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An Annotated Species List of Parasites Found in European Smelt Osmerus Eperlanus (L.)
Transactions of Karelian Research Centre of Труды Карельского научного центра РАН Russian Academy of Sciences № 7. 2017. С. 73–92 No. 7. 2017. P. 73–92 DOI: 10.17076/bg627 УДК 576.89:597.552.3 AN ANNOTATED SPECIES LIST OF PARASITES FOUND IN EUROPEAN SMELT OSMERUS EPERLANUS (L.) L. V. Anikieva, E. P. Ieshko Institute of Biology, Karelian Research Centre, Russian Academy of Sciences, Petrozavodsk, Russia This paper offers a summary of the data on parasites of European smelt based on own col- lections and materials published in journal reviews, scientific papers, conference procee- dings and theses. The system of parasitic organisms published in Catalogues of parasites of freshwater fishes of North Asia [Pugachev, 2001–2004] is used, taking into account new studies on the systematics of infusorians and trematodes. Other groups of parasites are considered within the frameworks of widely used classifications. The species struc- ture of European smelt and its ecological forms follow the classification by L. Berg [1948] and Yu. Reshetnikov [Atlas …, 2003]. Altogether 65 species/taxa of parasites have been recorded from the distribution range of European smelt (Conoidasida – 1, Haplophasea – 2, Ichthiosporea – 1, Myxosporidia – 1, Phyllopharyngea – 1, Oligohymenophorea – 3, Monogenea – 1, Cestoda – 9, Trematoda – 11, Nematoda – 19, Palaeacanthocephala – 7, Hirudinea – 1, Bivalvia – 1, Crustacea – 7). Each parasite species is briefly described; the species occurrence in different smelt ecoforms, sources for species records (prov- enance and author) are stated. For higher taxa, we analyzed the taxonomic diversity of smelt parasites, their zoogeographic zoning and distribution, as well as specificity, dis- tinctive morphological, biological and ecological traits. -
The Influence of Geological Structure on Glacial Erosion and Lake Basins Formation
SI: “The 4th International Conference Limnology and Freshwater Biology 2020 (4): 481-482 DOI:10.31951/2658-3518-2020-A-4-481 Palaeolimnology of Northern Eurasia” Short communication The influence of geological structure on glacial erosion and lake basins formation Amantov A.V.1*, Amantova M.G.1, Sapelko T.V.2 1 A.P. Karpinsky Russian Geological Research Institute (VSEGEI), St. Petersburg, Russia 2 Institute of Limnology, RAS, St. Petersburg, Russia ABSTRACT. The geomorphological evolution of several huge lake basins in the Pleistocene glacial and periglacial domains was analyzed with the combination of relevant modeling and geological data. It is found that most basins were occupied by large lakes classified as structural - denudational forms, when the pattern of uneven glacial erosion was influenced by geological and tectonic features. The basins were divided into groups on the basis of their peculiarities and resulting morphological changes. Keywords: Quaternary, large lakes, glaciation, geology, tectonics, erosion, modeling 1. Introduction landscape development to compare with the observed pattern. Extensive data were used to characterize the It is widely accepted that most lakes were formed subsurface geology. as a result of the Pleistocene glacial activity, and it shaped many basins linked to existing freshwater large 3. Discussion and conclusions lakes. They often represent small permanent remnants of the huge dammed temporary glacial lakes created in The first-order pre-glacial landscape elements front of the paleo-ice sheets of Northern Hemisphere. were among the major factors that could partly control There are ongoing discussions about “glacial” vs. ice basal velocities in favorable circumstances. In time, “tectonic” or “astrobleme” (e.g. -
Finnish-Russian Development Programme on Sustainable Forest Management and Conservation of Biological Diversity in Northwest Russia
FINNISH-RUSSIAN DEVELOPMENT PROGRAMME ON SUSTAINABLE FOREST MANAGEMENT AND CONSERVATION OF BIOLOGICAL DIVERSITY IN NORTHWEST RUSSIA Second Phase (NWRDP II) for 2001-2004) FOREWORD..................................................................................................................... 2 NATURE PROTECTION PROJECTS .......................................................................... 3 Nature Protection Areas of Saint Petersburg ...................................................................... 3 Gogland Island (Suursaari) ................................................................................................. 9 The Present State of the Nature Conservation Areas in Murmansk Region..................... 11 Mires of Eastern Fennoscandia: Scientific Basis of Their Sustainable Use and Protection ........................................................................................................................................... 13 The Ichthyofauna of the Vologda Region......................................................................... 14 FORESTRY PROJECTS ............................................................................................... 16 International Forest Machine Operator Training Centre, Svetogorsk, Russia. ................. 16 Forestry Training Need Analysis in the Leningrad Region .............................................. 18 The Development of Sustainable Forest Management in Northwest Russia (2001-2004)23 INTERNATIONAL PROJECTS.................................................................................. -
The Parasite Fauna of Ecological Forms of the European Smelt, Osmerus Eperlanus L
ПАРАЗИТОЛОГИЯ, 51, 5, 2017 УДК 576.89:597.552.3 THE PARASITE FAUNA OF ECOLOGICAL FORMS OF THE EUROPEAN SMELT, OSMERUS EPERLANUS L. © L. V. Anikieva,1 E. P. Ieshko,2 O. N. Pugachev3 12 Institute of Biology, Karelian Research Centre RAS 11 Pushkinskaya St., 185910 Petrozavodsk, Republic of Karelia 3 Zoological Institute RAS 1 Universitetskaya Nab., 199034 St Petersburg 1 E-mail: [email protected] Submitted 19.05.2017 Three ecological forms of smelt have been analyzed: an anadromous (marine) form from the North Sea drainage basin and two freshwater forms — smelt proper from lakes Ladoga, Onego and Pyaozero, and dwarf (lake) smelt from lakes Beloye, Vozhe and Peipus (Pskov-Chudskoye). It is demonstrated that ecological forms of smelt feature their specific sets of parasites and the taxonomic structure of their diversity as represented by the compo- sition of higher taxa. It is shown that ecological forms of smelt are characterized by a speci- fic set of parasites and systematic structure of its diversity, which is assessed on the compo- sition of the higher taxa. Most significant differences were detected between the anadromo- us form inhabiting waters of varying salinity and the freshwater form. These characteristics of the parasite fauna stem from smelt's high ecological plasticity, which enables the fish to inhabit both marine and fresh waters. Key words: smelt Osmerus eperlanus, ecological forms, parasite species composition, diversity structure. ПАРАЗИТОФАУНА ЭКОЛОГИЧЕСКИХ ФОРМ ЕВРОПЕЙСКОЙ КОРЮШКИ OSMERUS EPERLANUS L. © Л. В. Аникиева,1 Е. П. Иешко,2 О. Н. Пугачев3 12 Институт биологии Карельского научного центра РАН ул. Пушкинская, 11, Петрозаводск, Республика Карелия, 185910 3 Зоологический институт РАН Университетская наб., 1, Санкт-Петербург, 199034 1 [email protected] Поступила 19.05.2017 Проведен анализ паразитофауны трех экологических форм европейской корюш- ки: проходной (морской) из бассейна Северного моря и двух пресноводных форм — собственно корюшки из озер Ладожское, Онежское и Пяозеро и снетка из озер Белое, 369 Воже и Псковско-Чудское. -
Translation 5156
ISSN 0704-3716 Canadian Translation of Fisheries and Aquatic Sciences • No. 5156 Ecology and distribution of the oligochaete Potamothrix hammoniensis Mich. DF°ild#110b illittee GrigYalis Original title: (unknown) In: A. Kangur (ed.), Biologiya presnovodnykh organizmov Severozapada SSSR. Gidrobiol. Issled. 14. Institute of Zoology and Rotany, Academy of Sciences of the Estonian SSR, Tallin, U.S.S.R., p. 40-45, 1983 Original language: Russian Available from: Canada Institute for Scientific and Technical Information National Research Council Ottawa, Ontario, Canada KlA 0S2 1985 a, ocmans Eishesie L.% BRARN' DEC -1.5 Ins - 14 - 8 typescript pages toUr; z BOO Otéac, pêcb'z.J5 Secretary Secrétariat 90 —00097 / cep of State d'État MULTILINGUAL SERVICES DIVISION — DIVISION DES SERVICES MULTILINGUES TRANSLATION BUREAU BUREAU DES TRADUCTIONS 4 I LIBRARY IDENTIFICATION — FICHE SIGNALÉTIQUE cT r ■ei 5 5 /3".(a Translated from - Traduction de Into - En Russian lis h Author - Aufiur Grigyalis, A. Title in English or French - Titre anglais ou français Ecology and distribution of the oligochaete Potamothrix hammoniensis Mich. Title in foreign language (Transliterate foreign characters) Titre en langue étrangère (Transcrire en caractères romains) Reference in foreign language (Name of book or publication) in full, transliterate foreign characters. Référence en langue étrangère (Nom du livre ou publication), au complet, transcrire en caractères romains. Gidrobiologicheskie issledovaniya Reference in English or French - Référence en anglais ou français Hydrobiological Research Publisher - Editeur Page Numbers in original DATE OF PUBLICATION Numéros des pages dans Institute of Zoology and Botany, . DATE DE PUBLICATION l'original Academy of Sciences of the Estonian 40-45 SSR Year Issue No. -
Modern Researches of Osprey in Russia
Modern researches of Osprey in Russia MIROSLAV BABUSHKIN Darwin State Nature Biosphere Reserve, Russia, [email protected] ANDREY KUZNETSOV Darwin State Nature Biosphere Reserve, Russia, [email protected] Nesting range of osprey within Russian Federation Main areas within North-West of Russia where osprey studies are being conducted 1 cm = 50 kM Russian-Estonian project on study birds of prey in border territories Long-term monitoring Study of nest ecology Ringing Building artificial nests GPS-GSM-telemetry Actions on nest protection 1 cm = 50 kM Long-term monitoring on the territory of “Smolensk Lakeland” national park Monitoring of nest platforms 1 cm = 50 kM Building artificial nests Monitoring of nesting sites Long-term monitoring Ringing 1 cm = 50 kM Study Area Expansive territory (from River Volga upper reaches to the Kola Peninsula north) was surveyed during the course of summer and winter expeditions in the period from 1998 to 2018. 1 cm = 50 kM MODERN ABOUNDANCE AND DISTRIBUTION OF OSPREY ( PANDION HALIAETUS ) ON THE COASTS OF LARGE WATERBODIES OF RUSSIA’S NORTH-WEST In total 53060 km we recovered: -6860 of boat surveys, - 22500 km of car surveys, -2370 km snowmobile surveys, -Walking routes – 21 330 km - Territory of Vologda Lakeland was additionally surveyed from a helicopter in 1988, 1993, 1999, 2002 and 2008 (38 flight hours). Rybinsk reservoir Impounded in 1945 Darwin biosphere reserve - 1120 km 2 Lake Keret Lake Vygozero Lake Vodlozero The southern coast of Lake Onega Lake Beloye Lake Vozhe Sheksna reservoir Rybinsk reservoir Rybinsk reservoir 12 3 4 70 In 1980s, the Darwin Reserve became the center from which the migration of young birds to the adjacent waterbodies of the region took place. -
Historical Geography and Archaeology
FtfllUJSCandia Qrchaeologica Xl (1994) Nikolai A. Makarov PORTAGES OF THE RUSSIAN NORTH: HISTORICAL GEOGRAPHY AND ARCHAEOLOGY Abstract This article summarizes the results of archaeological research concerning portage sites in the Russian North. Extensive surveys and field work indicate that the medieval portages were routes through water partings and related settlements which were either individual or in groups. The concentrations of sites from the eleventh to the thirteenth centuries, the vicinities of portages and the character of finds clearly show that the colonization of these micro-areas was closely connected with the development of a general system of roads and routes linking the North with the Ancient Russian Metropolia. Nikolai A. Makorov, Institute of Archaeology, Russian Academy of Sciences, VI. Dimitri Vlyanova 19, Moscow 117036, Russia. River routes connected by portages at watersheds Eastern Europe were referred to with tbe term fonned the main communication system on the Zavolochie (Le. areas beyond a portage or porta Russian Plain in the Middle Ages. They are as typi ges) since the eleventh century. The term survived cal of the cultural and economic potential of medi in the Land Cadastre Books (Vasiliev 1971, 103- eval Rus as the paved roads were an embodiment of 109; Piswvye knigi Obunezhskoj Pyatiny 1930, the power of the Roman Empire. Much attention is 177; Piswvaya knig. Belozerskogo yuesda 1984, given to portages in medieval documents, begin 171) until the sixteenth century, clearly pointing to ning with the famous description of "tbe route the important role of portages that hoth separated from the Varangians to tbe Greeks" in Povest Vre the Russian North from the rest of Rus (owing to menych Let, and continuing to the description of the difficulty of access) and connected far-off re Yrmak's campaign to Siberia in the Strogaoov gions.