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Junior Cave Scientist Cave and Karst Program Activity Book Ages 5 – 12+
National Park Service U.S. Department of the Interior Geologic Resources Division Junior Cave Scientist Cave and Karst Program Activity Book Ages 5 – 12+ Name: Age: Explore • Learn • Protect 1 Become a Junior Cave Scientist Caves and karst landscapes are found throughout the United States. These features are important as part of our Nation's geologic heritage. In this book, you will explore a fascinating and fragile underground world, learn about the values of caves and karst landscapes, and complete fun educational activities. Explore magnificent and beautiful caves. You will find an amazing underground world just beneath your feet! Learn about caves and karst systems and the work that cave scientists do. Protect our natural environments and the things that make caves and karst areas special. To earn your badge, complete at least activities. (Your Age) Activities in this book are marked with an age indicator. Look for the symbols below: Flashlight Lantern Helmet and Headlamp Ages 5 - 7 Ages 8 – 11 Ages 12 and Older Put a check next to your age indicator on each page that you complete. I received this book from: After completing the activities, there are two ways to receive your Junior Cave Scientist badge: • Return the completed book to a ranger at a participating park, or 2 • Visit go.nps.gov/jrcavesci What are Speleo-Fact: Mammoth Cave is the longest cave in world with over 405 miles (652 km) of connected passageways. Caves and Karst? Caves are naturally occurring voids, cavities, interconnected passageways, or alcoves in the earth. Caves preserve fossils, minerals, ecosystems, and records of past climates. -
Hobbs, H.H., and D.C. Culver. 2009
of the L"SA _~arional ~Ylogical Society, Inc. -~- J the ~ational Speleological Society, Inc. 13 Cave Avenue Ennrsville.Alabama 35810-4431, U.S.A. 256-852-1300 E-mail: [email protected] Web page: http://www.caves.org All rights reserved, including the right to reproduce this book or portions thereof in any fonn or by any means, mechanical or electronic, including photocopying, recording, or by any information storage or retrieval system without permission in writing from the publisher. All inquiries should be addressed to the National Speleological Society. Editors: Arthur N. Palmer and Margaret V. Palmer Graphics: M.Y. Palmer andA.N. Palmer Formatting and photograph preparation: A.N. Palmer Library of Congress Control Number: 2007943932 ISBN: 9781879961289 Printed in the U.S.A. ged; and they, their contents, and their biota deserve our protection. Try to leave no trace of your _-hDDiJ:tmcm~ are on private property, and land-owner relations can be delicate. For these reasons, specific ~ ~ ~ IJM inrhuinf in publications of the National Speleological Society. Caves can also pose a danger to those 'T who lack experience. Access to caves, and assistance in meeting the requirements for safe .~ lUI!~aticjeJ i1:r rarwrrring local chapters of the NSS. 15 Cave Biology An Overview of Cave Biology in the USA The transition zone of caves is a dynamic region of constant darkn (aphotic), but where the microclimate is noticeably still affected Horton H. Hobbs III and David C. Culver surface events. Fluctuations in temperature and humidity, decreasi diversity of species, and lower biomass reflect the influences of bo AVES have traditionally been considered exotic and rare habitats, epigean and hypogean environments. -
Consequences of Evolutionary Transitions in Changing Photic Environments
bs_bs_banner Austral Entomology (2017) 56,23–46 Review Consequences of evolutionary transitions in changing photic environments Simon M Tierney,1* Markus Friedrich,2,3 William F Humphreys,1,4,5 Therésa M Jones,6 Eric J Warrant7 and William T Wcislo8 1School of Biological Sciences, The University of Adelaide, North Terrace, Adelaide, SA 5005, Australia. 2Department of Biological Sciences, Wayne State University, 5047 Gullen Mall, Detroit, MI 48202, USA. 3Department of Anatomy and Cell Biology, Wayne State University, School of Medicine, 540 East Canfield Avenue, Detroit, MI 48201, USA. 4Terrestrial Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, WA 6986, Australia. 5School of Animal Biology, University of Western Australia, Nedlands, WA 6907, Australia. 6Department of Zoology, The University of Melbourne, Melbourne, Vic. 3010, Australia. 7Department of Biology, Lund University, Sölvegatan 35, S-22362 Lund, Sweden. 8Smithsonian Tropical Research Institute, PO Box 0843-03092, Balboa, Ancón, Republic of Panamá. Abstract Light represents one of the most reliable environmental cues in the biological world. In this review we focus on the evolutionary consequences to changes in organismal photic environments, with a specific focus on the class Insecta. Particular emphasis is placed on transitional forms that can be used to track the evolution from (1) diurnal to nocturnal (dim-light) or (2) surface to subterranean (aphotic) environments, as well as (3) the ecological encroachment of anthropomorphic light on nocturnal habitats (artificial light at night). We explore the influence of the light environment in an integrated manner, highlighting the connections between phenotypic adaptations (behaviour, morphology, neurology and endocrinology), molecular genetics and their combined influence on organismal fitness. -
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. -
Hotspots of Subterranean Biodiversity in Caves and Wells
David C. Culver and Boris Sket - Hotspots of Subterranean Biodiversity in Caves and Wells. Journal of Cave and Karst Studies 62(1):11-17. HOTSPOTS OF SUBTERRANEAN BIODIVERSITY IN CAVES AND WELLS DAVID C. CULVER Department of Biology, American University, 4400 Massachusetts Ave., NW, Washington, DC 20016, USA, [email protected] BORIS SKET Department of Biology, Biotechnical Faculty, University of Ljubljana, P.O. Box 2995, 1001 Ljubljana, SLOVENIA, [email protected] We documented 18 caves and two karst wells that have 20 or more stygobites and troglobites. Crustacea dominated the aquatic fauna. Taxonomic composition of the terrestrial fauna varied, but Arachnida and Insecta together usually dominated. Geographically, the sites were concentrated in the Dinaric Karst (6 caves). Sites tended to have high primary productivity or rich organic input from the surface, be large caves, or have permanent groundwater (phreatic water). Dokumentirala sva 18 jam in dva kraška vodnjaka, iz katerih je znanih 20 ali vec vrst troglobiontov in stigobiontov. V vodni favni preladujejo raki. Taksonomski sestav kopenske favne je raznolik, vendar pajkovci in zuzelke skupaj navadno prevladujejo. Najvec takšnih jam (šest) je v Dinarskem krasu. Nadpovprecno so zastopane jame z lastno primarno produkcijo ali bogatim vnosom hrane s površja, obsezne jame in jame, ki vkljucujejo tudi freatsko plast. Over the past few years, there has been a growing aware- terns at individual sites. Even though most subterranean bio- ness and concern with biodiversity worldwide. Books and diversity results from the accumulation of different species monographs with a focus on biodiversity have appeared (e.g., from nearby sites, there are some outstanding examples of high Wilson 1992; Master et al. -
Stygofauna Survey – Exmouth Cape Aquifer: Scoping Document Describing Work Required to Determine Ecological Water Requirements for the Exmouth Cape Aquifer
Stygofauna Survey – Exmouth Cape Aquifer: Scoping Document Describing Work Required to Determine Ecological Water Requirements for the Exmouth Cape Aquifer Prepared for Department of Water by Bennelongia Pty Ltd April 2008 Report 2008/09 Bennelongia Pty Ltd Exmouth Cape Aquifer Stygofauna EWRs Stygofauna Survey – Exmouth Cape Aquifer: Scoping Document Describing Work Required to Determine Ecological Water Requirements for the Exmouth Cape Aquifer Bennelongia Pty Ltd 64 Jersey Street Jolimont WA 6913 www.bennelongia.com.au ACN 124 110 167 April 2008 Report 2008/09 i Bennelongia Pty Ltd Exmouth Cape Aquifer Stygofauna EWRs LIMITATION: This review has been prepared for use by the Department of Water and its agents. Bennelongia accepts no liability or responsibility in respect of any use or reliance on the review by any third party. Bennelongia has not attempted to verify the accuracy and completeness of all information supplied by the Department of Water. COPYRIGHT: The document has been prepared to the requirements of the Department of Water. Copyright and any other Intellectual Property associated with the document belong to Bennelongia and may not be reproduced without written permission of the Department of Water or Bennelongia. Client – Department of Water Report Version Prepared by Checked by Submitted to Client Method Date Draft report Vers. 1 Stuart Halse email 8.iv.08 Vers. 2 Stuart Halse email 10.iv.08 Vers. 3 Stuart Halse email 26.v.08 Final report Stuart Halse email 2.vii.08 K:/Projects/DoW_01/Report/BEC_Exmouth_EWRs_29vii08 ii Bennelongia Pty Ltd Exmouth Cape Aquifer Stygofauna EWRs Executive Summary Water resources on the Exmouth peninsula are very limited and future expansion of the Exmouth townsite will place considerable pressure on potable water supplies. -
Stygofauna of Karstic Ecosystem in Ponor Mountains, Western Bulgaria: Present Knowledge and Research Challenges
ACTA ZOOLOGICA BULGARICA Acta zool. bulg., 61 (2), 2009: 161-168 Stygofauna of Karstic Ecosystem in Ponor Mountains, Western Bulgaria: Present Knowledge and Research Challenges Vesela V. Evtimova1*, Ivan S. Pandourski1, Aleksey D. Benderev2 1 Institute of Zoology, Bulgarian Academy of Sciences, 1, Tsar Osvoboditel Blvd., 1000 Sofi a, Bulgaria; E-mails: [email protected]; [email protected]; 2 Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev str., bl. 24, 1113 Sofi a, Bulgaria; E-mail: [email protected] Abstract: The purpose of this research is to examine the relationships between the karstic complexes and the hydro- geological characteristics of karst on one hand, and the distribution of stygobiont species, on the other. The research was conducted in the karstic region of Ponor Mountains, part of Stara Planina range, Western Bulgaria, with an area of approximately 60 km2 and average elevation of about 1000 m a.s.l. The karstic springs in the foot of the mountains are the only water source for nearly 15 000 people. Two basic rock complexes can be distinguished regarding karstifi cation: Triassic karstic complex and Upper Jurassic complex. The principal collector of the groundwater is the Triassic complex with annual discharge of 2900 dm3/s from which 80% is leaving the system through the Iskretski izvori springs. The Jurassic complex is lacking superfi cial outfl ow which determines its precipitation alimentation. The stygofauna of Ponor Mountains is very heterogeneously distributed and its composition varies greatly from one station to another. Nevertheless, the similarity calculated on the basis of presence/absence of stygobiont species is high (above 0.7) for the locations from Quaternary and Jurassic complexes. -
Troglofauna Survey at Koolyanobbing
Troglofauna survey at Koolyanobbing Prepared for Portman Ltd by Bennelongia Pty Ltd November 2008 Report 2008/49 Troglofauna survey at Koolyanobbing Bennelongia Pty Ltd 64 Jersey Street Jolimont WA 6913 www.bennelongia.com.au ACN 124 110 167 November 2008 Report 2008/49 Bennelongia Pty Ltd Koolyanobbing troglofauna LIMITATION: This review has been prepared for use by Portman Ltd and its agents. Bennelongia accepts no liability or responsibility in respect of any use or reliance on the review by any third party. Bennelongia has not attempted to verify the accuracy and completeness of all information supplied by Portman. COPYRIGHT: The document has been prepared to the requirements of Portman. Copyright and any other Intellectual Property associated with the document belong to Bennelongia and may not be reproduced without written permission of Portman or Bennelongia. Client – Portman Ltd Report Version Prepared by Checked by Submitted to Client Method Date Draft report Vers. 1 Andrew Trotter Stuart Halse email 25.xi.08 Final report Andrew Trotter Stuart Halse email 12.xii.08 K:\Projects\B_PORT_01\Report\Koolyanobbing\BEC_Koolyanobbing_final_12.xii.08.docx ii Bennelongia Pty Ltd Koolyanobbing troglofauna Executive Summary This report provides the results of a troglofauna survey at Portman Ltd’s proposed mine sites in B and C Deposit (proposed B and C Pits) at Koolyanobbing, which is located approximately 50 km north of Southern Cross in the Yilgarn region of Western Australia. Portman is seeking environmental approval to mine B and C Deposits. The purpose of this survey was to document the troglofaunal community at the proposed mine sites and assess the potential impacts of the proposed mines on troglofauna. -
Troglobitic Specimens Recorded
655000 660000 665000 670000 675000 680000 685000 690000 695000 7450000 7445000 Deposit H Deposit I A3b (!*# (! Deposit B (! !((! Deposit G (! ^ 7440000 *# (! A2d Deposit C Legend (! (! Study Area Deposit D (! Deposit Deposit A Deposit F 7435000 Troglibitic specimens Mt Ella (! Anillini ‘sp. indet’. Deposit E (! Atelurinae ‘sp. indet.’ (! Cormocephalus 'CHI003'. A4 - -Pp (! Embioptera ‘sp. indet.’ 7430000 (! Hydrobiomorpha 'sp. indet.’ A4 - -Pp *# Meenoplidae ‘sp. indet.’ (! Nocticola ‘sp. indet.’ K A2d ^ Prethopalpus 'sp indet.' 0 2.5 5 !( Pseudodiploexochus ‘sp. nov.’ 7425000 Kilometres (! Trogiidae ‘sp. indet.’ Absolute Scale - 1:110,000 Figure: 4.3 Drawn: BG Project ID: 1459 Date: 12/2/2013 Troglobitic specimens recorded Coordinate System Unique Map ID: BG282 Name: GDA 1994 MGA Zone 50 Projection: Transverse Mercator Datum: GDA 1994 A3 Rio Tinto Greater West Angelas Subterranean Fauna Assessment This page has been left blank intentionally May 2013 34 Rio Tinto Greater West Angelas Subterranean Fauna Assessment 4.3 SUMMARY OF TROGLOFAUNA GROUPS RECORDED 4.3.1 Thysanura FAMILY NICOLETIIDAE Atelurinae ‘sp. Indet.’ A single specimen was collected from Deposit D in bore WAD 358. Pilbara thysanurans are poorly known and the taxonomy of Nicoletiidae is based on their DNA sequences rather than published species descriptions. Subterranean Atelurinae are well known throughout the Pilbara; however, nearly all of the species recognised to date appear to be range restricted. This specimen appears to be characteristic of the Pilbara nicoletiids. This species is a likely SRE. 4.3.2 Psocoptera FAMILY TROGIIDAE Trogiidae ‘sp. indet.’ A single specimen was collected from Deposit D in bore DDRC 006. Only identification to family level was possible. -
World Catalogue of Dytiscidae – Corrections and Additions, 3 (Coleoptera: Dytiscidae)
©Wiener Coleopterologenverein (WCV), download unter www.biologiezentrum.at Koleopterologische Rundschau 76 55–74 Wien, Juli 2006 World Catalogue of Dytiscidae – corrections and additions, 3 (Coleoptera: Dytiscidae) A.N. NILSSON &H.FERY Abstract A third set of corrections and additions is given to the World Catalogue of Dytiscidae (NILSSON 2001) including the first and second sets of corrections and additions (NILSSON 2003 & 2004). Megadytes lherminieri (GUÉRIN-MÉNEVILLE, 1829) has priority over M. giganteus (LAPORTE, 1835). The species name Dytiscus silphoides PONZA, 1805 is declared as a nomen oblitum, in order to ensure the continuous usage of its junior synonym Deronectes opatrinus (GERMAR, 1824) as a valid name (nomen protectum). The preoccupied name Hydroporus ruficeps AUBÉ, 1838 is replaced with Hydroporus pseudoniger nom.n. New taxa published before January 1, 2006 are added. The number of recent species of the family Dytiscidae is now 3959. Key words: Coleoptera, Dytiscidae, world, replacement name, catalogue, corrections, additions. Introduction The World catalogue of Dytiscidae (NILSSON 2001) was recently updated in two sets of corrections and additions (NILSSON 2003, 2004, here referred to as CA1 and CA2), covering works published up to January 1, 2004. This third update includes new taxa and other taxonomic acts published before January 1, 2006. The age of some fossil species have been reconsidered according to EVENHUIS (1994). The transfer of species from Copelatus to genus Papuadytes suggested by BALKE et al. (2004a) follows instructions given by BALKE (in litt.). The number of recent species of Dytiscidae is now 3959. Corrections Page 34: Ilybius wasastjernae: change original binomen to Dyticus wasastjernae. -
Mt Gibson Ranges - Iron Hill Deposits: Troglofauna Assessment
Mt Gibson Ranges - Iron Hill Deposits: Troglofauna Assessment Prepared for: Mount Gibson Mining February 2016 Final Report Iron Hill Deposit Troglofauna Mount Gibson Mining Mt Gibson Ranges - Iron Hill Deposits: Troglofauna Assessment Bennelongia Pty Ltd 5 Bishop Street Jolimont WA 6913 P: (08) 9285 8722 F: (08) 9285 8811 E: [email protected] ACN: 124 110 167 Report Number: 244 Report Version Prepared by Reviewed by Submitted to Client Method Date Draft Andrew Trotter Stuart Halse email 10 August 2015 Stuart Halse Andrew Trotter Draft email 11 February 2016 Danilo Harms Danilo Harms Final Renee Young Stuart Halse email 26 February 2016 K:\Projects\B_MGIB_02\Survey Report_BEC_Iron Hill Deposit Troglofauna Survey Assessment_final16ii16 This document has been prepared to the requirements of the Client and is for the use by the Client, its agents, and Bennelongia Environmental Consultants. Copyright and any other Intellectual Property associated with the document belong to Bennelongia Environmental Consultants and may not be reproduced without written permission of the Client or Bennelongia. No liability or responsibility is accepted in respect of any use by a third party or for purposes other than for which the document was commissioned. Bennelongia has not attempted to verify the accuracy and completeness of information supplied by the Client. © Copyright 2014 Bennelongia Pty Ltd. vi Iron Hill Deposit Troglofauna Mount Gibson Mining EXECUTIVE SUMMARY Mt Gibson Mining Limited is proposing the development of the Iron Hill Deposits as a southerly extension to the existing Mt Gibson Ranges mine operations, located 77 km north-east of Wubin in the Murchison Province of the Yilgarn Craton. -
Journal of Cave and Karst Studies
June 2020 Volume 82, Number 2 JOURNAL OF ISSN 1090-6924 A Publication of the National CAVE AND KARST Speleological Society STUDIES DEDICATED TO THE ADVANCEMENT OF SCIENCE, EDUCATION, EXPLORATION, AND CONSERVATION Published By BOARD OF EDITORS The National Speleological Society Anthropology George Crothers http://caves.org/pub/journal University of Kentucky Lexington, KY Office [email protected] 6001 Pulaski Pike NW Huntsville, AL 35810 USA Conservation-Life Sciences Julian J. Lewis & Salisa L. Lewis Tel:256-852-1300 Lewis & Associates, LLC. [email protected] Borden, IN [email protected] Editor-in-Chief Earth Sciences Benjamin Schwartz Malcolm S. Field Texas State University National Center of Environmental San Marcos, TX Assessment (8623P) [email protected] Office of Research and Development U.S. Environmental Protection Agency Leslie A. North 1200 Pennsylvania Avenue NW Western Kentucky University Bowling Green, KY Washington, DC 20460-0001 [email protected] 703-347-8601 Voice 703-347-8692 Fax [email protected] Mario Parise University Aldo Moro Production Editor Bari, Italy [email protected] Scott A. Engel Knoxville, TN Carol Wicks 225-281-3914 Louisiana State University [email protected] Baton Rouge, LA [email protected] Exploration Paul Burger National Park Service Eagle River, Alaska [email protected] Microbiology Kathleen H. Lavoie State University of New York Plattsburgh, NY [email protected] Paleontology Greg McDonald National Park Service Fort Collins, CO The Journal of Cave and Karst Studies , ISSN 1090-6924, CPM [email protected] Number #40065056, is a multi-disciplinary, refereed journal pub- lished four times a year by the National Speleological Society.