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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. -
1395 Kaim.Vp
Early Triassic gastropods from Salt Range, Pakistan ANDRZEJ KAIM, ALEXANDER NÜTZEL, MICHAEL HAUTMANN & HUGO BUCHER Five gastropod species are described from the Early Triassic (Smithian, Spathian) of the Salt Range in Pakistan, which is the first detailed documentation of gastropods from this key area of the Palaeozoic-Mesozoic transition. Bellerophontoidea are represented by Warthia hisakatsui. Bellerophontoidea were widespread in the Paleozoic and had their last appearance in the early Smithian. Anisian and later reports of this group are discussed, but currently remain doubtful. Soleniscidae, a typical Late Palaeozoic caenogastropod family, are present with two new species: Strobeus batteni and S. pakistanensis. The neritimorph genus Naticopsis and the caenogastropod Coelostylina are present with one species each, provisionally treated in open nomenclature. Naticopsis? sp. shows preservation of original colour pat- terns, which is very rare in Early Triassic gastropods. All identified genera originated during the Paleozoic (perhaps with the exception of Coelostylina) and are thus survivors or holdovers. Warthia and Strobeus survived the end-Permian mass extinction but went extinct during the Smithian when environmental conditions deteriorated again. • Key words: Gastropoda, Pakistan, Salt Range, Early Triassic, extinction, recovery, taxonomy. KAIM, A., NÜTZEL, A., HAUTMANN,M.&BUCHER, H. 2013. Early Triassic gastropods from Salt Range, Pakistan. Bul- letin of Geosciences 88(3), 505–516 (7 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript re- ceived November 9, 2012; accepted in revised form February 8, 2013; published online March 4, 2013; issued July 3, 2013. Andrzej Kaim, Instytut Paleobiologii PAN, ul. Twarda 51/55, 00-818 Warszawa, Poland; [email protected] • Alex- ander Nützel, Bayerische Staatssammlung für Paläontologie und Geologie, Ludwig-Maximilians-University Munich, Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Geobio-CenterLMU, Richard Wagner Str. -
Microstructural Evidence of the Stylophyllid Affinity of the Genus Cyathophora (Scleractinia, Mesozoic)
Annales Societatis Geologorum Poloniae (2016), vol. 86: 1–16. doi: http://dx.doi.org/10.14241/asgp.2015.023 MICROSTRUCTURAL EVIDENCE OF THE STYLOPHYLLID AFFINITY OF THE GENUS CYATHOPHORA (SCLERACTINIA, MESOZOIC) El¿bieta MORYCOWA1 & Ewa RONIEWICZ2 1 Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-630 Kraków, Poland; e-mail: [email protected] 2 Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, 01-818 Warszawa, Poland; e-mail: [email protected] Morycowa, E. & Roniewicz, E., 2016. Microstructural evidence of the stylophyllid affinity of the genus Cyatho- phora (Scleractinia, Mesozoic). Annales Societatis Geologorum Poloniae, 86: 1–16. Abstract: The genus Cyathophora Michelin, 1843 (Cyathophoridae) is removed from the suborder Stylinina Alloiteau, 1952 and transferred to the Stylophyllina Beauvais, 1980. Morphologically, it differs from stylinine corals in that rudimentary septa are developed in the form of ridges or spines on the wall and may continue onto the endothecal elements as amplexoid septa. Relics of primary aragonite microstructure, preserved in silicified colonies of Cyathophora steinmanni Fritzsche, 1924 (Barremian–early Aptian) and in a calcified colony of C. richardi Michelin, 1843 (middle Oxfordian), indicate a non-trabecular structure of their skeletons. The scleren- chyme of radial elements is differentiated into fascicles of fibres, and in the form of fascicles or a non-differen- tiated layer of fibres, it continues as the upper part of endothecal elements and as the incremental layers of the wall. A micro-lamellation of the skeleton corresponds to the accretionary mode of skeleton growth found in Recent corals. A similarity between the septal microstructure of Cyathophora and that of the stylophyllid genera, the Triassic Anthostylis Roniewicz, 1989 and the Triassic–Early Jurassic Stylophyllopsis Frech, 1890, is interpre- ted as a result of their being phylogenetically related. -
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). -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
Note on the Fine Skeletal Structures in Scleractinia and in Tabulata
Title Note on the Fine Skeletal Structures in Scleractinia and in Tabulata Author(s) Kato, Makoto Citation Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and mineralogy, 14(1), 51-56 Issue Date 1968-02 Doc URL http://hdl.handle.net/2115/35982 Type bulletin (article) File Information 14(1)_51-56.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP NOTE ON THE FINE SKELETAL STRUCTURES IN SCLERACTINIA AND IN TABULATA by Makoto KATo (with 1 Text-figure) (Contribution from the Department of Geology and Mineralogy, Faculty of Science, Hokl<aido University. No. 1069) On the fine sketetal structures in Scleractinia Scleractinia is a vast group including reef corals of recent time. Much knowl- edge on the ecology, physiology and so on of the recent Scleractinians has been accumulated up to the present by a number of research worlcers. By deduction, biological aspects of fossil Scleractinians may be readily sought in these data on recent corals. Being an extinct group, however, nothing definite has been ascertained as to the true biological aspects of Palaeozoic Rugosa, though many functional features or conditions of Scleractinia can be also attributed to Rugosa, since the former is the nearest ally to the latter. Hence, one must study in every detail the biology of the recent Scleractinia, for the thorough understanding of Palaeozoic Rugosa, It is well known that in Scleractinia microstructure of coral skeleton has been taken as a clue to major divisions of the group. (VAuGHAN 8c WELLs, 1943 : WEms, 1956) Recent comprehensive work on Scleractinia by ALLoiTEAu (1957) also gave importance to the microstructure in the classification of the said group, For the sake of comparison with Palaeozoic corals, the writer also examined many thin sections of Scleractinians kept at the British Museum of Natural History. -
Towards a New Synthesis of Evolutionary Relationships and Classification of Scleractinia
J. Paleont., 75(6), 2001, pp. 1090±1108 Copyright q 2001, The Paleontological Society 0022-3360/01/0075-1090$03.00 TOWARDS A NEW SYNTHESIS OF EVOLUTIONARY RELATIONSHIPS AND CLASSIFICATION OF SCLERACTINIA JAROSèAW STOLARSKI AND EWA RONIEWICZ Instytut Paleobiologii, Polska Akademia Nauk, Twarda 51/55, 00-818 Warszawa, Poland ,[email protected]., ,[email protected]. ABSTRACTÐThe focus of this paper is to provide an overview of historical and modern accounts of scleractinian evolutionary rela- tionships and classi®cation. Scleractinian evolutionary relationships proposed in the 19th and the beginning of the 20th centuries were based mainly on skeletal data. More in-depth observations of the coral skeleton showed that the gross-morphology could be highly confusing. Profound differences in microstructural and microarchitectural characters of e.g., Mesozoic microsolenine, pachythecaliine, stylophylline, stylinine, and rhipidogyrine corals compared with nominotypic representatives of higher-rank units in which they were classi®ed suggest their separate (?subordinal) taxonomic status. Recent application of molecular techniques resulted in hypotheses of evolutionary relationships that differed from traditional ones. The emergence of new and promising research methods such as high- resolution morphometrics, analysis of biochemical skeletal data, and re®ned microstructural observations may still increase resolution of the ``skeletal'' approach. Achieving a more reliable and comprehensive scheme of evolutionary relationships and classi®cation -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 72, NUMBER 7 SEA-LILIES AND FEATHER-STARS (With i6 Plates) BY AUSTIN H. CLARK (Publication 2620) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION 1921 C^e Both (§aitimove (prcee BALTIMORE, MD., U. S. A. SEA-LILIES AND FEATHER-STARS By AUSTIN H. CLARK (With i6 Plates) CONTENTS p^^E Preface i Number and systematic arrangement of the recent crinoids 2 The interrelationships of the crinoid species 3 Form and structure of the crinoids 4 Viviparous crinoids, and sexual differentiation lo The development of the comatulids lo Regeneration 12 Asymmetry 13 The composition of the crinoid skeleton 15 The distribution of the crinoids 15 The paleontological history of the living crinoids 16 The fossil representatives of the recent crinoid genera 17 The course taken by specialization among the crinoids 18 The occurrence of littoral crinoids 18 The relation of crinoids to temperature 20 Food 22 Locomotion 23 Color 24 The similarity between crinoids and plants 29 Parasites and commensals 34 Commensalism of the crinoids 39 Economic value of the living crinoids 39 Explanation of plates 40 PREFACE Of all the animals living in the sea none have aroused more general interest than the sea-lilies and the feather-stars, the modern repre- sentatives of the Crinoidea. Their delicate, distinctive and beautiful form, their rarity in collections, and the abundance of similar types as fossils in the rocks combined to set the recent crinoids quite apart from the other creatures of the sea and to cause them to be generally regarded as among the greatest curiosities of the animal kingdom. -
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. -
Excu 2015 Biodiversité, Stratigraphie Et
Journées Scientifiques du GFEJ 09 et 10 Avril 2015 Biodiversité, Stratigraphie et Paléogéographie du Jurassique Un hommage à Jacques Thierry Pierre PELLENARD & Pascal NEIGE Comité d'organisation: Benjamin BRIGAUD Pierre-Yves COLLIN Jean-Louis DOMMERGUES Christophe DURLET Pascal NEIGE Pierre PELLENARD Université de Bourgogne, UMR CNRS 6282 Biogéosciences Journées Scientifiques du GFEJ 09 et 10 Avril 2015 Université de Bourgogne, UMR CNRS 6282 Biogéosciences Biodiversité, Stratigraphie et Paléogéographie du Jurassique Un hommage à Jacques Thierry Pierre PELLENARD & Pascal NEIGE Comité d'organisation: Benjamin BRIGAUD Pierre-Yves COLLIN Jean-Louis DOMMERGUES Christophe DURLET Pascal NEIGE Pierre PELLENARD Ces journées scientifiques sont l'occasion d'échanger à la fois en salle et sur le terrain sur les thématiques de la biodiversité, de la paléoécologie, des méthodes et applications de la stratigraphie et de la paléogéographie pour les différentes périodes du Jurassique. A l'interface entre la paléontologie et la sédimentologie, ces thèmes, chers à Jacques Thierry, ancien professeur de l'Université de Bourgogne, nous permettront de lui rendre un dernier hommage en compagnie de ses anciens élèves, collègues et amis et de faire un point sur les avancées récentes de notre communauté. La journée du 09 Avril est consacrée à la visite de coupes "historiques" en Bourgogne sur le Jurassique inférieur et moyen (Semur-en-Auxois, Pouillenay, Massangis). La journée du 10 Avril est consacrée aux présentations orales sur les thématiques affichées et à l'assemblée générale du GFEJ. Participants: Simon ANDRIEU (Univ. Orsay), Cédric BAILLY (Univ. Bourgogne), Philippe BLANC (Lithologie Bourgogne), Cédric BOUGEAULT (Univ. Bourgogne), Alexandra BOUILLOT (Musée Semur-en- Auxois), Raphaël BOURILLOT (ENGESID Univ.