Dental Diversity in Early Chondrichthyans
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Memoirs of the National Museum, Melbourne January 1906
Memoirs of the National Museum, Melbourne January 1906 https://doi.org/10.24199/j.mmv.1906.1.01 ON A CARBONIFEROUS FISH-FAUNA FROM THE MANSFIELD DISTRICT, VICTORIA. f BY AWL'HUR SJnTu T oomYARD, LL.D., F.U..S. I.-IN'l1RODUC'I1ION. The fossil fish-remains colloctocl by 1fr. George Sweet, F.G.S., from the reel rncks of the Mansfield District, are in a very imperfect state of presern1tion. 'J1lic·y vary considerably in appea1·a11co according to the Hature of the stratum whence they were obtained. 'l'he specimens in the harder ealcm-oous layers retain their original bony ot· ealcifiocl tissue, which ndhores to tbe rock ancl cannot readily ho exposed without fractnre. 'l'he remains hnriecl in the more fcrruginous ancl sanely layers have left only hollmv moulds of their outm1rd shape, or arc much doeayod and thus Yeq difficult to recognise. MoreQvor, the larger fishes arc repr0sontNl only hy senttcrocl fragments, while the smaller fishes, eYon when approximately whole, arc more or less distorted and disintcgrato(l. Under these circumstancPs, with few materials for comparison, it is not Rnrprising that the latt: Sil' Broderick McCoy should haYe failed to pnbJii.,h a sntisfactory a(•eount of the Mansfield eollection. \Yith great skill, ho sPlcctcd nearly all the more important specimens to be drawn in the series of plates accom panying the present memoir. II0 also instructed ancl snp0rvif-ecl the artist, so thnt moRt of' tbc pl'ineipnl foaturcs of the fossils "\Yore duly 0111phasisc•cl. IIis preliminary determinations, however, published in 1800, 1 arc now shown to have been for the most part erroneous; while his main conelusions as to the affinities of 1 F. -
Biostratigraphy of Some Early Middle Silurian Ostracoda, Eastern Canada PART 11- Additional Silurian Arthropoda from Arctic and Eastern Canada
This document was produced by scanning the original publication. Ce document est Ie produit d'une numerisation par balayage de la publication originale. BULLETIN 200 PART I - Biostratigraphy of some early Middle Silurian Ostracoda, eastern Canada PART 11- Additional Silurian Arthropoda from Arctic and eastern Canada M. J. Copeland Ottawa Canada Price $1.50 1971 PART I - Biostratigraphy of some Early Middle Silurian Ostracoda, eastern Canada PART II-Additional Silurian Arthropoda from Arctic and eastern Canada 1,IOO.1970.6119 GEOLOGICAL SURVEY OF CANADA BULLETIN 200 PART I - Biostratigraphy of some Early Middle Silurian Ostracoda, eastern Canada PART II-Additional Silurian Arthropoda from Arctic and eastern Canada By M. J. Copeland DEPARTMENT OF ENERGY, MINES AND RESOURCES CANADA © Crown Copyrights reserved Available by mail from Information Canada, Ottawa, from neological Survey of Canada, 601 Booth St., Oltawa. and at the following Information Canada bookshops: HALIFAX 1735 Barrington Street MONTREAL Mterna-Vie Building, 1182 St. Catherine Street West OITAWA 171 Slater Street TORONTO 221 Yonge Street WINNIPEG Mall Center Building, 499 Portage Avenue VANCOUVER 657 Granville Street or through your bookseller A deposit copy of this publication is also available for reference in public libraries across Canada Price: $1.50 Catalogue No. M42-200 Price subject to change without notice Information Canada Ottawa, 1971 PREFACE As more detailed information is obtained on the stra tigraphic occurrence and systematic paleontology of Paleozoic Arthropoda, it is increasingly evident that these forms present a useful key for determining the paleontological zonation and age relationships of the enclosing rocks. They are particularly important in strata of lacustrine, brackish, or restricted marine environments in which rapidly evolving leperditiid ostra codes, eurypterids, and phyllocarids may occur to the exclusion of other distinctive faunal elements. -
Revised Correlation of Silurian Provincial Series of North America with Global and Regional Chronostratigraphic Units 13 and D Ccarb Chemostratigraphy
Revised correlation of Silurian Provincial Series of North America with global and regional chronostratigraphic units 13 and d Ccarb chemostratigraphy BRADLEY D. CRAMER, CARLTON E. BRETT, MICHAEL J. MELCHIN, PEEP MA¨ NNIK, MARK A. KLEFF- NER, PATRICK I. MCLAUGHLIN, DAVID K. LOYDELL, AXEL MUNNECKE, LENNART JEPPSSON, CARLO CORRADINI, FRANK R. BRUNTON AND MATTHEW R. SALTZMAN Cramer, B.D., Brett, C.E., Melchin, M.J., Ma¨nnik, P., Kleffner, M.A., McLaughlin, P.I., Loydell, D.K., Munnecke, A., Jeppsson, L., Corradini, C., Brunton, F.R. & Saltzman, M.R. 2011: Revised correlation of Silurian Provincial Series of North America with global 13 and regional chronostratigraphic units and d Ccarb chemostratigraphy. Lethaia,Vol.44, pp. 185–202. Recent revisions to the biostratigraphic and chronostratigraphic assignment of strata from the type area of the Niagaran Provincial Series (a regional chronostratigraphic unit) have demonstrated the need to revise the chronostratigraphic correlation of the Silurian System of North America. Recently, the working group to restudy the base of the Wen- lock Series has developed an extremely high-resolution global chronostratigraphy for the Telychian and Sheinwoodian stages by integrating graptolite and conodont biostratigra- 13 phy with carbonate carbon isotope (d Ccarb) chemostratigraphy. This improved global chronostratigraphy has required such significant chronostratigraphic revisions to the North American succession that much of the Silurian System in North America is cur- rently in a state of flux and needs further refinement. This report serves as an update of the progress on recalibrating the global chronostratigraphic correlation of North Ameri- can Provincial Series and Stage boundaries in their type area. -
Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
Chelicerata; Eurypterida) from the Campbellton Formation, New Brunswick, Canada Randall F
Document generated on 10/01/2021 9:05 a.m. Atlantic Geology Nineteenth century collections of Pterygotus anglicus Agassiz (Chelicerata; Eurypterida) from the Campbellton Formation, New Brunswick, Canada Randall F. Miller Volume 43, 2007 Article abstract The Devonian fauna from the Campbellton Formation of northern New URI: https://id.erudit.org/iderudit/ageo43art12 Brunswick was discovered in 1881 at the classic locality in Campbellton. About a decade later A.S. Woodward at the British Museum (Natural History) (now See table of contents the Natural History Museum, London) acquired specimens through fossil dealer R.F. Damon. Woodward was among the first to describe the fish assemblage of ostracoderms, arthrodires, acanthodians and chondrichthyans. Publisher(s) At the same time the museum also acquired specimens of a large pterygotid eurypterid. Although the vertebrates received considerable attention, the Atlantic Geoscience Society pterygotids at the Natural History Museum, London are described here for the first time. The first pterygotid specimens collected in 1881 by the Geological ISSN Survey of Canada were later identified by Clarke and Ruedemann in 1912 as Pterygotus atlanticus, although they suggested it might be a variant of 0843-5561 (print) Pterygotus anglicus Agassiz. An almost complete pterygotid recovered in 1994 1718-7885 (digital) from the Campbellton Formation at a new locality in Atholville, less than two kilometres west of Campbellton, has been identified as P. anglicus Agassiz. Like Explore this journal the specimens described by Clarke and Ruedemann, the material from the Natural History Museum, London is herein referred to P. anglicus. Cite this article Miller, R. F. (2007). Nineteenth century collections of Pterygotus anglicus Agassiz (Chelicerata; Eurypterida) from the Campbellton Formation, New Brunswick, Canada. -
Year in Review 2018/2019
Contents Shaping the Museum of the Future 2 Philanthropy on View 4 The Year at a Glance 8 Compelling Mix of Original and Touring Exhibitions 12 ROM Objects on Loan Locally and Globally 26 Leading-Edge Research 36 ROM Scholarship in Print 46 Community Connections 50 Access to First Peoples Art and Culture 58 Programming That Inspires 60 Learning at the ROM 66 Members and Volunteers 70 Digital Readiness 72 Philanthropy 74 ROM Leadership 80 Our Supporters 86 2 royal ontario museum year in review 2018–2019 3 One of the initiatives we were most proud of in 2018 was the opening of the Daphne Cockwell Gallery dedicated to First Peoples art & culture as free to the public every day the Museum is open. Initiatives such as this represent just one step on our journey. ROM programs and exhibitions continue to be bold, ambitious, and diverse, fostering discourse at home and around the world. Being Japanese Canadian: reflections on a broken world, Gods in My Home: Chinese New Year with Ancestor Portraits and Deity Prints and The Evidence Room helped ROM visitors connect past to present and understand forces and influences that have shaped our world, while #MeToo & the Arts brought forward a critical conversation about the arts, institutions, and cultural movements. Immersive and interactive exhibitions such as aptured in these pages is a pivotal Zuul: Life of an Armoured Dinosaur and Spiders: year for the Royal Ontario Museum. Fear & Fascination showcased groundbreaking Shaping Not only did the Museum’s robust ROM research and world-class storytelling. The Cattendance of 1.34 million visitors contribute to success achieved with these exhibitions set the our ranking as the #1 most-visited museum in stage for upcoming ROM-originals Bloodsuckers: the Canada and #7 in North America according to The Legends to Leeches, The Cloth That Changed the Art Newspaper, but a new report by Deloitte shows World: India’s Painted and Printed Cottons, and the the ROM, through its various activities, contributed busy slate of art, culture, and nature ahead. -
Note on Pterygotus Anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick Randall F
Document generated on 10/01/2021 12:30 a.m. Atlantic Geology Note on Pterygotus anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick Randall F. Miller Volume 32, Number 2, Summer 1996 Article abstract Fragments of the large euryptcrid Pterygotus, recently collected from the URI: https://id.erudit.org/iderudit/ageo32_2art01 Devonian Campbellton Formation at Atholville, New Brunswick, are identified as belonging to P. anglicus Agassiz. The only previous Pterygotus specimens See table of contents from this site, collected in 1881, were assigned to a new species P. atlanticus Clarke and Rucdemann, in 1912. Clarke and Rucdcmann's suggestion that P. atlanticus might turn out to be a small specimen of P. anglicus is supported by Publisher(s) this new find. However, possible revision of P. atlanticus awaits the discovery of additional, more complete, material. Atlantic Geoscience Society ISSN 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this article Miller, R. F. (1996). Note on Pterygotus anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick. Atlantic Geology, 32(2), 95–100. All rights reserved © Atlantic Geology, 1996 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ A tlantic Geology 95 Note on Pterygotus anglicus Agassiz (Eurypterida: Devonian) from the Campbellton Formation, New Brunswick Randall F. -
Copyrighted Material
06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago). -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Geology of the Grand River Watershed an Overview of Bedrock and Quaternary Geological Interpretations in the Grand River Watershed
Geology of the Grand River Watershed An Overview of Bedrock and Quaternary Geological Interpretations in the Grand River watershed Prepared by Bob Janzen, GIT December 2018 i Table of Contents List of Maps ..................................................................................................................... iii List of Figures .................................................................................................................. iii 1.0 Introduction ........................................................................................................... 1 2.0 Bedrock Geology .................................................................................................. 1 Algonquin Arch ......................................................................................................... 2 Bedrock Cuestas ...................................................................................................... 3 2.1 Bedrock Surface ................................................................................................. 4 2.2 Bedrock Formations of the Grand River watershed ........................................... 8 2.2.1 Queenston Formation ................................................................................ 15 2.2.2 Clinton–Cataract Group ............................................................................. 15 2.2.2.1 Whirlpool Formation ............................................................................ 16 2.2.2.2 Manitoulin Formation .......................................................................... -
Early Gnathostome Phylogeny Revisited: Multiple Method Consensus
RESEARCH ARTICLE Early Gnathostome Phylogeny Revisited: Multiple Method Consensus Tuo Qiao1, Benedict King2, John A. Long2, Per E. Ahlberg3, Min Zhu1* 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China, 2 School of Biological Sciences, Flinders University, Adelaide, South Australia, Australia, 3 Department of Organismal Biology, Evolutionary Biology Centre, Uppsala University, NorbyvaÈgen, Uppsala, Sweden * [email protected] a11111 Abstract A series of recent studies recovered consistent phylogenetic scenarios of jawed verte- brates, such as the paraphyly of placoderms with respect to crown gnathostomes, and anti- archs as the sister group of all other jawed vertebrates. However, some of the phylogenetic OPEN ACCESS relationships within the group have remained controversial, such as the positions of Ente- Citation: Qiao T, King B, Long JA, Ahlberg PE, Zhu lognathus, ptyctodontids, and the Guiyu-lineage that comprises Guiyu, Psarolepis and M (2016) Early Gnathostome Phylogeny Revisited: Achoania. The revision of the dataset in a recent study reveals a modified phylogenetic Multiple Method Consensus. PLoS ONE 11(9): hypothesis, which shows that some of these phylogenetic conflicts were sourced from a e0163157. doi:10.1371/journal.pone.0163157 few inadvertent miscodings. The interrelationships of early gnathostomes are addressed Editor: Hector Escriva, Laboratoire Arago, FRANCE based on a combined new dataset with 103 taxa and 335 characters, which is the most Received: May 2, 2016 comprehensive morphological dataset constructed to date. This dataset is investigated in a Accepted: September 2, 2016 phylogenetic context using maximum parsimony (MP), Bayesian inference (BI) and maxi- Published: September 20, 2016 mum likelihood (ML) approaches in an attempt to explore the consensus and incongruence between the hypotheses of early gnathostome interrelationships recovered from different Copyright: 2016 Qiao et al. -
Fossil Focus
www.palaeontologyonline.com Title: Fossil Focus: Acanthodians Author(s): Richard Dearden Volume: 5 Article: 10 Page(s): 1-12 Published Date: 01/10/2015 PermaLink: http://www.palaeontologyonline.com/articles/2015/fossil-focus-acanthodians/ IMPORTANT Your use of the Palaeontology [online] archive indicates your acceptance of Palaeontology [online]'s Terms and Conditions of Use, available at http://www.palaeontologyonline.com/site-information/terms-and- conditions/. COPYRIGHT Palaeontology [online] (www.palaeontologyonline.com) publishes all work, unless otherwise stated, under the Creative Commons Attribution 3.0 Unported (CC BY 3.0) license. This license lets others distribute, remix, tweak, and build upon the published work, even commercially, as long as they credit Palaeontology[online] for the original creation. This is the most accommodating of licenses offered by Creative Commons and is recommended for maximum dissemination of published material. Further details are available at http://www.palaeontologyonline.com/site-information/copyright/. CITATION OF ARTICLE Please cite the following published work as: Dearden, R. 2015. Fossil Focus: Acanthodians. Palaeontology Online, Volume 5, Article 10, 1-12. Published on: 01/10/2015| Published by: Palaeontology [online] www.palaeontologyonline.com |Page 1 Fossil Focus: Acanthodians by Richard Dearden*1 Introduction: The acanthodians are a mysterious extinct group of fishes, which lived in the waters of the Palaeozoic era (541 million to 252 million years ago). They are characterized by a superficially shark-like coating of tiny scales, and spines in front of their fins (Fig. 1). The acanthodians’ heyday was during the Devonian period, about 419 million to 359 million years ago, but their fossil record stretches back to the Silurian period (around 440 million years ago).