The African Coelacanth Genome Provides Insights Into Tetrapod Evolution
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ESS 345 Ichthyology
ESS 345 Ichthyology Evolutionary history of fishes 12 Feb 2019 (Who’s birthday?) Quote of the Day: We must, however, acknowledge, as it seems to me, that man with all his noble qualities... still bears in his bodily frame the indelible stamp of his lowly origin._______, (1809-1882) Evolution/radiation of fishes over time Era Cenozoic Fig 13.1 Fishes are the most primitive vertebrate and last common ancestor to all vertebrates They start the branch from all other living things with vertebrae and a cranium Chordata Notochord Dorsal hollow nerve cord Pharyngeal gill slits Postanal tail Urochordata Cephalochordata Craniates (mostly Vertebrata) Phylum Chordata sister is… Echinodermata Synapomorphy – They are deuterostomes Fish Evolutionary Tree – evolutionary innovations in vertebrate history Sarcopterygii Chondrichthyes Actinopterygii (fish) For extant fishes Osteichthyes Gnathostomata Handout Vertebrata Craniata Figure only from Berkeley.edu Hypothesis of fish (vert) origins Background 570 MYA – first large radiation of multicellular life – Fossils of the Burgess Shale – Called the Cambrian explosion Garstang Hypothesis 1928 Neoteny of sessile invertebrates Mistake that was “good” Mudpuppy First Vertebrates Vertebrates appear shortly after Cambrian explosion, 530 MYA – Conodonts Notochord replaced by segmented or partially segmented vertebrate and brain is enclosed in cranium Phylogenetic tree Echinoderms, et al. Other “inverts” Vertebrate phyla X Protostomes Deuterostomes Nephrozoa – bilateral animals First fishes were jawless appearing -
Our Fish Ageing Laboratory. This Is Where the Coastal
WELCOME TO OUR FISH AGEING LABORATORY. THIS IS WHERE THE COASTAL RESOURCES DIVISION OF THE GEORGIA DEPARTMENT OF NATURAL RESOURCES STUDIES THE DATA WE’VE COLLECTED TO MAKE THE BEST DECISIONS POSSIBLE IN MANAGING IMPORTANT FISH SPECIES. EFFECTIVE SPECIES MANAGEMENT HELPS TO ENSURE A HEALTHY AND ABUNDANT POPULATION OF RECREATIONAL AND COMMERCIAL FISH, AND PRESERVES OUR VITAL ECO-SYSTEM. COASTAL RESOURCES DIVISION BIOLOGISTS COLLECT, PROCESS, EVALUATE, AND PRESERVE THE “AGING STRUCTURES” OF PRIORITY FISH. “AGING STRUCTURES” ARE PARTS OF THE FISH ANATOMY THAT CAN BE EVALUATED TO DETERMINE THE AGE OF A FISH. BY KNOWING THE AGE OF FISH, SCIENTISTS CAN ESTIMATE GROWTH RATES OF THE SPECIES, MAXIMUM AGE, AGE-AT-MATURITY, AND TRENDS FOR FUTURE GENERATIONS. THIS INFORMATION CAN ASSIST IN DETERMINING THE HEALTH AND SUSTAINABILITY OF GEORGIA’S FISHERIES. OUR PROCESS BEGINS WITH THE HELP OF ANGLERS FROM ACROSS GEORGIA’S COAST. THE MARINE SPORTFISH CARCASS RECOVERY PROJECT ENCOURAGES ANGLERS TO DEPOSIT FILETED CARCASSES AT COLLECTION POINTS NEAR FISH CLEANING STATIONS, MARINAS AND PRIVATE DOCKS. ANGLERS PLACE THE CARCASSES IN CHEST FREEZERS AND COASTAL RESOURCES DIVISION STAFF LATER TRANSPORT THEM TO THE DIVISION’S AGING LAB IN BRUNSWICK. ANGLERS HAVE DONATED MORE THAN 65,000 CARCASSES SINCE THE PROJECT BEGAN IN 1997. AFTER EACH FISH IS IDENTIFIED, MEASURED, AND ITS SEX DETERMINED, THE AGING LABORATORY WILL REMOVE A SMALL BONE CALLED AN OTOLITH. THE OTOLITH IS USED TO DETERMINE THE AGE OF THE FISH. THESE SMALL BONES AID FISH IN BALANCE AND HEARING, FUNCTIONING IN A MANNER SIMILAR AS THE INNER EAR OF HUMANS. OTOLITHS ARE SOMETIMES REFERRED TO AS EAR STONES OR EAR BONES. -
Otolith Strontium Traces Environmental History of Subyearling American Shad Alosa Sapidissima
MARINE ECOLOGY PROGRESS SERIES Vol. 119: 25-35,1995 Published March 23 Mar. Ecol. Prog. Ser. Otolith strontium traces environmental history of subyearling American shad Alosa sapidissima Karin E. Limburg Institute of Ecosystem Studies, Box AB, Millbrook. New York 12545. USA ABSTRACT: Sagittal otoliths of young-of-year American shad Alosa sapidjssirna from the Hudson River estuary, New York, USA, were transected with an X-ray-dispersive microprobe to examine temporal patterns of strontium, a micro-constituent found in otolith aragonite. Otoliths were assayed from fish reared on known diets (freshwater zooplankton, followed by artificial diet containing marine fishmeal) in fresh water. The switch from freshwater plankton to artificial diet resulted in a significant rise in Sr:Ca ratio in the otolith (mean increase 3.2-fold, p < 0.001) both for fish reared at 12S°C and those reared at 22"C, although there was no significant difference in Sr:Ca increases between the 2 temperature treat- ments. In a field study, Sr:Ca values of otoliths from wild fish caught in the freshwater reaches of the Hudson were low (mean 0.79 X 10-~Sr:Ca * 0.32 SD, range 0.00 to 1.46X 10-~).Six fish captured in a single t.raw1in the lower estuary on 25 September 1990 had low Sr:Ca values on the inner parts of their otoliths (corresponding to younger age: mean Sr.Ca = 0.98 X 10'~* 0.38 SU),but the strontium content increased 3- to 5-fold (mean Sr:Ca = 3.62 X 10-32 0.71 SD) on the outer parts, corresponding to dates when the fish were older. -
Coelacanth Discoveries in Madagascar, with AUTHORS: Andrew Cooke1 Recommendations on Research and Conservation Michael N
Coelacanth discoveries in Madagascar, with AUTHORS: Andrew Cooke1 recommendations on research and conservation Michael N. Bruton2 Minosoa Ravololoharinjara3 The presence of populations of the Western Indian Ocean coelacanth (Latimeria chalumnae) in AFFILIATIONS: 1Resolve sarl, Ivandry Business Madagascar is not surprising considering the vast range of habitats which the ancient island offers. Center, Antananarivo, Madagascar The discovery of a substantial population of coelacanths through handline fishing on the steep volcanic 2Honorary Research Associate, South African Institute for Aquatic slopes of Comoros archipelago initially provided an important source of museum specimens and was Biodiversity, Makhanda, South Africa the main focus of coelacanth research for almost 40 years. The advent of deep-set gillnets, or jarifa, for 3Resolve sarl, Ivandry Business catching sharks, driven by the demand for shark fins and oil from China in the mid- to late 1980s, resulted Center, Antananarivo, Madagascar in an explosion of coelacanth captures in Madagascar and other countries in the Western Indian Ocean. CORRESPONDENCE TO: We review coelacanth catches in Madagascar and present evidence for the existence of one or more Andrew Cooke populations of L. chalumnae distributed along about 1000 km of the southern and western coasts of the island. We also hypothesise that coelacanths are likely to occur around the whole continental margin EMAIL: [email protected] of Madagascar, making it the epicentre of coelacanth distribution in the Western Indian Ocean and the likely progenitor of the younger Comoros coelacanth population. Finally, we discuss the importance and DATES: vulnerability of the population of coelacanths inhabiting the submarine slopes of the Onilahy canyon in Received: 23 June 2020 Revised: 02 Oct. -
Sturgeon and Paddlefish (Acipenseridae) Saggital Otoliths Are Composed of the Calcium Carbonate Polymorphs Vaterite and Calcite
Journal of Fish Biology (2016) doi:10.1111/jfb.13085, available online at wileyonlinelibrary.com Sturgeon and paddlefish (Acipenseridae) saggital otoliths are composed of the calcium carbonate polymorphs vaterite and calcite B. M. Pracheil*†, B. C. Chakoumakos‡, M. Feygenson§, G. W. Whitledge‖, R. P. Koenigs¶ and R. M. Bruch¶ *Environmental Science Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, U.S.A., ‡Quantum Condensed Matter Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, U.S.A., §Chemical and Engineering Materials Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, U.S.A., ‖Center for Fisheries, Aquaculture and Aquatic Sciences, Southern Illinois University, Carbondale, IL 62901, U.S.A. and ¶Wisconsin Department of Natural Resources, Oshkosh, WI 54903, U.S.A. This study sought to resolve whether sturgeon (Acipenseridae) sagittae (otoliths) contain a non-vaterite fraction and to quantify how large a non-vaterite fraction is using neutron diffraction analysis. This study found that all otoliths examined had a calcite fraction that ranged from 18 ± 6to36± 3% by mass. This calcite fraction is most probably due to biological variation during otolith formation rather than an artefact of polymorph transformation during preparation. © 2016 The Fisheries Society of the British Isles Key words: Acipenser fulvescens. Otoliths, the calcium carbonate (CaCO3) ear bones of Osteichthyes, are truly a wonder of the Animal Kingdom. These tri-part structures essential for hearing and balance in fishes are composed of some form of3 CaCO and can be used to determine fish environmental history as well as fish age through enumeration of daily and annular rings (Pracheil et al., 2014). -
The Lost Freshwater Goby Fish Fauna (Teleostei, Gobiidae) from the Early Miocene of Klinci (Serbia)
Swiss Journal of Palaeontology (2019) 138:285–315 https://doi.org/10.1007/s13358-019-00194-4 (0123456789().,-volV)(0123456789().,- volV) REGULAR RESEARCH ARTICLE The lost freshwater goby fish fauna (Teleostei, Gobiidae) from the early Miocene of Klinci (Serbia) 1 2,3 4 5 Katarina Bradic´-Milinovic´ • Harald Ahnelt • Ljupko Rundic´ • Werner Schwarzhans Received: 17 January 2019 / Accepted: 15 May 2019 / Published online: 1 June 2019 Ó The Author(s) 2019 Abstract Freshwater gobies played an important role in the Miocene paleolakes of central and southeastern Europe. Much data have been gathered from isolated otoliths, but articulated skeletons are relatively rare. Here, we review a rich assemblage of articulated gobies with abundant otoliths in situ from the late early Miocene lake deposits of Klinci in the Valjevo freshwater lake of the Valjevo-Mionica Basin of Serbia. The fauna was originally described by And¯elkovic´ in 1978, who noted many different fishes, including one goby (Gobius multipinnatus H. v. Meyer 1848), and was subsequently revised by Gaudant (1998), who collapsed all previously recognized species into a single gobiid species that he described as new, namely Gobius serbiensis Gaudant 1998. Our review resulted in the recognition of three highly adaptive extinct freshwater gobiid genera with four species being divided among them: Klincigobius andjelkovicae n.gen. and n.sp., Klincigobius serbiensis (Gaudant 1998), Rhamphogobius varidens n.gen. and n.sp., and Toxopyge campylus n.gen. and n.sp. Otoliths were found in situ in all four species, which allowed for the allocation of multiple previously described otolith-based species to these extinct gobiid genera. -
Preliminary Study & Growth of the Pelagic Clupeids in Lake
RESEARCH FOR THE MANAGEMENT OF THE FISHERIES ON LAKE GCP/RAF/271/FIN–TD/35 (En) TANGANYIKA GCP/RAF/271/FIN–TD/35 (En) June 1995 PRELIMINARY STUDY AND GROWTH OF THE PELAGIC CLUPEIDS IN LAKE TANGANYIKA ESTIMATED FROM DAILY OTOLITH INCREMENTS by Susanna Pakkasmaa and Jouko Sarvala FINNISH INTERNATIONAL DEVELOPMENT AGENCY FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Bujumbura, June 1995 The conclusions and recommendations given in this and other reports in the Research for the Management of the Fisheries on Lake Tanganyika Project series are those considered appropriate at the time of preparation. They may be modified in the light of further knowledge gained at subsequent stages of the Project. The designations employed and the presentation of material in this publication do not imply the expression of any opinion on the part of FAO or FINNIDA concerning the legal status of any country, territory, city or area, or concerning the determination of its frontiers or boundaries. PREFACE The Research for the Management of the Fisheries on Lake Tanganyika project (Lake Tanganyika Research) became fully operational in January 1992. It is executed by the Food and Agriculture Organization of the United Nations (FAO) and funded by the Finnish International Development Agency (FINNIDA) and the Arab Gulf Programme for United Nations Development Organizations (AGFUND). This project aims at the determination of the biological basis for fish production on Lake Tanganyika, in order to permit the formulation 0f a coherent lake—wide fisheries management policy for the four riparian States (Burundi, Tanzania, Zaïre and Zambia). Particular attention will be also given to the reinforcement of the skills and physical facilities of the fisheries research units in all four beneficiary countries as well as to the build— up of effective coordination mechanisms to ensure full collaboration between tha Governments concerned. -
The Diversity of Fish Otoliths, Past and Present
70 Book reviews. The diversity of fish otoliths, past and present Book reviews ‘The diversity of fish otoliths, past and present’, by Dirk Nolf Victor W.M. van Hinsbergh In this book Dirk Nolf summarizes his half a century of study on fossil and recent fish otoliths. From the beginning of his career onwards he advocated that fossil fish otoliths cannot be interpreted well without a thorough knowledge of the otoliths of living fishes. Such knowledge not only provides information about consistent features of species and families, but also about otolith variability within species, morphological changes during development, and malformations. All this information is required for proper identification and interpretation of fossil fish otoliths. In over forty-five years Dirk Nolf built up a unique collection of Recent fish otoliths; studied fishes and their otoliths in many famous museums; and travelled around to scrutinize collections and holotypes of fossil fish otoliths. Among his many publications he reissued and extended the classical work of Chaine & Duvergier on recent fish otoliths stressing the importance of knowledge about this subject (Nolf et al., 2009). In ‘The diversity of fish otoliths, past and present’ Dirk Nolf gives a testimony of his observations. He generously offers the reader the opportunity to profit from his own experience, together with his personal interpretation of previously published fossil otoliths and otolith-based nomenclature of fossil bony fishes. The core of the book is the Systematics section. In 104 pages and 359 plates depicting over 5,000 otoliths (around 1,500 species) the author provides a record of representative Recent otoliths of almost all families (and subfamilies) of Holostei and Teleostei as well as – as far as they are known – of many fossil species of these families. -
Making a Big Splash with Louisiana Fishes
Making a Big Splash with Louisiana Fishes Written and Designed by Prosanta Chakrabarty, Ph.D., Sophie Warny, Ph.D., and Valerie Derouen LSU Museum of Natural Science To those young people still discovering their love of nature... Note to parents, teachers, instructors, activity coordinators and to all the fishermen in us: This book is a companion piece to Making a Big Splash with Louisiana Fishes, an exhibit at Louisiana State Universi- ty’s Museum of Natural Science (MNS). Located in Foster Hall on the main campus of LSU, this exhibit created in 2012 contains many of the elements discussed in this book. The MNS exhibit hall is open weekdays, from 8 am to 4 pm, when the LSU campus is open. The MNS visits are free of charge, but call our main office at 225-578-2855 to schedule a visit if your group includes 10 or more students. Of course the book can also be enjoyed on its own and we hope that you will enjoy it on your own or with your children or students. The book and exhibit was funded by the Louisiana Board Of Regents, Traditional Enhancement Grant - Education: Mak- ing a Big Splash with Louisiana Fishes: A Three-tiered Education Program and Museum Exhibit. Funding was obtained by LSUMNS Curators’ Sophie Warny and Prosanta Chakrabarty who designed the exhibit with Southwest Museum Services who built it in 2012. The oarfish in the exhibit was created by Carolyn Thome of the Smithsonian, and images exhibited here are from Curator Chakrabarty unless noted elsewhere (see Appendix II). -
Giant Fossil Coelacanths from the Late Cretaceous of the Eastern
^rfij^i^v^^™, - » v ' - - 4 j/ N ^P"" ,- V ^™ V- -*^ >•;:-* ' ^ * -r;' David R. Schwimmer, Geologist, Columbus State University Introduction In Autumn, 1987, a sizeable mass of fossil bone was discovered by amateur collectors in the bed of a small creek in eastern Alabama. The bone-bearing rock, some 300 kg in weight, was collected by a party led by G. Dent Williams and transferred to the paleontology laboratory at Columbus State University. Williams prepared most of the material using air percussion tools, and I further cleared some bones with acetic acid. A mandible (lower jaw bone) of 502 mm length was the first bone prepared from the material. It strangely lacked evidence of both teeth and tooth sockets, and it was covered medially with coarse denticulation resembling #40 grit sandpaper. The jawbone conformed with no recognizable North American Late Cretaceous fish or four-legged animal, and, given the large size of the mandible, my initial search for an identification ranged from ankylosaurid dinosaurs, to mosasaurs, to the larger contemporary fish, such as Xiphactinus. Nothing known in the Late Cretaceous of North America matched the mandible nor any other bone which was subsequently prepared from this matrix. J.D. Stewart of the L.A. County Museum was prior fossil record of a North American coelacanth is concurrently studying fossils of small marine Diplurus newarki, from freshwater deposits of earliest coelacanths from the Late Cretaceous of western Kansas, Jurassic age (ca. 205 Myr.: Schaeffer, 1941, 1952). USA (which were also a new discovery at the time: see Forey (1981) and Maisey (1991) recognized two sub- Stewart et al., 1991). -
Campana, S.E. 2005. Otolith Science Entering the 21 St Century. Mar
CSIRO PUBLISHING www.publish.csiro.au/journals/mfr Marine and Freshwater Research, 2005, 56, 485–495 Review Otolith science entering the 21st century Steven E. Campana Marine Fish Division, Bedford Institute of Oceanography, PO Box 1006, Dartmouth, Nova Scotia, Canada B2Y 4A2. Email: [email protected] Abstract. A review of 862 otolith-oriented papers published since the time of the 1998 Otolith Symposium in Bergen, Norway suggests that there has been a change in research emphasis compared to earlier years. Although close to 40% of the papers could be classifed as ‘annual age and growth’studies, the remaining papers were roughly equally divided between studies of otolith microstructure, otolith chemistry and non-ageing applications. A more detailed breakdown of subject areas identified 15 diverse areas of specialisation, including age determination, larval fish ecology, population dynamics, species identification, tracer applications and environmental reconstructions. For each of the 15 subject areas, examples of representative studies published in the last 6 years were presented, with emphasis on the major developments and highlights. Among the challenges for the future awaiting resolution, the development of novel methods for validating the ages of deepsea fishes, the development of a physiologically- based otolith growth model, and the identification of the limits (if any) of ageing very old fish are among the most pressing. Introduction Recent changes in research emphasis Research involving otoliths continues to evolve and expand as Papers which reported the study or use of otoliths, and pub- we enter the 21st century. A search of the literature indicates lished between 1999 and the early months of 2004, were that the number of primary publications reporting research split between four major otolith disciplines: annual age on, or application of, otoliths has increased almost linearly and growth, chemistry, microstructure and other non-ageing over the past 35 years. -
Quantifying Physiological Influences on Otolith Microchemistry
Methods in Ecology and Evolution 2015, 6, 806–816 doi: 10.1111/2041-210X.12381 Quantifying physiological influences on otolith microchemistry Anna M. Sturrock1, 2*, Ewan Hunter3, J. Andrew Milton1,EIMF4, Rachel C. Johnson5, Colin P. Waring6 and Clive N. Trueman1* 1Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK; 2Department of Environmental Science, Policy & Management, University of California, Berkeley, 130 Mulford Hall #3114, Berkeley, CA 94720, USA; 3Centre for Environment, Fisheries and Aquaculture Science, Pakefield Road, Lowestoft, Suffolk NR33 0HT, UK; 4Edinburgh Ion Microprobe Facility, School of GeoSciences, The University of Edinburgh, Grant Institute, The King’s Buildings, James Hutton Road, Edinburgh EH9 3FE, UK; 5National Marine Fisheries Service, Southwest Fisheries Science Center, 110 Shaffer Road, Santa Cruz, CA 95060, USA; 6Institute of Marine Sciences, University of Portsmouth, Ferry Road, Eastney, Hampshire PO4 9LY, UK Summary 1. Trace element concentrations in fish earstones (‘otoliths’) are widely used to discriminate spatially discrete populations or individuals of marine fish, based on a commonly held assumption that physiological influences on otolith composition are minor, and thus variations in otolith elemental chemistry primarily reflect changes in ambient water chemistry. 2. We carried out a long-term (1-year) experiment, serially sampling seawater, blood plasma and otoliths of mature and immature European plaice (Pleuronectes platessa L.)totestrelationshipsbetweenotolithchemistry and environmental and physiological variables. 3. Seasonal variations in otolith elemental composition did not track seawater concentrations, but instead reflected physiological controls on metal transport and biokinetics, which are likely moderated by ambient tem- perature. The influence of physiological factors on otolith composition was particularly evident in Sr/Ca ratios, the most widely used elemental marker in applied otolith microchemistry studies.