Advanced Online Publication

Total Page:16

File Type:pdf, Size:1020Kb

Advanced Online Publication DOI: 10.19615/j.cnki.2096-9899.210519 Online Supplementary Material A new species of Pteronisculus from the Middle Triassic (Anisian) of Luoping, Yunnan, China, and phylogenetic relationships of early actinopterygian fishes Table of Contents 1. Occurrences of Pteronisculus 2. Comparisons of pterygial formula 3. Taxa and principal sources of data Advanced4. Supplementary figure online publication 5. Character list 6. References to supplementary information 1 1. Occurrences of Pteronisculus White, 1933, according to the published literature Species Occurrence Age References Pteronisculus cicatrosus Northwest Early Triassic White (1933), Lehman Madagascar (1952), Uyeno (1978) P. macropterus Northwest Early Triassic White (1933), Lehman Madagascar (1952) P. arambourgi Northwest Early Triassic Lehman (1952) Madagascar P. broughi Northwest Early Triassic Lehman (1952) Madagascar P. gyrolepidoides Spitsbergen Early Triassic Stensiö (1921), Véran (Svalbard) (1988) P. arcticus Greenland Early Triassic Stensiö (1932), Nielsen (1936, 1942) AdvancedP. stensioi Greenlandonline Early Triassicpublication Nielsen (1942) P. gunnari Greenland Early Triassic Nielsen (1942) P. magnus Greenland Early Triassic Nielsen (1942) P. aldingeri Greenland Early Triassic Nielsen (1942) P. nevadanus Nevada (USA) Early Triassic Romano et al. (2019) P. nielseni Yunnan (China) Middle Triassic Xu et al. (2014) P. changae Yunnan (China) Middle Triassic This study 2. Comparisons of pterygial formula in selected species of Pteronisculus Species D P A T P. arctica 33–35 14 30 55–59 P. stensioi 41–43 20 35 63 P. aldingeri ~40 16–18 37 ~65 P. nielseni 36–38 14 29–30 60–61 P. changae 53 15 44 83 2 3. Taxa and principal sources of data Taxon Source Guiyu oneiros (out group) Zhu et al., 2009; Qiao and Zhu, 2010 Acipenser brevirostrum Nieuwenhuys, 1982; Hilton et al., 2011 Aesopichthys erinaceus Poplin and Lund, 2000 Amia calva Grande and Bemis, 1998; Sallan, 2014 Asialepidotus shingyiensis Su, 1959; Xu and Ma, 2017 Amphicentrum granulosum Traquair, 1875; Bradley-Dyne, 1939 Atractosteus spatula Grande, 2010 Australosomus kochi Nielsen, 1949 Beagiascus pulcherrimus Mickle et al., 2009 Beishanichthys brevicaudalis Xu and Gao, 2011 Birgeria groenlandica Nielsen, 1949 AdvancedBirgeria stensioi onlineAldinger, 1931; Romano publication and Brinkmann, 2009 Bobasatrania groenlandica Stensiö, 1932 Boreosomus piveteaui Nielsen, 1942 Caturus furcatus Patterson, 1975; Lambers, 1994; Grande and Bemis, 1998 Cheirolepis canadensis Arratia and Cloutier, 1996; Arratia, 2009 Cheirolepis schultzei Cloutier and Arratia, 2004 Cheirolepis trailli Pearson and Westoll, 1979; Giles et al., 2015a Chondrosteus acipenseroides Hilton and Forey 2011; Hilton et al., 2011 Cosmoptychius striatus Schaeffer, 1971; Coates, 1999 Cyranorhis bergeraci Lund et al., 1997 Discoserra pectinodon Lund, 2000; Hurley et al., 2007 Donnrosenia schaefferi Long et al., 2008 Dorsetichthys bechei Patterson, 1968, 1973, 1975; Grande and Bemis, 1998 Ebenaqua ritchei Campbell and Le Duy Phuoc, 1983 Elops hawaiensis Forey, 1973 Erpetoichthys calabaricus Claeson et al., 2007; Claeson and Hagadorn, 2008 Evenkia eunoptera Berg, 1942; Selezneva, 1985; Sytchevskaya, 1999 Fouldenia ischiptera Sallan and Coates, 2013 Fukangichthys longidorsalis Xu et al., 2014a Howqualepis rostridens Long, 1988; Choo, 2009 Ionoscopus cyprinoides Grande and Bemis, 1998; Maisey, 1999 Kalops monophyrum Poplin and Lund, 2000 Kentuckia deani Rayner, 1951; Giles and Friedman, 2014 Balfour and Parker, 1882; Rayner, 1937; Mathiesen and Lepisosteus osseus Popper, 1987; Grande, 2010 Louwoichthys pusillus Xu, 2020 Luganoia lepidosteoides Bürgin, 1992 Jain and Robinson, 1963; Wenz, 1967; Patterson, 1975; Macrosemimimus lennieri Schröder et al., 2012 3 Macrosemius rostratus Bartram, 1977 Melanecta anneae Coates, 1998 Mesopoma planti Coates, 1999 Mimipiscis bartrami Gardiner, 1984; Choo, 2011 Mimipiscis toombsi Gardiner, 1984; Choo, 2011; Giles and Friedman, 2014 Moythomasia lineata Jessen, 1968; Choo 2015 Moythomasia nitida Jessen, 1968; Choo 2015 Moythomasia durgaringa Gardiner, 1984; Long and Trinajstic, 2010; Choo 2015 Obaichthys decoratus Grande, 2010 Ophiopsiella attenuata Wagner, 1863; Bartram, 1975; Lane and Ebert, 2015 Osorioichthys marginis Taverne, 1997 Polyodon spathula Walbaum, 1792; Grande and Bemis, 1991 Allis, 1922; Jollie, 1984; Bjerring, 1991; Bartsch and Polypterus bichir Advanced onlineGemballa, 1992; Ba publicationrtsch et al., 1997; Grande, 2010 Propterus elongatus Bartram, 1977 Pteronisculus changae sp. nov. This study Pteronisculus cicatrosus Lehman, 1952 Pteronisculus magnus Nielsen, 1942 Pteronisculus nielseni Xu et al., 2014b Pteronisculus stensioi Nielsen 1942; Coates, 1998 Raynerius splendens Giles et al., 2015b Saurichthys madagascariensis Kogan et al., 2016 Saurichthys ornatus Stensiö, 1925; Mutter et al., 2008 Saurichthys sp. Stensiö, 1925; Minikh, 1981 Semionotus elegans Olsen and McCune, 1991 Styracopterus fulcratus Sallan and Coates, 2013 Teffichthys madagascariensis Piveteau, 1934; Marramà et al., 2017 Venusichthys comptus Xu and Zhao, 2016 Watsonulus eugnathoides Olsen, 1984; Grande and Bemis, 1998 Woodichthys bearsdeni Coates, 1998 Yelangichthys macrocephalus Wu et al., 2013 4 4. Supplementary figure Advanced online publication Fig. 1S Strict consensus of 12 most parsimonious trees with character states supporting the nodes and terminal taxa 5 5. Character list Characters 1–275 are taken from Argyriou et al. (2018), which in turn is modified from Giles et al. (2017; see for character notes and provenance). Changes in coding and the source of additional characters (Chas. 276–282) are noted in the description. The states of 18 characters (Chas. 1, 2, 28, 37, 94, 99, 127, 128, 135, 140, 147, 150, 176, 208, 230, 234, 238, and 250) are constant throughout the selected taxa and are not included when performing this phylogenetic analysis. Ordered multistate characters (91, 93, 155, 177, 251 and 260) are indicated with an asterisk (*). General 1. Large dermal plates (Forey, 1980; Gardiner, 1984; Zhu and Schultze, 2001; Zhu et al., 2001, 2006, 2009, 2013; Zhu and Yu, 2002; Friedman, 2007; Brazeau, 2009; Friedman and Brazeau; 2010; Davis et al., 2012; Brazeau and Friedman, 2014; Giles et al., 2015b, 2017; Wilson et al., 2018; Argyriou et al., 2018) 0 absent 1 present Advanced2. Sensory lines online publication (Brazeau, 2009; Zhu et al., 2013; Giles et al., 2015b, 2017; Wilson et al., 2018; Argyriou et al., 2018) 0 preserved as open grooves 1 pass through canals Dermal skull 3. Premaxilla as distinct ossification (Hurley et al., 2007; Xu et al., 2014a; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018. Typically, the premaxilla is a short, paired or median bone that contributes to the orbital margin anterior to the maxilla. The coding for Australosomus kochi is revised to ‘?’) 0 present 1 absent 4. Premaxillae, contact at midline (Cloutier and Ahlberg, 1996; Taverne, 1997; Schultze and Cumbaa, 2001; Zhu and Schultze, 2001; Zhu and Yu, 2002; Cloutier and Arratia, 2004; Friedman and Blom, 2006; Zhu et al., 2006; Friedman, 2007; Long et al., 2008; Swartz, 2009; Choo, 2011; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018) 0 present 1 absent 5. Premaxilla fused at midline (Xu et al., 2012, 2015; Xu and Zhao, 2016; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018. Coded as inapplicable in taxa lacking any ossification in the position typically occupied by the premaxilla (e.g. Acipenser and Cyranorhis) and where the premaxilla appears fused with the rostral (e.g. Bobasatrania, Styracopterus and Luganoia)) 0 absent 1 present 6. Premaxilla (Friedman, 2007; Giles et al., 2015b, 2017; Wilson et al., 2018; Argyriou et al., 2018. Coded as inapplicable in taxa lacking any ossification in the position typically occupied by the premaxilla (e.g. Acipenser and Cyranorhis) and in taxa where the premaxillae do not contact at the midline. The coding for Watsonulus eugnathoides is revised to ‘1’) 6 0 reaches or extends past anterior margin of orbit 1 confined to region anterior to orbit 7. Premaxilla contributes to orbital margin (Cloutier and Ahlberg, 1996; Schultze and Cumbaa, 2001; Zhu and Schultze, 2001; Zhu et al., 2001, 2006, 2009, 2013; Zhu and Yu, 2002; Cloutier and Arratia, 2004; Friedman, 2007; Long et al., 2008; Swartz, 2009; Xu and Gao, 2011; Xu et al., 2014a; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018. The coding for Pteronisculus stensioi is revised to ‘?’) 0 absent 1 present 8. Teeth on premaxillae (Cloutier and Arratia, 2004, Xu et al., 2014a; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018. The coding for Pteronisculus stensioi is revised to ‘?’) 0 present 1 absent Advanced9. Mobile premaxilla online publication (Arratia, 1999; Cavin and Suteethorn, 2006; Hurley et al., 2007; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018) 0 absent 1 present 10. Olfactory nerve pierces premaxilla (Grande, 2010; Xu et al., 2015; Xu and Shen, 2015; Xu and Zhao, 2016; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018. The codings for Watsonulus eugnathoides and Macrosemius rostratus are revised to ‘0’) 0 absent 1 present 11. Nasal process of premaxilla (Gardiner and Schaeffer, 1989; Gardiner et al., 1996, 2005; Cavin and Suteethorn, 2006; Hurley et al., 2007; Grande, 2010; Lopez-Arbarello, 2011; Xu and Wu, 2012; Xu et al., 2014a; Xu and Shen, 2015; Xu and Zhao, 2016; Giles et al., 2017; Wilson et al., 2018; Argyriou et al., 2018) 0 absent 1 short 2
Recommended publications
  • 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.
    [Show full text]
  • 35-51 New Data on Pleuropholis Decastroi (Teleostei, Pleuropholidae)
    Geo-Eco-Trop., 2019, 43, 1 : 35-51 New data on Pleuropholis decastroi (Teleostei, Pleuropholidae), a “pholidophoriform” fish from the Lower Cretaceous of the Eurafrican Mesogea Nouvelles données sur Pleuropholis decastroi (Teleostei, Pleuropholidae), un poisson “pholidophoriforme” du Crétacé inférieur de la Mésogée eurafricaine Louis TAVERNE 1 & Luigi CAPASSO 2 Résumé: Le crâne et le corps de Pleuropholis decastroi, un poisson fossile de l’Albien (Crétacé inférieur) du sud de l’Italie, sont redécrits en détails. P. decastroi diffère des autres espèces du genre par ses deux nasaux en contact médian et qui séparent complètement le dermethmoïde ( = rostral) des frontaux. Avec son maxillaire extrêmement élargi qui couvre la mâchoire inférieure et son supramaxillaire fortement réduit, P. decastroi semble plus nettement apparenté avec Pleuropholis cisnerosorum, du Jurassique supérieur du Mexique, qu’avec les autres espèces du genre. Par ses mâchoires raccourcies et ses nombreux os orbitaires, Pleuropholis apparaît également comme le genre le plus spécialisé de la famille. La position systématique des Pleuropholidae au sein du groupe des « pholidophoriformes » est discutée. Mots-clés: Pleuropholis decastroi, Albien, Italie du sud, Pleuropholis, Pleuropholidae, “Pholidophoriformes”, ostéologie, position systématique. Abstract: The skull and the body of Pleuropholis decastroi, a fossil fish from the marine Albian (Lower Cretaceous) of southern Italy, are re-described in details. P. decastroi differs from the other species of the genus by their two nasals that are in contact along the mid-line, completely separating the dermethmoid (= rostral) from the frontals. With its extremely broadened maxilla that covers the lower jaw and its strongly reduced supramaxilla, P. decastroi seems more closely related to Pleuropholis cisnerosorum, from the Upper Jurassic of Mexico, than to the other species of the genus.
    [Show full text]
  • Table S1.Xlsx
    Bone type Bone type Taxonomy Order/series Family Valid binomial Outdated binomial Notes Reference(s) (skeletal bone) (scales) Actinopterygii Incertae sedis Incertae sedis Incertae sedis †Birgeria stensioei cellular this study †Birgeria groenlandica cellular Ørvig, 1978 †Eurynotus crenatus cellular Goodrich, 1907; Schultze, 2016 †Mimipiscis toombsi †Mimia toombsi cellular Richter & Smith, 1995 †Moythomasia sp. cellular cellular Sire et al., 2009; Schultze, 2016 †Cheirolepidiformes †Cheirolepididae †Cheirolepis canadensis cellular cellular Goodrich, 1907; Sire et al., 2009; Zylberberg et al., 2016; Meunier et al. 2018a; this study Cladistia Polypteriformes Polypteridae †Bawitius sp. cellular Meunier et al., 2016 †Dajetella sudamericana cellular cellular Gayet & Meunier, 1992 Erpetoichthys calabaricus Calamoichthys sp. cellular Moss, 1961a; this study †Pollia suarezi cellular cellular Meunier & Gayet, 1996 Polypterus bichir cellular cellular Kölliker, 1859; Stéphan, 1900; Goodrich, 1907; Ørvig, 1978 Polypterus delhezi cellular this study Polypterus ornatipinnis cellular Totland et al., 2011 Polypterus senegalus cellular Sire et al., 2009 Polypterus sp. cellular Moss, 1961a †Scanilepis sp. cellular Sire et al., 2009 †Scanilepis dubia cellular cellular Ørvig, 1978 †Saurichthyiformes †Saurichthyidae †Saurichthys sp. cellular Scheyer et al., 2014 Chondrostei †Chondrosteiformes †Chondrosteidae †Chondrosteus acipenseroides cellular this study Acipenseriformes Acipenseridae Acipenser baerii cellular Leprévost et al., 2017 Acipenser gueldenstaedtii
    [Show full text]
  • Great Canadian Lagerstätten 4. the Devonian Miguasha Biota
    Document généré le 29 sept. 2021 18:57 Geoscience Canada Great Canadian Lagerstätten 4. The Devonian Miguasha Biota (Québec): UNESCO World Heritage Site and a Time Capsule in the Early History of Vertebrates Richard Cloutier Volume 40, numéro 2, 2013 Résumé de l'article Au cours des 170 dernières années, le biote du Dévonien supérieur de URI : https://id.erudit.org/iderudit/geocan40_2ser02 Miguasha de l’Est du Canada a fourni un assemblage aquatique diversifié, comprenant 20 espèces de vertébrés inférieurs (anaspides, ostéostracés, Aller au sommaire du numéro placodermes, acanthodiens, actinoptérygiens et sarcoptérygiens) et un assemblage peu diversifié d’invertébrés ainsi qu’une composante continentale, représentée par des plantes, des scorpions et des mille-pattes. À l’origine Éditeur(s) interprété comme un milieu lacustre d’eau douce, les dernières preuves paléontologiques, taphonomiques, sédimentologiques et géochimiques The Geological Association of Canada confirment un environ-nement saumâtre rappelant celui d’un estuaire. Plus de 18,000 fossiles de poissons ont été découverts montrant différents états de ISSN conservation, notamment en trois dimensions et la préservation de tissus mous. La plupart des vertébrés sont connus par de nombreux spécimens 0315-0941 (imprimé) complets et articulés. Des spécimens de larves et de juvéniles, 1911-4850 (numérique) exceptionnellement bien conservés, ont été identifiées pour 14 des 20 espèces de poissons permettant des études détaillées de leur croissance. De nombreux Découvrir la revue horizons au sein de la Formation d’Escuminac sont inter-prétés soit comme des Konservat– ou Konzentrat–Lagerstätten. Citer cet article Cloutier, R. (2013). Great Canadian Lagerstätten 4. The Devonian Miguasha Biota (Québec): UNESCO World Heritage Site and a Time Capsule in the Early History of Vertebrates.
    [Show full text]
  • The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
    XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution.
    [Show full text]
  • Leo Semenovich Berg and the Biology of Acipenseriformes: a Dedication
    Environmental Biology of Fishes 48: 15–22, 1997. 1997 Kluwer Academic Publishers. Printed in the Netherlands. Leo Semenovich Berg and the biology of Acipenseriformes: a dedication Vadim J. Birstein1 & William E. Bemis2 1 The Sturgeon Society, 331 West 57th Street, Suite 159, New York, NY 10019, U.S.A. 2 Department of Biology and Graduate Program in Organismic and Evolutionary Biology, University of Massachusetts, Amherst, MA 01003, U.S.A. Received 5.3.1996 Accepted 23.5.1996 Key words: T. Dobzhansky, A. Sewertzoff, T. Lysenko, Paleonisciformes, biogeography This volume is dedicated to the memory of Leo Semenovich Berg (1876–1950), a Russian ichthyologist and geographer. In the foreword to the English translation of Berg’s remarkable treatise, ‘Nomogenesis or evolu- tion according to law’, Theodosius Dobzhansky wrote: ‘Berg was one of the outstanding intellects among Russian scientists. The breadth of his interests and the depth as well as the amplitude of his scholarship were remarkable. He had the reputation of being a ‘walking library’, because of the amount of information he could produce from his memory’ (Dobzhansky 1969, p. xi). Berg was prolific, publishing 217 papers and monographs on ichthyology, 30 papers on general zoology and biology, 20 papers on paleontology, 32 papers on zoogeo- graphy, 320 papers and monographs on geography, geology, and ethnography, as well as 290 biographies, obituaries, and popular articles (Berg 1955, Sokolov 1955). Berg was born 120 years ago, on 14 March 1876, in Sciences. Berg was never formally recognized by the town of Bendery. According to laws of the Rus- the Soviet Academy for his accomplishments in sian Empire, Berg could not enter the university as biology, and only later (1946) was he elected a mem- a Jew, so he was baptized and became a Lutheran, ber of the Geography Branch of the Soviet Acade- which allowed him to study and receive his diploma my of Sciences (Figure 1).
    [Show full text]
  • A Middle Triassic Kyphosichthyiform from Yunnan, China, and Phylogenetic Reassessment of Early Ginglymodians
    SUPPLEMENTARY DATA A Middle Triassic kyphosichthyiform from Yunnan, China, and phylogenetic reassessment of early ginglymodians XU Guang-Hui1,2 MA Xin-Ying1,2,3 WU Fei-Xiang1,2 REN Yi1,2,3 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) (2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044) (3 University of Chinese Academy of Sciences Beijing 100049) Part A Material examined and references Amia calva and Solnhofenamia elongata (Grande and Bemis, 1998); Araripelepidotes temnurus (Maisey, 1991; Thies, 1996); Asialepidotus shingyiensis (Xu and Ma, 2018); Atractosteus spatula, Cuneatus wileyi, Dentilepisosteus laevis, Lepisosteus osseus, Masillosteus janeae, and Obaichthys decoratus (Grande, 2010); Caturus furcatus (Patterson, 1975; Lambers, 1992; Grande and Bemis, 1998; FMNH UC2057); Dorsetichthys (‘Pholidophorus’) bechei (Patterson, 1975; Grande and Bemis, 1998; Arratia, 2013); Elops hawaiensis (Forey, 1973); Fuyuanichthys wangi (Xu et al., 2018); Ichthyokentema purbeckensis (Griffith and Patterson, 1963); Ionoscopus cyprinoides (Grande and Bemis, 1998; Maisey, 1999; FMNH P15472); Isanichthys palustris (Cavin and Suteethorn, 2006); Kyphosichthys grandei (Xu and Wu, 2012; Sun and Ni, 2018); Lashanichthys (‘Sangiorgioichthys’) sui (López-Arbarello et al., 2011); Lashanichthys (‘Sangiorgioichthys’) yangjuanensis (Chen et al, 2014); Lepidotes gigas (Thies,
    [Show full text]
  • Gar (Lepisosteidae)
    Indiana Division of Fish and Wildlife’s Animal Information Series Gar (Lepisosteidae) Gar species found in Indiana waters: -Longnose Gar (Lepisosteus osseus) -Shortnose Gar (Lepisosteus platostomus) -Spotted Gar (Lepisosteus oculatus) -Alligator Gar* (Atractosteus spatula) *Alligator Gar (Atractosteus spatula) Alligator gar were extirpated in many states due to habitat destruction, but now they have been reintroduced to their old native habitat in the states of Illinois, Missouri, Arkansas, and Kentucky. Because they have been stocked into the Ohio River, there is a possibility that alligator gar are either already in Indiana or will be found here in the future. Alligator gar are one of the largest freshwater fishes of North America and can reach up to 10 feet long and weigh 300 pounds. Alligator gar are passive, solitary fishes that live in large rivers, swamps, bayous, and lakes. They have a short, wide snout and a double row of teeth on the upper jaw. They are ambush predators that eat mainly fish but have also been seen to eat waterfowl. They are not, however, harmful to humans, as they will only attack an animal that they can swallow whole. Photo Credit: Duane Raver, USFWS Other Names -garpike, billy gar -Shortnose gar: shortbill gar, stubnose gar -Longnose gar: needlenose gar, billfish Why are they called gar? The Anglo-Saxon word gar means spear, which describes the fishes’ long spear-like appearance. The genus name Lepisosteus contains the Greek words lepis which means “scale” and osteon which means “bone.” What do they look like? Gar are slender, cylindrical fishes with hard, diamond-shaped and non-overlapping scales.
    [Show full text]
  • 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.
    [Show full text]
  • Ecology of the Alligator Gar, Atractosteusspatula, in the Vicente G1;Jerreroreservoir, Tamaulipas, Mexico
    THE SOUTHWESTERNNATURALIST 46(2):151-157 JUNE 2001 ECOLOGY OF THE ALLIGATOR GAR, ATRACTOSTEUSSPATULA, IN THE VICENTE G1;JERRERORESERVOIR, TAMAULIPAS, MEXICO .-., FRANCISCO J. GARCiA DE LEON, LEONARDO GoNzALEZ-GARCiA, JOSE M. HERRERA-CAsTILLO, KIRK O. WINEMILLER,* AND ALFONSO BANDA-VALDES Laboratorio de Biologia lntegrativa, lnstituto Tecnol6gicode Ciudad Victoria, Boulevard Emilio Fortes Gil1301, Ciudad Victoria, CP 87010, Tamaulipas, Mexico (F]GL, LGG,]MHC) Department of Wildlife and FisheriesSciences, Texas A&M University, CollegeStation, TX 77843-2258 (KO~ Direcci6n Generalde Pescadel Gobiernodel Estado de Tamaulipas, Ciudad Victoria, Tamaulipas, Mexico (ABV) * Correspondent:[email protected] ABsTRACf-We provide the first ecological account of the alligator gar, Atractosteusspatula, in the Vicente Guerrero Reservoir, Tamaulipas, Mexico. During March to September, 1998, the local fishery cooperative captured more than 23,000 kg of alligator gar from the reservoir. A random sample of their catch was dominated by males, which were significantly smaller than females. Males and females had similar weight-length relationships. Relative testicular weight varied little season- ally, but relative ovarian weight showed a strong seasonal pattern that indicated peak spawning activity during July and August. Body condition of both sexes also varied in a pattern consistent with late summer spawning. Fishing for alligator gar virtually ceased from October to February, when nonreproductive individuals were presumed to move offshore to deeper water. Alligator gar fed primarily on largemouth bass, Micropterus salmoides,and less frequently on other fishes. The gillnet fishery for alligator gar in the reservoir appears to be based primarily on individuals that move into shallow, shoreline areas to spawn. Males probably remain in these habitats longer than females.
    [Show full text]
  • The Early Triassic Jurong Fish Fauna, South China Age, Anatomy, Taphonomy, and Global Correlation
    Global and Planetary Change 180 (2019) 33–50 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Research article The Early Triassic Jurong fish fauna, South China: Age, anatomy, T taphonomy, and global correlation ⁎ Xincheng Qiua, Yaling Xua, Zhong-Qiang Chena, , Michael J. Bentonb, Wen Wenc, Yuangeng Huanga, Siqi Wua a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China b School of Earth Sciences, University of Bristol, BS8 1QU, UK c Chengdu Center of China Geological Survey, Chengdu 610081, China ARTICLE INFO ABSTRACT Keywords: As the higher trophic guilds in marine food chains, top predators such as larger fishes and reptiles are important Lower Triassic indicators that a marine ecosystem has recovered following a crisis. Early Triassic marine fishes and reptiles Fish nodule therefore are key proxies in reconstructing the ecosystem recovery process after the end-Permian mass extinc- Redox condition tion. In South China, the Early Triassic Jurong fish fauna is the earliest marine vertebrate assemblage inthe Ecosystem recovery period. It is constrained as mid-late Smithian in age based on both conodont biostratigraphy and carbon Taphonomy isotopic correlations. The Jurong fishes are all preserved in calcareous nodules embedded in black shaleofthe Lower Triassic Lower Qinglong Formation, and the fauna comprises at least three genera of Paraseminotidae and Perleididae. The phosphatic fish bodies often show exceptionally preserved interior structures, including net- work structures of possible organ walls and cartilages. Microanalysis reveals the well-preserved micro-structures (i.e. collagen layers) of teleost scales and fish fins.
    [Show full text]
  • Lombardy 2012 Part A
    Pan-European Correlation of the Triassic 9th International Field Workshop September 1-5, 2012 The Middle-Late Triassic of Lombardy (I) and Canton Ticino (CH) By Flavio Jadoul and Andrea Tintori 2 This Field Trip had support from: Convenzione dei Comuni italiani del Monte San Giorgio/UNESCO Fondazione UNESCO- Monte San Giorgio Svizzera Comunità Montana della Valsassina, Valvarrone, Val d’Esino e Riviera Parco Regionale della Grigna Settentrionale 3 September 2, first day by Andrea Tintori and Markus Felber MONTE SAN GIORGIO IS UNESCO WORLD HERITAGE SITE Monte San Giorgio is among the most important fossil-bearing sites in the world, in particular concerning the middle Triassic fauna (245-230 million years ago). Following the UNESCO inscription of the Swiss side of the mountain in 2003, the Italian side has been inscribed in 2010, stating that: “Monte San Giorgio is the only and best known evidence of the marine Triassic life but also preserves some important remains of terrestrial organisms. The numerous and diverse fossil finds are exceptionally preserved and complete. The long history of the research and the controlled management of the paleontological resources have allowed thorough studies and the classification of exceptional specimens which are the basis for a rich scientific paper production. For all these reasons Monte San Giorgio represents the main reference in the world concerning the Triassic faunas.” 4 THE GEOLOGICAL HISTORY OF MONTE SAN GIORGIO Monte San Giorgio belongs to the broad tectonic feature named Sudalpino , which encompasses all the rock formations lying South of the Insubric Line. The oldest rocks of Monte San Giorgio outcrop in spots along the shores of the Ceresio Lake, between the Brusino Arsizio custom house and the built-up area of Porto Ceresio.
    [Show full text]