Apertural Constrictions in Some Oncocerid Cephalopods
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Nautiloid Shell Morphology
MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOWER STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOIVER 1964 STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EXOFFICIO THEHONORABLEJACKM.CAMPBELL ................................ Governor of New Mexico LEONARDDELAY() ................................................... Superintendent of Public Instruction APPOINTEDMEMBERS WILLIAM G. ABBOTT ................................ ................................ ............................... Hobbs EUGENE L. COULSON, M.D ................................................................. Socorro THOMASM.CRAMER ................................ ................................ ................... Carlsbad EVA M. LARRAZOLO (Mrs. Paul F.) ................................................. Albuquerque RICHARDM.ZIMMERLY ................................ ................................ ....... Socorro Published February 1 o, 1964 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.50 Contents Page ABSTRACT ....................................................................................................................................................... 1 INTRODUCTION -
CR #15 Palaeontological Impact Assessment
PALAEONTOLOGICAL ASSESSMENT Graymont Western Canada Inc. Parsons Creek Resources Project Township 90, Range 9, W4M Permit Number Bohach-2007-05 FMA1646.PL07 Prepared For Graymont Western Canada Inc. #200, 10991 Shellbridge Way Richmond, British Columbia On Behalf Of Millennium EMS Solutions Ltd. 208, 4207-98th Street Edmonton, Alberta Prepared By FMA Heritage Resources Consultants Inc. 200, 1719-10th Avenue S.W. Calgary, Alberta July 2008 Executive Summary The proposed Parsons Creek Resources Project (the Project) was assessed for potential impacts to palaeontological resources by field surveys on August 14 to 15, 2007 and examination of the drill cores on October 16, 2007. The Project is a limestone mine and processing facility located along the north boundary of the City of Fort McMurray, mainly within Township 90, Range 9, West of the Fourth Meridian. The Project is situated on relatively flat ground within the Athabasca River valley. It will mine limestone of Devonian age from the Moberly Member of the Waterways Formation. The Moberly Member contains fossiliferous limestone layers and the fossils within these layers will be destroyed when the rock is crushed and processed. Most of the fossils are invertebrates, which are relatively common fossils and individual specimens are typically not unique. This is in contrast to vertebrate fossils, which are rare by comparison and each specimen can provide unique information about the species. Baseline reconnaissance surveys found fossils of medium to high heritage value in exposures along the Athabasca River, including: • previously unrecorded fish fossils from Unit M II • exceptionally preserved brachiopods with intact spines and original colour patterns from Unit M IV • exceptionally preserved brachiopod death horizons from Unit M V Executive Summary i Executive Summary ii Without mitigation, negative effects on palaeontological resources are expected. -
Palaeontological Impact Assessment
PALAEONTOLOGICAL ASSESSMENT Graymont Western Canada Inc. Parsons Creek Resources Project Township 90, Range 9, W4M Permit Number Bohach-2007-05 FMA1646.PL07 Prepared For Graymont Western Canada Inc. #200, 10991 Shellbridge Way Richmond, British Columbia On Behalf Of Millennium EMS Solutions Ltd. 208, 4207-98th Street Edmonton, Alberta Prepared By FMA Heritage Resources Consultants Inc. 200, 1719-10th Avenue S.W. Calgary, Alberta July 2008 Executive Summary The proposed Parsons Creek Resources Project (the Project) was assessed for potential impacts to palaeontological resources by field surveys on August 14 to 15, 2007 and examination of the drill cores on October 16, 2007. The Project is a limestone mine and processing facility located along the north boundary of the City of Fort McMurray, mainly within Township 90, Range 9, West of the Fourth Meridian. The Project is situated on relatively flat ground within the Athabasca River valley. It will mine limestone of Devonian age from the Moberly Member of the Waterways Formation. The Moberly Member contains fossiliferous limestone layers and the fossils within these layers will be destroyed when the rock is crushed and processed. Most of the fossils are invertebrates, which are relatively common fossils and individual specimens are typically not unique. This is in contrast to vertebrate fossils, which are rare by comparison and each specimen can provide unique information about the species. Baseline reconnaissance surveys found fossils of medium to high heritage value in exposures along the Athabasca River, including: • previously unrecorded fish fossils from Unit M II • exceptionally preserved brachiopods with intact spines and original colour patterns from Unit M IV • exceptionally preserved brachiopod death horizons from Unit M V Executive Summary i Executive Summary ii Without mitigation, negative effects on palaeontological resources are expected. -
FOSSILS and STRATA 18 (1985) Silurian Oncocerid Cephalopods Fr Om Gotland 5
FOSSILS AND STRATA Editor science without national limitations or preferences. Fossils and Strata, howeve r, is an outlet fo r more comprehensive systematic and regional Stefan Bengtson, Institute of Palaeontology, Box 558, descriptions dealing with areas in the five countries of Norden, or S-751 22 Uppsala, Sweden. writ ten by palaeontologists and stratigraphers from these countries. Contributions by colleagues in other countries may also be included as Editorial and administrative board far as this series is deemed to be the appropriate medium with regard to distribution and availability. Articles can normally be accepted only if Stefan Bengtson (Uppsala), Fredrik Bockelie (Bergen), and they are heavily subsidized by the national Research Council in their country of origin or by other fu nds. All income is re-invested in Valdemar Poulsen (Copenhagen). fo rthcoming numbers of the series. Manuscripts intended fo r typographical composition should con Publisher fo rm with the Instructions on page 3 0fthis cover, which are essentially the same as fo r Boreas and Lethaia. Manuscripts to be printed from Universitetsforlaget, Postboks 2959, Tøyen, Oslo 6, Norway. camera-ready typescript are also accepted but necessitate contacts with the editor at the ear!iest stage of manuscript planning. Articles in English, German, and French are accepted; the use of the Fossils and Strata is an internationally distributed series ofmonographs English language is preferred. A card abstraet in English should always and memoirs in palaeontology and stratigraphy. It is issued in Numbers be provided, and non-English artic!es should always be provided with with individual pagination, listed cumulatively on the back of each English versions of the figure captions. -
Middle and Upper Ordovician Nautiloid Cephalopods of the Cincinnati Arch Region of Kentucky, Indiana, and Ohio
Middle and Upper Ordovician Nautiloid Cephalopods of the Cincinnati Arch Region of Kentucky, Indiana, and Ohio U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1066-P Prepared in cooperation with the Commonwealth ofKentucky, University ofKentucky, and Kentucky Geological Survey AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current- year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publica tions released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may be no longer available. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey offices, of general interest (such as leaflets, pamphlets, booklets), single all of which are authorized agents of the Superintendent of copies of Earthquakes & Volcanoes, Preliminary Determination of Documents: Epicenters, and some miscellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • ANCHORAGE, Alaska—Rm. -
Origin of the Cephalopoda
ACTA PALAEONTOLOGICA- POLONICA Vol. 26 198 1 No. 2 JERZY DZIK ORIGIN OF THE CEPHALOPODA DZIK, J.: Origin of the Cephalopoda. Acta Palaeont. Polonica 26, 2, 161-191. Cephalopods are postulated to have evolved from planktic monoplacophorans pos- sibly related to the circothecid hyoliths. It is suggested that secretion of a liquid characterized by a density lower than sea water preceded development of a gas containing phragmocone. Phragrnocone formation was due to a prolongation of the functioning of the larval hydrostatic apparatus in the adult stages. Attach- ment of the larval pedal retractor to the apex of the larval shell was a reason why the soft tissue (siphon) remained in the apical parts of the shell and was subsequently surrounded by diaphragms (septa). A possible mode of producing of the light liquid is removal of salt by an ionic pump. The origin of the rhythmic alteration in the septa and liquid seoretio~was the next step. An osmotic pressure caused by removal of salt from the liquid resulted in slow removal of camera1 liquid from older chambers and diffusion of gas from the liquid under conditions of lowered pressure. A model for the evolutionary trans- formation of the monoplacophoran operculum into the cephalopod lower jaw is presented. Externally calcifying aptychi of the Palaeozoic orthoceratids and the Mesozoic ammonites were produced in the same way 2s opercula of Recent gastro- pods Natica and Turbo. The early evolution of the class is reviewed. K e y w o r d s: Origin, Cephalopoda, Nautiloidea, phylogeny, phragmocone, larval development, aptychi, jaws. Jerzy Dzik, Zaktad Paleobiologii, Polska Akademia Nauk, Al. -
Northern Gondwanan Siluro-Devonian Palaeogeography Assessed by Cephalopods
Palaeontologia Electronica http://palaeo-electronica.org NORTHERN GONDWANAN SILURO-DEVONIAN PALAEOGEOGRAPHY ASSESSED BY CEPHALOPODS Maurizio Gnoli Department of the Museum of Paleobiology and Botanical Garden (Palaeontology), Modena and Reggio Emilia University, Italy, e-mail: [email protected] ABSTRACT Worldwide distribution of cephalopod limestone biofacies distribution is used herein to assess the reconstruction of the North Gondwana margin, with implications for southern hemisphere palaeobiogeography during the Silurian-Early Devonian. Three areas are of concern: the Tinduf Basin (Northwest Sahara, Morocco), the Uppony Mountains (Northeast Hungary), and perhaps the Ukrainian continental plat- form, which may have been part of northern Gondwana. Key words – Palaeobiogeography, cephalopod biofacies, faunal similarity Gondwana. Copyright: Palaeontological Association. 14 March 2003 Submission: 28 March 2003 Acceptance: 24 October 2002 INTRODUCTION persal patterns in the Ludford-Prídolí interval and Silurian-Devonian boundary (Richardson et al. During the Silurian-Early Devonian, cephalo- 2001), Silurian stromatoporoids (Nestor 1990), pod limestone biofacies represent one of the best Devonian stromatoporoids (Stock 1990), rugose documented sedimentary deposits in the strati- corals (Pedder and Oliver 1990), algae (Poncet graphic column. Reconstruction of the northern 1990), and Early-Middle Devonian gastropods margin of Gondwana by means of cephalopod (Blodgett et al. 1990). Nevertheless, in his discus- limestone biofacies also represents one of the sion of Silurian biogeography Boucot (1990, pp. most interesting topics of Early Palaeozoic palaeo- 191-196) noted that, “A number of potentially use- biogeography. ful groups such as the nautiloids and stony bryozo- Several authors have investigated the geo- ans remain largely unstudied.” As reported graphical position of various fossil groups during previously by Holland (1971, p. -
Biostratigraphy of British Silurian Nautiloid Cephalopods
Bollettino della Società Paleontologica Italiana, 53 (1), 2014, 19-26. Modena Biostratigraphy of British Silurian nautiloid cephalopods Charles Hepworth HOLLAND C.H. Holland, Department of Geology, Trinity College, Dublin 2, Ireland; [email protected] KEY WORDS - Nautiloid cephalopods, Silurian, Britain, biostratigraphy. ABSTRACT - Distribution of nautiloid cephalopods in the Silurian of England, Wales, and Scotland is reviewed stratigraphically and geographically. Genera are considered first and then species. Seven orders are present: Endocerida (one genus), Actinocerida (three), Orthocerida (17), Ascocerida (one), Oncocerida (at least ten), Discocerida (three), and Tarphycerida (seven). Wenlock and Ludlow faunas are more abundant than those of the Llandovery. Records from the Pridoli are very rare. RIASSUNTO - [Biostratigrafia a cefalopodi nautiloidi nel Siluriano della Gran Bretagna] - La distribuzione dei cefalopodi nautiloidi nel Siluriano dell’Inghilterra, Galles e Scozia viene qui rivista in termini stratigrafici e geografici. L’analisi è stata fatta a livello generico e poi specifico. Sette ordini sono documentati: Endocerida (un genere), Actinocerida (tre), Orthocerida (17), Ascocerida (uno), Oncocerida (almeno dieci), Discocerida (tre) e Tarphycerida (sette). Le faune del Wenlock e del Ludlow sono più abbondanti di quelle del Llandovery. Le testimonianze dei nautiloidi del Pridoli sono invece rare. INTRODUCTION the oldest part of the series, which have yielded very few examples of a relict cephalopod fauna confined This paper records the results of long examination of to the Order Orthocerida. It includes Cyrtocycloceras, British Silurian nautiloid cephalopods, including those Kionoceras, Leurocycloceras, Orthocycloceras, and from the large collections of the Natural History Museum Polygrammoceras (Holland, 2000a). in London, the British Geological Survey at Keyworth, and the Shropshire County Museum at Ludlow, as well as material from many other museum and university DISTRIBUTION OF GENERA collections. -
Revision of Middle Ordovician Orthoceratacean Nautiloids from Baltoscandia
Revision of Middle Ordovician orthoceratacean nautiloids from Baltoscandia BJÖRN KRÖGER Kröger, B. 2004. Revision of Middle Ordovician orthoceratacean nautiloids from Baltoscandia. Acta Palaeontologica Polonica 49 (1): 57–74. The fauna of the Baltoscandic Orthocerataceae is important because it fills a documentary gap between the Lower Ordo− vician fauna of North America and the upper Middle Ordovician fauna of China and North America. A revision of the Orthoceratidae, Geisonoceratidae, and Arionoceratidae is given on a material of more than 450 specimens. Intraspecific and ontogenetic variations were observed. The following new taxa are erected: Plagiostomoceras fragile sp. nov., Archigeisonoceras repplingense sp. nov., Archigeisonoceras picus sp. nov. Archigeisonoceras folkeslundense sp. nov., Nilssonoceras latisiphonatum gen. et sp. nov., Kinnekulloceras kinnekullense gen. et sp. nov., and Arionoceras lotskirkense sp. nov. The genus Archigeisonoceras is described for the first time in the Baltoscandic area and the oldest occurrence of the genus Arionoceras is documented from the Middle Ordovician of Baltoscandia. It is shown that the endosiphuncular deposits of the Middle Ordovician orthoceratacaceans are highly variable and widespread in the apical parts of the phragmocone. Key words: Cephalopoda, Nautiloidea, Orthoceratacea, Ordovician, Baltoscandia. Björn Kröger [[email protected]],Geologisch−Paläontologisches Institut und Museum,Universität Hamburg,Bunde − sstr. 55, D−20146 Hamburg, Germany. Introduction Mutvei (1982), of the Siljan District of Dalarna by Jaanusson (1965a), and of Östergotland and Närke by Tjernvik (1956). The Baltoscandic Orthoceratite Limestone is a thinly bedded Information on the stratigraphical zonation and origin of limestone or calcareous shale which is in parts extremely rich the erratics of northern Poland and northern Germany were in macrofossils. -
Northern Gondwanan Siluro-Devonian Palaeogeography Assessed by Cephalopods
Palaeontologia Electronica http://palaeo-electronica.org NORTHERN GONDWANAN SILURO-DEVONIAN PALAEOGEOGRAPHY ASSESSED BY CEPHALOPODS Maurizio Gnoli Department of the Museum of Paleobiology and Botanical Garden (Palaeontology), Modena and Reggio Emilia University, Italy, e-mail: [email protected] ABSTRACT Worldwide distribution of cephalopod limestone biofacies distribution is used herein to assess the reconstruction of the North Gondwana margin, with implications for southern hemisphere palaeobiogeography during the Silurian-Early Devonian. Three areas are of concern: the Tinduf Basin (Northwest Sahara, Morocco), the Uppony Mountains (Northeast Hungary), and perhaps the Ukrainian continental plat- form, which may have been part of northern Gondwana. Key words – Palaeobiogeography, cephalopod biofacies, faunal similarity Gondwana. Copyright: Palaeontological Association. 14 March 2003 Submission: 28 March 2002 Acceptance: 24 October 2002 INTRODUCTION persal patterns in the Ludford-Prídolí interval and Silurian-Devonian boundary (Richardson et al. During the Silurian-Early Devonian, cephalo- 2001), Silurian stromatoporoids (Nestor 1990), pod limestone biofacies represent one of the best Devonian stromatoporoids (Stock 1990), rugose documented sedimentary deposits in the strati- corals (Pedder and Oliver 1990), algae (Poncet graphic column. Reconstruction of the northern 1990), and Early-Middle Devonian gastropods margin of Gondwana by means of cephalopod (Blodgett et al. 1990). Nevertheless, in his discus- limestone biofacies also represents one of the sion of Silurian biogeography Boucot (1990, pp. most interesting topics of Early Palaeozoic palaeo- 191-196) noted that, “A number of potentially use- biogeography. ful groups such as the nautiloids and stony bryozo- Several authors have investigated the geo- ans remain largely unstudied.” As reported graphical position of various fossil groups during previously by Holland (1971, p.