FISHES and NECTURUS by EDWARD PHELPS ALLIS, JR
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Table S1.Xlsx
Bone type Bone type Taxonomy Order/series Family Valid binomial Outdated binomial Notes Reference(s) (skeletal bone) (scales) Actinopterygii Incertae sedis Incertae sedis Incertae sedis †Birgeria stensioei cellular this study †Birgeria groenlandica cellular Ørvig, 1978 †Eurynotus crenatus cellular Goodrich, 1907; Schultze, 2016 †Mimipiscis toombsi †Mimia toombsi cellular Richter & Smith, 1995 †Moythomasia sp. cellular cellular Sire et al., 2009; Schultze, 2016 †Cheirolepidiformes †Cheirolepididae †Cheirolepis canadensis cellular cellular Goodrich, 1907; Sire et al., 2009; Zylberberg et al., 2016; Meunier et al. 2018a; this study Cladistia Polypteriformes Polypteridae †Bawitius sp. cellular Meunier et al., 2016 †Dajetella sudamericana cellular cellular Gayet & Meunier, 1992 Erpetoichthys calabaricus Calamoichthys sp. cellular Moss, 1961a; this study †Pollia suarezi cellular cellular Meunier & Gayet, 1996 Polypterus bichir cellular cellular Kölliker, 1859; Stéphan, 1900; Goodrich, 1907; Ørvig, 1978 Polypterus delhezi cellular this study Polypterus ornatipinnis cellular Totland et al., 2011 Polypterus senegalus cellular Sire et al., 2009 Polypterus sp. cellular Moss, 1961a †Scanilepis sp. cellular Sire et al., 2009 †Scanilepis dubia cellular cellular Ørvig, 1978 †Saurichthyiformes †Saurichthyidae †Saurichthys sp. cellular Scheyer et al., 2014 Chondrostei †Chondrosteiformes †Chondrosteidae †Chondrosteus acipenseroides cellular this study Acipenseriformes Acipenseridae Acipenser baerii cellular Leprévost et al., 2017 Acipenser gueldenstaedtii -
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. -
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). -
Anewlatepermianray-Finned(Actinopterygian)Fishfrom the Beaufort Group, South Africa
Palaeont. afr., 38, 33-47 (2002) ANEWLATEPERMIANRAY-FINNED(ACTINOPTERYGIAN)FISHFROM THE BEAUFORT GROUP, SOUTH AFRICA by Patrick Bender Council for Geoscience, Private Bag X112, Pretoria, South Africa. e-mail: [email protected] ABSTRACT A new genus and species of actinopterygian (ray-finned) fish, Kompasia delaharpei, is described from Late Permian (Tatarian) fluvio-lacustrine, siltstone dominated deposits within the lower Beaufort Group of South Africa. It is currently known from two localities on adjoining farms, Wilgerbosch and Ganora, both in the New Bethesda district of the Eastern Cape Karoo region. The fossils were recovered from an uncertain formation, possibly closely equivalent to the Balfour Formation, within the Dicynodon Assemblage Zone. Kompasia delaharpei differs from previously described early actinopterygians, including the recently described new lower Beaufort Group taxon Bethesdaichthys kitchingi, on the basis of a combination of skull and post cranial characters. The genus is characterised by: a uniquely shaped subrectangular posterior blade of the maxilla, a shortened dorsal limb of the preopercular, and a dermopterotic and dermosphenotic contacting the nasal; furthermore, the subopercular is equal to or longer than the opercular, the dorsal fin is situated in the posterior third of the body, slightly behind the position of the anal fin, and the anterior rnidflank scales exhibit a smooth dermal pattern or surface, with a number of faint ganoine ridges present parallel to the posterior and ventral scale margins. Kompasia appears to exhibit a relatively conservative morphology similar to that in the lower Beaufort Group taxon Bethesdaichthys kitchingi. As such, Kompasia is derived relative to stem-actinopterans such as Howqualepis, Mimia and Moythomasia, and also derived relative to earlier southern African Palaeozoic actinopterygians such as Mentzichthys jubbi and Namaichthys schroederi, but basal to stem-neopterygians such as Australosomus and Saurichthys. -
A New Actinopterygian Fish Species from the Late Permian Beaufort Group, South Africa
Palaeont. a.fr., 37, 25-40 (2001) A NEW ACTINOPTERYGIAN FISH SPECIES FROM THE LATE PERMIAN BEAUFORT GROUP, SOUTH AFRICA by Patrick Bender Council for Geoscience, Private Bag Xl12, Pretoria, South Africa. e-mail·bender@.?li:co.za ABSTRACT A new genus and species of actinopterygian (ray-finned) fish, Bethesdaichthys kitchingi, is described from the Tatarian, Late Permian, Lower Beaufort Group of South Africa. Bethesdaichthys is presently known from three localities, two in the New Bethesda and one in the Victoria West districts of the Karoo region respectively. The fossils were recovered from within the Abrahamskraal Formation Tapinocephalus Assemblage Zone at the Victoria West locality, and from an uncertain Formation possibly closely equivalent to the Balfour Formation, within the Dicynodon Assemblage Zone at the New Bethesda sites. Bethesdaichthys kitchingi is a fusiform fish, up to approximately 300mm in total length, with the skull displaying a moderately oblique suspensorium, and a maxilla with a large sub-rectangular postorbital blade. Furthermore there is a complex offour suborbital bones adjacent to the orbit. The pectoral fin is large relative to body size and the tail is heterocercal with an elongate tapered dorsal body lobe. The anterior midflank scales in particular exhibit a distinctive dermal ornamentation consisting of numerous ganoineridges. The phylogenetics and interrelationships of Bethesdaichthys kitchingiare examined. It appears to exhibit a relatively conservative morphology similar to that found in possibly related Carboniferous taxa such as the South African taxa Australichthysand Willomorichthys. Bethesdaichthys kitchingiis derived relative to stem-actinopterans such as the Howqualepis and Mimia, and also derived relative to southern African Palaeozoic actinoptyerygians such as Mentzichthys jubbl; and Namaichthys schroeden; but basal to stem neopterygians such as Australosomus, Perleldus and Saurichthys. -
A New Actinopterygian Cheirolepis Jonesi Nov. Sp. from the Givetian of Spitsbergen, Svalbard Michael J
NORWEGIAN JOURNAL OF GEOLOGY https://dx.doi.org/10.1785/njg101-1-3 A new actinopterygian Cheirolepis jonesi nov. sp. from the Givetian of Spitsbergen, Svalbard Michael J. Newman¹, Carole J. Burrow², Jan L. den Blaauwen³ & Sam Giles4 ¹Vine Lodge, Vine Road, Johnston, Haverfordwest, Pembrokeshire, SA62 3NZ, UK. ²Geosciences, Queensland Museum, 122 Gerler Road, Hendra, 4011 Queensland, Australia. ³University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands. 4School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK. E-mail corresponding author (Michael J. Newman): [email protected] Keywords: Two specimens of a new early actinopterygian Cheirolepis jonesi nov. gen. et sp. have been collected • Devonian from the lagoonal Middle Devonian (Givetian) Fiskekløfta Member, the upper member of the Tordalen • Arctic Formation in the Mimerdalen Subgroup of Spitsbergen. This is the second oldest Cheirolepis species • Actinopterygii known from articulated remains. The holotype consists of an articulated head and the anterior trunk. • Marine • Histology The other specimen is an articulated skull which was 3D scanned to determine the internal structure and general architecture. The new taxon differs from other Cheirolepis species in the relative dimensions of the bones of the head, including a narrow anterior end of the dentary, longer accessory operculum and Received: 23. September 2020 correspondingly shorter dermohyal, as well as a longer premaxilla and proportionally larger quadratojugal, and the organisation and relative size of the teeth. Accepted: 7. January 2021 Published online: Introduction 26. April 2021 A new species of actinopterygian Cheirolepis jonesi sp. nov. is here described from the Middle Devonian (Givetian) of Mimerdalen in Spitsbergen, Svalbard. -
The Annals Magazine of Natural History
THE ANNALS AND MAGAZINE OF NATURAL HISTORY. [FOURTH SERIES.] No. 88. APRIL 1875. XXX.--On the Structure and Systematic Position of the Genus Cheirolepis. By R. H. TRAQUAIR, M.D., F.G.S., Keeper of the Natural-History Collections in the Edin- burgh Museum of Science and Art. [Plate XVII.] Tins very interesting genus of Devonian fishes was originally describedby the late Prof. Agassiz, in the second volume of his 'Poissons Fossiles/ p. 178, and was then included by him in his family of" Lepidoides." The first step towards the breaking-up of that heterogeneous assemblage was taken by Agassiz himself, in the course of the publication of the same great work, when he constituted the family of Acanthodidm for the genera Cheiracanthus, Acanthodes~ and Che&olepls; and this classification was retained in his special work on the Fossil Fishes of the Old Red Sandstone. The founder of fossil ichthyology seems, however, to have had but a slight and not very correct conception of the structure of the fishes with which he associated CheiroleTis, as may be seen both from his restored figures and his remark that, as the bones which he had been able to distinguish in Cheirolepis, " such as the frontal, humerus~ temporal, have the same structure as in ordinary osseous fishes," one may conclude "that the Acanthodians in general had a complete osseous system~ and not merely a chorda dorsalis as in the Coccostei and other fishes of the same epoch "*. Subsequent investigations into poissons Fossiles du vieux Gr~s Rouge~p. 44. Ann. & Mag. N. Hist. -
Three New Palaeoniscoid Fishes from the Bear Gulch Limestone
Three new palaeoniscoid fi shes from the Bear Gulch Limestone (Serpukhovian, Mississippian) of Montana (USA) and the relationships of lower actinopterygians Kathryn E. MICKLE University of Kansas, Department of Ecology and Evolutionary Biology, Natural History Museum and Biodiversity Research Center, 1345 Jayhawk boulevard, Lawrence, Kansas 66045 (USA) [email protected] Richard LUND 18 Hillside road, Mount Holly, New Jersey 08060 (USA) [email protected] Eileen D. GROGAN Saint Joseph’s University, Department of Biology, 5600 City Line avenue, Philadelphia, Pennsylvania 19131 (USA) [email protected] Mickle K. E., Lund R. & Grogan E. D. 2009. — Three new palaeoniscoid fi shes from the Bear Gulch Limestone (Serpukhovian, Mississippian) of Montana (USA) and the relationships of lower actinopterygians. Geodiversitas 31 (3) : 623-668. ABSTRACT Th ree new palaeoniscoid fi shes (Osteichthyes, Actinopterygii), representing two new genera, Lineagruan judithi n. gen., n. sp., L. snowyi n. gen., n. sp., Beagias- cus pulcherrimus n. gen., n. sp., are described from the Bear Gulch Limestone Member of the Heath Formation (Serpukhovian) of Montana, a 318 million year old lagerstätte. Morphological, morphometric, and meristic data were ana- lyzed and compared to data for other Paleozoic actinopterygians. Diff erences among the species were noted in character complexes that may have played a role in feeding or propulsive regimes and fi ne-scale niche partitioning. A matrix of 111 characters and 40 taxa was constructed using relatively complete taxa ranging from the Devonian to the Recent. Cladistic analysis using Hennig86 KEY WORDS Bear Gulch Limestone, and Winclada resulted in two trees. Branch-and-bound treatment generated Palaeoniscoids, one tree, in which the palaeoniscoids were paraphyletic. -
By Kathryn E. Mickle
UNRAVELING THE SYSTEMATICS OF PALAEONISCOID FISHES—LOWER ACTINOPTERYGIANS IN NEED OF A COMPLETE PHYLOGENETIC REVISION by Kathryn E. Mickle Submitted to the Department of Ecology and Evolutionary Biology and the Faculty of the Graduate School of the University of Kansas in partial fufillment of the requirements for the degree of Doctor of Philosophy ___________________________________________ Hans-Peter Schultze, Co-Chair ___________________________________________ Edward O. Wiley, Co-Chair ___________________________________________ Linda Trueb ___________________________________________ Sharon Billings ___________________________________________ Bruce Lieberman Date Defended: April 10, 2012 The Dissertation Committee for Kathryn E. Mickle certifies that this is the approved version of the following Dissertation: UNRAVELING THE SYSTEMATICS OF PALAEONISCOID FISHES—LOWER ACTINOPTERYGIANS IN NEED OF A COMPLETE PHYLOGENETIC REVISION Committee: ___________________________________________ Hans-Peter Schultze, Co-Chair ___________________________________________ Edward O. Wiley, Co-Chair ___________________________________________ Linda Trueb ___________________________________________ Sharon Billings ___________________________________________ Bruce Lieberman Date Approved: April 10, 2012 ii ABSTRACT Actinopterygian fishes are the most diverse and speciose vertebrates on the planet. Lower actinopterygians, or fishes basal to teleosts, are critical to our understanding of the early evolution of this group, but extant lower actinopterygians are -
Fishes of the World
Fishes of the World Fishes of the World Fifth Edition Joseph S. Nelson Terry C. Grande Mark V. H. Wilson Cover image: Mark V. H. Wilson Cover design: Wiley This book is printed on acid-free paper. Copyright © 2016 by John Wiley & Sons, Inc. All rights reserved. Published by John Wiley & Sons, Inc., Hoboken, New Jersey. Published simultaneously in Canada. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, scanning, or otherwise, except as permitted under Section 107 or 108 of the 1976 United States Copyright Act, without either the prior written permission of the Publisher, or authorization through payment of the appropriate per-copy fee to the Copyright Clearance Center, 222 Rosewood Drive, Danvers, MA 01923, (978) 750-8400, fax (978) 646-8600, or on the web at www.copyright.com. Requests to the Publisher for permission should be addressed to the Permissions Department, John Wiley & Sons, Inc., 111 River Street, Hoboken, NJ 07030, (201) 748-6011, fax (201) 748-6008, or online at www.wiley.com/go/permissions. Limit of Liability/Disclaimer of Warranty: While the publisher and author have used their best efforts in preparing this book, they make no representations or warranties with the respect to the accuracy or completeness of the contents of this book and specifically disclaim any implied warranties of merchantability or fitness for a particular purpose. No warranty may be createdor extended by sales representatives or written sales materials. The advice and strategies contained herein may not be suitable for your situation. -
Endocranial Preservation of a Carboniferous Actinopterygian from Lancashire, UK, and the Interrelationships of Primitive Actinopterygians
Endocranial preservation of a Carboniferous actinopterygian from Lancashire, UK, and the interrelationships of primitive actinopterygians Michael I. Coates Department of Biology, Darwin Building, University College London, Gower Street, London WC1E 6BT, UK ([email protected]) CONTENTS PAGE 1. Introduction 435 2. Material 437 3. Methods 437 4. Systematic palaeontology 437 5. Taxonomic note 439 6. Description 439 (a) External morphology 439 (b) Internal morphology: general features 440 (c) The `brain cast' and otic capsule 442 7. Discussion 445 (a) Characters used in analysis 445 (b) Results of phylogenetic analysis 452 (c) Phylogenetic conclusions 454 (d) Patterns of evolution in the gross features of actinopterygian brains 455 Appendix A 457 (a) List of abbreviations used in ¢gures 457 (b) List of nodal character states for ¢gure 9a 457 Appendix B 458 References 459 The gross brain structure of an Upper Carboniferous (ca. 310 Myr ago) ray-¢nned ¢sh (Actinopterygii) is described from exceptionally well-preserved fossil material from the Burnley region of Lancashire, UK. Previously identi¢ed as `Rhadinichthys'planti, the species is reassigned to the genus Mesopoma. Morphological characters derived from these data are combined with reviews of cranial skeletal anatomy, enamel composi- tion, oculomoter muscle insertion and paired ¢n morphology to test and reanalyse hypotheses of primitive actinopterygian interrelationships. Results indicate that ancestral chondrostean (sturgeon and paddle¢sh) and neopterygian (teleost, amiid and gar) lineages diverged earlier than current theories suggest. Palaeo- nisciformes, a taxonomic group widely used to include most Palaeozoic actinopterygians, include a signi¢cant number of primitive neopterygians, several of which may form a distinct monophyletic clade. -
The Lower Actinopterygian Fauna from the Lower Carboniferous Albert
Foss. Rec., 20, 47–67, 2017 www.foss-rec.net/20/47/2017/ doi:10.5194/fr-20-47-2017 © Author(s) 2017. CC Attribution 3.0 License. The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada – a review of previously described taxa and a description of a new genus and species Kathryn E. Mickle1,2 1College of Science, Health, and the Liberal Arts, Philadelphia University, 4201 Henry Ave, Philadelphia, PA 19114, USA 2University of Kansas Biodiversity Institute, 1345 Jayhawk Blvd, Lawrence, KS 66045, USA Correspondence to: Kathryn E. Mickle ([email protected]) Received: 7 September 2016 – Revised: 21 November 2016 – Accepted: 21 November 2016 – Published: 31 January 2017 Abstract. The Lower Carboniferous Albert shale formation ous fishes and rarely seen in Devonian fishes were present of New Brunswick, Canada, is well-known for the preserva- early in the Carboniferous. tion of countless articulated lower actinopterygian palaeonis- coid fishes. This site is at the boundary between the De- vonian and the Lower Carboniferous, making the lower 1 Introduction actinopterygians preserved at this site important. The taxo- nomic history of previously described Albert shale forma- 1.1 The Albert shale formation tion actinopterygians is reviewed here. Many of the earliest described actinopterygian taxa from the Albert Formation are For over 150 years, lower actinopterygian, or palaeoniscoid, represented by poorly preserved type specimens and have the fishes have been described from the Albert shales of south- distinction of being moved from one paraphyletic genus to eastern New Brunswick, Canada (Fig. 1). The term Albert another paraphyletic genus.