Living Fossils

Total Page:16

File Type:pdf, Size:1020Kb

Living Fossils A reprint from American Scientist the magazine of Sigma Xi, The Scientific Research Society This reprint is provided for personal and noncommercial use. For any other use, please send a request to Permissions, American Scientist, P.O. Box 13975, Research Triangle Park, NC, 27709, U.S.A., or by electronic mail to [email protected]. ©Sigma Xi, The Scientific Research Society and other rightsholders The Evolutionary Truth About Living Fossils Appearances to the contrary, no species is exempt from selection, even when changes are difficult to detect in the fossil record. Alexander J. Werth and William A. Shear o gaze upon a horseshoe crab to have gone extinct in the Late Cre- is to glimpse a prehistoric Or- taceous until the discovery of living dovician sea of nearly half a Latimeria in 1938. Likewise, the dawn billion years ago. So moved redwood tree, Metasequoia, was known Twas Charles Darwin by the appear- only from fossils (10 to 100 million ance of these and similarly ancient- years old) before it was found alive in looking creatures—lungfish, lampreys, a remote Chinese valley in 1943; today lampshells, and lycopods—that he it is a common ornamental that grows coined the term living fossil to describe readily in temperate regions. them. In his landmark 1859 treatise On Living fossil is a perfectly appropri- the Origin of Species, he wrote that such ate and evocative term for such extant apparently primitive species are “rem- forms even today. It conveys the jar- nants of a once preponderant order… ring surprise that such species conjure which, like fossils, connect to a certain by retaining anatomical structures out extent orders now widely separated in of deep geologic time. This curious the natural scale.” These “anomalous phenomenon raises evolutionary and forms,” he wrote, nonetheless “have ecological questions at once simple endured to the present day.” and profound, such as why these taxa Like modern biologists, Darwin was appear to have persisted unchanged Visuals Unlimited/naturepl.com struck by the unusually archaic form for so long, and how we can distin- of the three widely scattered lung- guish species over long stretches of evident, apparently retained from long- fishes (Protopterus, Neoceratodus, and Earth history without gene pools or lost eras. This morphological conserva- Lepidosiren of Africa, Australia, and other reproductive features essential to tism, readily seen in horseshoe crabs South America, respectively), whose our current comprehension of specia- and coelacanths, is made all the more large lungs; cartilaginous notochord; tion. No doubt living fossils offer, as remarkable by our knowledge of strik- and fleshy, lobed fins resemble those Darwin anticipated, an unprecedented ingly similar fossil forms from ancient of creatures known only from the fossil opportunity to study—with fascinat- geologic ages. Living fossils are repre- record. Similarly, the coelacanth (Lati- ing, attention-grabbing narratives— sentatives of otherwise extinct groups, meria), another lobe-finned fish, was major questions concerning extinction, often common in the fossil record. well known from fossils but thought competition, and rates of evolutionary Some were thought to be extinct. None- change, both morphological and ge- theless, a known fossil connection or Alexander J. Werth is Venable Professor of Biol- netic. They also reveal important and “twin” is not necessary for living fossil ogy and William A. Shear is Trinkle Professor often intractable difficulties of under- status. The eel species Protoanguilla pa- of Biology, both at Hampden-Sydney College in standing the concept of species over lau, discovered in 2010, is estimated to Virginia. Each earned a PhD in organismic and vast periods of time. have diverged from other eels around evolutionary biology from Harvard University, 200 million years ago and has been de- Shear in 1971 and Werth in 1992. Werth’s re- What Is a Living Fossil? scribed as a primitive living fossil with- search focuses on the functional morphology and The term living fossil itself, despite the out a known fossil record. biomechanics of feeding in baleen and toothed seductive appeal inherent in its apt de- Much of the surprise that greeted whales, and on the evolution of complexity. scriptiveness, poses challenges for the the coelacanth’s discovery in 1938 can Shear conducts research on the systematics of scientist and layperson alike. But even be ascribed to the fact that fossil coel- millipedes and other myriapods, and on the evo- lution of early terrestrial ecosystems. Shear has if this ambiguous term is not easily or acanthiforms were widely recognized published four previous feature articles in Amer- universally defined, it nonetheless re- by paleontologists, but no extant spe- ican Scientist. Address: Department of Biology, tains heuristic value. One of the chief cies were known. In truth there has Hampden-Sydney College, Hampden-Sydney, characteristics of living fossils is an an- never been any fossil find of the extant Virginia 23943. E-mail: [email protected]. cient or archaic form, at least externally Latimeria chalumnae or L. menadoensis photo courtesy of Jim Brace-Thompson 434 American Scientist, Volume 102 © 2014 Sigma Xi, The Scientific Research Society. Reproduction with permission only. Contact [email protected]. The term living fossil has been used since Darwin coined it, referring to organisms that appear unchanged compared to fossil speci- mens, such as the gingko tree (Gingko bilo- ba). However, the term has been confusingly applied as the field of biology has advanced in understanding evolution and genetics. Is the concept useful? www.americanscientist.org © 2014 Sigma Xi, The Scientific Research Society. Reproduction 2014 November–December 435 with permission only. Contact [email protected]. photo courtesy of Jim Brace-Thompson Angelo Giampiccolo/naturepl.com An Ordovician fossil, Lunataspis aurora (left), looks nearly identical or so. Even if biologists could trace its evolution back ancestor by to today‘s Atlantic horseshoe crab (Limulus polyphemus, at right). ancestor, we could not define the point at which one species became Without genetic information from fossils, it is very difficult to know another. Nevertheless, we know that they could not interbreed and how much the organism has changed over the past 445 million years are therefore two different species. (West Indian Ocean and Indonesian species neither disprove nor provide forerunners of the diminutive living coelacanths), undercutting the claim any evidence counter to our under- fossil lycopod and horsetail plants un- that Latimeria is, strictly speaking, a standing of evolution, which remains derfoot today. living fossil, and thereby deflating as- the cornerstone of biological science. Conservative features alone are not sertions that such species demonstrate There are no “unevolved” species, no enough to paint a complete picture an absence of evolution. Still, living reanimated fossils that have literally of what constitutes a living fossil. Al- fossil taxa tend to have only fossil (not come back to life, and no living organ- though Escherichia coli and other bac- modern) counterparts. isms that are truly identical to extinct teria retain many traits of Earth’s first Unfortunately, creationists bent on species known in the fossil record. life forms (and as such are closer than denying the factual basis of evolu- What makes living fossils special, most species to the universal ancestor tion have increasingly misappropri- according to Harvard University evo- of all living things), no one would call ated the term living fossil. In the Atlas lutionary biologist Piotr Naskrecki, is them living fossils, not so much due of Creation, which pairs photographs simply that they superficially resemble to their simplicity as their ubiquity. If of living fossils with similar ancient their predecessors as members of an- living fossils were defined solely by fossils, Turkish author and Islamic cient genetic lines that have not been archaic form, one could claim we are creationist Harun Yahya erroneously extinguished, even as they “wither surrounded by them on land and at argues that “Darwinists are desperate through time and turn from roaring sea given the profusion of earthworms when confronted by these fossils, for rivers of species to a trickle before dis- and jellyfish. Scarcity is thus typically they prove that the evolution process appearing altogether.” Still, they may a key feature: Living fossils are usually has never existed.” Entry of “living live on in surprising ways. Naskrecki rare, with little taxonomic diversity. fossil” into Internet search engines points out that our fossil fuel economy They may stand out, like the ginkgo yields a preponderance of creationist is powered by once-dominant trees tree, as exceptional organisms that are websites, despite the fact that these of Carboniferous coal swamp forests, not closely related to any other living photo courtesy of Jim Brace-Thompson Doug Perrine/SeaPics.com The living coelacanth fish (Latimeria, shown at right) is strikingly same species. This fish was heralded as a fossil come to life upon its similar to and obviously closely related to extinct forms (at left, a De- discovery by South African naturalist Marjorie Courtenay-Latimer in vonian coelacanth). But appearances are deceiving: They are not the the Indian Ocean in 1938. 436 American Scientist, Volume 102 © 2014 Sigma Xi, The Scientific Research Society. Reproduction with permission only. Contact [email protected].
Recommended publications
  • The World at the Time of Messel: Conference Volume
    T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203.
    [Show full text]
  • The MBL Model and Stochastic Paleontology
    216 Chapter seven ised exciting new avenues for research, that insights from biology and ecology could more profi tably be applied to paleontology, and that the future lay in assembling large databases as a foundation for analysis of broad-scale patterns of evolution over geological history. But in compar- ison to other expanding young disciplines—like theoretical ecology— paleobiology lacked a cohesive theoretical and methodological agenda. However, over the next ten years this would change dramatically. Chapter Seven One particular ecological/evolutionary issue emerged as the central unifying problem for paleobiology: the study and modeling of the his- “Towards a Nomothetic tory of diversity over time. This, in turn, motivated a methodological question: how reliable is the fossil record, and how can that reliability be Paleontology”: The MBL Model tested? These problems became the core of analytical paleobiology, and and Stochastic Paleontology represented a continuation and a consolidation of the themes we have examined thus far in the history of paleobiology. Ultimately, this focus led paleobiologists to groundbreaking quantitative studies of the inter- The Roots of Nomotheticism play of rates of origination and extinction of taxa through time, the role of background and mass extinctions in the history of life, the survivor- y the early 1970s, the paleobiology movement had begun to acquire ship of individual taxa, and the modeling of historical patterns of diver- Bconsiderable momentum. A number of paleobiologists began ac- sity. These questions became the central components of an emerging pa- tively building programs of paleobiological research and teaching at ma- leobiological theory of macroevolution, and by the mid 1980s formed the jor universities—Stephen Jay Gould at Harvard, Tom Schopf at the Uni- basis for paleobiologists’ claim to a seat at the “high table” of evolution- versity of Chicago, David Raup at the University of Rochester, James ary theory.
    [Show full text]
  • Chordates (Phylum Chordata)
    A short story Leathem Mehaffey, III, Fall 201993 The First Chordates (Phylum Chordata) • Chordates (our phylum) first appeared in the Cambrian, 525MYA. 94 Invertebrates, Chordates and Vertebrates • Invertebrates are all animals not chordates • Generally invertebrates, if they have hearts, have dorsal hearts; if they have a nervous system it is usually ventral. • All vertebrates are chordates, but not all chordates are vertebrates. • Chordates: • Dorsal notochord • Dorsal nerve chord • Ventral heart • Post-anal tail • Vertebrates: Amphioxus: archetypal chordate • Dorsal spinal column (articulated) and skeleton 95 Origin of the Chordates 96 Haikouichthys Myllokunmingia Note the rounded extension to Possibly the oldest the head bearing sensory vertebrate: showed gill organs bars and primitive vertebral elements Early and primitive agnathan vertebrates of the Early Cambrian (530MYA) Pikaia Note: these organisms were less Primitive chordate, than an inch long. similar to Amphioxus 97 The Cambrian/Ordovician Extinction • Somewhere around 488 million years ago something happened to cause a change in the fauna of the earth, heralding the beginning of the Ordovician Period. • Rather than one catastrophe, the late-Cambrian extinction seems to be a series of smaller extinction events. • Historically the change in fauna (mostly trilobites as the index species) was thought to be due to excessive warmth and low oxygen. • But some current findings point to an oxygen spike due perhaps to continental drift into the tropics, driving rapid speciation and consequent replacement of old with new organisms. 98 Welcome to the Ordovician YOU ARE HERE 99 The Ordovician Sea, 488 million years 100 ago The Ordovician Period lasted almost 45 million years, from 489 to 444 MYA.
    [Show full text]
  • 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.
    [Show full text]
  • Multiple Molecular Evidences for a Living Mammalian Fossil
    Multiple molecular evidences for a living mammalian fossil Dorothe´ e Huchon†‡, Pascale Chevret§¶, Ursula Jordanʈ, C. William Kilpatrick††, Vincent Ranwez§, Paulina D. Jenkins‡‡, Ju¨ rgen Brosiusʈ, and Ju¨ rgen Schmitz‡ʈ †Department of Zoology, George S. Wise Faculty of Life Sciences, Tel Aviv University, Tel Aviv 69978, Israel; §Department of Paleontology, Phylogeny, and Paleobiology, Institut des Sciences de l’Evolution, cc064, Universite´Montpellier II, Place E. Bataillon, 34095 Montpellier Cedex 5, France; ʈInstitute of Experimental Pathology, University of Mu¨nster, D-48149 Mu¨nster, Germany; ††Department of Biology, University of Vermont, Burlington, VT 05405-0086; and ‡‡Department of Zoology, The Natural History Museum, London SW7 5BD, United Kingdom Edited by Francisco J. Ayala, University of California, Irvine, CA, and approved March 18, 2007 (received for review February 11, 2007) Laonastes aenigmamus is an enigmatic rodent first described in their classification as a diatomyid suggests that Laonastes is a 2005. Molecular and morphological data suggested that it is the living fossil and a ‘‘Lazarus taxon.’’ sole representative of a new mammalian family, the Laonastidae, The two research teams also disagreed on the taxonomic and a member of the Hystricognathi. However, the validity of this position of Laonastes. According to Jenkins et al. (2), Laonastes family is controversial because fossil-based phylogenetic analyses is either the most basal group of the hystricognaths (Fig. 2A)or suggest that Laonastes is a surviving member of the Diatomyidae, nested within the hystricognaths (Fig. 2B). According to Dawson a family considered to have been extinct for 11 million years. et al. (3), Laonastes and the other Diatomyidae are the sister According to these data, Laonastes and Diatomyidae are the sister clade of the family Ctenodactylidae (i.e., gundies), a family that clade of extant Ctenodactylidae (i.e., gundies) and do not belong does not belong to the Hystricognathi, but to which it is to the Hystricognathi.
    [Show full text]
  • New York Ocean Action Plan 2016 – 2026
    NEW YORK OCEAN ACTION PLAN 2016 – 2026 In collaboration with state and federal agencies, municipalities, tribal partners, academic institutions, non- profits, and ocean-based industry and tourism groups. Acknowledgments The preparation of the content within this document was developed by Debra Abercrombie and Karen Chytalo from the New York State Department of Environmental Conservation and in cooperation and coordination with staff from the New York State Department of State. Funding was provided by the New York State Environmental Protection Fund’s Ocean & Great Lakes Program. Other New York state agencies, federal agencies, estuary programs, the New York Ocean and Great Lakes Coalition, the Shinnecock Indian Nation and ocean-based industry and user groups provided numerous revisions to draft versions of this document which were invaluable. The New York Marine Sciences Consortium provided vital recommendations concerning data and research needs, as well as detailed revisions to earlier drafts. Thank you to all of the members of the public and who participated in the stakeholder focal groups and for also providing comments and revisions. For more information, please contact: Karen Chytalo New York State Department of Environmental Conservation [email protected] 631-444-0430 Cover Page Photo credits, Top row: E. Burke, SBU SoMAS, M. Gove; Bottom row: Wolcott Henry- 2005/Marine Photo Bank, Eleanor Partridge/Marine Photo Bank, Brandon Puckett/Marine Photo Bank. NEW YORK OCEAN ACTION PLAN | 2016 – 2026 i MESSAGE FROM COMMISSIONER AND SECRETARY The ocean and its significant resources have been at the heart of New York’s richness and economic vitality, since our founding in the 17th Century and continues today.
    [Show full text]
  • 8. Primate Evolution
    8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America.
    [Show full text]
  • Science Journals
    SCIENCE ADVANCES | RESEARCH ARTICLE OCEANOGRAPHY Copyright © 2020 The Authors, some rights reserved; Algal plankton turn to hunting to survive and recover exclusive licensee American Association from end-Cretaceous impact darkness for the Advancement Samantha J. Gibbs1*†, Paul R. Bown2†, Ben A. Ward1†, Sarah A. Alvarez3,2, Hojung Kim2, of Science. No claim to 2‡ 4 5 6 7 original U.S. Government Odysseas A. Archontikis , Boris Sauterey , Alex J. Poulton , Jamie Wilson , Andy Ridgwell Works. Distributed under a Creative The end-Cretaceous bolide impact triggered the devastation of marine ecosystems. However, the specific kill Commons Attribution mechanism(s) are still debated, and how primary production subsequently recovered remains elusive. We used NonCommercial marine plankton microfossils and eco-evolutionary modeling to determine strategies for survival and recovery, License 4.0 (CC BY-NC). finding that widespread phagotrophy (prey ingestion) was fundamental to plankton surviving the impact and also for the subsequent reestablishment of primary production. Ecological selectivity points to extreme post- impact light inhibition as the principal kill mechanism, with the marine food chain temporarily reset to a bacteria- dominated state. Subsequently, in a sunlit ocean inhabited by only rare survivor grazers but abundant small prey, it was mixotrophic nutrition (autotrophy and heterotrophy) and increasing cell sizes that enabled the eventual reestablishment of marine food webs some 2 million years later. Downloaded from INTRODUCTION evidence suggest that at least partial recovery occurred quickly The asteroid impact at the Cretaceous-Paleogene (K/Pg) boundary (years to tens of years), with ubiquitous, prokaryotic cyanobacteria 66 million years (Ma) ago triggered a cascading mass extinction through likely being the main primary producers as light levels improved http://advances.sciencemag.org/ the entirety of the global food web that occurred in a geological in- (4, 12–14).
    [Show full text]
  • INTRODUCTION to PALEOBIOLOGY and the FOSSIL RECORD Died out During Normal Times Than During the MASS EXTINCTIONS More Spectacular Mass Extinctions
    Chapter 7 Mass extinctions and biodiversity loss Key points • During mass extinctions, 20–90% of species were wiped out; these include a broad range of organisms, and the events appear to have happened rapidly. • It is diffi cult to study mass extinctions in the Precambrian, but there seems to have been a Neoproterozoic event between the Ediacaran and Early Cambrian faunas. • The “big fi ve” Phanerozoic mass extinctions occurred in the end-Ordovician, the Late Devonian, the end of the Permian, the end of the Triassic and the end of the Cretaceous. Of these, the Late Devonian and end-Triassic events seem to have lasted some time and involved depressed origination as much as heightened extinction. • The end-Permian mass extinction was the largest of all time, and probably caused by a series of Earth-bound causes that began with massive volcanic eruptions, leading to acid rain and global anoxia. • The end-Cretaceous mass extinction has been most studied, and it was probably caused by a major impact on the Earth. • Smaller-scale extinction events include the loss of mammals at the end of the Pleistocene, perhaps the result of climate change and human hunting. • Recovery from mass extinctions can take a long time; fi rst on the scene may be some unusual disaster taxa that cope well in harsh conditions; they give way to the longer- lived taxa that rebuild normal ecosystems. • Extinction is a major concern today, with calculated species loss as high as during any mass extinction of the past. The severity of the current extinction episode is still debated.
    [Show full text]
  • 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).
    [Show full text]
  • Class SARCOPTERYGII Order COELACANTHIFORMES
    click for previous page Coelacanthiformes: Latimeriidae 3969 Class SARCOPTERYGII Order COELACANTHIFORMES LATIMERIIDAE (= Coelacanthidae) Coelacanths by S.L. Jewett A single species occurring in the area. Latimeria menadoensis Pouyaud, Wirjoatmodjo, Rachmatika, Tjakrawidjaja, Hadiaty, and Hadie, 1999 Frequent synonyms / misidentifications: None / Nearly identical in appearance to Latimeria chalumnae Smith, 1939 from the western Indian Ocean. FAO names: En - Sulawesi coelacanth. Diagnostic characters: A large robust fish. Caudal-peduncle depth nearly equal to body depth. Head robust, with large eye, terminal mouth, and large soft gill flap extending posteriorly from opercular bone. Dorsal surface of snout with pits and reticulations comprising part of sensory system. Three large, widely spaced pores on each side of snout, 1 near tip of snout and 2 just anterior to eye, connecting internally to rostral organ. Anterior nostrils form small papillae located at dorsolateral margin of mouth, at anterior end of pseudomaxillary fold (thick, muscularized skin which replaces the maxilla in coelacanths). Ventral side of head with prominent paired gular plates, longitudinally oriented along midline; skull dorsally with pronounced paired bony plates, just above and behind eyes, the posterior margins of which mark exterior manifestation of intracranial joint (or hinge) that divides braincase into anterior and posterior portions (found only in coelacanths). First dorsal fin typical, with 8 stout bony rays. Second dorsal (28 rays), anal (30), paired pectoral (each 30 to 33), and paired pelvic (each 33) fins lobed, i.e. each with a fleshy base, internally supported by an endoskeleton with which terminal fin rays articulate. Caudal fin atypical, consisting of 3 parts: upper and lower portions with numerous rays more or less symmetrically arranged along dorsal and ventral midlines, and a separate smaller terminal portion (sometimes called epicaudal fin) with symmetrically arranged rays.
    [Show full text]
  • Giant Mesozoic Coelacanths (Osteichthyes, Actinistia) Reveal High Body Size Disparity Decoupled from Taxic Diversity
    Giant Mesozoic Coelacanths (Osteichthyes, Actinistia) Reveal High Body Size Disparity Decoupled From Taxic Diversity Lionel Cavin ( [email protected] ) Natural History Museum of Geneva André Piuz Natural History Museum of Geneva Christophe Ferrante Natural History Museum of Geneva Guillaume Guinot Institut des Sciences de l'Evolution de Montpellier Research Article Keywords: morphological evolution, taxic diversication, Genomic and physiological characteristics Posted Date: March 2nd, 2021 DOI: https://doi.org/10.21203/rs.3.rs-245480/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 2 Giant Mesozoic coelacanths (Osteichthyes, Actinistia) reveal high 3 body size disparity decoupled from taxic diversity 4 5 Lionel Cavin1*, André Piuz1, Christophe Ferrante1,2 & Guillaume Guinot3 6 7 8 1 Department of Geology and Palaeontology, Natural History Museum of Geneva, Geneva, 9 Switzerland 10 2 Department of Earth Sciences, University of Geneva, Rue des Maraîchais 13, 1205 Genève, 11 Switzerland 12 3 Institut des Sciences de l’Evolution de Montpellier (Université de Montpellier, CNRS, IRD, 13 EPHE), Montpellier, France 14 15 * Corresponding author 16 Email: [email protected] 17 1 18 Abstract 19 20 The positive correlation between speciation rates and morphological evolution expressed by 21 body size is a macroevolutionary trait of vertebrates. Although taxic diversification and 22 morphological evolution are slow in coelacanths, their fossil record indicates that large and 23 small species coexisted, which calls into question the link between morphological and body 24 size disparities. Here, we describe and reassess fossils of giant coelacanths. Two genera 25 reached up to 5 meters long, placing them among the ten largest bony fish that ever lived.
    [Show full text]