Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)
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This content downloaded from 157.193.10.229 on Tue, 07 Jul 2015 14:17:10 UTC All use subject to JSTOR Terms and Conditions CLEMENT and BOISVERT-DEVONIAN LUNGFISH FROM BELGIUM 277 tra. In addition to his incorrect taxonomic attribution, Lohest idae Berg, 1940 (including Fleurantia and Jarvikia); and Rhyn- misinterpreted the operculum as a scapula, the cleithrum as a chodipteridae Moy-Thomas, 1939 (including Rhynchodipterus, coracoid, and the E bone as an isolated rib (Fig. 2A, B). How- Griphognathus, and Soederberghia). Schultze (1993) defined the ever, he accurately identified a pleural rib (Fig. 2A, B). Rhynchodipteridae as including at least Soederberghia, Jarvikia, and Fleurantia. Later, Schultze (2001) presented a cladogram of SYSTEMATIC PALEONTOLOGY Devonian dipnoans that included a radiation of denticulated forms: Barwickia [Fleurantia + Rhynchodipteridae], in which included SARCOPTERYGII Romer, 1955 Rhynchodipteridae Griphognathus [Rhynchodipterus + The and affinities of the DIPNOMORPHA Ahlberg, 1991 [Soederberghia Jarvikia]]. monophyly DIPNOI 1845 Rhynchodipteridae have been reviewed by Ahlberg et al. (2001), Muiller, who that be unrelated RHYNCHODIPTERIDAE Moy-Thomas, 1939 tentatively suggested Griphognathus may to Rhynchodipterus and Soederberghia, but regarded Rhyncho- Remarks-Campbell and Barwick (1990) proposed that the dipterus and Soederberghia as most closely related to each other. denticulated lungfish lineage should be recognized as suborder However, Friedman (2003b) considered this suggestion prema- Uranolophina which incorporates four families: Uranolophidae ture and suggested that the Rhynchodipteridae, if defined as Miles, 1977; Holodontidae Gorizdro-Kulczycka, 1950; Fleuranti- including only Soederberghia, Rhynchodipterus, and Griphogna- FIGURE 2. Soederberghiasp. indet. Modave, Liege Province, Belgium, upper Famennian,Upper Devonian. Liege University, paleontology collection no. 5390a,b. A, no. -
RESPIRATORY CONTROL in the LUNGFISH, NEOCERATODUS FORSTERI (KREFT) KJELL JOHANSEN, CLAUDE LENFANT and GORDON C
Comp. Biochem. Physiol., 1967, Vol. 20, pp. 835-854 RESPIRATORY CONTROL IN THE LUNGFISH, NEOCERATODUS FORSTERI (KREFT) KJELL JOHANSEN, CLAUDE LENFANT and GORDON C. GRIGG Abstract-1. Respiratory control has been studied in the lungfish, Neoceratodus forsteri by measuring ventilation (Ve), oxygen uptake (VO2), per cent O2 extraction from water, breathing rates of branchial and aerial respiration and changes in blood gas and pulmonary gas composition during exposure to hypoxia and hypercarbia. 2. Hypoxic water represents a strong stimulus for compensatory increase in both branchial and aerial respiration. Water ventilation increases by a factor of 3 or 4 primarily as a result of increased depth of breathing. 3. The ventilation perfusion ratio decreased during hypoxia because of a marked increase in cardiac output. Hypoxia also increased the fraction of total blood flow perfusing the lung. Injection of nitrogen into the lung evoked no compensatory changes. 4. It is concluded that the chemoreceptors eliciting the compensatory changes are located on the external side facing the ambient water or in the efferent branchial blood vessels. 5. Elevated pCO2 in the ambient water depressed the branchial respiration but stimulated aerial respiration. 6. It is suggested that the primary regulatory effect of the response to increased ambient pCO2 is to prevent CO2 from entering the animal, while the secondary stimulation of air breathing is caused by hypoxic stimulation of chemoreceptors located in the efferent branchial vessels. INTRODUCTION I t i s generally accepted that vertebrates acquired functional lungs before they possessed a locomotor apparatus for invasion of a terrestrial environment. Shortage of oxygen in the environment is thought to have been the primary driving force behind the development of auxiliary air breathing. -
Cambridge University Press 978-1-107-17944-8 — Evolution And
Cambridge University Press 978-1-107-17944-8 — Evolution and Development of Fishes Edited by Zerina Johanson , Charlie Underwood , Martha Richter Index More Information Index abaxial muscle,33 Alizarin red, 110 arandaspids, 5, 61–62 abdominal muscles, 212 Alizarin red S whole mount staining, 127 Arandaspis, 5, 61, 69, 147 ability to repair fractures, 129 Allenypterus, 253 arcocentra, 192 Acanthodes, 14, 79, 83, 89–90, 104, 105–107, allometric growth, 129 Arctic char, 130 123, 152, 152, 156, 213, 221, 226 alveolar bone, 134 arcualia, 4, 49, 115, 146, 191, 206 Acanthodians, 3, 7, 13–15, 18, 23, 29, 63–65, Alx, 36, 47 areolar calcification, 114 68–69, 75, 79, 82, 84, 87–89, 91, 99, 102, Amdeh Formation, 61 areolar cartilage, 192 104–106, 114, 123, 148–149, 152–153, ameloblasts, 134 areolar mineralisation, 113 156, 160, 189, 192, 195, 198–199, 207, Amia, 154, 185, 190, 193, 258 Areyongalepis,7,64–65 213, 217–218, 220 ammocoete, 30, 40, 51, 56–57, 176, 206, 208, Argentina, 60–61, 67 Acanthodiformes, 14, 68 218 armoured agnathans, 150 Acanthodii, 152 amphiaspids, 5, 27 Arthrodira, 12, 24, 26, 28, 74, 82–84, 86, 194, Acanthomorpha, 20 amphibians, 1, 20, 150, 172, 180–182, 245, 248, 209, 222 Acanthostega, 22, 155–156, 255–258, 260 255–256 arthrodires, 7, 11–13, 22, 28, 71–72, 74–75, Acanthothoraci, 24, 74, 83 amphioxus, 49, 54–55, 124, 145, 155, 157, 159, 80–84, 152, 192, 207, 209, 212–213, 215, Acanthothoracida, 11 206, 224, 243–244, 249–250 219–220 acanthothoracids, 7, 12, 74, 81–82, 211, 215, Amphioxus, 120 Ascl,36 219 Amphystylic, 148 Asiaceratodus,21 -
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
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. -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
REPRINTED from KOOLEWONG Vol
REPRINTED FROM KOOLEWONG Vol. 4, No. 2 The Lungfish-Creature from the Past by GORDON C. GRIGG The survivor from prehistoric times, the salmon-fleshed Queensland lungfish, may fall victim to agricultural destruction of its habitat. Along the more remote reaches of Queensland's Burnett River, particularly toward evening, it is easy to believe that prehistoric creatures exist in the still, dark pools. Yet despite the heavily primeval atmosphere of the river it has so far produced only one genuine survivor from prehistoric times-the Queensland lungfish, Neoceratodus forsteri. Dissection of a lungfish (above) reveals the structure of its single lung. The lungfish also has a set of gills and can breathe air or water at will. Photo by Gordon C. Grigg. Fossil evidence suggests that this fish has remained essentially unaltered by any evolutionary processes for at least the last 150 million years. The lungfish is a member of an extraordinary group of fishes, the Dipnoi, which have lungs as well as gills, allowing them to breathe air as well as water. Of the once widespread Dipnoan fish, only three survive today: Neoceratodus in Queensland, Protopterus in Africa and Lepidosiren in South America. Neoceratodus appears to be more primitive than its overseas cousins. It is the closest surviving relative of the fish from which the first land vertebrates, the labyrinthodonts, arose about 325 million years ago. This makes it of particular interest to zoologists. The Queensland lungfish inhabits waterholes in rivers where the channel widens, deepens and flows more slowly. During the day it remains on the bottom and can sometimes be seen in the shade of overhanging trees. -
The Fishesof Uganda-I
1'0 of the Pare (tagu vaIley.': __ THE FISHES OF UGANDA-I uku-BujukUf , high peaks' By P. H. GREENWOOD Fons Nilus'" East African Fisheries Research Organization ~xplorersof' . ;ton, Fresh_ CHAPTER I I\.bruzzi,Dr: knowledge : INTRODUCTION ~ss to it, the ,THE fishes of Uganda have been subject to considerable study. Apart from .h to take it many purely descriptive studies of the fishes themselves, three reports have . been published which deal with the ecology of the lakes in relation to fish and , fisheries (Worthington (1929a, 1932b): Graham (1929)).Much of the literature is scattered in various scientific journals, dating back to the early part of the ; century and is difficult to obtain iIi Uganda. The more recent reports also are out of print and virtually unobtainable. The purpose .of this present survey is to bring together the results of these many researches and to present, in the light of recent unpublished information, an account of the taxonomy and biology of the many fish species which are to be found in the lakes and rivers of Uganda. Particular attention has been paid to the provision of keys, so that most of the fishesmay be easily identified. It is hardly necessary to emphasize that our knowledge of the East African freshwater fishes is still in an early and exploratory stage of development. Much that has been written is known to be over-generalized, as conclusions were inevitably drawn from few and scattered observations or specimens. From the outset it must be stressed that the sections of this paper dealing with the classification and description of the fishes are in no sense a full tax- onomicrevision although many of the descriptions are based on larger samples than were previously available. -
Protopterus Annectens (OWEN) in IDAH AREA of RIVER NIGER, NIGERIA
Animal Research International (2010) 7(3): 1264 – 1266 1264 LENGTH-WEIGHT RELATIONSHIP AND CONDITION FACTOR OF Protopterus annectens (OWEN) IN IDAH AREA OF RIVER NIGER, NIGERIA ADEYEMI, Samuel Olusegun Department of Biological Sciences, Kogi State University, PMB 1008, Anyigba Email: [email protected] Phone: +234 8062221968 ABSTRACT A total of 62 samples of Protopterus annectens (Owen) were examined for this study from Idah area of River Niger between August and November 2008. The length-weight relationship calculated for species gave a b-value of 2.55 which is indicative of negative allometric growth. It attained a length of 59cm and weight of 397g. The condition factor varied from 0.23 to 0.76 with a mean of 0.39+0.08 and showed that the fish was well and in good environment for growth and survival. Keywords: Protopterus annectens, Allometric growth, Survival, Length-weight relationship, Condition INTRODUCTION factor of P. annectens in order to aid its management in the river. Fish found in tropical and sub-tropical water system experience frequency growth MATERIALS AND METHODS fluctuations due to changes in food composition, environmental variables and spawning Study Area: The study area is Idah area of conditions among others. Length-weight and River Niger in Idah Local Government Area of length-length relationships can be used to asses Kogi State, Nigeria. The river extends from the influence of these factors in fish. Kulbicki et Lokoja via Ajaokuta, Itobe to Idah. The river is al. (1993) and King (1996) reported that fish located on latitude 7007N and longitude 6044E. growth, mean weight at a given body length of The water temperature range between 220C and fish and the relative wellbeing in fish can be 310C, Idah has a tropical savannah climate with known through this relationship. -
The Carboniferous Evolution of Nova Scotia
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. -
Megapleuronzange3321schu.Pdf
UNIVERSE ftJJMOlS H URBA^-CHAMPAIGN LXLOGY b i/FIELDIANA J/ Geology Published by Field Museum of Natural History Volume 33, No. 21 January 28,1977 This volume is dedicated to Dr. Rainer Zangerl Megapleuron zangerli A New Dipnoan from the Pennsylvanian, Illinois HANS-PETER SCHULTZE APL. PROFESSOR GEOL.-PALXONT. INSTITUT, UNIVERSITXT GOTTINGEN ABSTRACT Megapleuron rochei Gaudry 1881 from the lower Permian of France is redescribed. Small juvenile specimens from the Middle Pennsylvanian of Illinois are placed in the same genus as the new species M. zangerli. The genus differs from all other contem- poraneous dipnoans in the arrangement of the bones in the skull roof. INTRODUCTION Denison ( 1969, pp. 208-209) described but did not name two juve- nile dipnoans with the tooth-plates in an early stage of develop- ment. A few additional specimens of the species have since been collected. The best preserved specimen, chosen as the type of a new species, was given first to Dr. D. Baird, Princeton, who offered it to me for description during my stay at Field Museum, Chicago. After realizing that the pattern of the bones of the skull roof differs from that in Sagenodus, I found an identical pattern in the poorly pre- served type and only specimen of Megapleuron rochei Gaudry 1881. The type specimen of M. rochei will be described first for proper comparison with the specimens from the Middle Pennsylvanian of Illinois. During my stay at Field Museum, I prepared polysulfide rubber casts of all specimens. These casts and the specimens have been investigated in Field Museum and in the GeoL-PalSont.