durch Geraden der allgemeinen 5. Im Anschluß an die Metamorphose des Brachial­ Form y = ax + b bzw. y = ax — b beschrieben apparates von Rhaetina gregaria (Suess ) spaltet werden können, müssen durch Translation der Ori­ sich die Population in zwei quantitativ ermittelte ginaldaten in die allgemeine Form y = ax gebracht Teilkollektive auf, die sich zahlenmäßig etwa wie werden. Die aus den translatierten Originaldaten 1:1 verhalten. Es wird Sexual-Dimorphismus ver­ zu bildenden Quotienten sind als Tangens-Werte mutet. aufzufassen. 6. Alle gemessenen Daten, bzw. die aus ihnen errech- 4. An Populationen, deren mittleres relatives Wachs­ neten Kennwerte, haben primär nur Gültigkeit für tum einer gekrümmten Linie folgt, ist Schichtung die fossile Fauna, von der sie genommen wur­ dermaßen nach dem relativen Individualalter (z. den. Sie können, müssen aber nicht den quantitati­ B. x) vorzunehmen, daß die Schichten Teilabschnit­ ven „Zustand“ der Fauna vor ihrer Einbettung und te annähernd linearen Wachstums darstellen. Fossilisierung wiedergeben. ') Dr. Ch . Klören , 810 Blvd. Campbell, Chibougamau, P. Q., Canada. © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 4 Summary Using a Rhaetian Terebratulid fauna (Brachiopoda) as an 5. The construction of the quotients y /x or x/y (if y = ax), example, quantitative investigation techniques are discussed or respectively the construction of tangents or cotangents and applied. after transposing original data, is equally correct if the grouping of the population according to relative age is Theoretical Results not undertaken. If the data, representing relative age 1. The criteria of homogenity in obtaining an optimal are grouped, they are placed in the denominator of the random sample can only be approximately fulfilled in fraction. the framework of paleontological random sampling, be­ 6. The evaluation of correlation coefficients for the onto- cause the factors which produce inhomogenity, as far as genitically changed characteristic pairs of a population their effectivity (dimension and direction) is concerned, do not deliver rationally interpretable results. can only be realized theoretically, but cannot be concre­ tely eliminated. Faunistical Results 2. The quotient y lx, constructed from the individual data 1. The analysed individuals belong to the species Rhaetina (x and y) is independent of the ontogenetic state of those gregaria (Suess ) and Rhaetina pyriformis (Suess ). individuals as long as the average relative growth of the 2. Both of these populations are to be considered „life population adheres to a linear equation having the gene­ assemblages" after Boucot . ral form y = ax. When the relative growth of a popu­ lation can be described by the general equation y = ax 3. Qualitative différenciation of individuals larger than + b or y = ax —b, the quotients, constructed from data about 14 mm is possible in both populations. Smaller derived from the individuals, are dependent upon the forms can only be distinguished by formal quantitative ontogenetic state of development of the individuals de­ means. livering the data. Therefore, such quotients do not re­ 4. The brachial apparatus of Rhaetina gregaria (Suess ) un­ flect rationally interpretable distributions. dergoes metamorphosis. 3. The original data of populations, which can be described 5. Following the metamorphosis of the brachial apparatus by the general equation y = ax + b or y = ax —b, of Rhaetina gregaria (Suess ), this population splits up must be transposed into the form y = ax. The quotients into two, quantitatively distinct, collectives in a 1 : 1 which are formed from the transposed original data are proportion. Sexual dimorphism is supposed. to be considered as tangent values. 6. All measured data, and respectively the index values 4. When the average relative growth describes a curve, the calculated there from, have validity only for the fossile population is to be grouped according to the relative age fauna from which they were derived. These data may, of the individuals (e. g. x), so that the single groups but must not necessarilly, reflect upon the quantitative approximately represent linear growth. state of the fauna before its burial and fossilisation. Inhalt Vorwort ........................................................................................................................................ 5 1. E inleitung................................................................................................................................... 5 2. M e th o d ik ................................................................................................................................... 6 2.1 Homogenität .................................................................................................................... 6 2.2 Das relative W achstum ..................................................................................................... 9 2.3 Q u o tie n te n ......................................................................................................................... 10 2.4 T a n g e n s .............................................................................................................................. 11 2.5 Nichtlineares relatives Wachstum im Rahmen des tg -K o n zep tes .............................. 12 2.6 Test auf Normalverteilung ........................................................................................... 14 2.7 Zerlegung von Misch Verteilungen ................................................................................. 15 2.8 K o rrelatio n ......................................................................................................................... 15 3. Das qualitative Erscheinungsbild der Terebratuliden-Fauna ............................................. 16 3.1 Rhaetina gregaria (Suess ), 1854 ...................................................................................... 16 3.2 Rhaetina pyriformis (Suess ), 1854 ................................................................................. 17 4. Ergebnisse der quantitativen Analyse ................................................................................. 18 4.1 Rhaetina gregaria (Suess ), 1854 ...................................................................................... 18 4.1.1 Die Häufigkeiten der Stadien des relativen A lte r s ............................................. 18 4.1.2 Das relative Wachstum von Dicke und Breite der G eh ä u se ............................... 18 4.1.3 Das relative Wachstum von Höhe und Breite
Recommended publications
  • Program, Elěadáskivonatok, Kirándulásvezetě 7. Magyar Ěslénytani Vándorgyķlés
    PROGRAM, ELěADÁSKIVONATOK, KIRÁNDULÁSVEZETě 7. MAGYAR ěSLÉNYTANI VÁNDORGYĶLÉS 2004. MÁJUS 6–8. BEREMEND A MAGYARHONI FÖLDTANI TÁRSULAT ěSLÉNYTANI-RÉTEGTANI SZAKOSZTÁLYA RENDEZÉSÉBEN 7. MAGYAR ėSLÉNYTANI VÁNDORGYĥLÉS PROGRAMJA BEREMEND, 2004. MÁJUS 6–8. ELėADÓÜLÉS – 1. NAP (CSÜTÖRTÖK) DélelĘtt – LevezetĘ elnök: Vörös Attila 11:30 Heindl József Köszöntés és megnyitó (Beremend polgármestere) Pálfy József 11:40 – 12:00 ėsi Attila NövényevĘ krokodil a magyarországi felsĘ-krétából (Bakony) 12:00 – 12:20 Pászti Andrea Rhenanoperca minuta Gaudant et Micklich (Pisces, Perciformes) a középsĘ-eocén Messeli Formációból (Messel, Németország) 12:20 – 12:40 Gál Erika FelsĘ pleisztocén madárcsontleletek a Kálvária 4. sz. barlangból 12:40 – 13:00 DezsĘ József, A beremendi SzĘlĘhegy hasadékai és kitöltéseik a Tóth Judit morfológiai megfigyelések tükrében 13:00 – 14:30 EBÉDSZÜNET, POSZTEREK Délután 1. – LevezetĘ elnök: Galácz András 14:30 – 15:00 Vörös Attila ÜledékképzĘdési epizódok és faunaváltozások a villányi jura rétegsorban 15:00 – 15:20 Görög Ágnes A mecseki foltos márga foraminiferái 15:20 – 15:40 Szabó János Magyarországi terrének jura Ęsföldrajzi helyzete a Tethys és a kapcsolódó tengerek új gastropoda- faunisztikai eredményeinek tükrében 15:40 – 16:00 Dulai Alfréd, Lobothyris ? subgregaria: egy kora-jura Elvis faj a Pálfy József Nyugati-Tethys területén 16:00 – 16:30 KÁVÉSZÜNET Délután 2. – LevezetĘ elnök: Dulai Alfréd 16:30 – 16:50 FĘzy István, Négy eltĦnt réteg nyomában. Milyen korú volt az Nico M.M. Janssen ammoniteszes pad a zirci Márványbányában? 16:50 – 17:10 Galácz András Paleocén Nautiloideák Líbiából 17:10 – 17:30 Katona Lajos Pannóniai puhatestĦ faunák a Balaton-felvidék feltárásaiból Este – Nyilvános elĘadás 17:45 – 19:00 Kordos László Beremend és a magyar gerinces paleontológia 19:30 VACSORA (a Zokogó Majom étteremben) 7.
    [Show full text]
  • From the Western of the United
    from the Western of the United GEOLOGICAL SURVEY P R® BES&lON AL PAPER 1057 Early Triassic Terebratulid Brachiopods from the Western Interior of the United States By PETER R. HOOVER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1057 Description and illustration offive species of terebratulid brachiopods, and discussion of their distribution and developmental and evolutionary history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Hoover, Peter R. Early Triassic Terebratulid Brachiopods from the Western Interior of the United States (Geological Survey Professional Paper 1057) Bibliography: p. 19 Includes index Supt. of Docs. No.: I 19:16:1057 1. Terebratulida, Fossil. 2. Paleontology Triassic. 3. Paleontology The West. I. Title. II. Series: United States Geological Survey Professional Paper 1057 QE797.T29H66 564'.8 77-608314 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03182-5 CONTENTS Page Page Systematic paleontology Continued Abstract ....................... 1 Family Dielasmatidae Continued Introduction .................... 1 Subfamily Dielasmatinae. Previous work................ 1 Rhaetina Waagen ..... Present study ................ 3 Family Terebratulidae ......... 9 Acknowledgments ............ 3 Subfamily Plectoconchiinae. 9 Fossil localities cited in this report. .... 3 Vex, n. gen. ......... 9 Stratigraphic setting of the brachiopods 4 Family Cryptonellidae ......... 11 Faunal relationships. .............. 6 Subfamily Cryptacanthiinae . 11 Biostratigraphic implications........ 6 Obnixia, n. gen. ...... 11 Systematic paleontology............ 7 Family Zeilleriidae ............ 17 Family Dielasmatidae.......... 7 Periallus, n. gen. ......... 17 Subfamily Zugmayeriinae . 7 References cited. ................. 19 Portneufia, n. gen. .... 7 Index ......................... 21 ILLUSTRATIONS [Plates follow index] PLATE 1.
    [Show full text]
  • REVIEW of the UPPER TRIASSIC BRACHIOPODS in the NORTHERN CALCAREOUS ALPS Shallow-Water Carnian Brachiopod Fauna of the NCA Is R
    ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Berichte Geol. B.-A., 76 (ISSN 1017-8880) – Upper Triassic …Bad Goisern (28.09 - 02.10.2008) REVIEW OF THE UPPER TRIASSIC BRACHIOPODS IN THE NORTHERN CALCAREOUS ALPS Miloš SIBLÍK Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 269, CZ-16500 Praha 6. [email protected] Shallow-water Carnian brachiopod fauna of the NCA is relatively poor in its diversity (e.g. Adygella and some species of Cruratula and koninckinids in the Raibl and Cardita Beds). It is markedly different not only from partially synchronous assemblages of the Hallstatt Limestone, which lived in deeper parts of the Tethys but totally from those of the Norian and Rhaetian. At that time the diversification of the brachiopod assemblages was already more intensive. The Hallstatt facies yielded already more varied, often smooth fauna of the Carnian and Norian age. The differences in composition between them are rather insignificant. Some brachiopod taxa (Camerothyris, some species of the characteristic genus Austriellula – A. nux, A. longicollis, A. dilatata etc.) are known from both Carnian and Norian levels, some other (terebratulids Nucleatula and Juvavella, athyridid Pexidella strohmayeri, and rhynchonellids Austriellula juvavica, A. laevis, Norella geyeri etc.) are reported from the Norian only. Curious local neptunian dyke “Weisser Crinoidenkalk“ on the GSSP candidate Steinbergkogel near Hallstatt is according to KRYSTYN et al. (2007a) the youngest fossil horizon of the Hallstatt Limestone (top of Paracochloceras suessi Zone). It yielded according to BITTNER (1890) „Juvavella Suessii, Rhynchonella Geyeri, Rhynchonella nux, Koninckina blandula and Spirigera deslongchampsi“, all of them held for the Norian species.
    [Show full text]
  • Paléobiologie
    REVUE DE VOLUME 35 (2 ) – 2016 PALÉOBIOLOGIE Une institution Ville de Genève www.museum-geneve.ch Revue de Paléobiologie, Genève (décembre 2016) 35 (2): 385-416 ISSN 0253-6730 Die Brachiopoden der Klippendecke (Préalpes médianes) in den Préalpes romandes der Südwestschweiz, des Chablais und der zentralschweizerischen Klippen: eine Übersicht und paläogeographische Beziehungen Heinz SULSER Paläontologisches Institut und Museum der Universität Zürich, Karl Schmid-Str. 4, CH-8006 Zürich. E-Mail: [email protected] Zusammenfassung Die Kenntnis der Brachiopoden der Préalpes romandes in der Südwestschweiz (Kantone Bern, Freiburg und Waadt), des fränzösi- schen Chablais und der Klippenregion der Zentralschweiz beruht zum grossen Teil auf den klassischen Arbeiten früherer Autoren. Die Brachiopoden kommen fast ausschliesslich in der Klippendecke (Préalpes médianes) vor. Die Klippendecke besteht aus einer nahezu lückenlosen Abfolge von mesozoischen Sedimenten. In fast allen stratigraphischen Stufen kommen Brachiopoden vor, doch mit unter- schiedlicher Häufigkeit und Frequenz. In der vorliegenden Arbeit werden über 60 Arten der Ordnungen Rhynchonellida, Spiriferinida und Terebratulida diskutiert. Zwei neue Arten (Septaliphoria felberi nov. sp., Aulacothyris maendlii nov. sp.) aus dem Dogger der My- then werden beschrieben. Obwohl die von älteren Autoren aufgestellten Arten neu untersucht und teilweise revidiert werden müssen, ist der besondere Charakter dieser Brachiopoden offensichtlich. In der Trias lassen sich die Brachiopoden mit Vorkommen in ganz Europa vergleichen. Im späten Dogger und Malm zeigen sich deutliche Analogien zu Formen der Ost- und Südalpen. Die Brachiopoden der Mytilus-Schichten sind eher endemisch. Im frühen und mittleren Lias erscheint eine gemischte Fauna mit Arten aus Jura und Alpen. Diese Affinitäten passen recht gut in den gegebenen tektonischen Rahmen: nach der Trennung des Kontinents Pangaea in einen euro- päischen Nord- und afrikanischen Südteil am Ende der Trias entstanden in der Bruchzone Mikrokontinente (Ostalpen, Briançonnais).
    [Show full text]
  • Stratigraphie and Environmental Correlations in the Fatra- and Norovica- Formation (Upper Triassic, Western Carpathians)
    Schriftenreihe der Erdwissenschaftlichen Kommissionen, Band 5, Seiten 267-276 Copyright© 1983 by Österreichische Akademie der Wissenschaften Veröffentlichung des Österreichischen Nationalkomitees für das International Geological Correlation Programme Project Nr. 73/1/4. Triassic of the Tethys Realm Stratigraphie and environmental correlations in the Fatra- and Norovica­ Formation (Upper Triassic, Western Carpathians) JozEF MICHALiK and ANDRZEJ GAZDZICKI*) 4 text-figs. Abstract Two formations of several Upper Triassic developments in the Western Carpathians are compared: the Fatric restricted marine basin has been bounded by extensive shallows in the Hronic, where Norovica Fm. originated. Though both the formations have several common features (biogenic carbonate sediments arising in a hot climate with periodic violent storms under slow transgressive conditions etc.), they differ in some principal characteristics. The informal and formal lithostratigraphical division and the most important biostratigraphical features are dealt more in detail. 1. Introduction Both the Fatra- and Norovica-Formations, produced by shallow marine carbonate sedimentation, represent two of the principal development patterns of West Carpathian top Triassic sedimentary sequences (compare Fig.1). The development of the uppermost Triassic sediments in the Fatric has been previously named "Koessener Schichten", or simplier, but incorrectly "Rhaetian". Later, in 1974 it has been entitled by J. MICHALiK as "Fatra-Schichten". Its type profile has been described by J. MICHALiK in 197 6 in the Dedosova dolina - valley in Vel'kä Fatra Mts. The same author formerly regarded the "Fatra-Member" and "Hybe-member" as two (partially synchronous) members of the so-called "Carpa­ thian Koessen Formation". Later (in J. MICHALiK et al., 1979 etc.) he has recognized that it is more reasonable to consider this Fatra-complex as an independent formation.
    [Show full text]
  • Map, Tables, and Summary of Fossil and Isotopic Age Data, Mount Hayes Quadrangle, Eastern Alaska Range, Alaska
    U.S. DEPARTMENf OF TilE INfERIOR FOUO OF TilE MOUN!' HAYES QUADRANGLE U.S. GEOLOGICAL SURVEY TO ACCOMPANY MAP MF-1996-D MAP, TABLES, AND SUMMARY OF FOSSIL AND ISOTOPIC AGE DATA, MOUNT HAYES QUADRANGLE, EASTERN ALASKA RANGE, ALASKA By Warren J. Nokleberg, John N. Aleinikoff, J. Thomas Dutro, Jr., Marvin A. Lanphere, Norman J. Silberling, Steven R. Silva, Thomas E. Smith, and Donald L. Turner INTRODUCTION sutures separating terranes, and younger Cenozoic faults thiit are present chiefly within terranes. This report describes, summarizes, and interprets all In the last three decades, the Mount Hayes quadrangle has known bedrock fossil and isotopic age studies for the Mount been the focus of many bedrock geologic studies. Bedrock Hayes quadrangle, eastern Alaska Range, Alaska. The geologic maps were published by Holmes (1965), Pewe and accompanying map shows the location of all known bedrock Holmes (1964), Rose (1965; 1966a, b; 1967), Rose and fossil and isotopic sample localities in the quadrangle on a Saunders (1965), Matteson (1973), Bond (1976), Stout (1976), generalized geologic base map. These fossil and isotopic age Richter and others (1977), and Nokleberg and others (1982). data are obtained from new studies, unpublished data of the U.S. The geologic base for this study is based partly on that Geological Survey, contributed unpublished data, and geology and to a greater degree on 1:63,360-scale geologic published data. This report is one result of a five-year mineral­ mapping of the entire quadrangle that was· done for the mineral resource assessment of the quadrangle that was done during the resource assessment study of the area (Nokleberg and others, summers of 1978 through 1982, with additional topical studies­ 1990).
    [Show full text]
  • On the Find of Triassic Brachiopod Fauna in the Variegated Micrites on the Dachstein Plateau
    91 Slovak Geol. Mag., 7, 1(2001 ),91-94 On the find of Triassic brachiopod fauna in the variegated micrites on the Dachstein Plateau MlLOS SlBUK Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojova 135, 165 00 Praha 6 - Suchdol Abstract: Triassic age of the variegated micritic marly limestones sporadically occurring in the Dachstein Formation on the Dachstein Plateau SSW of Hallstatt was documented with the finds of Upper Triassic tere- bratulid Triadithyris gregariaeformis (Zugmayer, 1880) and of remains of dasycladacean algae. Key words: Northern Calcareous Alps, Triassic, Dachstein Formation, brachiopods Introduction more about the age of the carbonate matrix. Nevertheless, from the geological point of view both these colleagues Rich Liassic brachiopod fauna is well-known from were rather sceptical as to the Liassic age of the rock (per- white and red biosparitic fissure-fillings in the monoto- sonal communications). According to Lobitzer, the micritic nously grey Dachstein Limestone on the Dachstein massif marly limestones are equivalents of Member A sensu SSW of Hallstatt and it was described in detail already Fischer (1964). At studied outcrops typical Lofer cycles are many years ago (e.g. from Hierlatz by Oppel, 1861 and not developed but surrounding Dachstein Limestone is Geyer, 1889). The present study was prompted by the clearly of lagoonal origin and nearby various types of com- discovery of biplicate terebratulid brachiopods occurring plete or ..amputated,, Lofer cycles can be observed. Maybe not far from Hierlatz in the yellow, reddish, ochrous or most of the micritic sediment is of pedogenic origin with greenish micrites which form irregular spots - not fissure temporary influence of marine sedimentation (Lobitzer, fillings - in the Dachstein Limestone on the Plateau, S of written communication).
    [Show full text]
  • Effect of Extrinsic Factors on Biofabric and Brachiopod Alteration in a Shallow Intraplatform Carbonate Setting (Upper Triassic, West Carpathians)
    RESEARCH REPORTS 349 Effect of Extrinsic Factors on Biofabric and Brachiopod Alteration in a Shallow Intraplatform Carbonate Setting (Upper Triassic, West Carpathians) ADAM TOMASÆ OVYÂ CH Institut fuÈ r PalaÈontologie, WuÈ rzburg UniversitaÈ t, Pleicherwall 1, 97070 WuÈ rzburg, Germany, Email: [email protected] PALAIOS, 2004, V. 19, p. 349±371 potential of brachiopods due to differential extrinsic factors (e.g., between hard- and soft-bottom settings) can substan- Upper Triassic assemblages containing the terebratulid tially bias the understanding their ecology and temporal brachiopod Rhaetina gregaria from a shallow, intraplat- shifts in environmental preferences. Data about substantial form carbonate setting of the Fatra Formation are classi®ed bioerosion/micritization of brachiopods in some deposit according to biofabric, geometry, and internal structure types indicate their higher durability and inherently higher into 6 deposit types, which are interpreted as: (1) autochtho- preservation potential in contrast to actualistic data about nous primary biogenic, (2) autochthonous winnowed or sed- the poor resistance of modern brachiopods to destruction. iment starved, (3) parautochthonous storm-wave, (4) par- autochthonous storm wave/¯ow, (5) amalgamated storm- reworked, and (6) allochthonous (long-term current/wave) INTRODUCTION deposits. Their distribution on the bed scale correlates with depth-related environmental gradients in regard to the po- In actualistic studies of death assemblages, quantita- sition of fair-weather
    [Show full text]
  • 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).
    [Show full text]
  • Dear Author, Here Are the Proofs of Your Article. • You Can Submit Your Corrections Online, Via E-Mail Or by Fax. • for On
    Dear Author, Here are the proofs of your article. • You can submit your corrections online, via e-mail or by fax. • For online submission please insert your corrections in the online correction form. Always indicate the line number to which the correction refers. • You can also insert your corrections in the proof PDF and email the annotated PDF. • For fax submission, please ensure that your corrections are clearly legible. Use a fine black pen and write the correction in the margin, not too close to the edge of the page. • Remember to note the journal title, article number, and your name when sending your response via e-mail or fax. • Check the metadata sheet to make sure that the header information, especially author names and the corresponding affiliations are correctly shown. • Check the questions that may have arisen during copy editing and insert your answers/ corrections. • Check that the text is complete and that all figures, tables and their legends are included. Also check the accuracy of special characters, equations, and electronic supplementary material if applicable. If necessary refer to the Edited manuscript. • The publication of inaccurate data such as dosages and units can have serious consequences. Please take particular care that all such details are correct. • Please do not make changes that involve only matters of style. We have generally introduced forms that follow the journal’s style. Substantial changes in content, e.g., new results, corrected values, title and authorship are not allowed without the approval of the responsible editor. In such a case, please contact the Editorial Office and return his/her consent together with the proof.
    [Show full text]
  • Field Trips in the Eastern and Southern Alps (Austria, Italy)
    Berichte der Geologischen Bundesanstalt (ISSN 1017-8880) Band 111 Field trips in the Eastern and Southern Alps (Austria, Italy) Sylvain Richoz [ed.] Berichte der Geologischen Bundesanstalt (ISSN 1017-8880), Band 111, Wien 2015 STRATI 2015 Impressum Berichte der Geologischen Bundesanstalt, 111 ISSN 1017-8880 Wien, im Juli 2015 Field trips in the Eastern and Southern Alps (Austria, Italy) Sylvain Richoz [ed.] Umschlaggestaltung: Monika Brüggemann-Ledolter, Geologische Bundesanstalt Cover: Setting of the Golden Spike by Stanley Finney (Chair of the International Commission on Stratigraphy) during the inaugural of the Triassic/Jurassic-Boundary GSSP, Kuhjoch (Tirol, Austria), August, 20th 2011 (Photo: Werner E. Piller). Alle Rechte für das In- und Ausland vorbehalten © Geologische Bundesanstalt Medieninhaber, Herausgeber und Verleger: Geologische Bundesanstalt, Neulinggasse 38, 1030 Wien www.geologie.ac.at Satz und Layout: Thomas J. Suttner, Geologische Bundesanstalt Druck: Riegelnik Ges.m.b.H, Piaristengasse 17–19, 1080 Wien Die Autoren sind für den Inhalt ihrer Arbeit verantwortlich und mit der digitalen Verbreitung ihrer Arbeit im Internet einverstanden. Ziel der „Berichte der Geologischen Bundesanstalt“ ist die Verbreitung wissenschaftlicher Ergebnisse durch die Geologische Bundesanstalt. Die „Berichte der Geologischen Bundesanstalt“ sind im Buchhandel nicht erhältlich. 2 Berichte der Geologischen Bundesanstalt (ISSN 1017-8880), Band 111, Wien 2015 STRATI 2015 CONTENTS STRATI 2015 – Conference and Field Trips schedule 4 The Pre-Variscan sequence of the Carnic Alps 5 Abstract 6 1. Topics and area of the Field Trip 6 2. Geological overview 7 2.1. Palaeogeographic remarks 8 2.2. The Pre-Variscan sequence 8 2.3. Summary of the lithostratigraphic units 12 3. The Field Trip 12 3.1.
    [Show full text]
  • Brachiopoda, Terebratulida) from the Middle Triassic of Makhtesh Ramon, Southern Israel
    Annales Societatis Geologorum Poloniae (2017), vol. 87: 89–99. doi: http://dx.doi.org/10.14241/asgp.2017.004 TUNETHYRIS BLODGETTI SP. NOV. (BRACHIOPODA, TEREBRATULIDA) FROM THE MIDDLE TRIASSIC OF MAKHTESH RAMON, SOUTHERN ISRAEL Howard R. FELDMAN Biology Department, Touro College, American Museum of Natural History, 227 W. 60th Street, New York 10023, USA; e-mail: [email protected] Feldman, H. R., 2017. Tunethyris blodgetti sp. nov. (Brachiopoda, Terebratulida) from the Middle Triassic of the Makhtesh Ramon, southern Israel. Annales Societatis Geologorum Poloniae, 87: 89–99. Abstract: Tunethyris blodgetti sp. nov. from the Triassic Saharonim Formation, Makhtesh Ramon, an erosional cirque in southern Israel, is erected on the basis of a suite of 39 articulated specimens. The shells are very strongly sulciplicated, a feature that seems to be more prevalent in the Mesozoic than the Palaeozoic. The Saharonim Formation was deposited under quasi-normal, calm, relatively shallow marine conditions. Faunal constituents of the Saharonim Formation include conodonts, ostracods, foraminiferans, bivalves, cephalopods, gastropods, echi- noderms and vertebrate remains that belong to the Sephardic Province and are diagnostic of the Middle Triassic series of Israel. The faunal composition and shallow depositional environment of the strata may help differentiate the Sephardic Province from the Germanic Muschelkalk and the Alpine Tethyan faunas to the north. Key words: Brachiopoda, Triassic, Sephardic Province, Ladinian, Makhtesh Ramon, palaeoecology, palaeobio- geography. Manuscript received 4 May 2016, accepted 20 April 2017 INTRODUCTION The first recognition of Triassic rocks in the Middle Leda cf. fibula, Palaeoneilo elliptica, Elegantia elegans, East was the discovery of Carnian fossils near Latakia in Lyriomyphoria germanica, Costatoria coxi, Costatoria Syria, in 1915 (Picard and Flexer, 1974).
    [Show full text]