Shining a Light on Fish at Night: an Overview of Fish and Fisheries in the Dark of Night, and in Deep and Polar Seas Neil Hammerschlag University of Miami
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5. Bibliography
click for previous page 101 5. BIBLIOGRAPHY Akazaki, M., 1958. Studies on the orbital bones of sparoid fishes. Zool.Mag., Tokyo, 67:322-25 -------------,1959. Comparative morphology of pentapodid fishes. Zool.Mag., Tokyo, 68(10):373-77 -------------,1961. Results of the Amami Islands expedition no. 4 on a new sparoid fish, Gymnocranius japonicus with special reference to its taxonomic status. Copeia, 1961 (4):437-41 -------------,1962. Studies on the spariform fishes. Anatomy, phylogeny, ecology and taxonomy. Misaki Mar.Biol.Inst.,Kyoto Univ., Spec. Rep. , No. 1, 368 p. Aldonov, KV.& A.D. Druzhinin, 1979. Some data on scavenger (family Lethrinidae) from the Gulf of Aden region. Voprosy Ikhthiologii, 18(4):527-35 Allen, G.R. & R.C. Steene, 1979. The fishes of Christmas Island, Indian Ocean. Aust.nat.Parks Wildl.Serv.Spec.Publ., 2:1-81 -------------, 1987. Reef fishes of the Indian Ocean. T.F.H. Publications, Neptune City, 240 p., 144 pls -------------, 1988. Fishes of Christmas Island, Indian Ocean. Christmas Island Natural History Association, 199 p. Allen, G. R. & R. Swainston, 1988. The Marine fishes of North-western Australia. A field guide for anglers and divers. Western Australian Museum, Perth, 201 p. Alleyne, H.G. & W. Macleay, 1877. The ichthyology of the Chevert expedition. Proc. Linn.Soc. New South Wales, 1:261-80, pls.3-9. Amesbury, S. S. & R. F. Myers, 1982. Guide to the coastal resources of Guam, Volume I. The Fishes. University of Guam Press, 141 p. Asano, H., 1978. On the tendencies of differentiation in the composition of the vertebral number of teleostean fishes. Mem.Fac.Agric.Kinki Univ., 10(1977):29-37 Baddar, M.K , 1987. -
Polar Winds from VIIRS
Polar Winds from VIIRS Jeff Key*, Richard Dworak+, Dave Santek+, Wayne Bresky@, Steve Wanzong+ ! Jaime Daniels#, Andrew Bailey@, Chris Velden+, Hongming Qi^, Pete Keehn#, Walter Wolf#! ! *NOAA/National Environmental Satellite, Data, and Information Service, Madison, WI! + Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison! #NOAA/National Environmental Satellite, Data, and Information Service, Camp Springs, MD! ^NOAA/National Environmental Satellite, Data, and Information Service, Camp Springs, MD! @I.M. Systems Group (IMSG), Rockville, MD USA! 11th International Winds Workshop, Auckland, 20-24 February 2012 The Polar Wind Product Suite MODIS Polar Winds LEO-GEO Polar Winds •" Aqua and Terra separately, bent pipe •" Combination of may geostationary data source Operational and polar-orbiting imagers •" Aqua and Terra combined, bent pipe •" Fills the 60-70 degree latitude gap •" Direct broadcast (DB) at EW –" McMurdo, Antarctica (Terra, Aqua) VIIRS Polar Winds –" Tromsø, Norway (Terra only) •" (Details on following slides) –" Sodankylä, Finland (Terra only) –" Fairbanks, Alaska (Terra, from UAF) EW AVHRR Polar Winds •" Global Area Coverage (GAC) for NOAA-15, -16, -17, -18, -19 Operational •" Metop Operational •" HRPT (High Resolution Picture Transmission = direct readout) at –" Barrow, Alaska, NOAA-16, -17, -18, -19 –" Rothera, Antarctica, NOAA-17, -18, -19 •" Historical GAC winds, 1982-2009. Two satellites throughout most of the time series. Polar Wind Product History Operational NWP Users of Polar Winds! 13 NWP centers in 9 countries: •" European Centre for Medium-Range Weather Forecasts (ECMWF) - since Jan 2003.! •" NASA Global Modeling and Assimilation Office (GMAO) - since early 2003.! •" Deutscher Wetterdienst (DWD) – MODIS since Nov 2003. DB and AVHRR.! •" Japan Meteorological Agency (JMA), Arctic only - since May 2004.! •" Canadian Meteorological Centre (CMC) – since Sep 2004. -
Parasites of Coral Reef Fish: How Much Do We Know? with a Bibliography of Fish Parasites in New Caledonia
Belg. J. Zool., 140 (Suppl.): 155-190 July 2010 Parasites of coral reef fish: how much do we know? With a bibliography of fish parasites in New Caledonia Jean-Lou Justine (1) UMR 7138 Systématique, Adaptation, Évolution, Muséum National d’Histoire Naturelle, 57, rue Cuvier, F-75321 Paris Cedex 05, France (2) Aquarium des lagons, B.P. 8185, 98807 Nouméa, Nouvelle-Calédonie Corresponding author: Jean-Lou Justine; e-mail: [email protected] ABSTRACT. A compilation of 107 references dealing with fish parasites in New Caledonia permitted the production of a parasite-host list and a host-parasite list. The lists include Turbellaria, Monopisthocotylea, Polyopisthocotylea, Digenea, Cestoda, Nematoda, Copepoda, Isopoda, Acanthocephala and Hirudinea, with 580 host-parasite combinations, corresponding with more than 370 species of parasites. Protozoa are not included. Platyhelminthes are the major group, with 239 species, including 98 monopisthocotylean monogeneans and 105 digeneans. Copepods include 61 records, and nematodes include 41 records. The list of fish recorded with parasites includes 195 species, in which most (ca. 170 species) are coral reef associated, the rest being a few deep-sea, pelagic or freshwater fishes. The serranids, lethrinids and lutjanids are the most commonly represented fish families. Although a list of published records does not provide a reliable estimate of biodiversity because of the important bias in publications being mainly in the domain of interest of the authors, it provides a basis to compare parasite biodiversity with other localities, and especially with other coral reefs. The present list is probably the most complete published account of parasite biodiversity of coral reef fishes. -
Water Ice Clouds in the Martian Atmosphere: General Circulation Model Experiments with a Simple Cloud Scheme Mark I
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. E9, 5064, doi:10.1029/2001JE001804, 2002 Water ice clouds in the Martian atmosphere: General circulation model experiments with a simple cloud scheme Mark I. Richardson Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA R. John Wilson Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration, Princeton, New Jersey, USA Alexander V. Rodin Space Research Institute, Planetary Physics Division, Moscow, Russia Received 17 October 2001; revised 31 March 2002; accepted 5 June 2002; published 20 September 2002. [1] We present the first comprehensive general circulation model study of water ice condensation and cloud formation in the Martian atmosphere. We focus on the effects of condensation in limiting the vertical distribution and transport of water and on the importance of condensation for the generation of the observed Martian water cycle. We do not treat cloud ice radiative effects, ice sedimentation rates are prescribed, and we do not treat interactions between dust and cloud ice. The model generates cloud in a manner consistent with earlier one-dimensional (1-D) model results, typically evolving a uniform (constant mass mixing ratio) vertical distribution of vapor, which is capped by cloud at the level where the condensation point temperature is reached. Because of this vertical distribution of water, the Martian atmosphere is generally very far from fully saturated, in contrast to suggestions based upon interpretation of Viking data. This discrepancy results from inaccurate representation of the diurnal cycle of air temperatures in the Viking Infrared Thermal Mapper (IRTM) data. In fact, the model suggests that only the northern polar atmosphere in summer is consistently near its column-integrated holding capacity. -
Appendices Appendices
APPENDICES APPENDICES APPENDIX 1 – PUBLICATIONS SCIENTIFIC PAPERS Aidoo EN, Ute Mueller U, Hyndes GA, and Ryan Braccini M. 2015. Is a global quantitative KL. 2016. The effects of measurement uncertainty assessment of shark populations warranted? on spatial characterisation of recreational fishing Fisheries, 40: 492–501. catch rates. Fisheries Research 181: 1–13. Braccini M. 2016. Experts have different Andrews KR, Williams AJ, Fernandez-Silva I, perceptions of the management and conservation Newman SJ, Copus JM, Wakefield CB, Randall JE, status of sharks. Annals of Marine Biology and and Bowen BW. 2016. Phylogeny of deepwater Research 3: 1012. snappers (Genus Etelis) reveals a cryptic species pair in the Indo-Pacific and Pleistocene invasion of Braccini M, Aires-da-Silva A, and Taylor I. 2016. the Atlantic. Molecular Phylogenetics and Incorporating movement in the modelling of shark Evolution 100: 361-371. and ray population dynamics: approaches and management implications. Reviews in Fish Biology Bellchambers LM, Gaughan D, Wise B, Jackson G, and Fisheries 26: 13–24. and Fletcher WJ. 2016. Adopting Marine Stewardship Council certification of Western Caputi N, de Lestang S, Reid C, Hesp A, and How J. Australian fisheries at a jurisdictional level: the 2015. Maximum economic yield of the western benefits and challenges. Fisheries Research 183: rock lobster fishery of Western Australia after 609-616. moving from effort to quota control. Marine Policy, 51: 452-464. Bellchambers LM, Fisher EA, Harry AV, and Travaille KL. 2016. Identifying potential risks for Charles A, Westlund L, Bartley DM, Fletcher WJ, Marine Stewardship Council assessment and Garcia S, Govan H, and Sanders J. -
June Solstice Activities (PDF)
Arctic Connection Linking Your Place to the MOSAiC Expedition June Solstice Edition Introduction As I write this, it is the June Solstice. The exact moment of solstice occurred a few hours ago, at 21:44 Universal Daylight Time. This was at 1:44 pm today here in Homer, Alaska. This moment marked when Earth’s north pole leaned most toward the sun, and the Earth’s south pole was tilted most away from the sun. On this day, the sun appears directly overhead at local noon for those living at 23.5 degrees north (the Tropic of Cancer), as far north as the sun ever gets. And during the December solstice, the sun appears directly overhead for those living at 23.5 degrees south (the Tropic of Capricorn). (In case you need a refresher, here’s the basic science from Earth & Sky.) In the northern hemisphere, the June Solstice is called the summer solstice and represents the day(s) with the most amount of daylight. I say days because in some parts of the northern hemisphere, the sun has stayed above the horizon for multiple days now and won’t rise again until the next month. This is often called the Midnight Sun, and the ice camp at the Polarstern has been bathed in light for many days. This is good news for the scientists of Leg 4, who are just now arriving to the floe. The extended daylight will help make all of the research tasks a little bit easier than those Leg 1 and Leg 2 researchers who had to work through the Polar Night. -
A Quantitative Comparison of Recreational Spearwshing and Linewshing on the Great Barrier Reef: Implications for Management of Multi-Sector Coral Reef Wsheries
Coral Reefs (2008) 27:85–95 DOI 10.1007/s00338-007-0293-z REPORT A quantitative comparison of recreational spearWshing and lineWshing on the Great Barrier Reef: implications for management of multi-sector coral reef Wsheries A. J. Frisch · R. Baker · J-P. A. Hobbs · L. Nankervis Received: 3 May 2007 / Accepted: 6 August 2007 / Published online: 25 August 2007 © Springer-Verlag 2007 Abstract This study compared the catch composition, equitably across both Wshing sectors. A management strategy catch per unit eVort, and incidental impacts of spearWshers of this type will simplify enforcement of Wsheries regulations and lineWshers engaged in a structured Wshing program and avoid discrimination of particular Wshers in local whereby Wshing eVort was standardized across time, space communities where both Wshing methods are socially or and skill level. It was found that (1) the catch composition culturally important. of both groups of Wshers overlapped considerably, (2) the numbers of target Wsh caught by spearWshers (156) and Keywords SpearWshing · LineWshing · Catch per unit lineWshers (168) were not signiWcantly diVerent, (3) the eVort · Selectivity · Coral trout · Bycatch mean size of target Wsh caught by spearWshers (1.95 § 0.1 kg, §SE) was signiWcantly larger than the mean size of target Wsh caught by lineWshers (1.27 § 0.06 kg), and (4) spear- Introduction Wshers retained 43% more biomass of target species than did lineWshers (304 versus 213 kg, respectively). However, OverWshing is deemed to be one of the greatest threats to lineWshers used »1 kg of bait for every 3 kg of target Wsh the future of coral reefs (Jackson et al. -
Solar Cycle, Seasonal, and Diurnal Variations of the Mars Upper
JournalofGeophysicalResearch: Planets RESEARCH ARTICLE Mars Global Ionosphere-Thermosphere Model: 10.1002/2014JE004715 Solar cycle, seasonal, and diurnal variations Key Points: of the Mars upper atmosphere • The Mars Global 1 2 3 4 5 6 Ionosphere-Thermosphere Model S. W. Bougher ,D.Pawlowski ,J.M.Bell , S. Nelli , T. McDunn , J. R. Murphy , (MGITM) is presented and validated M. Chizek6, and A. Ridley1 • MGITM captures solar cycle, seasonal, and diurnal trends observed above 1Atmospheric, Oceanic, and Space Sciences Department, University of Michigan, Ann Arbor, Michigan, USA, 2Physics 100 km 3 • MGITM variations will be compared Department, Eastern Michigan University, Ypsilanti, Michigan, USA, National Institute of Aerospace, Hampton, Virginia, 4 5 6 to key episodic variations in USA, Harris, ITS, Las Cruces, New Mexico, USA, Jet Propulsion Laboratory, Pasadena, California, USA, Astronomy future studies Department, New Mexico State University, Las Cruces, New Mexico, USA Correspondence to: S. W. Bougher, Abstract A new Mars Global Ionosphere-Thermosphere Model (M-GITM) is presented that combines [email protected] the terrestrial GITM framework with Mars fundamental physical parameters, ion-neutral chemistry, and key radiative processes in order to capture the basic observed features of the thermal, compositional, and Citation: dynamical structure of the Mars atmosphere from the ground to the exosphere (0–250 km). Lower, middle, Bougher, S. W., D. Pawlowski, and upper atmosphere processes are included, based in part upon formulations used in previous lower and J. M. Bell, S. Nelli, T. McDunn, upper atmosphere Mars GCMs. This enables the M-GITM code to be run for various seasonal, solar cycle, and J. R. -
Rhythms During the Polar Night
Rhythms during the polar night: evidence of clock-gene oscillations in the Arctic scallop Chlamys islandica Mickael Perrigault, Hector Andrade, Laure Bellec, Carl Ballantine, Lionel Camus, Damien Tran To cite this version: Mickael Perrigault, Hector Andrade, Laure Bellec, Carl Ballantine, Lionel Camus, et al.. Rhythms during the polar night: evidence of clock-gene oscillations in the Arctic scallop Chlamys islandica. Pro- ceedings of the Royal Society B: Biological Sciences, Royal Society, The, 2020, 287 (1933), pp.20201001. 10.1098/rspb.2020.1001. hal-03053508 HAL Id: hal-03053508 https://hal.archives-ouvertes.fr/hal-03053508 Submitted on 6 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Rhythms during the polar night: Evidence of clock-gene oscillations 2 in the Arctic scallop Chlamys islandica 3 4 5 Mickael Perrigault 1.2, Hector Andrade 3, Laure Bellec1,2, Carl Ballantine 3, Lionel Camus 3, 6 Damien Tran 1.2 7 8 9 1 University of Bordeaux, EPOC, UMR 5805, 33120 Arcachon, France 10 2 CNRS, EPOC, UMR 5805, 33120 Arcachon, France 11 3 Akvaplan-niva AS, Fram Centre, 9296 Tromsø, Norway 12 13 Keywords: clock genes, polar night, arctic, bivalve, behavior, marine chronobiology 14 15 Corresponding author: [email protected] 16 1 17 Abstract 18 Arctic regions are highly impacted by climate change and are characterized by drastic 19 seasonal changes in light intensity and duration with extended periods of permanent light or 20 darkness. -
Regions and Counties in Norway
Regions and counties in Norway REGIONS AND COUNTIES IN NORWAY Northern Norway Northern Norway is located in the north and is also the most eastern region. This region comprises the two counties Troms og Finnmark and Nordland. If you visit Northern Norway in December or January, you can experience the polar night. The polar night is when the sun is under the horizon the whole day. In Northern Norway, you can see the northern lights in winter. Norway is divided into five regions. Northern Norway is located in the north of Northern lights. Photo: Pxhere.com the country. Trøndelag is located in the middle of the country. Western Norway is During summer, you can see the midnight in the west, and Eastern Norway is in the sun in Northern Norway. The midnight sun east. The region located in the south is is when the sun does not set, and a part of called Southern Norway. the sun is visible above the horizon all night. Every part of the country is divided into counties. There are 11 counties in Norway. Troms and Finnmark Troms og Finnmark is located furthest north and east and borders Russia, Finland 1 The National Centre of Multicultural Education, Native languages, morsmal.no Regions and counties in Norway and Sweden. Tromsø is the largest city in Troms og Finnmark. Norway's northernmost point, Knivskjellodden, is located in Troms og Finnmark. The North Cape (Nordkapp) is better known and is located almost as far north as Knivskjellodden. The North Cape is a famous tourist destination in Norway. Skrei cod hanging to dry on a rack. -
5-Review-Fish-Habita
United Nations UNEP/GEF South China Sea Global Environment Environment Programme Project Facility UNEP/GEF/SCS/RWG-F.8/5 Date: 12th October 2006 Original: English Eighth Meeting of the Regional Working Group for the Fisheries Component of the UNEP/GEF Project: “Reversing Environmental Degradation Trends in the South China Sea and Gulf of Thailand” Bangka Belitung Province, Indonesia 1st - 4th November 2006 INFORMATION COLLATED BY THE FISHERIES AND HABITAT COMPONENTS OF THE SOUTH CHINA SEA PROJECT ON SITES IMPORTANT TO THE LIFE- CYCLES OF SIGNIFICANT FISH SPECIES UNEP/GEF/SCS/RWG-F.8/5 Page 1 IDENTIFICATION OF FISHERIES REFUGIA IN THE GULF OF THAILAND It was discussed at the Sixth Meeting of the Regional Scientific and Technical Committee (RSTC) in December 2006 that the Regional Working Group on Fisheries should take the following two-track approach to the identification of fisheries refugia: 1. Review known spawning areas for pelagic and invertebrate species, with the aim of evaluating these sites as candidate spawning refugia. 2. Evaluate each of the project’s habitat demonstration sites as potential juvenile/pre-recruit refugia for significant demersal species. Rationale for the Two-Track Approach to the Identification of Fisheries Refugia The two main life history events for fished species are reproduction and recruitment. It was noted by the RSTC that both of these events involve movement between areas, and some species, often pelagic fishes, migrate to particular spawning areas. It was also noted that many species also utilise specific coastal habitats such as coral reefs, seagrass, and mangroves as nursery areas. In terms of the effects of fishing, most populations of fished species are particularly vulnerable to the impacts of high levels of fishing effort in areas and at times where there are high abundances of (a) stock in spawning condition, (b) juveniles and pre-recruits, or (c) pre-recruits migrating to fishing grounds. -
Habitat Use and Trophic Ecology of the Introduced
HABITAT USE AND TROPHIC ECOLOGY OF THE INTRODUCED SNAPPER LUTJANUS KASMIRA AND NATIVE GOATFISHES IN HAWAI‘I A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI‘I IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN ZOOLOGY (Marine Biology) AUGUST 2011 By Brett D. Schumacher Dissertation Committee: Alan Friedlander, Chairperson Charles Birkeland Kim Holland William Walsh Jeffrey Drazen UMI Number: 3485487 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent on the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI 3485487 Copyright 2011 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, MI 48106 - 1346 iii ACKNOWLEDGEMENTS I would like to gratefully acknowledge James Parrish for his loyal and longstanding support of my research as my original advisor and committee chair. I would also like to thank Alan Friedlander for taking over as chair after Dr. Parrish’s well- deserved retirement. I sincerely appreciate the suggestions and advice I received from my other committee members, Charles Birkeland, Curt Daehler, Jeff Drazen, Kim Holland and Bill Walsh. I am greatly indebted to Jeremy Claisse, Eric Conklin, Katie Howard, and Craig Musberger, dedicated research assistants who were willing to go into the field at all hours and in any kind of weather.