The Cranial Endocast of Dipnorhynchus Sussmilchi (Sarcopterygii: Dipnoi) and the Interrelationships of Stem-Group Lungfishes
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
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 -
Identifying Heterogeneity in Rates of Morphological Evolution: Discrete Character Change in the Evolution of Lungfish (Sarcopterygii; Dipnoi)
ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2011.01460.x IDENTIFYING HETEROGENEITY IN RATES OF MORPHOLOGICAL EVOLUTION: DISCRETE CHARACTER CHANGE IN THE EVOLUTION OF LUNGFISH (SARCOPTERYGII; DIPNOI) Graeme T. Lloyd,1,2 Steve C. Wang,3 and Stephen L. Brusatte4,5 1Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom 2E-mail: [email protected] 3Department of Mathematics and Statistics, Swarthmore College, Swarthmore, Pennsylvania 19081 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 5Department of Earth and Environmental Sciences, Columbia University, New York, New York 10025 Received February 9, 2010 Accepted August 15, 2011 Data Archived: Dryad: doi:10.5061/dryad.pg46f Quantifying rates of morphological evolution is important in many macroevolutionary studies, and critical when assessing possible adaptive radiations and episodes of punctuated equilibrium in the fossil record. However, studies of morphological rates of change have lagged behind those on taxonomic diversification, and most authors have focused on continuous characters and quantifying patterns of morphological rates over time. Here, we provide a phylogenetic approach, using discrete characters and three statistical tests to determine points on a cladogram (branches or entire clades) that are characterized by significantly high or low rates of change. These methods include a randomization approach that identifies branches with significantly high rates and likelihood ratio tests that pinpoint either branches or clades that have significantly higher or lower rates than the pooled rate of the remainder of the tree. As a test case for these methods, we analyze a discrete character dataset of lungfish, which have long been regarded as “living fossils” due to an apparent slowdown in rates since the Devonian. -
A New Osteolepidid Fish From
Rea. West. Aust. MU8. 1985, 12(3): 361-377 ANew Osteolepidid Fish from the Upper Devonian Gogo Formation, Western Australia J.A. Long* Abstract A new osteolepidid crossopterygian, Gogonasus andrewsi gen. et sp. nov., is des cribed from a single fronto-ethmoidal shield and associated ethmosphenoid, from the Late Devonian (Frasnian) Gogo Formation, Western Australia. Gogonasus is is distinguished from other osteolepids by the shape and proportions of the fronto ethmoidal shield, absence of palatal fenestrae, well developed basipterygoid pro cesses and moderately broad parasphenoid. The family Osteolepididae is found to be paraphyletic, with Gogonasus being regarded as a plesiomorphic osteolepidid at a similar level of organisation to Thursius. Introduction Much has been published on the well-preserved Late Devonian fish fauna from the Gogo Formation, Western Australia, although to date all the papers describing fish have been on placoderms (Miles 1971; Miles and Dennis 1979; Dennis and Miles 1979-1983; Young 1984), palaeoniscoids (Gardiner 1973, 1984; Gardiner and Bartram 1977) or dipnoans (Miles 1977; Campbell and Barwick 1982a, 1982b, 1983, 1984a). This paper describes the only osteolepiform from the fauna (Gardiner and Miles 1975), a small snout with associated braincase, ANU 21885, housed in the Geology Department, Australian National University. The specimen, collected by the Australian National University on the 1967 Gogo Expedition, was prepared by Dr S.M. Andrews (Royal Scottish Museum) and later returned to the ANU. Onychodus is the only other crossopterygian in the fauna. In its proportions and palatal structure the new specimen provides some additional new points of the anatomy of osteolepiforms. Few Devonian crossopte rygians are known from Australia, and so the specimen is significant in having resemblances to typical Northern Hemisphere species. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
A Redescription of the Lungfish Eoctenodus Hills 1929, with Reassessment of Other Australian Records of the Genus Dipterns Sedgwick & Murchison 1828
Ree. West. Aust. Mus. 1987, 13 (2): 297-314 A redescription of the lungfish Eoctenodus Hills 1929, with reassessment of other Australian records of the genus Dipterns Sedgwick & Murchison 1828. J.A. Long* Abstract Eoctenodus microsoma Hills 1929 (= Dipterus microsoma Hills, 1931) from the Frasnian Blue Range Formation, near Taggerty, Victoria, is found to be a valid genus, differing from Dipterus, and other dipnoans, by the shape of the parasphenoid and toothplates. The upper jaw toothp1ates and entopterygoids, parasphenoid, c1eithrum, anoc1eithrum and scales of Eoctenodus are described. Eoctenodus may represent the earliest member of the Ctenodontidae. Dipterus cf. D. digitatus. from the Late Devonian Gneudna Formation, Western Australia (Seddon, 1969), is assigned to Chirodipterus australis Miles 1977; and Dipterus sp. from the Late Devonian of Gingham Gap, New South Wales (Hills, 1936) is thought to be con generic with a dipnoan of similar age from the Hunter Siltstone, New South Wales. This form differs from Dipterus in the shape of the parasphenoid. The genus Dipterus appears to be restricted to the Middle-Upper Devonian of Europe, North America and the USSR (Laurasia). Introduction Although Hills (1929) recognised a new dipnoan, Eoctenodus microsoma, in the Late Devonian fish remains from the Blue Range Formation, near Taggerty, he later (Hills 1931) altered the generic status of this species after a study trip to Britain in which D,M.S. Watson pointed out similarities between the Australian form and the British genus Dipterus Sedgwick and Murchison 1828. Studies of the head of Dipterus by Westoll (1949) and White (1965) showed the structure of the palate and, in particular, the shape of the parasphenoid which differs from that in the Taggerty dipnoan. -
A Lungfish Survivor of the End-Devonian Extinction and an Early Carboniferous Dipnoan
1 A Lungfish survivor of the end-Devonian extinction and an Early Carboniferous dipnoan 2 radiation. 3 4 Tom J. Challands1*, Timothy R. Smithson,2 Jennifer A. Clack2, Carys E. Bennett3, John E. A. 5 Marshall4, Sarah M. Wallace-Johnson5, Henrietta Hill2 6 7 1School of Geosciences, University of Edinburgh, Grant Institute, James Hutton Road, Edinburgh, 8 EH9 3FE, UK. email: [email protected]; tel: +44 (0) 131 650 4849 9 10 2University Museum of Zoology Cambridge, Downing Street, Cambridge CB2 3EJ, UK. 11 12 3Department of Geology, University of Leicester, Leicester LE1 7RH, UK. 13 14 4School of Ocean & Earth Science, University of Southampton, National Oceanography Centre, 15 European Way, University Road, Southampton, SO14 3ZH , UK. 16 17 5Sedgwick Museum, Department of Earth Sciences, University of Cambridge, Downing St., 18 Cambridge CB2 3EQ, UK 1 19 Abstract 20 21 Until recently the immediate aftermath of the Hangenberg event of the Famennian Stage (Upper 22 Devonian) was considered to have decimated sarcopterygian groups, including lungfish, with only 23 two taxa, Occludus romeri and Sagenodus spp., being unequivocally recorded from rocks of 24 Tournaisian age (Mississippian, Early Carboniferous). Recent discoveries of numerous 25 morphologically diverse lungfish tooth plates from southern Scotland and northern England indicate 26 that at least ten dipnoan taxa existed during the earliest Carboniferous. Of these taxa, only two, 27 Xylognathus and Ballgadus, preserve cranial and post-cranial skeletal elements that are yet to be 28 described. Here we present a description of the skull of a new genus and species of lungfish, 29 Limanichthys fraseri gen. -
I Ecomorphological Change in Lobe-Finned Fishes (Sarcopterygii
Ecomorphological change in lobe-finned fishes (Sarcopterygii): disparity and rates by Bryan H. Juarez A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science (Ecology and Evolutionary Biology) in the University of Michigan 2015 Master’s Thesis Committee: Assistant Professor Lauren C. Sallan, University of Pennsylvania, Co-Chair Assistant Professor Daniel L. Rabosky, Co-Chair Associate Research Scientist Miriam L. Zelditch i © Bryan H. Juarez 2015 ii ACKNOWLEDGEMENTS I would like to thank the Rabosky Lab, David W. Bapst, Graeme T. Lloyd and Zerina Johanson for helpful discussions on methodology, Lauren C. Sallan, Miriam L. Zelditch and Daniel L. Rabosky for their dedicated guidance on this study and the London Natural History Museum for courteously providing me with access to specimens. iii TABLE OF CONTENTS ACKNOWLEDGEMENTS ii LIST OF FIGURES iv LIST OF APPENDICES v ABSTRACT vi SECTION I. Introduction 1 II. Methods 4 III. Results 9 IV. Discussion 16 V. Conclusion 20 VI. Future Directions 21 APPENDICES 23 REFERENCES 62 iv LIST OF TABLES AND FIGURES TABLE/FIGURE II. Cranial PC-reduced data 6 II. Post-cranial PC-reduced data 6 III. PC1 and PC2 Cranial and Post-cranial Morphospaces 11-12 III. Cranial Disparity Through Time 13 III. Post-cranial Disparity Through Time 14 III. Cranial/Post-cranial Disparity Through Time 15 v LIST OF APPENDICES APPENDIX A. Aquatic and Semi-aquatic Lobe-fins 24 B. Species Used In Analysis 34 C. Cranial and Post-Cranial Landmarks 37 D. PC3 and PC4 Cranial and Post-cranial Morphospaces 38 E. PC1 PC2 Cranial Morphospaces 39 1-2. -
Du Dévonien Supérieur De Miguasha, Québec, Canada
UNIVERSITÉ DU QUÉBEC À RIMOUSKI Développement larvaire et juvénile de Scaumenacia curta (Sarcopterygii : Dipnoi) du Dévonien supérieur de Miguasha, Québec, Canada Mémoire présenté dans le cadre du programme de maîtrise en gestion de la fa un e et de ses habitats en vue de l'obtention du grade de maître ès sciences PAR © ISABELLE BÉCHARD Juin 2011 UNIVERSITÉ DU QUÉBEC À RIMOUSKI Service de la bibliothèque Avertissement La diffusion de ce mémoire ou de cette thèse se fait dans le respect des droits de son auteur, qui a signé le formulaire « Autorisation de reproduire et de diffuser un rapport, un mémoire ou une thèse ». En signant ce formulaire, l’auteur concède à l’Université du Québec à Rimouski une licence non exclusive d’utilisation et de publication de la totalité ou d’une partie importante de son travail de recherche pour des fins pédagogiques et non commerciales. Plus précisément, l’auteur autorise l’Université du Québec à Rimouski à reproduire, diffuser, prêter, distribuer ou vendre des copies de son travail de recherche à des fins non commerciales sur quelque support que ce soit, y compris l’Internet. Cette licence et cette autorisation n’entraînent pas une renonciation de la part de l’auteur à ses droits moraux ni à ses droits de propriété intellectuelle. Sauf entente contraire, l’auteur conserve la liberté de diffuser et de commercialiser ou non ce travail dont il possède un exemplaire. Il Composition du jury: Nathalie R. Le François, présidente du jury, Université du Québec à Rimouski, [email protected] Richard Cloutier, directeur de recherche, Université du Québec à Rimouski, [email protected] Philippe Janvier, examinateur externe, Muséum national d'Histoire naturelle de Paris, UMR 5143 du CNRS, [email protected] Dépôt initial le 16 décembre 2010 Dépôt final le 29 juin 20 Il IV REMERCIEMENTS J'aimerais remercier ma famille pour le support inconditionnel qu'ils m'ont apporté tout au long de mon retour aux études. -
Fossils Provide Better Estimates of Ancestral Body Size Than Do Extant
Acta Zoologica (Stockholm) 90 (Suppl. 1): 357–384 (January 2009) doi: 10.1111/j.1463-6395.2008.00364.x FossilsBlackwell Publishing Ltd provide better estimates of ancestral body size than do extant taxa in fishes James S. Albert,1 Derek M. Johnson1 and Jason H. Knouft2 Abstract 1Department of Biology, University of Albert, J.S., Johnson, D.M. and Knouft, J.H. 2009. Fossils provide better Louisiana at Lafayette, Lafayette, LA estimates of ancestral body size than do extant taxa in fishes. — Acta Zoologica 2 70504-2451, USA; Department of (Stockholm) 90 (Suppl. 1): 357–384 Biology, Saint Louis University, St. Louis, MO, USA The use of fossils in studies of character evolution is an active area of research. Characters from fossils have been viewed as less informative or more subjective Keywords: than comparable information from extant taxa. However, fossils are often the continuous trait evolution, character state only known representatives of many higher taxa, including some of the earliest optimization, morphological diversification, forms, and have been important in determining character polarity and filling vertebrate taphonomy morphological gaps. Here we evaluate the influence of fossils on the interpretation of character evolution by comparing estimates of ancestral body Accepted for publication: 22 July 2008 size in fishes (non-tetrapod craniates) from two large and previously unpublished datasets; a palaeontological dataset representing all principal clades from throughout the Phanerozoic, and a macroecological dataset for all 515 families of living (Recent) fishes. Ancestral size was estimated from phylogenetically based (i.e. parsimony) optimization methods. Ancestral size estimates obtained from analysis of extant fish families are five to eight times larger than estimates using fossil members of the same higher taxa. -
Universidade Do Estado Do Rio De Janeiro Centro Biomédico Instituto De Biologia Roberto Alcântara Gomes
Universidade do Estado do Rio de Janeiro Centro Biomédico Instituto de Biologia Roberto Alcântara Gomes Raphael Miguel da Silva Biogeografia Histórica de Celacantos (Sarcopterygii: Actinistia) Rio de Janeiro 2016 Raphael Miguel da Silva Biogeografia Histórica de Celacantos (Sarcopterygii: Actinistia) Tese apresentada, como requisito parcial para obtenção do título de Doutor, ao Programa de Pós-graduação em Ecologia e Evolução, da Universidade do Estado do Rio de Janeiro. Orientadora: Prof.a Dra. Valéria Gallo da Silva Rio de Janeiro 2016 CATALOGAÇÃO NA FONTE UERJ / REDE SIRIUS / BIBLIOTECA CTC-A SS586XXX Silva, Raphael Miguel da. Biogeografia histórica de Celacantos (Sarcopterygii: Actinistia) / Raphael Miguel da Silva. - 2016. 271 f. : il. Orientador: Valéria Gallo da Silva. Tese (Doutorado em Ecologia e Evolução) - Universidade do Estado do Rio de Janeiro, Instituto de Biologia Roberto Alcântara Gomes. 1. Biologia marinha - Teses. 2. Peixe – Teses. I. Silva, Valéria Gallo. II. Universidade do Estado do Rio de Janeiro. Instituto de Biologia Roberto Alcântara Gomes. III. Título. CDU 504.4 Autorizo para fins acadêmicos e científicos, a reprodução total ou parcial desta tese, desde que citada a fonte. ___________________________ ________________________ Assinatura Data Raphael Miguel da Silva Biogeografia Histórica de Celacantos (Sarcopterygii: Actinistia) Tese apresentada, como requisito parcial para obtenção do título de Doutor, ao Programa de Pós-graduação em Ecologia e Evolução, da Universidade do Estado do Rio de Janeiro. Aprovada em 15 de fevereiro de 2016. Orientadora: Prof.a Dra. Valéria Gallo da Silva Instituto de Biologia Roberto Alcantara Gomes - UERJ Banca Examinadora: ____________________________________________ Prof. Dr. Paulo Marques Machado Brito Instituto de Biologia Roberto Alcantara Gomes - UERJ ____________________________________________ Prof.ª Dra. -
Fotw Classification Detailed Version
1 Classification of fishes from Fishes of the World 5th Edition. Nelson, JS, Grande, TC, and Wilson, MVH. 2016. This is a more detailed version of the listing in the book’s Table of Contents. Order and Family numbers are in parentheses; the page number follows a comma; † indicates extinct taxon. If you spot errors, please let us know at [email protected]. Latest update January 11, 2018. PHYLUM CHORDATA, 13 SUBPHYLUM UROCHORDATA—tunicates, 15 Class ASCIDIACEA—ascidians, 15 Class THALIACEA—salps, 15 Order PYROSOMIDA, 15 Order DOLIOLIDA, 15 Order SALPIDA, 15 Class APPENDICULARIA, 15 SUBPHYLUM CEPHALOCHORDATA, 16 Order AMPHIOXIFORMES—lancelets, 16 Family BRANCHIOSTOMATIDAE, 16 Family EPIGONICHTHYIDAE, 16 †SUBPHYLUM CONODONTOPHORIDA—conodonts, 17 †Class CONODONTA, 17 SUBPHYLUM CRANIATA, 18 INFRAPHYLUM MYXINOMORPHI, 19 Class MYXINI, 20 Order MYXINIFORMES (1)—hagfishes, 20 Family MYXINIDAE (1)—hagfishes, 20 Subfamily Rubicundinae, 21 Subfamily Eptatretinae, 21 Subfamily Myxininae, 21 INFRAPHYLUM VERTEBRATA—vertebrates, 22 †Anatolepis, 22 Superclass PETROMYZONTOMORPHI, 23 Class PETROMYZONTIDA, 23 Order PETROMYZONTIFORMES (2)—lampreys, 23 †Family MAYOMYZONTIDAE, 24 Family PETROMYZONTIDAE (2)—northern lampreys, 24 Subfamily Petromyzontinae, 24 Subfamily Lampetrinae, 25 Family GEOTRIIDAE (3)—southern lampreys, 25 Family MORDACIIDAE (4)—southern topeyed lampreys, 26 †Superclass PTERASPIDOMORPHI, 26 †Class PTERASPIDOMORPHA, 26 Subclass ASTRASPIDA, 27 †Order ASTRASPIDIFORMES, 27 Subclass ARANDASPIDA, 27 †Order ARANDASPIDIFORMES,