Paleozoic Species of Bairata and Related Genera
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Devonian Bryozoans of the Holy Cross Mountains, Poland
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. XVIII 1973 No.4 MARIA KIEPURA DEVONIAN BRYOZOANS OF THE HOLY CROSS MOUNTAINS, POLAND. PART II. CYCLOSTOMATA AND CYSTOPORATA Abstract. - Descriptions are given of 33, species of Middle Devonian Bryozoa from the Holy Cross Mts., belonging to the orders Cyclostomata and Cystoporata. Cyclo stomata are represented by 26 species (4 new: Corynotrypa (Corynotrypa) skalensis, C. (C.) basiplata, Stomatopora varigemmata and Diversipora bitubulata n. gen.). Cystoporata are represented by 7 new species: Ceramoporella orbiculata, C. grandi cystica, Favositella integrimuralis, Fistulipora boardmani, F. emphantica, Cyclotrypa nekhoroshevi and Fistuliramus astrovae. The systematic assignment of the genus Hederella Hall, 1881 has been discussed and the "tabulate-like" microstructure of the zooecial walls of this genus examined. In addition, the epifauna and associated assemblages have been characterized as well as the geological and palaeoecological conditions in which the described Bryozoa occurred. INTRODUCTION Among the Middle Devonian Bryozoa of the Holy Cross Mts., the present author has, up to now, described Ctenostomata (Kiepura, 1965). The present paper is a continuation of her investigations on the Middle Devonian Bryozoa of this region and contains descriptions of 33 species belonging to 9 genera of the orders Cyclostomata and Cystoporata occur ring in the Grzegorzowice - Skaly profile. The bryozoan collection of the Palaeozoological Institute of the Polish Academy of Sciences also contains a rich material representing the orders Trepostomata and Cryptostomata from the Middle Devonian of the Holy Cross Mts., which will be described at a future date. The material described in the present paper was collected by the author during several years of fieldwork (1950-1954). -
Environmental Overview Data
ENVIRONMENTAL OVERVIEW DATA for LYON and CALDWELL COUNTIES US 641 CORRIDOR FROM EDDYVILLE TO FREDONIA ITEM NUMBER: NOT ASSIGNED Prepared For KENTUCKY TRANSPORTATION CABINET DIVISION OF PLANNING Prepared By Palmer Engineering 400 Shoppers Drive Winchester, Kentucky 40392 859-744-1218 JUNE 2004 Revised July 2004 TABLE OF CONTENTS Introduction....................................................................................................................................1 General Characteristics of the Project and Project Area ..........................................................1 Project Description and Purpose......................................................................................1 Project Area Physiological and Soils Characteristics.....................................................4 Project Area Water Resources .........................................................................................7 Project Area Land Use ......................................................................................................7 Environmental Overview Considerations....................................................................................7 Land Use .........................................................................................................................................7 Air Quality Considerations ...............................................................................................8 Highway Noise Considerations .........................................................................................9 -
Ostracoda of the Limestones of the Permian System
OSTRACODA OF TEE / . SY, .D DAVIS . ., Aanaas State Colic of .~'C and Applied Science, 1950 A THESIS submitted in partial fulf illnent of tlie re, - I -ts for the decree [ Department of Geology and Geography K . : COLLEGE OP AGRICUL LIED SCIENCE • :' LO T4 i Pua i or t i Area Covered h .3 Irrv nation ••••••• 1 Stra ;!it ••••••••«•••••• 3 Pi. ads La • Methods* ••••• •• Identification of the - % *•#*«•*# ll|, . , 17 . Stra c DIstx- • . ..-oi'ossiln. « . s . 9k . .rposo o I Xxxvefl tion This investigation of the ostracode r.iicrofauna C . 10 line stones of the WoIfcamp seizes In Kansas v;as undertaken to obtain data on the abundance, and the strati/graphic and paloo- ccolocical distribution of the ostracodes. pus Studies of microfaunas have been devoted almost exclusively to bods of shale with only scattered sampling of the limestone..; of ore, it was felt that an investigation of this nature would add to our know- ledge of the micropaleontology of ostracodes. The spars ity of information on techniques of samolinr and prepax^ing limestones for mieropaleontological examination were other factors which posed a problem. It was fully realised that this problem would necessitate various trial and error methods both in the field and laboratory before a satisfactory technique could be developed. Although the main emphasis of the study was to be . ;n to the ostracodes of the limestones, other mierofossiis were not to be die . _'ded; on the contrary, they night yield valuable strat- -•aphic information, She forms, other than ostracodes, consid- ered to be most valuable stratigraphlcally were the foraminifers and the conodonts. -
Palaeoecology of a Hypersaline Carboniferous Ostracod Fauna
J.rnicropalueontol., 6(2): 29-33, November 1987 Palaeoecology of a hypersaline Carboniferous ostracod fauna Chris P. Dewey Department of Geology and Geography, Mississippi State University, Mississippi State, MS 39762, U.S.A. ABSTRACT- A high abundance, low diversity ostracod fauna has been collected from the Lower Carboniferous Dimock and Phillips limestones in Nova Scotia, Canada. The ostracod fauna consists of Paraparchites sp. aff. P. kellettae Sohn and Beyrichiopsis lophota Copeland, as well as rare specimens of Acratia acuta (Jones & Kirkby), Bythocypris aequalis (Jones & Kirkby), and Chamishaella sirborbiculata (Munster). Growth parameters for the dominant ostracod, Paraparchites sp. aff. P. kellettae, show that a multi-generation, progenetic, parthenogenetic population developed. This reproduc- tive strategy caused rapid population growth and thereby allowed the species to take advantage of the available environmental resources. When considered together, the ostracod fauna and the sedimentology indicate that physiologically stressful hypersaline conditions prevailed. The combined data therefore provide evidence for hypersalinity tolerance and heterochronous development amongst Carboniferous ostracods. INTRODUCTION (Dewey, 1983, 1985, in press). Most of the assemblages Lower Carboniferous deposits in the Maritime Basin are dominated by paraparchitacean ostracods, which of Nova Scotia, Canada, document a series of eustati- are often considered to be indicative of nearshore cally controlled, transgressive-regressive cycles (Giles, environments (van Ameron ef d..1Y70; Becker et af., 1981). Tectonic activity resulted in the development of 1974; Bless, 1983). several interconnected sub-basins (Howie & Barss, This paper exam i n e s t 11 e para parch i t a c ea n - 1975; Bradley, 1982). Consequently. the complex dominated ostracod fauna of a carbonate sabkha interaction of eustacy, tectonism and climate resulted environment from the Windsor Group of the Minas- in a range of palaeoenvironments that include alluvial Shubenacadie Sub-Basin in Nova Scotia (Fig. -
Columnals (PDF)
2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown. -
15 International Symposium on Ostracoda
Berliner paläobiologische Abhandlungen 1-160 6 Berlin 2005 15th International Symposium on Ostracoda In Memory of Friedrich-Franz Helmdach (1935-1994) Freie Universität Berlin September 12-15, 2005 Abstract Volume (edited by Rolf Kohring and Benjamin Sames) 2 ---------------------------------------------------------------------------------------------------------------------------------------- Preface The 15th International Symposium on Ostracoda takes place in Berlin in September 2005, hosted by the Institute of Geological Sciences of the Freie Universität Berlin. This is the second time that the International Symposium on Ostracoda has been held in Germany, following the 5th International Symposium in Hamburg in 1974. The relative importance of Ostracodology - the science that studies Ostracoda - in Germany is further highlighted by well-known names such as G.W. Müller, Klie, Triebel and Helmdach, and others who stand for the long tradition of research on Ostracoda in Germany. During our symposium in Berlin more than 150 participants from 36 countries will meet to discuss all aspects of living and fossil Ostracoda. We hope that the scientific communities working on the biology and palaeontology of Ostracoda will benefit from interesting talks and inspiring discussions - in accordance with the symposium's theme: Ostracodology - linking bio- and geosciences We wish every participant a successful symposium and a pleasant stay in Berlin Berlin, July 27th 2005 Michael Schudack and Steffen Mischke CONTENT Schudack, M. and Mischke, S.: Preface -
Taxonomy of Quaternary Deep-Sea Ostracods from the Western North Atlantic Ocean
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2009 Taxonomy Of Quaternary Deep-Sea Ostracods From The Western North Atlantic Ocean Moriaki Yasuhara National Museum of Natural History, Smithsonian Institution, [email protected] Hisayo Okahashi National Museum of Natural History, Smithsonian Institution, [email protected] Thomas M. Cronin U.S. Geological Survey, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Yasuhara, Moriaki; Okahashi, Hisayo; and Cronin, Thomas M., "Taxonomy Of Quaternary Deep-Sea Ostracods From The Western North Atlantic Ocean" (2009). USGS Staff -- Published Research. 242. https://digitalcommons.unl.edu/usgsstaffpub/242 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. [Palaeontology, Vol. 52, Part 4, 2009, pp. 879–931] TAXONOMY OF QUATERNARY DEEP-SEA OSTRACODS FROM THE WESTERN NORTH ATLANTIC OCEAN by MORIAKI YASUHARA*, HISAYO OKAHASHI* and THOMAS M. CRONIN *Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, PO Box 37012, Washington, DC 20013-7012, USA; e-mails: [email protected] or [email protected] (M.Y.), [email protected] (H.O.) U.S. Geological Survey, -
Spore-Pollen Biostratigraphy and Paleoecology of Mesozoic and Lower Tertiary Samples from the Surghar and Salt Ranges, Northern Pakistan
Spore-Pollen Biostratigraphy and Paleoecology of Mesozoic and Lower Tertiary Samples from the Surghar and Salt Ranges, Northern Pakistan By N.O. Frederiksen, U.S. Geological Survey T.P. Sheehan, U.S. Geological Survey V.A.S. Andrle, U.S. Geological Survey Chapter D of Regional Studies of the Potwar Plateau Area, Northern Pakistan Edited by Peter D. Warwick and Bruce R. Wardlaw Prepared in cooperation with the Geological Survey of Pakistan, under the auspices of the U.S. Agency for International Development, U.S. Department of State, and the Government of Pakistan Bulletin 2078–D U.S. Department of the Interior U.S. Geological Survey iii Contents Abstract ........................................................................................................................................................D1 Introduction.....................................................................................................................................................1 Acknowledgments ................................................................................................................................1 Previously Reported Ages of Formations ..................................................................................................1 Determination of Spore-Pollen Ages ..........................................................................................................3 Palynological Methods .................................................................................................................................5 -
Cypris 2016-2017
CYPRIS 2016-2017 Illustrations courtesy of David Siveter For the upper image of the Silurian pentastomid crustacean Invavita piratica on the ostracod Nymphateline gravida Siveter et al., 2007. Siveter, David J., D.E.G. Briggs, Derek J. Siveter, and M.D. Sutton. 2015. A 425-million-year- old Silurian pentastomid parasitic on ostracods. Current Biology 23: 1-6. For the lower image of the Silurian ostracod Pauline avibella Siveter et al., 2012. Siveter, David J., D.E.G. Briggs, Derek J. Siveter, M.D. Sutton, and S.C. Joomun. 2013. A Silurian myodocope with preserved soft-parts: cautioning the interpretation of the shell-based ostracod record. Proceedings of the Royal Society London B, 280 20122664. DOI:10.1098/rspb.2012.2664 (published online 12 December 2012). Watermark courtesy of Carin Shinn. Table of Contents List of Correspondents Research Activities Algeria Argentina Australia Austria Belgium Brazil China Czech Republic Estonia France Germany Iceland Israel Italy Japan Luxembourg New Zealand Romania Russia Serbia Singapore Slovakia Slovenia Spain Switzerland Thailand Tunisia United Kingdom United States Meetings Requests Special Publications Research Notes Photographs and Drawings Techniques and Methods Awards New Taxa Funding Opportunities Obituaries Horst Blumenstengel Richard Forester Franz Goerlich Roger Kaesler Eugen Kempf Louis Kornicker Henri Oertli Iraja Damiani Pinto Evgenii Schornikov Michael Schudack Ian Slipper Robin Whatley Papers and Abstracts (2015-2007) 2016 2017 In press Addresses Figure courtesy of Francesco Versino, -
Database of Bibliography of Living/Fossil
www.shark-references.com Version 16.01.2018 Bibliography database of living/fossil sharks, rays and chimaeras (Chondrichthyes: Elasmobranchii, Holocephali) Papers of the year 2017 published by Jürgen Pollerspöck, Benediktinerring 34, 94569 Stephansposching, Germany and Nicolas Straube, Munich, Germany ISSN: 2195-6499 DOI: 10.13140/RG.2.2.32409.72801 copyright by the authors 1 please inform us about missing papers: [email protected] www.shark-references.com Version 16.01.2018 Abstract: This paper contains a collection of 817 citations (no conference abstracts) on topics related to extant and extinct Chondrichthyes (sharks, rays, and chimaeras) as well as a list of Chondrichthyan species and hosted parasites newly described in 2017. The list is the result of regular queries in numerous journals, books and online publications. It provides a complete list of publication citations as well as a database report containing rearranged subsets of the list sorted by the keyword statistics, extant and extinct genera and species descriptions from the years 2000 to 2017, list of descriptions of extinct and extant species from 2017, parasitology, reproduction, distribution, diet, conservation, and taxonomy. The paper is intended to be consulted for information. In addition, we provide data information on the geographic and depth distribution of newly described species, i.e. the type specimens from the years 1990 to 2017 in a hot spot analysis. New in this year's POTY is the subheader "biodiversity" comprising a complete list of all valid chimaeriform, selachian and batoid species, as well as a list of the top 20 most researched chondrichthyan species. Please note that the content of this paper has been compiled to the best of our abilities based on current knowledge and practice, however, possible errors cannot entirely be excluded. -
The Joggins Cliffs of Nova Scotia: B2 the Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H
GAC-MAC-CSPG-CSSS Pre-conference Field Trips A1 Contamination in the South Mountain Batholith and Port Mouton Pluton, southern Nova Scotia HALIFAX Building Bridges—across science, through time, around2005 the world D. Barrie Clarke and Saskia Erdmann A2 Salt tectonics and sedimentation in western Cape Breton Island, Nova Scotia Ian Davison and Chris Jauer A3 Glaciation and landscapes of the Halifax region, Nova Scotia Ralph Stea and John Gosse A4 Structural geology and vein arrays of lode gold deposits, Meguma terrane, Nova Scotia Rick Horne A5 Facies heterogeneity in lacustrine basins: the transtensional Moncton Basin (Mississippian) and extensional Fundy Basin (Triassic-Jurassic), New Brunswick and Nova Scotia David Keighley and David E. Brown A6 Geological setting of intrusion-related gold mineralization in southwestern New Brunswick Kathleen Thorne, Malcolm McLeod, Les Fyffe, and David Lentz A7 The Triassic-Jurassic faunal and floral transition in the Fundy Basin, Nova Scotia Paul Olsen, Jessica Whiteside, and Tim Fedak Post-conference Field Trips B1 Accretion of peri-Gondwanan terranes, northern mainland Nova Scotia Field Trip B2 and southern New Brunswick Sandra Barr, Susan Johnson, Brendan Murphy, Georgia Pe-Piper, David Piper, and Chris White The Joggins Cliffs of Nova Scotia: B2 The Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H. Calder, M.R. Gibling, and M.C. Rygel Lyell & Co's "Coal Age Galapagos” B3 Geology and volcanology of the Jurassic North Mountain Basalt, southern Nova Scotia Dan Kontak, Jarda Dostal, -
Fossil Microbial Shark Tooth Decay Documents in Situ Metabolism Of
www.nature.com/scientificreports OPEN Fossil microbial shark tooth decay documents in situ metabolism of enameloid proteins as nutrition source in deep water environments Iris Feichtinger1*, Alexander Lukeneder1, Dan Topa2, Jürgen Kriwet3*, Eugen Libowitzky4 & Frances Westall5 Alteration of organic remains during the transition from the bio- to lithosphere is afected strongly by biotic processes of microbes infuencing the potential of dead matter to become fossilized or vanish ultimately. If fossilized, bones, cartilage, and tooth dentine often display traces of bioerosion caused by destructive microbes. The causal agents, however, usually remain ambiguous. Here we present a new type of tissue alteration in fossil deep-sea shark teeth with in situ preservation of the responsible organisms embedded in a delicate flmy substance identifed as extrapolymeric matter. The invading microorganisms are arranged in nest- or chain-like patterns between fuorapatite bundles of the superfcial enameloid. Chemical analysis of the bacteriomorph structures indicates replacement by a phyllosilicate, which enabled in situ preservation. Our results imply that bacteria invaded the hypermineralized tissue for harvesting intra-crystalline bound organic matter, which provided nutrient supply in a nutrient depleted deep-marine environment they inhabited. We document here for the frst time in situ bacteria preservation in tooth enameloid, one of the hardest mineralized tissues developed by animals. This unambiguously verifes that microbes also colonize highly mineralized dental capping tissues with only minor organic content when nutrients are scarce as in deep-marine environments. Teeth and bones are ofen the only evidence of ancient vertebrate life because of the mineralized nature of tissues. Tere are numerous possibilities for chemical alteration during the transition from the bio- to the lithosphere of which bacterial catabolysis of these tissues and organic matter within the carcass is an important example 1,2.