The Use of the MĕOri Language in Species Nomenclature
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Tylosaurine Mosasaurs (Squamata) from the Late Cretaceous of Northern Germany
Netherlands Journal of Geosciences —– Geologie en Mijnbouw | 94 – 1 | 55-71 | 2015 doi: 10.1017/njg.2014.31 Tylosaurine mosasaurs (Squamata) from the Late Cretaceous of northern Germany J.J. Hornung1,2,* &M.Reich3,4 1 Georg-August University Gottingen,¨ Geoscience Centre, Department of Geobiology, Goldschmidt-Straße 3, 37077 Gottingen,¨ Germany 2 Current address: Fuhlsbuttler¨ Str. 611, 22337 Hamburg, Germany 3 SNSB - Bavarian State Collection for Palaeontology and Geology, Richard-Wagner-Str. 10, 80333 Munich, Germany 4 Department of Earth and Environmental Sciences, Ludwig-Maximilians University Munchen,¨ Richard-Wagner-Str. 10, 80333 Munich, Germany * Corresponding author. Email: [email protected] Manuscript received: 27 April 2014, accepted: 18 September 2014 Abstract Two genera of tylosaurine mosasaurs, Tylosaurus and Hainosaurus, are recorded for the first time from Germany. Tylosaurus sp. is represented by two isolated tooth crowns, originally described as Mosasaurus? alseni (here considered a nomen dubium) from the latest Santonian–Early Campanian, which are very similar to T. ivoensis and T. gaudryi.ThematerialofHainosaurus sp. comprises a maxillary with associated postorbitofrontal, two pterygoid teeth and several indeterminate cranial fragments. The specimen from the Late Campanian is slightly less derived than H. bernardi from the Maastrichtian in retaining labiolingually less compressed anterior maxillary teeth and unserrated pterygoid teeth with only very weak carinae. Despite only minor skeletal differences, the genus Hainosaurus is considered to be distinct from Tylosaurus because of its significant modification of the dental apparatus compared to the plesiomorphic condition in the latter. This dental morphology suggests a phylogenetic trend from a generalised-piercing marginal dentition in Tylosaurus towards the increasingly labiolingually compressed, symmetrical, strongly bicarinate cutting marginal teeth in Hainosaurus spp. -
Lowest Paleogene Strata on Vega Island, Antarctica
Palaeogeography, Palaeoclimatology, Palaeoecology 402 (2014) 55–72 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Stratigraphy and vertebrate paleoecology of Upper Cretaceous–?lowest Paleogene strata on Vega Island, Antarctica Eric M. Roberts a,⁎, Matthew C. Lamanna b, Julia A. Clarke c, Jin Meng d, Eric Gorscak e, Joseph J.W. Sertich f, Patrick M. O'Connor e, Kerin M. Claeson g,RossD.E.MacPheeh a School of Earth and Environmental Sciences, James Cook University, Townsville, QLD 4811, Australia b Section of Vertebrate Paleontology, Carnegie Museum of Natural History, 4400 Forbes Ave., Pittsburgh, PA 15213, USA c Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, 1 University Station C1100, Austin, TX 78712, USA d Department of Paleontology, American Museum of Natural History, Central Park West at 79th St., New York, NY 10024, USA e Department of Biomedical Sciences, Heritage College of Osteopathic Medicine, Ohio University, Athens, OH 45701, USA f Department of Earth Sciences, Denver Museum of Nature and Science, 2001 Colorado Blvd., Denver, CO 80205, USA g Department of Biomedical Sciences, Philadelphia College of Osteopathic Medicine, Philadelphia, PA 19131, USA h Department of Mammalogy, American Museum of Natural History, Central Park West at 79th St., New York, NY 10024, USA article info abstract Article history: The Upper Cretaceous (Maastrichtian) Sandwich Bluff Member of the López de Bertodano Formation is well Received 24 October 2013 exposed on Vega Island in the James Ross Basin off the northeastern coast of the Antarctic Peninsula. Although Received in revised form 18 February 2014 this unit is one of the richest sources of end-Cretaceous vertebrate fossils in Antarctica, it is also one of the Accepted 3 March 2014 least sedimentologically and stratigraphically characterized units in the basin. -
Updated Checklist of Marine Fishes (Chordata: Craniata) from Portugal and the Proposed Extension of the Portuguese Continental Shelf
European Journal of Taxonomy 73: 1-73 ISSN 2118-9773 http://dx.doi.org/10.5852/ejt.2014.73 www.europeanjournaloftaxonomy.eu 2014 · Carneiro M. et al. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:9A5F217D-8E7B-448A-9CAB-2CCC9CC6F857 Updated checklist of marine fishes (Chordata: Craniata) from Portugal and the proposed extension of the Portuguese continental shelf Miguel CARNEIRO1,5, Rogélia MARTINS2,6, Monica LANDI*,3,7 & Filipe O. COSTA4,8 1,2 DIV-RP (Modelling and Management Fishery Resources Division), Instituto Português do Mar e da Atmosfera, Av. Brasilia 1449-006 Lisboa, Portugal. E-mail: [email protected], [email protected] 3,4 CBMA (Centre of Molecular and Environmental Biology), Department of Biology, University of Minho, Campus de Gualtar, 4710-057 Braga, Portugal. E-mail: [email protected], [email protected] * corresponding author: [email protected] 5 urn:lsid:zoobank.org:author:90A98A50-327E-4648-9DCE-75709C7A2472 6 urn:lsid:zoobank.org:author:1EB6DE00-9E91-407C-B7C4-34F31F29FD88 7 urn:lsid:zoobank.org:author:6D3AC760-77F2-4CFA-B5C7-665CB07F4CEB 8 urn:lsid:zoobank.org:author:48E53CF3-71C8-403C-BECD-10B20B3C15B4 Abstract. The study of the Portuguese marine ichthyofauna has a long historical tradition, rooted back in the 18th Century. Here we present an annotated checklist of the marine fishes from Portuguese waters, including the area encompassed by the proposed extension of the Portuguese continental shelf and the Economic Exclusive Zone (EEZ). The list is based on historical literature records and taxon occurrence data obtained from natural history collections, together with new revisions and occurrences. -
A Genus-Level Supertree of Adephaga (Coleoptera) Rolf G
ARTICLE IN PRESS Organisms, Diversity & Evolution 7 (2008) 255–269 www.elsevier.de/ode A genus-level supertree of Adephaga (Coleoptera) Rolf G. Beutela,Ã, Ignacio Riberab, Olaf R.P. Bininda-Emondsa aInstitut fu¨r Spezielle Zoologie und Evolutionsbiologie, FSU Jena, Germany bMuseo Nacional de Ciencias Naturales, Madrid, Spain Received 14 October 2005; accepted 17 May 2006 Abstract A supertree for Adephaga was reconstructed based on 43 independent source trees – including cladograms based on Hennigian and numerical cladistic analyses of morphological and molecular data – and on a backbone taxonomy. To overcome problems associated with both the size of the group and the comparative paucity of available information, our analysis was made at the genus level (requiring synonymizing taxa at different levels across the trees) and used Safe Taxonomic Reduction to remove especially poorly known species. The final supertree contained 401 genera, making it the most comprehensive phylogenetic estimate yet published for the group. Interrelationships among the families are well resolved. Gyrinidae constitute the basal sister group, Haliplidae appear as the sister taxon of Geadephaga+ Dytiscoidea, Noteridae are the sister group of the remaining Dytiscoidea, Amphizoidae and Aspidytidae are sister groups, and Hygrobiidae forms a clade with Dytiscidae. Resolution within the species-rich Dytiscidae is generally high, but some relations remain unclear. Trachypachidae are the sister group of Carabidae (including Rhysodidae), in contrast to a proposed sister-group relationship between Trachypachidae and Dytiscoidea. Carabidae are only monophyletic with the inclusion of a non-monophyletic Rhysodidae, but resolution within this megadiverse group is generally low. Non-monophyly of Rhysodidae is extremely unlikely from a morphological point of view, and this group remains the greatest enigma in adephagan systematics. -
Fordyce, RE 2006. New Light on New Zealand Mesozoic Reptiles
Fordyce, R. E. 2006. New light on New Zealand Mesozoic reptiles. Geological Society of New Zealand newsletter 140: 6-15. The text below differs from original print format, but has the same content. P 6 New light on New Zealand Mesozoic reptiles R. Ewan Fordyce, Associate Professor, Otago University ([email protected]) Jeff Stilwell and coauthors recently (early 2006) published the first report of dinosaur bones from Chatham Island. The fossils include convincing material, and the occurrence promises more finds. Questions remain, however, about the stratigraphic setting. This commentary summarises the recent finds, considers earlier reports of New Zealand Mesozoic vertebrates, and reviews some broader issues of Mesozoic reptile paleobiology relevant to New Zealand. The Chatham Island finds A diverse team reports on the Chathams finds. Jeff Stilwell (fig. 1 here) is an invertebrate paleontologist with research interests on Gondwana breakup and Southern Hemisphere Cretaceous-early Cenozoic molluscs (e.g. Stilwell & Zinsmeister 1992), including Chatham Islands (1997). Several authors are vertebrate paleontologists – Chris Consoli, Tom Rich, Pat Vickers-Rich, Steven Salisbury, and Phil Currie – with diverse experience of dinosaurs. Rupert Sutherland and Graeme Wilson (GNS) are well-known for their research on tectonics and biostratigraphy. The Chathams article describes a range of isolated bones attributed to theropod (“beast-footed,” carnivorous) dinosaurs, including a centrum (main part or body of a vertebra), a pedal phalanx (toe bone), the proximal head of a tibia (lower leg bone, at the knee joint), a manual phalanx (finger bone) and a manual ungual (terminal “claw” of a finger). On names of groups, fig. -
Issue Information
Systematic Entomology (2017), 42, 240–266 DOI: 10.1111/syen.12209 Molecular phylogeny of Sericostomatoidea (Trichoptera) with the establishment of three new families KJELL ARNE JOHANSON1, TOBIAS MALM1 andMARIANNE ESPELAND2 1Department of Zoology, Swedish Museum of Natural History, Stockholm, Sweden and 2Arthropoda Department, Zoological Research Museum Alexander Koenig, Bonn, Germany Abstract. We inferred the phylogenetic relationships among 58 genera of Sericostom- atoidea, representing all previously accepted families as well as genera that were not placed in established families. The analyses were based on five fragments of the protein coding genes carbamoylphosphate synthetase (CPSase of CAD), isocitrate dehydroge- nase (IDH), Elongation factor 1a (EF-1a), RNA polymerase II (POL II) and cytochrome oxidase I (COI). The data set was analysed using Bayesian methods with a mixed model, raxml, and parsimony. The various methods generated slightly different results regarding relationships among families, but the shared results comprise support for: (i) a monophyletic Sericostomatoidea; (ii) a paraphyletic Parasericostoma due to inclusion of Myotrichia murina, leading to synonymization of Myotrichia with Parasericostoma; (iii) a polyphyletic Sericostomatidae, which is divided into two families, Sericostom- atidae sensu stricto and Parasericostomatidae fam.n.; (iv) a polyphyletic Helicophidae which is divided into Helicophidae sensu stricto and Heloccabucidae fam.n.; (v) hypoth- esized phylogenetic placement of the former incerta sedis genera Ngoya, Seselpsyche and Karomana; (vi) a paraphyletic Costora (Conoesucidae) that should be divided into several genera after more careful examination of morphological data; (vii) reinstatement of Gyrocarisa as a valid genus within Petrothrincidae. A third family, Ceylanopsychi- dae fam.n., is established based on morphological characters alone. A hypothesis of the relationship among 14 of the 15 families in the superfamily is presented. -
Revision of the Genusaxonya ANDREWES, 1923
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Zeitschrift der Arbeitsgemeinschaft Österreichischer Entomologen Jahr/Year: 1999 Band/Volume: 51 Autor(en)/Author(s): Dostal Alexander, Zettel Herbert Artikel/Article: Revision of the genus Axonya Andrewes, 1923 (Coleoptera: Carabidae). 109-118 ©Arbeitsgemeinschaft Österreichischer Entomologen, Wien, download unter www.biologiezentrum.at Z.Arb.Gem.Öst.Ent. 51 109-118 Wien, 15. 12. 1999 ISSN 0375-5223 Revision of the genus Axonya ANDREWES, 1923 (Coleoptera: Carabidae) Alexander DOSTAL and Herbert ZETTEL Abstract The genus Axonya ANDREWES, 1923 is revised. Two species are newly described: Axonya farsica nov. spec, from Iran and Axonya similis nov. spec, from Nepal and Northeast India. Axonya championi ANDREWES, 1923 is redescribed and revised, and a lectotype is designated. A key to the species is provided. Zusammenfassung Es wird die Gattung Axonya ANDREWES, 1923 revidiert. Zwei Arten werden neu beschrie- ben: Axonya farsica nov. spec, aus dem Iran und Axonya similis nov. spec, von Nepal und Nordost-Indien. Axonya championi ANDREWES, 1923 wird neu definiert und beschrieben sowie ein Lectotypus festgelegt. Die Arten werden in einer Bestimmungstabelle aufge- schlüsselt. Key words: Coleoptera, Carabidae, Broscinae, Axonya, new species, key, lectotype designation, India, Iran, Nepal. Introduction The Genus Axonya ANDREWES, 1923 belongs to the subfamily Broscinae. Its description is based on a single reference species, A. championi ANDREWES, 1923, with a few records from North India. No further species has been included so far, and no publications on Axonya are available since ANDREWES (1935). The surprising finding of a new species of Axonya in southern Iran encouraged the authors to carry out a more detailed taxonomic study on this poorly known genus. -
Coleoptera: Carabidae) Peter W
30 THE GREAT LAKES ENTOMOLOGIST Vol. 42, Nos. 1 & 2 An Annotated Checklist of Wisconsin Ground Beetles (Coleoptera: Carabidae) Peter W. Messer1 Abstract A survey of Carabidae in the state of Wisconsin, U.S.A. yielded 87 species new to the state and incorporated 34 species previously reported from the state but that were not included in an earlier catalogue, bringing the total number of species to 489 in an annotated checklist. Collection data are provided in full for the 87 species new to Wisconsin but are limited to county occurrences for 187 rare species previously known in the state. Recent changes in nomenclature pertinent to the Wisconsin fauna are cited. ____________________ The Carabidae, commonly known as ‘ground beetles’, with 34, 275 described species worldwide is one of the three most species-rich families of extant beetles (Lorenz 2005). Ground beetles are often chosen for study because they are abun- dant in most terrestrial habitats, diverse, taxonomically well known, serve as sensitive bioindicators of habitat change, easy to capture, and morphologically pleasing to the collector. North America north of Mexico accounts for 2635 species which were listed with their geographic distributions (states and provinces) in the catalogue by Bousquet and Larochelle (1993). In Table 4 of the latter refer- ence, the state of Wisconsin was associated with 374 ground beetle species. That is more than the surrounding states of Iowa (327) and Minnesota (323), but less than states of Illinois (452) and Michigan (466). The total count for Minnesota was subsequently increased to 433 species (Gandhi et al. 2005). Wisconsin county distributions are known for 15 species of tiger beetles (subfamily Cicindelinae) (Brust 2003) with collection records documented for Tetracha virginica (Grimek 2009). -
I Exploring the Relationship Between Paleobiogeography, Deep-Diving
Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs By Andrew M. Connolly Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Arts. __________________________________ Stephen T. Hasiotis, Chairperson __________________________________ Rafe M. Brown __________________________________ Jennifer A. Roberts Date Defended: March 25, 2016 i The Thesis Committee for Andrew M. Connolly certifies that this is the approved version of the following thesis: Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs __________________________________ Stephen T. Hasiotis, Chairperson Date Approved: March 25, 2016 ii ABSTRACT Andrew M. Connolly, M.S. Department of Geology, March 2015 University of Kansas The parietal eye (PE) in modern squamates (Reptilia) plays a major role in regulating body temperature, maintaining circadian rhythms, and orientation via the solar axis. This study is the first to determine the role, if any, of the PE in an extinct group of lizards. We analyzed variation in relative size of the parietal foramen (PF) of five mosasaur genera to explore the relationship between PF size and paleolatitudinal distribution. We also surveyed the same specimens for the presence of avascular necrosis—a result of deep- diving behavior—in the vertebrae. Plioplatecarpus had the largest PF followed by Platecarpus, Tylosaurus, Mosasaurus, and Clidastes. A weak relationship exists between paleolatitudinal distribution and PF size among genera, as Plioplatecarpus had the highest paleolatitudinal distribution (~78°N) and the largest PF among genera. -
Page Numbers in Bold Refer to Tables. a Batus 158 Actinoceramus
Index Page numbers in italics refer to Figures; page numbers in bold refer to Tables. A batus 158 Arrhoges spp. Actinoceramus concentricus 11 A. arcuacheilos 158 Actinoperygii 91-92 A. diversicostata 158 Alepisauriformes 94, 97 Ascodinium sp. 11 Elopomorpha 92, 96 A. serratum 11 Ichthyodectiformes 86, 92-94, 96-97 Asterosoma 24 Teleostei 94 Astrapotheria 179 Aeneator tawsi 158 Atherospermataceae 52 Agathoxylon 66 Atherospermoxylon bulboradiatum 70 Albuliformes 86 Atlantic Gateway 58 Alepisauriformes 94, 97 Aucellina 11 Alexander Island 64 Albian flora 68 Baculites 15 stratigraphy 65 belemnites 11 ammonites 11,14, 23 bennettitaleans 68, 69 angiosperms see leaf fossils also wood fossils Bibby Point Member 11,12,15 Anisodonta subovata 158 birds of the A. nordenskjoeldi biozone 159 Antarctiberyx seymouri 86, 94 bivalves 11,13,14, 23, 30 Antarctic Peninsula of the A. nordenskjoeldi biozone 158 floristic record 65--66 body size, climatic significance of 183-185 Cretaceous 66-74 bony fish see Osteichthyes Neogene 74-76 Botany Bay Group, fossil wood 66 Palaeogene 74 Botula pirriei 158 formation of 1 Bouchardia 158 geological setting 64-65 brachiopods 11,14, 23 Antarctodolopsdailyi see Polydolops dailyi Brandy Bay Member 9,10,12,11-14,16,17 Antarctohoges Brassospora 72 A. arcuacheilos 158 bread-crust bombs 25, 43 A. diversicostata 158 bryophytes 69, 75 Antarctoxylon spp. 70, 71 bryozoans 11, 14, 24 A. heterosporosum 70 BuUa glacialis 158 A. junglandoides 70 A. livingstonensis 70 Callorhinchus sp. 113,114,115, 120 A. multiseriatum 70 Canninginopsis denticulata 15 A. uniperforatum 70 Cape Melville Formation 188 Anthropornis spp. 151,152 Carcharias sp. 88, 89 A. -
Stewart Island/Rakiura Conservation Management Strategy and Rakiura National Park Management Plan © Copyright March 2012, New Zealand Department of Conservation
Stewart Island/Rakiura Conservation Management Strategy and Rakiura National Park Management Plan © Copyright March 2012, New Zealand Department of Conservation ISBN: 978-0-478-14936-4 (Hardcopy) ISBN: 978-0-478-14937-1 (Web PDF) Published by: Southland Conservancy Department of Conservation Te Papa Atawhai March 2012 Stewart Island/Rakiura Conservation Management Strategy and Rakiura National Park Management Plan 2011-2021 Prepared by: Southland Conservancy Department of Conservation PO Box 743, Invercargill New Zealand MARCH 2012 The Beginning Te muranga o Rakiura ka tau iho i runga i Te Punga o Te Waka a Māui. He whare wānanga, He whare tiaki taonga nō Tāne mō Papatūānuku me Tangaroa. Otirā, mō te ira tāngatā ngā hekenga o Ngāi Tahu, Ngāti Māmoe, me Waitaha. Ka whakamaua kia tina, tina! Haumi e, Hui e, Taiki e. The aura that are the glowing skies that envelop the anchor of the waka of Māui. A house of learning, a house full of the treasures from Tane for Papatuanuku and Tangaroa, indeed, and also for we the descendents of generations of Ngāi Tahu, Ngati Mamoe and Waitaha Binding this tightly, tightly. Together, tightly, all is bound. CONTENTS Structure of this conservation planning resource 3 Section One – Stewart Island/Rakiura Conservation Management Strategy 5 Foreword 7 Structure of the Stewart Island/Rakiura Conservation Management Strategy 11 Introduction 12 Part One: Management objectives and policies 14 Part Two: Places 83 Part Three: Implementation, monitoring, reporting, review and milestones 113 Part Four: Land inventory -
A Key to the Genera of the Ground-Beetle Larvae (Coleoptera, Carabidae) of the Paleartic Region
ISSN 0392-758 X MUSEO REGIONALE DI SCIENZE NATURALI A key to the genera of the Ground-beetle larvae (Coleoptera, Carabidae) of the Paleartic region Kirill V. Makarow ESTRATTO dal Bollettino del Museo Regionale di Scienze Naturali - Torino Volume 12 - N. 1 - 1994 Boll. Mus. reg. Sci. nat. Torino Vol. 12 - N. 1 pp. 221-254 4-5-1994 K.irill V. MAKAR.ow* A key to the genera of the Ground-beetle larvae (Coleoptera, Carabidae) of the Palearctic region INTRODUCTION It is necessary to use the data about the preimaginal stages, especially lar vae, forthe successful decision of many taxonomic and ecological questions, but it's rather difficult, because of the little knowledge on the larvae biology and morphology as well as the absence of modern identification keys. So, van Emden's monograph (1942) appears hitherto the most complete generalizing work. The available keys for the USSR (Sharova, 1958, 1964) and Middle Europe carabid larvae (Hurka, 1978; Arndt, 1991) do not contain a number of larval descriptions, published from 1942-1991. Besides, the finemorphologi cal investigations ofY. Bousquet and H. Goulet (Goulet, 1979; Bousquet and Goulet, 1984) produced on new opportunities forlarval descriptions. Unfor tunately, this method is currently poorly used (Arndt, 1989a, b; Arndt and Hurka, 1990; Bousquet, 1985a, b; 1986; Hurka, 1986; Makarow and Shilenkov, 1991 etc.) and can not be considered as a basis of the practical keys. The present work contains a key for determination of the main Palearctic carabid groups and takes into account most of the works that followed van Emden's monograph.