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9 Paleontological Conference Th
Polish Academy of Sciences Institute of Paleobiology 9th Paleontological Conference Warszawa, 10–11 October 2008 Abstracts Warszawa Praha Bratislava Edited by Andrzej Pisera, Maria Aleksandra Bitner and Adam T. Halamski Honorary Committee Prof. Oldrich Fatka, Charles University of Prague, Prague Prof. Josef Michalík, Slovak Academy of Sciences, Bratislava Assoc. Prof. Jerzy Nawrocki, Polish Geological Institute, Warszawa Prof. Tadeusz Peryt, Polish Geological Institute, Warszawa Prof. Grzegorz Racki, Institute of Paleobiology, Warszawa Prof. Jerzy Trammer, University of Warsaw, Warszawa Prof. Alfred Uchman, Jagiellonian University, Kraków Martyna Wojciechowska, National Geographic Polska, Warszawa Organizing Committee Dr Maria Aleksandra Bitner (Secretary), Błażej Błażejewski, MSc, Prof. Andrzej Gaździcki, Dr Adam T. Halamski, Assoc. Prof. Anna Kozłowska, Assoc. Prof. Andrzej Pisera Sponsors Institute of Paleobiology, Warszawa Polish Geological Institute, Warszawa National Geographic Polska, Warszawa Precoptic Co., Warszawa Cover picture: Quenstedtoceras henrici Douvillé, 1912 Cover designed by Aleksandra Hołda−Michalska Copyright © Instytut Paleobiologii PAN Nakład 150 egz. Typesetting and Layout: Aleksandra Szmielew Warszawska Drukarnia Naukowa PAN ABSTRACTS Paleotemperature and paleodiet reconstruction on the base of oxygen and carbon isotopes from mammoth tusk dentine and horse teeth enamel during Late Paleolith and Mesolith MARTINA ÁBELOVÁ State Geological Institute of Dionýz Štúr, Mlynská dolina 1, SK−817 04 Bratislava 11, Slovak Republic; [email protected] The use of stable isotopes has proven to be one of the most effective methods in re− constructing paleoenvironments and paleodiet through the upper Pleistocene period (e.g. Fricke et al. 1998; Genoni et al. 1998; Bocherens 2003). This study demonstrates how isotopic data can be employed alongside other forms of evidence to inform on past at great time depths, making it especially relevant to the Palaeolithic where there is a wealth of material potentially available for study. -
A New Passerine Bird from the Early Oligocene of Poland
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector J Ornithol (2011) 152:1045–1053 DOI 10.1007/s10336-011-0693-2 ORIGINAL ARTICLE A new passerine bird from the early Oligocene of Poland Zbigniew M. Bochen´ski • Teresa Tomek • Małgorzata Bujoczek • Krzysztof Wertz Received: 15 December 2010 / Revised: 25 January 2011 / Accepted: 31 March 2011 / Published online: 21 April 2011 Ó The Author(s) 2011. This article is published with open access at Springerlink.com Abstract We describe a nearly complete articulated Zusammenfassung Wir beschreiben ein fast vollsta¨ndig specimen representing a new species and genus, Jamna artikuliertes Exemplar einer neuen Sperlingsvogel-Art und szybiaki gen. et sp. nov., of an early Oligocene passeriform -Gattung, Jamna szybiaki gen. et sp. nov., aus dem fru¨hen bird from Poland. In overall osteology, the specimen Oligoza¨n in Polen. In seinem Knochenbau erinnert das resembles extant Passeriformes but it differs from that Exemplar an heutige Sperlingsartige, unterscheidet sich group in several characters including the not bifurcated jedoch von dieser Gruppe in einigen Merkmalen wie z.B. spina externa (sternum) and the absence of a hooked pro- dem ungegabelten Brustbein (sternum) und dem nicht cessus acrocoracoideus (coracoid). Its affinities within vorhandenen eingehakten Rabenschnabelfortsatz processus Passeriformes cannot be resolved at the moment due to the acrocoracoideus (coracoid). Die Verwandtschaft mit den lack of characters that would support its position within Sperlingsvo¨geln ist derzeit noch nicht ganz klar, weil either Oscines or Suboscines. For the first time in Paleo- Merkmale fehlen, die seine Stellung innerhalb entweder gene passerines, wing and tail feathers are visible which der Oscines, oder der Suboscines festlegen wu¨rden. -
A Complete Passerine Foot from the Late Oligocene of Poland
Palaeontologia Electronica palaeo-electronica.org A complete passerine foot from the late Oligocene of Poland Zbigniew M. Bochenski, Teresa Tomek, and Ewa Swidnicka ABSTRACT The paper describes a nearly complete articulated specimen of a passerine foot imprinted on a slab and counter slab of the siliceous clayey shales belonging to the upper part of the Menilite Formation of the Outer Carpathians in southeastern Poland and dated to the late Oligocene (Chattian, ca. 25 m.y.a.). It is one of the very few Paleogene specimens of passerines and just the third with a complete foot preserved. Its passerine affinities were established on the basis of a combination of characteristic features but owing to the incompleteness of the specimen its more precise systematic position within Passeriformes cannot be resolved. For the same reason the specimen is not described as a new extinct species although it differs from all known Oligocene passerines. The proportions of phalanges, size of the tarsometatarsus and shape of claws point to an arboreal bird, which increases the known Paleogene diversity of this bird group. Zbigniew M. Bochenski. Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Slawkowska 17, 31-016 Krakow, Poland, [email protected] Teresa Tomek. Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Slawkowska 17, 31-016 Krakow, Poland, [email protected] Ewa Swidnicka. Department of Palaeozoology, Chair of Evolutionary Biology and Ecology, University of Wrocław, Sienkiewicza 21, 50-335 Wrocław, Poland, [email protected] Keywords: Fossil birds; Passeriformes; Menilite shales; Carpathian flysch; Oligocene; Paleogene INTRODUCTION 1995, 1997), but unquestionable remains of pas- seriforms come from the Oligocene of Europe. -
Polish-2013 84.Pdf
13 20 3 Contents Address by PAS President Medical Sciences ..................................... 91 Professor Michał Kleiber ........................... 3 International Relations ............................ 101 Presidium of the Polish Academy of Sciences ................................................. 5 Educational and Promotional Activity .....107 Members of the Polish Academy of Sciences .................................................. 7 Th e FNP Prizes for 2012 .........................112 Humanities and Social Sciences .................13 Selected Statistics .....................................116 Biological and Agricultural Sciences .......... 43 Foreign Scientifi c Centers ........................118 Mathematics, Physics, Chemistry, and Earth Sciences .................. 56 Research Units and Branches ...................119 Engineering Sciences ................................. 74 Scientifi c and Task Force Committees ..... 126 Scientific Council: © Copyright 2011 Polish Academy of Sciences Marek C. Chmielewski – Editor-in-Chief Stanisław Filipowicz Offi ce of Science Promotion Andrzej Jerzmanowski PKiN, Pl. Defi lad 1, 00-901 Warsaw, Poland Marek Grad www.pan.pl Marian P. Kaźmierkowski Sławomir Majewski ISSN 1640-3754 Published by: On the cover: Th e vicinity of Halicz on the Josephine map of Galicia, Offi ce of Science Promotion 1779-1783, scale 1:28 800, fragment of sheet 300, original Edited by: (Image courtesy of the Kriegsarchiv, Vienna) Elżbieta Jamroz Medical and Surgery Academy, Warsaw (now: the Polish Katarzyna Kalinowska -
Vertebrate Anatomy Morphology Palaeontology ISSN 2292-1389 Published 4 May, 2020 Meeting Logo Design: © Francisco Riolobos, 2019 Editors: Alison M
Vertebrate Anatomy Morphology Palaeontology ISSN 2292-1389 Published 4 May, 2020 Meeting Logo Design: © Francisco Riolobos, 2019 Editors: Alison M. Murray, Victoria Arbour and Robert B. Holmes © 2020 by the authors DOI 10.18435/vamp29365 Vertebrate Anatomy Morphology Palaeontology is an open access journal http://ejournals.library.ualberta.ca/index.php/VAMP Article copyright by the author(s). This open access work is distributed under a Creative Commons Attribution 4.0 International (CC By 4.0) License, meaning you must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use. No additional restrictions — You may not apply legal terms or technological measures that legally restrict others from doing anything the license permits. Canadian Society of Vertebrate Palaeontology 2020 Abstracts 8th Annual Meeting Canadian Society of Vertebrate Palaeontology June 6–7, 2020 Victoria, B.C. Abstracts 9 Vertebrate Anatomy Morphology Palaeontology 8:7–66 10 Canadian Society of Vertebrate Palaeontology 2020 Abstracts Message from the Host Committee 20 April 2020 2020 has proven to be a strange and disruptive year for the Canadian vertebrate palaeontology community. A novel coronavirus, Covid-19, began circulating in China in December 2019, and had made its way to North America in January 2020, with the first cases reported in Canada on January 25th. Although concern about the impacts of this new virus were mounting throughout February, business seemed to be moving ahead as usual in most of our lives. -
Systematics and Phylogeny of the Zygodactylidae (Aves, Neognathae) with Description of a New Species from the Early Eocene of Wyoming, USA
Systematics and phylogeny of the Zygodactylidae (Aves, Neognathae) with description of a new species from the early Eocene of Wyoming, USA N. Adam Smith1, Aj M. DeBee2 and Julia A. Clarke2 1 Campbell Geology Museum, Clemson University, Clemson, SC, USA 2 Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA ABSTRACT Zygodactylidae are an extinct lineage of perching birds characterized by distinct morphologies of the foot and wing elements. Although the clade has a complex taxonomic history, current hypotheses place Zygodactylidae as the sister taxon to Passeriformes (i.e., songbirds). Given the rather sparse fossil record of early passeriforms, the description of zygodactylid taxa is important for inferring potentially ancestral states in the largest radiation of living birds (i.e., the ∼6,000 species of extant passeriforms). Despite the exceptional preservation of many specimens and considerable species diversity in Zygodactylidae, the relationships among species have not been previously evaluated in a phylogenetic context. Herein, we review the fossil record of Zygodactylidae from North America and describe five new well-preserved fossils from the early Eocene Green River Formation of Wyoming. Two specimens are identified as representing a new species and the first records of the taxon Zygodactylus outside Europe. Anatomical comparisons with previously named taxa and the results of phylogenetic analysis including newly described specimens and previously named zygodactylid taxa provide the first Submitted 24 February 2018 hypothesis of the species-level relationships among zygodactylids. The monophyly Accepted 16 May 2018 of Zygodactylidae is supported in these new analyses. However, the monophyly Published 25 June 2018 of Primozygodactylus and the taxonomic distinction between Zygodactylus and Corresponding authors Eozygodactylus remain unresolved and would likely benefit from the description of N. -
D:\Dostęp\Ela\Jamna Gotowe\Jamna 1-3Vp.Vp
Hanna MATYJA SUMMARY This report contains the results of both early analyses and the Zechstein strata (Jamno IG 1). The Zechstein deposits recent stratigraphic, sedimentological, petrographical and geo- were analysed for petrographical microfacies and diagenetic chemical investigations based on modern research methods and investigations. Some informations were also presented on within the chronostratigraphic units recommended by the Inter- the Zechstein salt deposits in the Jamno IG 1 section. national Commission on Stratigraphy. The Mesozoic succession is represented by the Triassic, Ordovician, Devonian, Permian, Triassic, Jurassic, Cretace- Jurassic and Cretaceous. ous and Neogene and/or Quaternary deposits were encountered Triassic deposits of all the boreholes seem to be represen- in the Jamno IG 1, Jamno IG 2 and Jamno IG 3 boreholes. ted by the almost complete stratigraphic range of the system. The oldest rocks drilled in the boreholes are Ordovician Thirteen lithostratigraphic units of group, formation and beds deposits represented by strongly tectonically deformed rank have been identified within the succession. These are fine-grained siliciclastics (mostly claystones and mudstones) (from oldest to youngest): Lower Buntsandstein (Baltic For- characterized by the presence of thin clayey siderite interbeds, mation), Middle Buntsandstein (Pomorze and Po³czyn forma- lenses and concretions as well as small crystalline pyrite con- tions), Upper Buntsandstein (Barwice Formation), Lower, cretions and aggregates. Graptolite fauna found in claystones Middle and Upper Muschelkalk, Lower Keuper (Sulechów indicates the gracilis Zone (Jamno IG 2) and the multidens Beds) and ?Upper Keuper (?Red Sandstein), and Drawno, Jar- Zone (Jamno IG 1 and Jamno IG 2), corresponding to the lo- kowo, Zb¹szynek and Wielichowo beds. -
Bayesian Node Dating Based on Probabilities of Fossil Sampling Supports Trans-Atlantic Dispersal of Cichlid Fishes
Supporting Information Bayesian Node Dating based on Probabilities of Fossil Sampling Supports Trans-Atlantic Dispersal of Cichlid Fishes Michael Matschiner,1,2y Zuzana Musilov´a,2,3 Julia M. I. Barth,1 Zuzana Starostov´a,3 Walter Salzburger,1,2 Mike Steel,4 and Remco Bouckaert5,6y Addresses: 1Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biosciences, University of Oslo, Oslo, Norway 2Zoological Institute, University of Basel, Basel, Switzerland 3Department of Zoology, Faculty of Science, Charles University in Prague, Prague, Czech Republic 4Department of Mathematics and Statistics, University of Canterbury, Christchurch, New Zealand 5Department of Computer Science, University of Auckland, Auckland, New Zealand 6Computational Evolution Group, University of Auckland, Auckland, New Zealand yCorresponding author: E-mail: [email protected], [email protected] 1 Supplementary Text 1 1 Supplementary Text Supplementary Text S1: Sequencing protocols. Mitochondrial genomes of 26 cichlid species were amplified by long-range PCR followed by the 454 pyrosequencing on a GS Roche Junior platform. The primers for long-range PCR were designed specifically in the mitogenomic regions with low interspecific variability. The whole mitogenome of most species was amplified as three fragments using the following primer sets: for the region between position 2 500 bp and 7 300 bp (of mitogenome starting with tRNA-Phe), we used forward primers ZM2500F (5'-ACG ACC TCG ATG TTG GAT CAG GAC ATC C-3'), L2508KAW (Kawaguchi et al. 2001) or S-LA-16SF (Miya & Nishida 2000) and reverse primer ZM7350R (5'-TTA AGG CGT GGT CGT GGA AGT GAA GAA G-3'). The region between 7 300 bp and 12 300 bp was amplified using primers ZM7300F (5'-GCA CAT CCC TCC CAA CTA GGW TTT CAA GAT GC-3') and ZM12300R (5'-TTG CAC CAA GAG TTT TTG GTT CCT AAG ACC-3'). -
PDF Linkchapter
Index 2-D Gravity Inversion: p. 656 Austroalpine system: p. 718, 719 Austroalpine units: p. 19, 30, 31 Austroalpine wedge toe: p. 720 A Autochthonous Paleogene: p. 77–80 Accommodation space: p. 493 Autochthonous unit: p. 354, 355, 380, 390 Accretionary prism: p. 28, 787, 795, 801, 804, 805 Avalonia: p. 11, 17, 19 Accretionary wedge: p. 720, 724 Amplitude vs. offset analyses: p. 625 Active continental margins: p. 67 Active rifting: p. 738, 739 B Adam oil mine (oil, gas field): p. 820 Babche fold: p. 463 Aderklaa Conglomerate: p. 195, 198, 207, 208, 587 Adnet Member: p. 578 Babica Clays: p. 238 Adria (Apulia): p. 12, 21, 31 Bacau: p. 527 Advancing Carpathian orogen: p. 767 Bacau County: p. 522 African Plate: p. 21, 642, 670, 789 Back arc: p. 720, 726 African shelf: p. 636 Back arc basin: p. 63 Afro-Arabic lithospheric plate: p. 585 Back thrusting: p. 112, 117, 720 Alabama-Oklahoma transform fault: p. 795 Backthrust system: p. 514 Albanian foredeep: p. 116 Bacterial sulfate reduction: p. 438 Albinov Tuff: p. 588 Baden Clay: p. 622 ALCAPA (Alcapa) terrane (supertarrane, microplate): p. 21, 31, 33, 35, 223, 700, Badenian: p. 198, 307, 313, 315, 317, 324, 329, 333, 337, 340, 612 743, 802, 804 Badenian evaporates: p. 316, 325, 327, 329, 330 Algyo field: p. 619, 620, 622, 623, 625, 627, 629, 630, 631 Badenian (Langhian) marine transgression: p. 337 Algyo Formation: p. 623 Bahneanu Sandstone: p. 546 Algyo high: p. 620, 621, 622, 623, 624, 627, 630 Bailesti Depression: p. 531, 534 Alkaline volcanism: p. -
Probable Existence of a Gondwana
J. Earth Syst. Sci. (2017) 126:81 c Indian Academy of Sciences DOI 10.1007/s12040-017-0866-3 Probable existence of a Gondwana transcontinental rift system in western India: Implications in hydrocarbon exploration in Kutch and Saurashtra offshore: A GIS-based approach S Mazumder1,* , Blecy Tep1, K K S Pangtey1,KKDas2 and DSMitra1 1Remote Sensing and Geomatics, KDMIPE, ONGC, Dehradun 248 195, India. 2Sedimentology Division, KDMIPE, ONGC, Dehradun 248 195, India. *Corresponding author. e-mail: [email protected] MS received 31 October 2016; revised 21 February 2017; accepted 5 March 2017; published online 31 August 2017 The Gondwanaland assembly rifted dominantly during Late Carboniferous–Early Permian forming several intracratonic rift basins. These rifts were subsequently filled with a thick sequence of continental clastic sediments with minor marine intercalations in early phase. In western part of India, these sediments are recorded in enclaves of Bikaner–Nagaur and Jaisalmer basins in Rajasthan. Facies correlatives of these sediments are observed in a number of basins that were earlier thought to be associated with the western part of India. The present work is a GIS based approach to reconnect those basins to their position during rifting and reconstruct the tectono-sedimentary environment at that time range. The study indicates a rift system spanning from Arabian plate in the north and extending to southern part of Africa that passes through Indus basin, western part of India and Madagascar, and existed from Late Carboniferous to Early Jurassic. Extensions related to the opening of Neo-Tethys led to the formation of a number of cross trends in the rift systems that acted as barriers to marine transgressions from the north as well as disrupted the earlier continuous longitudinal drainage systems. -
Coastal Change on the Time Scale of Decadesto Millennia in the Late Quaternary
Acknowledgements Program Contents Authors Navigation tips THENON-STEADYSTATEOFTHEINNERSHELFANDSHORELINE: COASTALCHANGEONTHETIMESCALEOFDECADESTOMILLENNIA1 November 9-12, 1999 University of Hawaii, Honolulu, Hawaii A conference held as part of International Geological Correlation Programme, Project 437: Coastal Environmental Change During Sea-Level Highstands: A Global Synthesis With Implications For Management of Future Coastal Change ORGANIZING COMMITTEE: Charles H. Fletcher, III (Chip), Conference Chairman Colin V. Murray-Wallace, Leader IGCP Project #437 (1999 - 2004) Orson van de Plassche, Leader IGCP Project #247 (1988-1993) 1 This PDF version of the abstracts volume differs in pagination and format from the printed version. The correct citation is: Fletcher, C.H. and Matthews, J.V. (editors), 1999. The Non-steady State of the Inner Shelf and Shoreline: Coastal Change on the Time Scale of Decadesto Millennia in the late Quaternary. PDF version of Abstracts with Programs, Inaugural Meeting of IGCP Project #437 "Coastal Environmental Change During Sea Level Highstands," University of Hawaii, Honolu- lu, USA, Nov. 9-12, 230p. Acknowledgements Program Contents Authors Navigation tips Acknowledgements and Introductory Statements ACKNOWLEDGEMENTS: This meeting and planning workshop could not have been possible without the generous financial support of 1) Geology and Paleontology Program of the National Science Foundation 2) U.S. Geological Survey Coastal and Marine Geology Program 3) Hawaii Sea Grant College 4) University of Hawaii Department of Geology and Geophysics The Organizing Committee is sincerely appreciative of the skilled assistance provided by Janet Kwak and Lauren Hirao for handling the planning and logistical needs of the conference, and for the outstanding graphics and publication efforts of May Izumi and Brooks Bays. -
Memoirs of the Geological Survey of India
: MEMOIRS OF THE GEOLOGICAL SURVEY OF INDIA. VOLUME XXXV, PART i. GEOLOGICAL'SURVEY OF INDIA. Director. C. L. Griesbach, C.I.E., F.G.S. Superintendents. R. D. Oldham, A.R.S.M., F.G.S. : Tom D. La Touche, B.A. (Cantab), F.G.S. C. S. Middlemiss, B.A. (Cantab). Deputy Superintendents. P. N. Bose, B Sc. (London), F.G.S. T. H. Holland, A.R.C.S., F.G.S.: P. N. Datta, B.Sc. (London), F.G.S.; F. H. Smith, A.R.C.S. Assistant Superintendents. II. H. Hayden, B.A., B.E. : E. Vredenburg, B.L., B.Sc. (Paris), A.R.C.S. Palaeontologist. Fritz Noetling, Ph.D. (Bertin), F.G.S. Specialist. R. R. Simpson, B.Sc. (Dunelm). Sub-Assistants. Hira Lal : Kishen Singh, F.G.S. Artist. Assistant Curator. H . B. W. Garrick. T. R. Blyth. Registrar. A. E. MacA Audsley. Geological Museum, Library, and Office, Calcutta. 1 t [)[,'; IQ02. — MEMOIRS OF THE GEOLOGICAL SURVEY OF INDIA. Vol. I. Royal 8vo, pp. 309, 1859 (out of print). Pt. I, 1856 (price I Re.) : Preliminary notice on the Coal and Iron of Talchir.—On the geological structure and relations of the Talchir Coal-field. — Gold-yielding deposits of Upper Assam. On specimens of gold and gold dust from Shue-gween. Pt. 2, 1858 {price 2 Rs.) : On the geological structure of a portion of the Khasi Hills. —On the geological structure of the Nilghiri Hills (Madras). Pt. 3, 1859 {price 2 Rs.) : On the geological structure and physical fes 'res of the districts of Bankura, Midnapore and Orissa.