Some Regularities in the Distribution of The
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"National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary."
Intro 1996 National List of Vascular Plant Species That Occur in Wetlands The Fish and Wildlife Service has prepared a National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary (1996 National List). The 1996 National List is a draft revision of the National List of Plant Species That Occur in Wetlands: 1988 National Summary (Reed 1988) (1988 National List). The 1996 National List is provided to encourage additional public review and comments on the draft regional wetland indicator assignments. The 1996 National List reflects a significant amount of new information that has become available since 1988 on the wetland affinity of vascular plants. This new information has resulted from the extensive use of the 1988 National List in the field by individuals involved in wetland and other resource inventories, wetland identification and delineation, and wetland research. Interim Regional Interagency Review Panel (Regional Panel) changes in indicator status as well as additions and deletions to the 1988 National List were documented in Regional supplements. The National List was originally developed as an appendix to the Classification of Wetlands and Deepwater Habitats of the United States (Cowardin et al.1979) to aid in the consistent application of this classification system for wetlands in the field.. The 1996 National List also was developed to aid in determining the presence of hydrophytic vegetation in the Clean Water Act Section 404 wetland regulatory program and in the implementation of the swampbuster provisions of the Food Security Act. While not required by law or regulation, the Fish and Wildlife Service is making the 1996 National List available for review and comment. -
Novaya Zemlya Archipelago (Russian Arctic)
This is a repository copy of First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic). White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/127196/ Version: Accepted Version Article: Mazei, Yuri, Tsyganov, Andrey N, Chernyshov, Viktor et al. (2 more authors) (2018) First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic). Polar Biology. ISSN 0722-4060 https://doi.org/10.1007/s00300-018-2273-x Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 First records of testate amoebae from the Novaya Zemlya archipelago (Russian Arctic) 2 Yuri A. Mazei1,2, Andrey N. Tsyganov1, Viktor A. Chernyshov1, Alexander A. Ivanovsky2, Richard J. 3 Payne1,3* 4 1. Penza State University, Krasnaya str., 40, Penza 440026, Russia. 5 2. Lomonosov Moscow State University, Leninskiye Gory, 1, Moscow 119991, Russia. 6 3. University of York, Heslington, York YO10 5DD, United Kingdom. -
Satellite Ice Extent, Sea Surface Temperature, and Atmospheric 2 Methane Trends in the Barents and Kara Seas
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-237 Manuscript under review for journal The Cryosphere Discussion started: 22 November 2018 c Author(s) 2018. CC BY 4.0 License. 1 Satellite ice extent, sea surface temperature, and atmospheric 2 methane trends in the Barents and Kara Seas 1 2 3 2 4 3 Ira Leifer , F. Robert Chen , Thomas McClimans , Frank Muller Karger , Leonid Yurganov 1 4 Bubbleology Research International, Inc., Solvang, CA, USA 2 5 University of Southern Florida, USA 3 6 SINTEF Ocean, Trondheim, Norway 4 7 University of Maryland, Baltimore, USA 8 Correspondence to: Ira Leifer ([email protected]) 9 10 Abstract. Over a decade (2003-2015) of satellite data of sea-ice extent, sea surface temperature (SST), and methane 11 (CH4) concentrations in lower troposphere over 10 focus areas within the Barents and Kara Seas (BKS) were 12 analyzed for anomalies and trends relative to the Barents Sea. Large positive CH4 anomalies were discovered around 13 Franz Josef Land (FJL) and offshore west Novaya Zemlya in early fall. Far smaller CH4 enhancement was found 14 around Svalbard, downstream and north of known seabed seepage. SST increased in all focus areas at rates from 15 0.0018 to 0.15 °C yr-1, CH4 growth spanned 3.06 to 3.49 ppb yr-1. 16 The strongest SST increase was observed each year in the southeast Barents Sea in June due to strengthening of 17 the warm Murman Current (MC), and in the south Kara Sea in September. The southeast Barents Sea, the south 18 Kara Sea and coastal areas around FJL exhibited the strongest CH4 growth over the observation period. -
GEOGRAPHY Teacher’S Resource A/AS Level for AQA GEOGRAPHY Teacher’S Resource
Brighter Thinking GEOGRAPHY Teacher’s Resource A/AS Level for AQA GEOGRAPHY Teacher’s Resource A/AS Level for AQA University Printing House, Cambridge CB2 8BS, United Kingdom Cambridge University Press is part of the University of Cambridge. It furthers the University’s mission by disseminating knowledge in the pursuit of education, learning and research at the highest international levels of excellence. www.cambridge.org Information on this title: www.cambridge.org/9781316603314 (Cambridge Elevate edition) www.cambridge.org/9781316603321 (Free Online) © Cambridge University Press 2016 This publication is in copyright. Subject to statutory exception and to the provisions of relevant collective licensing agreements, no reproduction of any part may take place without the written permission of Cambridge University Press. First published 2016 A catalogue record for this publication is available from the British Library ISBN 978-1-316-60331-4 Cambridge Elevate edition ISBN 978-1-316-60332-1 Free Online Additional resources for this publication at www.cambridge.org/education Cambridge University Press has no responsibility for the persistence or accuracy of URLs for external or third-party internet websites referred to in this publication, and does not guarantee that any content on such websites is, or will remain, accurate or appropriate. NOTICE TO TEACHERS IN THE UK It is illegal to reproduce any part of this work in material form (including photocopying and electronic storage) except under the following circumstances: (i) where you are abiding -
Atlas of Rare Endemic Vascular Plants of the Arctic
Atlas of Rare Endemic Vascular Plants of the Arctic Technical Report No. 3 About CAFF Theprogram for the Conservation of Arctic Flora and Fauna (CAFF) of the Arctic Council was established lo address the special needs of Arctic ecosystems, species and thcir habitats in the rapid ly developing Arctic region. Itwas initiated as one of'four programs of the Arctic Environmental Protcction Strategy (AEPS) which was adopted by Canada, Denmark/Greenland, Finland, lceland, Norway, Russia, Swcdcn and the United States through a Ministeria! Declaration at Rovaniemi, Finland in 1991. Other programs initi ated under the AEPS and overlaken hy the Are.tie Council are the ArcticMonitoring and assessment Programme (AMAP), the program for Emergency Prevention, Preparcd ness and Response (EPPR) and the program for Protection of the Arctic Marine Envi ronment (PAME). Sinceits inaugural mccti.ng in Ottawa, Canada in 1992, the CAFF program has provided scientists, conscrvation managers and groups, and indigenous people of the north with a distinct forum in which lo tackle a wide range of Arctic conservation issues at the cir cumpolar level. CAFF's main goals, which are achieved in keeping with the concepts of sustainable developrnertt and utilisation, are: • to conserve Arctic Jlora and fauna, thcir diversity and thcir habitats; • to protect the Arctic ecosystems from threats; • to improve conservation management laws, reg ulations and practices for the Arclic; • to integrale Arctic interests into global conservation fora. CAFF operates rhrough a system of Designated Agencies and National Representatives responsible for CAFF in thcir rcspcctivc countries. CAFF also has an International Work ing Group wh.ith has met annually to assess progrcss and to develop Annual WorkPlans. -
Exceptional Retreat of Novaya Zemlya's Marine
The Cryosphere, 11, 2149–2174, 2017 https://doi.org/10.5194/tc-11-2149-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Exceptional retreat of Novaya Zemlya’s marine-terminating outlet glaciers between 2000 and 2013 J. Rachel Carr1, Heather Bell2, Rebecca Killick3, and Tom Holt4 1School of Geography, Politics and Sociology, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK 2Department of Geography, Durham University, Durham, DH13TQ, UK 3Department of Mathematics & Statistics, Lancaster University, Lancaster, LA1 4YF, UK 4Centre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 4RQ, UK Correspondence to: J. Rachel Carr ([email protected]) Received: 7 March 2017 – Discussion started: 15 May 2017 Revised: 20 July 2017 – Accepted: 24 July 2017 – Published: 8 September 2017 Abstract. Novaya Zemlya (NVZ) has experienced rapid ice al., 2013). This ice loss is predicted to continue during loss and accelerated marine-terminating glacier retreat dur- the 21st century (Meier et al., 2007; Radic´ et al., 2014), ing the past 2 decades. However, it is unknown whether and changes are expected to be particularly marked in the this retreat is exceptional longer term and/or whether it has Arctic, where warming of up to 8 ◦C is forecast (IPCC, persisted since 2010. Investigating this is vital, as dynamic 2013). Outside of the Greenland Ice Sheet, the Russian high thinning may contribute substantially to ice loss from NVZ, Arctic (RHA) accounts for approximately 20 % of Arctic but is not currently included in sea level rise predictions. glacier ice (Dowdeswell and Williams, 1997; Radic´ et al., Here, we use remotely sensed data to assess controls on NVZ 2014) and is, therefore, a major ice reservoir. -
Floral Preformation in the Warming Boreal Forest: the Effects of Temperature on the Development of Vaccinium Vitis-Idaea Eileen Schaub [email protected]
University of Connecticut OpenCommons@UConn Master's Theses University of Connecticut Graduate School 8-30-2019 Floral Preformation in the Warming Boreal Forest: the Effects of Temperature on the Development of Vaccinium vitis-idaea Eileen Schaub [email protected] Recommended Citation Schaub, Eileen, "Floral Preformation in the Warming Boreal Forest: the Effects of Temperature on the Development of Vaccinium vitis-idaea" (2019). Master's Theses. 1434. https://opencommons.uconn.edu/gs_theses/1434 This work is brought to you for free and open access by the University of Connecticut Graduate School at OpenCommons@UConn. It has been accepted for inclusion in Master's Theses by an authorized administrator of OpenCommons@UConn. For more information, please contact [email protected]. Floral Preformation in the Warming Boreal forest: the Effects of Temperature on the Development of Vaccinium vitis-idaea Eileen Patricia Schaub B.A., Western Connecticut State University, 2013 A Thesis Submitted in Partial Fulfillment of the Requirements of the Degree of Master of Science At the University of Connecticut 2019 Copyright by Eileen Patricia Schaub 2019 ii Approval Page Master of Science Thesis Floral Preformation in the Warming Boreal Forest: the Effects of Temperature on the Development of Vaccinium vitis-idaea Presented by Eileen P. Schaub, B.A. Major Advisor _________________________________________________________________ Pamela K. Diggle Associate Advisor ______________________________________________________________ Cynthia S. Jones Associate Advisor ______________________________________________________________ Donald Les University of Connecticut 2019 iii Introduction The boreal zone, located between 50 and 70º north latitude, is the largest terrestrial biome, comprising 11% of Earth’s landmass across North America, Europe, and Asia (Brandt, 2009). It consists primarily of coniferous forest, with some deciduous tree species and numerous shrub and grass species. -
Radioactivity in the Arctic Seas
IAEA-TECDOC-1075 XA9949696 Radioactivity in the Arctic Seas Report for the International Arctic Seas Assessment Project (IASAP) ffl INTERNATIONAL ATOMIC ENERGY AGENCA / Y / 1JrrziZr^AA 30-16 The originating Section of this publication in the IAEA was: Radiometrics Section International Atomic Energy Agency Marine Environment Laboratory B.P. 800 MC 98012 Monaco Cedex RADIOACTIVITY IN THE ARCTIC SEAS IAEA, VIENNA, 1999 IAEA-TECDOC-1075 ISSN 1011-4289 ©IAEA, 1999 Printe IAEe th AustriAn y i d b a April 1999 FOREWORD From 199 o 1993t e Internationa6th l Atomic Energy Agency's Marine Environment Laboratory (IAEA-MEL s engage IAEA'e wa ) th n di s International Arctic Seas Assessment Project (IASAP whicn i ) h emphasi bees ha sn place criticaa n do l revie f environmentawo l conditions in the Arctic Seas. IAEA-MEe Th L programme, organize framewore th n dIASAi e th f ko P included: (i) an oceanographic and an ecological description of the Arctic Seas; provisioe th (ii )centra a f no l database facilitIASAe th r yfo P programm collectione th r efo , synthesi interpretatiod san datf nmarino n ao e radioactivit Arctie th n yi c Seas; (iii) participation in official expeditions to the Kara Sea organized by the joint Russian- Norwegian Experts Group (1992, 1993 and 1994), the Russian Academy of Sciences (1994), and the Naval Research Laboratory and Norwegian Defence Research Establishment (1995); (iv) assistance wit d n laboratorsiti han u y based radiometric measurement f curreno s t radionuclide concentrations in the Kara Sea; (v) organization of analytical quality assurance intercalibration exercises among the participating laboratories; (vi) computer modellin e potentiath f o g l dispersa f radionuclideo l s released froe mth dumped f assessmeno wast d associatee ean th f o t d radiological consequencee th f o s disposals on local, regional and global scales; (vii) in situ and laboratory based assessment of distribution coefficients (Kd) and concentration factor sArctie (CFth r c)fo environment. -
The Representation of Wetland Types and Species in RAMSAR Sites in The
The representation of wetland types and species in RAMSAR sites in the Baltic Sea Catchment Area The representation of wetland types and species in RAMSAR sites in the Baltic Sea Catchment Area | 1 2 | The representation of wetland types and species in RAMSAR sites in the Baltic Sea Catchment Area White waterlily, Nymphaea alba The representation of wetland types and species in RAMSAR sites in the Baltic Sea Catchment Area In order to get a better reference the future and long-term planning of activities aimed for the protection of wetlands and their ecological functions, WWF Sweden initiated an evaluation of the representation of wetland types and species in the RAMSAR network of protected sites in the Baltic Sea Catchment Area. The study was contracted to Dr Mats Eriksson (MK Natur- och Miljökonsult HB, Sweden), who has been assisted by Mrs Alda Nikodemusa, based in Riga, for the compilation of information from the countries in Eastern Europe. Mats O.G. Eriksson MK Natur- och Miljökonsult HB, Tommered 6483, S-437 92 Lindome, Sweden With assistance by Alda Nikodemusa, Kirsu iela 6, LV-1006 Riga, Latvia The representation of wetland types and species in RAMSAR sites in the Baltic Sea Catchment Area | 3 Contents Foreword 5 Summary 6 Sammanfattning på svenska 8 Purpose of the study 10 Background and introduction 10 Study area 12 Methods 14 Land-use in the catchment area 14 Definitions and classification of wetland types 14 Country-wise analyses of the representation of wetland types 15 Accuracy of the analysis 16 Overall analysis of the -
Kenai National Wildlife Refuge Species List, Version 2018-07-24
Kenai National Wildlife Refuge Species List, version 2018-07-24 Kenai National Wildlife Refuge biology staff July 24, 2018 2 Cover image: map of 16,213 georeferenced occurrence records included in the checklist. Contents Contents 3 Introduction 5 Purpose............................................................ 5 About the list......................................................... 5 Acknowledgments....................................................... 5 Native species 7 Vertebrates .......................................................... 7 Invertebrates ......................................................... 55 Vascular Plants........................................................ 91 Bryophytes ..........................................................164 Other Plants .........................................................171 Chromista...........................................................171 Fungi .............................................................173 Protozoans ..........................................................186 Non-native species 187 Vertebrates ..........................................................187 Invertebrates .........................................................187 Vascular Plants........................................................190 Extirpated species 207 Vertebrates ..........................................................207 Vascular Plants........................................................207 Change log 211 References 213 Index 215 3 Introduction Purpose to avoid implying -
The Circumpolar Arctic Vegetation Map - 267
Journal of Vegetation Science 16: 267-282, 2005 © IAVS; Opulus Press Uppsala. - The Circumpolar Arctic vegetation map - 267 The Circumpolar Arctic vegetation map Walker, Donald A.1*; Raynolds, Martha K.1; Daniëls, Fred J.A.2; Einarsson, Eythor3; Elvebakk, Arve4; Gould, William A.5; Katenin, Adrian E.6; Kholod, Sergei S.6,7; Markon, Carl J.8; Melnikov, Evgeny S.8,9; Moskalenko, Natalia G.8,10; Talbot, Stephen S.11; Yurtsev, Boris A.(†)6 & the other members of the CAVM Team12 1Alaska Geobotany Center, Institute of Arctic Biology, University of Alaska Fairbanks, 311 Irving, P.O. Box 757000, Fairbanks, AK 99775, USA; 2Institute für Botanik und Botanischer Garten, Westfälische Wilhelms-Universität, Schloßgarten 3, D-48149 Münster, Germany; E-mail [email protected]; 3Icelandic Museum of Natural History, P.O. Box 5320, Reykjavik, Iceland; E-mail [email protected]; 4Institute of Biology and Geology, University of Tromsø, N-9037 Tromsø, Norway; E-mail [email protected]; 5International Institute for Tropical Forestry, USDA Forest Service, 1201 Calle Ceiba, San Juan, Puerto Rico, PR 00927-1119, USA; E-mail [email protected]; 6Department of Far North Vegetation, Komarov Botanical Institute RAS, Prof. Popov str. 2, 197376 St. Petersburg, Russia; E-mail [email protected]; 7E-mail [email protected]; 8USGS Alaska Geographic Science Office, 4230 University Dr., Anchorage, AK 99508-4664 USA; E-mail [email protected]; 8 Earth Cryosphere Institute SB RAS, Vavilov str. 30/6, r. 85, Moscow 119991, Russia; 9E-mail [email protected]; 10E-mail [email protected]; -
Arctic National Wildlife Refuge Volume 2
Appendix F Species List Appendix F: Species List F. Species List F.1 Lists The following list and three tables denote the bird, mammal, fish, and plant species known to occur in Arctic National Wildlife Refuge (Arctic Refuge, Refuge). F.1.1 Birds of Arctic Refuge A total of 201 bird species have been recorded on Arctic Refuge. This list describes their status and abundance. Many birds migrate outside of the Refuge in the winter, so unless otherwise noted, the information is for spring, summer, or fall. Bird names and taxonomic classification follow American Ornithologists' Union (1998). F.1.1.1 Definitions of classifications used Regions of the Refuge . Coastal Plain – The area between the coast and the Brooks Range. This area is sometimes split into coastal areas (lagoons, barrier islands, and Beaufort Sea) and inland areas (uplands near the foothills of the Brooks Range). Brooks Range – The mountains, valleys, and foothills north and south of the Continental Divide. South Side – The foothills, taiga, and boreal forest south of the Brooks Range. Status . Permanent Resident – Present throughout the year and breeds in the area. Summer Resident – Only present from May to September. Migrant – Travels through on the way to wintering or breeding areas. Breeder – Documented as a breeding species. Visitor – Present as a non-breeding species. * – Not documented. Abundance . Abundant – Very numerous in suitable habitats. Common – Very likely to be seen or heard in suitable habitats. Fairly Common – Numerous but not always present in suitable habitats. Uncommon – Occurs regularly but not always observed because of lower abundance or secretive behaviors.