Aquatic Stem Group Myriapods Close a Gap Between Molecular Divergence Dates and the Terrestrial Fossil Record
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Diplopoda: Polydesmida)
Records of the Hawaii Biological Survey for 1997—Part 2: Notes 43 P-0244 HAWAI‘I: East slope of Mauna Loa, Kïpuka Ki Weather Station, 1220 m, pitfall trap, 10–12.iv.1972, J. Jacobi P-0257 HAWAI‘I: East slope of Mauna Loa, 1280–1341 m, pitfall trap, 8–10.v.1972, J. Jacobi P-0268 HAWAI‘I: East slope of Mauna Loa, 1890 m, pitfall trap, 5–7.vi.1972, J. Jacobi P-0269 HAWAI‘I: East slope of Mauna Loa, 1585 m, pitfall trap, 5–7.vi.1972, J. Jacobi P-0271 HAWAI‘I: East slope of Mauna Loa, 1280–1341 m, pitfall trap, 5–7.vi.1972, J. Jacobi P-0281 HAWAI‘I: East slope of Mauna Loa, 1981 m, pitfall trap, 10–12.vii.1972, J. Jacobi P-0284 HAWAI‘I: East slope of Mauna Loa, 1585 m, pitfall trap, 10–12.vii.1972, J. Jacobi P-0286 HAWAI‘I: East slope of Mauna Loa, Kïpuka Ki Weather Station, 1220 m, pitfall trap, 10–12.vii.1971, J. Jacobi P-0291 HAWAI‘I: East slope of Mauna Loa, Kilauea Forest Reserve, 1646 m, pitfall trap, 10–12.vii.1972 J. Jacobi P-0294 HAWAI‘I: East slope of Mauna Loa, 1981 m, pitfall trap, 14–16.viii.1972, J. Jacobi P-0300 HAWAI‘I: East slope of Mauna Loa, Kilauea Forest Reserve, 1646 m, pitfall trap, J. Jacobi P-0307 HAWAI‘I: East slope of Mauna Loa, 1981 m, pitfall trap, 17–19.ix.1972, J. Jacobi P-0313 HAWAI‘I: East slope of Mauna Loa, Kilauea Forest Reserve, 1646 m, pitfall trap, 17–19.x.1972, J. -
Lehman Caves Management Plan
National Park Service U.S. Department of the Interior Great Basin National Park Lehman Caves Management Plan June 2019 ON THE COVER Photograph of visitors on tour of Lehman Caves NPS Photo ON THIS PAGE Photograph of cave shields, Grand Palace, Lehman Caves NPS Photo Shields in the Grand Palace, Lehman Caves. Lehman Caves Management Plan Great Basin National Park Baker, Nevada June 2019 Approved by: James Woolsey, Superintendent Date Executive Summary The Lehman Caves Management Plan (LCMP) guides management for Lehman Caves, located within Great Basin National Park (GRBA). The primary goal of the Lehman Caves Management Plan is to manage the cave in a manner that will preserve and protect cave resources and processes while allowing for respectful recreation and scientific use. More specifically, the intent of this plan is to manage Lehman Caves to maintain its geological, scenic, educational, cultural, biological, hydrological, paleontological, and recreational resources in accordance with applicable laws, regulations, and current guidelines such as the Federal Cave Resource Protection Act and National Park Service Management Policies. Section 1.0 provides an introduction and background to the park and pertinent laws and regulations. Section 2.0 goes into detail of the natural and cultural history of Lehman Caves. This history includes how infrastructure was built up in the cave to allow visitors to enter and tour, as well as visitation numbers from the 1920s to present. Section 3.0 states the management direction and objectives for Lehman Caves. Section 4.0 covers how the Management Plan will meet each of the objectives in Section 3.0. -
Millipedes (Diplopoda) from Caves of Portugal
A.S.P.S. Reboleira and H. Enghoff – Millipedes (Diplopoda) from caves of Portugal. Journal of Cave and Karst Studies, v. 76, no. 1, p. 20–25. DOI: 10.4311/2013LSC0113 MILLIPEDES (DIPLOPODA) FROM CAVES OF PORTUGAL ANA SOFIA P.S. REBOLEIRA1 AND HENRIK ENGHOFF2 Abstract: Millipedes play an important role in the decomposition of organic matter in the subterranean environment. Despite the existence of several cave-adapted species of millipedes in adjacent geographic areas, their study has been largely ignored in Portugal. Over the last decade, intense fieldwork in caves of the mainland and the island of Madeira has provided new data about the distribution and diversity of millipedes. A review of millipedes from caves of Portugal is presented, listing fourteen species belonging to eight families, among which six species are considered troglobionts. The distribution of millipedes in caves of Portugal is discussed and compared with the troglobiont biodiversity in the overall Iberian Peninsula and the Macaronesian archipelagos. INTRODUCTION All specimens from mainland Portugal were collected by A.S.P.S. Reboleira, while collectors of Madeiran speci- Millipedes play an important role in the decomposition mens are identified in the text. Material is deposited in the of organic matter, and several species around the world following collections: Zoological Museum of University of have adapted to subterranean life, being found from cave Copenhagen, Department of Animal Biology, University of entrances to almost 2000 meters depth (Culver and Shear, La Laguna, Spain and in the collection of Sofia Reboleira, 2012; Golovatch and Kime, 2009; Sendra and Reboleira, Portugal. 2012). Although the millipede faunas of many European Species were classified according to their degree of countries are relatively well studied, this is not true of dependence on the subterranean environment, following Portugal. -
Number of Living Species in Australia and the World
Numbers of Living Species in Australia and the World 2nd edition Arthur D. Chapman Australian Biodiversity Information Services australia’s nature Toowoomba, Australia there is more still to be discovered… Report for the Australian Biological Resources Study Canberra, Australia September 2009 CONTENTS Foreword 1 Insecta (insects) 23 Plants 43 Viruses 59 Arachnida Magnoliophyta (flowering plants) 43 Protoctista (mainly Introduction 2 (spiders, scorpions, etc) 26 Gymnosperms (Coniferophyta, Protozoa—others included Executive Summary 6 Pycnogonida (sea spiders) 28 Cycadophyta, Gnetophyta under fungi, algae, Myriapoda and Ginkgophyta) 45 Chromista, etc) 60 Detailed discussion by Group 12 (millipedes, centipedes) 29 Ferns and Allies 46 Chordates 13 Acknowledgements 63 Crustacea (crabs, lobsters, etc) 31 Bryophyta Mammalia (mammals) 13 Onychophora (velvet worms) 32 (mosses, liverworts, hornworts) 47 References 66 Aves (birds) 14 Hexapoda (proturans, springtails) 33 Plant Algae (including green Reptilia (reptiles) 15 Mollusca (molluscs, shellfish) 34 algae, red algae, glaucophytes) 49 Amphibia (frogs, etc) 16 Annelida (segmented worms) 35 Fungi 51 Pisces (fishes including Nematoda Fungi (excluding taxa Chondrichthyes and (nematodes, roundworms) 36 treated under Chromista Osteichthyes) 17 and Protoctista) 51 Acanthocephala Agnatha (hagfish, (thorny-headed worms) 37 Lichen-forming fungi 53 lampreys, slime eels) 18 Platyhelminthes (flat worms) 38 Others 54 Cephalochordata (lancelets) 19 Cnidaria (jellyfish, Prokaryota (Bacteria Tunicata or Urochordata sea anenomes, corals) 39 [Monera] of previous report) 54 (sea squirts, doliolids, salps) 20 Porifera (sponges) 40 Cyanophyta (Cyanobacteria) 55 Invertebrates 21 Other Invertebrates 41 Chromista (including some Hemichordata (hemichordates) 21 species previously included Echinodermata (starfish, under either algae or fungi) 56 sea cucumbers, etc) 22 FOREWORD In Australia and around the world, biodiversity is under huge Harnessing core science and knowledge bases, like and growing pressure. -
Evolutionary and Historical Biogeography of Animal Diversity Learning Objectives
Evolutionary and historical biogeography of animal diversity Learning objectives • The students can explain the common ancestor of animal kingdom. • The students can explain the historical biogeography of animal. • The students can explain the invasion of animal from aquatic to terrestrial habitat. • The students can explain the basic mechanism of speciation, allopatric and non-allopatric. The Common Ancestor of Animal Kingdom Characteristics of Animals • Animals or “metazoans” are typically heterotrophic, multicellular organisms with diploid, eukaryotic cells. • Trichoplax adhaerens is defined as an animal by the presence of different somatic (i.e., non-reproductive) cell types and by impermeable cell–cell connections. Trichoplax adhaerens Blackstone, 2009 Two Hypotheses for the Branching Order of Groups at the Root of the Metazoan Tree 1 2 The choanoflagellates serve as an outgroup in the Bilaterians are the sister group to the placozoan + analysis, and sponges are the sister group to the sponge + ctenophore + cnidarian clade, while placozoans placozoan + cnidarian + ctenophore + bilaterian are the sister group to the sponge + ctenophore + clade. cnidarian clade. Blackstone, 2009 Ancestry and evolution of animal–bacterial interactions • Choanoflagellates as the last common ancestor of animal kingdom. • Urmetazoan is the group of animal with multicellular and produce differentiated cell types (ex. Egg & sperm) R.A. Alegado & N. King, 2014 Conserved morphology and ultrastructure of Choanoflagellates and Sponge choanocytes The collar complex is conserved in choanoflagellates (A. S. rosetta) and sponge collar cells (B. Sycon coactum) flagellum (fL), microvilli (mv), a nucleus (nu), and a food vacuole (fv) Brunet & King, 2017 The Historical Biogeography of Animal Zoogeographic regions Old New Cox, 2001 Plate tectonic regulation of global marine animal diversity A. -
FALL 2017 President’S Reflections
PriscumPriscum NEWSLETTER OF THE VOLUME 24, ISSUE 1 President’s Reflections Paleobiology, the finances of both journals appear secure for INSIDE THIS ISSUE: the foreseeable future, and with a much-improved online presence for both journals. To be sure, more work lies ahead, Report on Student but we are collaborating with Cambridge to expand our au- 3 Diversity and Inclusion thor and reader bases, and, more generally, to monitor the ever-evolving publishing landscape. Our partnership with The Dry Dredgers of 10 Cambridge is providing additional enhancements for our Cincinnati, Ohio members, including the digitization of the Society’s entire archive of special publications; as of this writing, all of the PS Embraces the 13 Hydrologic Cycle Society’s short course volumes are now available through the member’s portal, and all remaining Society publications will be made available soon. We are also exploring an exciting PS Events at 2017 GSA 14 new outlet through Cambridge for all future Special Publica- By Arnie Miller (University of tions. Stay tuned! Book Reviews 15 Cincinnati), President In my first year as President, the Society has continued to These are challenging times for move forward on multiple fronts, as we actively explore and Books Available for 28 scientists and for the profes- pursue new means to carry out our core missions of enhanc- Review Announcement sional societies that represent ing and broadening the reach of our science and of our Socie- them. In the national political ty, and providing expanded developmental opportunities for arena, scientific findings, policies, and funding streams that all of our members. -
An Analysis of Multiple Trackways of Protichnites Owen, 1852, from the Potsdam Sandstone (Late Cambrian), St
AN ANALYSIS OF MULTIPLE TRACKWAYS OF PROTICHNITES OWEN, 1852, FROM THE POTSDAM SANDSTONE (LATE CAMBRIAN), ST. LAWRENCE VALLEY, NY by Matthew E. Burton-Kelly A Bachelors Thesis Submitted to the Faculty of the Department of Geology of St. Lawrence University in partial fulfillment of the requirements for the degree of Bachelor of Science with Honors in Geology Canton, New York 2005 1 2 3 This thesis submitted by in partial fulfillment of the requirements for the degree of Bachelor of Science with Honors in Geology from St. Lawrence University is hereby approved by the Faculty Advisor under whom the work was done. Faculty Advisor Date Department Chairman Date ii 4 ACKNOWLEDGMENTS The author would like to thank Dr. J. Mark Erickson for his assistance and guidance throughout the course of this project, as well as the St. Lawrence University Geology Department, which provided research materials and covered transportation costs. Attendance at the annual meeting of the Northeastern Section of the Geological Society of America to present preliminary results was funded by the Jim Street Fund, St. Lawrence University Geology. Jim Dawson provided vital insight into the nature of these trackways. Any number of additional people provided support for the author, most notably Camille Partin, Trisha Smrecak, and Joanne Cavallerano, but thanks go out to all the members of the St. Lawrence University Geology Department and the St. Lawrence University Track and Field teams. iii 5 TABLE OF CONTENTS THESIS APPROVAL..........................................................................................................ii -
Biochemical Divergence Between Cavernicolous and Marine
The position of crustaceans within Arthropoda - Evidence from nine molecular loci and morphology GONZALO GIRIBET', STEFAN RICHTER2, GREGORY D. EDGECOMBE3 & WARD C. WHEELER4 Department of Organismic and Evolutionary- Biology, Museum of Comparative Zoology; Harvard University, Cambridge, Massachusetts, U.S.A. ' Friedrich-Schiller-UniversitdtJena, Instituifiir Spezielte Zoologie und Evolutionsbiologie, Jena, Germany 3Australian Museum, Sydney, NSW, Australia Division of Invertebrate Zoology, American Museum of Natural History, New York, U.S.A. ABSTRACT The monophyly of Crustacea, relationships of crustaceans to other arthropods, and internal phylogeny of Crustacea are appraised via parsimony analysis in a total evidence frame work. Data include sequences from three nuclear ribosomal genes, four nuclear coding genes, and two mitochondrial genes, together with 352 characters from external morphol ogy, internal anatomy, development, and mitochondrial gene order. Subjecting the com bined data set to 20 different parameter sets for variable gap and transversion costs, crusta ceans group with hexapods in Tetraconata across nearly all explored parameter space, and are members of a monophyletic Mandibulata across much of the parameter space. Crustacea is non-monophyletic at low indel costs, but monophyly is favored at higher indel costs, at which morphology exerts a greater influence. The most stable higher-level crusta cean groupings are Malacostraca, Branchiopoda, Branchiura + Pentastomida, and an ostracod-cirripede group. For combined data, the Thoracopoda and Maxillopoda concepts are unsupported, and Entomostraca is only retrieved under parameter sets of low congruence. Most of the current disagreement over deep divisions in Arthropoda (e.g., Mandibulata versus Paradoxopoda or Cormogonida versus Chelicerata) can be viewed as uncertainty regarding the position of the root in the arthropod cladogram rather than as fundamental topological disagreement as supported in earlier studies (e.g., Schizoramia versus Mandibulata or Atelocerata versus Tetraconata). -
Arachnida, Solifugae) with Special Focus on Functional Analyses and Phylogenetic Interpretations
HISTOLOGY AND ULTRASTRUCTURE OF SOLIFUGES Comparative studies of organ systems of solifuges (Arachnida, Solifugae) with special focus on functional analyses and phylogenetic interpretations HISTOLOGIE UND ULTRASTRUKTUR DER SOLIFUGEN Vergleichende Studien an Organsystemen der Solifugen (Arachnida, Solifugae) mit Schwerpunkt auf funktionellen Analysen und phylogenetischen Interpretationen I N A U G U R A L D I S S E R T A T I O N zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) an der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Anja Elisabeth Klann geboren am 28.November 1976 in Bremen Greifswald, den 04.06.2009 Dekan ........................................................................................................Prof. Dr. Klaus Fesser Prof. Dr. Dr. h.c. Gerd Alberti Erster Gutachter .......................................................................................... Zweiter Gutachter ........................................................................................Prof. Dr. Romano Dallai Tag der Promotion ........................................................................................15.09.2009 Content Summary ..........................................................................................1 Zusammenfassung ..........................................................................5 Acknowledgments ..........................................................................9 1. Introduction ............................................................................ -
Phylogenomic Resolution of Sea Spider Diversification Through Integration Of
bioRxiv preprint doi: https://doi.org/10.1101/2020.01.31.929612; this version posted February 2, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Phylogenomic resolution of sea spider diversification through integration of multiple data classes 1Jesús A. Ballesteros†, 1Emily V.W. Setton†, 1Carlos E. Santibáñez López†, 2Claudia P. Arango, 3Georg Brenneis, 4Saskia Brix, 5Esperanza Cano-Sánchez, 6Merai Dandouch, 6Geoffrey F. Dilly, 7Marc P. Eleaume, 1Guilherme Gainett, 8Cyril Gallut, 6Sean McAtee, 6Lauren McIntyre, 9Amy L. Moran, 6Randy Moran, 5Pablo J. López-González, 10Gerhard Scholtz, 6Clay Williamson, 11H. Arthur Woods, 12Ward C. Wheeler, 1Prashant P. Sharma* 1 Department of Integrative Biology, University of Wisconsin–Madison, Madison, WI, USA 2 Queensland Museum, Biodiversity Program, Brisbane, Australia 3 Zoologisches Institut und Museum, Cytologie und Evolutionsbiologie, Universität Greifswald, Greifswald, Germany 4 Senckenberg am Meer, German Centre for Marine Biodiversity Research (DZMB), c/o Biocenter Grindel (CeNak), Martin-Luther-King-Platz 3, Hamburg, Germany 5 Biodiversidad y Ecología Acuática, Departamento de Zoología, Facultad de Biología, Universidad de Sevilla, Sevilla, Spain 6 Department of Biology, California State University-Channel Islands, Camarillo, CA, USA 7 Départment Milieux et Peuplements Aquatiques, Muséum national d’Histoire naturelle, Paris, France 8 Institut de Systématique, Emvolution, Biodiversité (ISYEB), Sorbonne Université, CNRS, Concarneau, France 9 Department of Biology, University of Hawai’i at Mānoa, Honolulu, HI, USA Page 1 of 31 bioRxiv preprint doi: https://doi.org/10.1101/2020.01.31.929612; this version posted February 2, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. -
Continental Invertebrate and Plant Trace Fossils in Space and Time: State of the Art and Prospects
48 3RD INTERNATIONAL CONFERENCE OF CONTINENTAL ICHNOLOGY, ABSTRACT VOLUME & FIELD TRIP GUIDE Continental invertebrate and plant trace fossils in space and time: State of the art and prospects M. GABRIELA MANGANO1 *, LUIS A. BUATOIS1 1 Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon SK S7N 5E2, Canada * presenting author, [email protected] Continental invertebrate ichnology has experienced a substantial development during the last quarter of century. From being a field marginal to mainstream marine ichnology, represented by a handful of case studies, continental ichnology has grown to occupy a central position within the field of ani- mal-substrate interactions. This evolution is illustrated not only through the accumulation of ichnolog- ic information nurtured by neoichnologic observations and a detailed scrutiny of ancient continental successions, but also through the establishment of new concepts and methodologies. From an ichnofacies perspective, various recurrent associations were defined B( UATOIS & MÁNGANO 1995; GENISE et al. 2000, 2010, 2016; HUNT & LUCAS 2007; EKDALE et al. 2007; KRAPOVICKAS et al. 2016), a situation sharply contrasting with the sole recognition of the Scoyenia ichnofacies as the only valid one during the seventies and eighties (Table 1; Fig. 1). The ichnofacies model now includes not only freshwater ich- nofacies, but also terrestrial ones, most notably those reflecting the complex nature of paleosol trace fossils (GENISE 2017). Trace fossils are now being increasingly used to establish a chronology of the colonization of the land and to unravel the patterns and processes involved in the occupation of ecospace in continental set- tings (e.g. BUATOIS & MÁNGANO 1993; BUATOIS et al. -
MYRIAPODS 767 Volume 2 (M-Z), Pp
In: R. Singer, (ed.), 1999. Encyclopedia of Paleontology, MYRIAPODS 767 volume 2 (M-Z), pp. 767-775. Fitzroy Dearborn, London. MYRIAPODS JVlyriapods are many-legged, terrestrial arthropods whose bodies groups, the Trilobita, Chelicerata, Crustacea, and the Uniramia, the are divided into two major parts, a head and a trunk. The head last consisting of the Myriapoda, Hexapoda, and Onychophora (vel- bears a single pair of antennae, highly differentiated mandibles (or vet worms). However, subsequent structural and molecular evidence jaws), and at least one pair of maxillary mouthparts; the trunk indicates that there are several characters uniting major arthropod region consists of similar "metameres," each of which is a func- taxa. Moreover, paleobiologic, embryologie, and other evidence tional segment that bears one or two pairs of appendages. Gas demonstrates that myriapods and hexapods are fiindamentally exchange is accomplished by tracheae•a branching network of polyramous, having two major articulating appendages per embry- specialized tubules•although small forms respire through the ological body segment, like other arthropods. body wall. Malpighian organs are used for excretion, and eyes con- A fourth proposal (Figure ID) suggests that myriapods are sist of clusters of simple, unintegrated, light-sensitive elements an ancient, basal arthropod lineage, and that the Hexapoda that are termed ommatidia. These major features collectively char- emerged as an independent, relatively recent clade from a rather acterize the five major myriapod clades: Diplopoda (millipeds), terminal crustacean lineage, perhaps the Malacostraca, which con- Chilopoda (centipeds), Pauropoda (pauropods), Symphyla (sym- tains lobsters and crabs (Ballard et al. 1992). Because few crusta- phylans), and Arthropleurida (arthropleurids). Other features cean taxa were examined in this analysis, and due to the Cambrian indicate differences among these clades.