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  • Edmonton : University of Alberta Press
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  • 1
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    American Chemical Society | ACS Publications
    Online: 1(1).2021 –
    Publisher: American Chemical Society , ACS Publications
    Electronic ISSN: 2691-3704
    Topics: Chemistry and Pharmacology
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  • 2
    Journal cover
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    American Chemical Society | ACS Publications
    Online: 1.1879 –
    Publisher: American Chemical Society , ACS Publications
    Print ISSN: 0002-7863
    Electronic ISSN: 1520-5126
    Topics: Chemistry and Pharmacology
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  • 3
    Call number: AWI Bio-97-0308
    In: Flora of the Russian Arctic, Volume 1
    Description / Table of Contents: Families in Volume 1: I. Polypodiaceae - True Ferns. - II. Ophioglossaceae - Adder's Tongue. - III. Equisetaceae - Horsetails. - IV. Lycopodiaceae - Club-Moss. - V. Selaginellaceae - Selaginella. - VI. Pinaceae - Pine. - VII. Cupressaceae - Cypress. - VIII. Sparganiaceae - Bur-Reed. - IX. Potamogetonaceae - Pondweed. - X. Juncaginaceae - Arrow-Grass. - XI. Alismataceae - Water-Plantain. - XII. Butomaceae - Flowering Rush. - XIII. Gramineae - Grasses
    Description / Table of Contents: This volume - the first of six - launches the first comprehensive English-language flora of the Russian Arctic. Flora of the Russian Arctic translates Arkticheskaya Flora SSSR, the authoritative work of botanists of the Komarov Botanical Institute prepared under the editorship of A. I. Trolmachev and B. A. Yurtsev. This unexcerpted translation was prepared by distinguished systematist G. C. D: Griffiths under the editorship of J. G. Packer, Professor Emeritus of Botany at the University of Alberta. It represents the first time this work has been made available in a language other than Russian. This first volue of Flora of the Russian Arctic describes the thirteen families here listed. Together, the six volumes will treat some 360 genera, 1650 species and 220 infraspecific taxa, including many new combinations and previously undescribed species and subspecies. Detailed keys to genera and species and the original distribution maps complement the species discussions. The Russian Arctic spans 145 degrees of longitude, from the Barents Sea to the Bering Strait. The comprehensive content and accomplished scholarship of this work, along with the size of the area covered, make Flora of the Russian Arctic an essential part of every botanical library.
    Type of Medium: Monograph available for loan
    Pages: XXXVIII, 330 Seiten , Illustrationen
    Edition: First English edition
    ISBN: 0888642695
    Series Statement: Flora of the Russian Arctic : a critical review of the vascular plants occurring in the Arctic region of the former Soviet Union 1
    Uniform Title: Arktičeskaja flora SSSR
    Language: English , Latin
    Note: Contents Acknowledgements Editor's Preface Translator's Preface Preface to Volume I of the Russian edition, Polypodiaceae-Butomaceae Preface to Volume II of the Russian edition, Gramineae Abbreviations Used in Citing Floristic and Systematic Literature FAMILY I / Polypodiaceae—True Ferns GENUS 1 / Woodsia—Woodsia GENUS 2 / Cystopteris—Bladder Fern GENUS 3 / Dryopteris—Shield Fern GENUS 4 / Thelypteris—Thelypteris GENUS 5 / Gymnocarpium—Oak Fern GENUS 6 / Polystichum—Holly Fern GENUS 7 / Athyrium—Lady Fern GENUS 8 / Asplenium—Spleenwort GENUS 9 / Cryptogramma—Rock Brake GENUS 10 / Polypodium—Polypody FAMILY II / Ophioglossaceae—Adder's Tongue Family GENUS L / Botrychium—Moonwort FAMILY III / Equisetaceae—Horsetails GENUS 1 / Equisetum—Horsetail FAMILY IV / Lycopodiaceae—Club-Mosses GENUS 1 / Lycopodium—Club-Moss FAMILY V / Selaginellaceae—Selaginella Family GENUS 1 / Selaginella—Selaginella, Little Club-Moss FAMILY VI / Pinaceae—Pine Family GENUS IA / Abies—Fir GENUS 1 / Picea—Spruce GENUS 2 / Larix—Larch GENUS 3 / Pinus—Pine FAMILY VII / Cupressaceae—Cypress Family GENUS 1 / Juniperus—Juniper FAMILY VIII / Sparganiaceae—Bur-Reed Family GENUS 1 / Sparganium—Bur-Reed FAMILY IX / Potamogetonaceae—Pondweed Family GENUS 1 / Potamogeton—Pondweed GENUS 2 / Zostera—Eel-Grass FAMILY X / Juncaginaceae—Arrow-Grass Family GENUS 1 / Triglochin—Arrow Grass GENUS 2 / Scheuchzeria—Scheuchzeria FAMILY XI / Alismataceae—Water-Plantain Family GENUS 1 / Alisma—Water-Plantain FAMILY XII / Butomaceae—Flowering Rush Family GENUS 1 / Butomus—Flowering Rush FAMILY XIII / Gramineae—Grasses GENUS 1 / Typhoides—Reed Canary Grass GENUS 2 / Anthoxanthum—Vernal-Grass GENUS 3 / Hierochloe—Sweet Grass GENUS 4 / Milium—Wood Millet GENUS 5 / Phleum—Timothy GENUS 6 / Alopecurus—Foxtail GENUS 7 / Arctagrostis—Arctagrostis GENUS 8 / Agrostis—Bent GENUS 9 / Calamagrostis—Reed Grass GENUS 10 / Apera—Silky Bent GENUS 11 / Vahlodea—Vahlodea GENUS 12 / Deschampsia—Hair Grass GENUS 13 / Trisetum—Trisetum GENUS 14 / Helictotrichon—Oat Grass GENUS 15 I Beckmannia—Slough Grass GENUS 16 / Phragmites—Reed GENUS 17 / Molinia—Moor Grass GENUS 18 / Koeleria—June Grass GENUS 19 / Melica—Melic GENUS 20 / Pleuropogon—Semaphore Grass GENUS 21 / Dactylis—Cocksfoot GENUS 22 / Poa—Bluegrass GENUS 23 / Dupontia—Dupontia GENUS 24 / Arctophila—Arctophila GENUS 25 / Colpodium—Colpodium GENUS 26 / Catabrosa—Brook Grass GENUS 27 / Phippsia—Phippsia GENUS 27A / Glyceria—Manna Grass GENUS 28 / Puccinellia—Alkali Grass GENUS 29 / Festuca—Fescue GENUS 30 / Zerna—Perennial Brome Grass GENUS 31 / Bromus—Brome Grass GENUS 32 / Nardus—Matgrass GENUS 33 / Roegneria—Rhizomeless WheatGrass GENUS 34 / Elytrigia—WheatGrass GENUS 35 / Leymus—Wild Rye GENUS 36 / Hordeum—Barley APPENDIX I I Summary of Data on the Geographical Distribution of Vascular Plants of the Soviet Arctic TABLE 1 / Distribution of Vascular Plants of the Soviet Arctic, Polypodiaceae-Butomaceae TABLE 2 / Distribution of Vascular Plants of the Soviet Arctic, Gramineae Index of Plant Names
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 4
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    PANGAEA
    In:  Supplement to: Walther, Kathleen; Sartoris, Franz-Josef; Pörtner, Hans-Otto (2011): Impacts of temperature and acidification on larval calcium incorporation of the spider crab Hyas araneus from different latitudes (54° vs. 79°N). Marine Biology, 158(9), 2043-2053, https://doi.org/10.1007/s00227-011-1711-x
    Publication Date: 2023-03-16
    Description: The combined effects of ocean warming and acidification were compared in larvae from two popula- tions of the cold-eurythermal spider crab Hyas araneus, from one of its southernmost populations (around Helgo- land, southern North Sea, 54°N, habitat temperature 3-18°C; collection: January 2008, hatch: January-February 2008) and from one of its northernmost populations (Svalbard, North Atlantic, 79°N, habitat temperature 0-6°C; collection: July 2008, hatch: February-April 2009). Larvae were exposed to temperatures of 3, 9 and 15°C combined with present-day normocapnic (380 ppm CO2) and projected future CO2 concentrations (710 and 3,000 ppm CO2). Calcium content of whole larvae was measured in freshly hatched Zoea I and after 3, 7 and 14 days during the Megalopa stage. Significant differences between Helgoland and Svalbard Megalopae were observed at all investigated temperatures and CO2 condi- tions. Under 380 ppm CO2, the calcium content increased with rising temperature and age of the larvae. At 3 and 9°C, Helgoland Megalopae accumulated more calcium than Svalbard Megalopae. Elevated CO2 levels, especially 3,000 ppm, caused a reduction in larval calcium contents at 3 and 9°C in both populations. This effect set in early, at 710 ppm CO2 only in Svalbard Megalopae at 9°C. Fur- thermore, at 3 and 9°C Megalopae from Helgoland replenished their calcium content to normocapnic levels and more rapidly than Svalbard Megalopae. However, Svalbard Megalopae displayed higher calcium contents under 3,000 ppm CO2 at 15°C. The findings of a lower capacity for calcium incorporation in crab larvae living at the cold end of their distribution range suggests that they might be more sensitive to ocean acidification than those in temperate regions.
    Keywords: Animalia; Arctic; Arthropoda; AWI_EcolChem; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Coast and continental shelf; Ecological Chemistry @ AWI; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Hyas araneus; Laboratory experiment; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Pelagos; Polar; Single species; Temperate; Temperature; Zooplankton
    Type: Dataset
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  • 5
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    PANGAEA
    In:  Supplement to: Kravchishina, Marina D; Lisitzin, Alexander P (2011): Grain-size composition of the suspended particulate matter in the marginal filter of the Severnaya Dvina River. Translated from Okeanologiya, 2011, 51(1), 94-109, Oceanology, 51(1), 89-104, https://doi.org/10.1134/S0001437011010097
    Publication Date: 2023-03-16
    Description: Quantitative distribution and grain size composition of suspended particulate matter (SPM) in the marginal filter of the North (Severnaya) Dvina River during summer low water periods of 2001-2005 were analyzed in water on board immediately after sampling (without preliminary treatment) using a Coulter counter. This analysis revealed main regularities in transformation of grain size spectra at successive salinity steps of the marginal filter, as well as boundaries between these steps based on data obtained by direct complex studies of SPM dispersion. It is established that water salinity is the main factor that controls changes in grain size distribution and composition of suspended matter in the marginal filter. Concentrations of 〈0.01 mm size fraction and salinity demonstrate negative correlations between each other. It is shown that areas characterized by mass development of phytoplankton are located along the outer boundary of the marginal filter (at the biological step), where salinity reaches 23-24 psu. Contents of particulate forms of some chemical (lithogenic) elements and organic carbon indicating genetic composition of SPM and their relations with grain size composition of SPM are studied.
    Keywords: Archive of Ocean Data; ARCOD; Bottle, Niskin; Bucket, plastic; IPE-57-1; IPE-57-13; IPE-57-15; IPE-57-17; IPE-57-19; IPE-57-2; IPE-57-22; IPE-57-26; IPE-57-5; IPE-57-9; KL-11rk; KL-14rk; KL-2rk; KL-5rk; KL-7rk; KL-9rk; KL-MF-1; KL-MF-12; KL-MF-13; KL-MF-14; KL-MF-15; KL-MF-16; KL-MF-17; KL-MF-18; KL-MF-19; KL-MF-20; KL-P-2; NIS; North Dvina mouth area; Professor Shtokman; PSh-4921; PSh-6401; PSh71; PSh-7109; PSh-7111; PSh-7112; PSh-7115; PSh-7116; PSh-7120; WB; White Sea
    Type: Dataset
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  • 6
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    PANGAEA
    In:  Supplement to: Goroslavskaya, E I; Galkin, Sergey V (2011): Benthic fauna associated with mussel beds and shrimp swarms at hydrothermal fields on the Mid-Atlantic Ridge. Translated from Okeanologiya, 2011, 51(1), 74-84, Oceanology, 51(1), 69-79, https://doi.org/10.1134/S0001437011010048
    Publication Date: 2023-03-16
    Description: Macrofaunal assemblages with prevalence of Bresiliidae shrimps and Mytilidae mussels are abundant in at hydrothermal vents along the Mid-Atlantic Ridge. Mussels inhabit zones of diffuse seeps of hydrothermal fluids with temperature abnormalities up to several degrees. Shrimps inhabit an extreme biotope in a mixed interface between seawater and hydrothermal fluids at temperature up to 20-30°C. We studied the mussel and shrimp assemblages in three hydrothermal vent fields: Rainbow, Broken Spur, and Snake Pit. Species richness of the mussel assemblages within at least two fields (Broken Spur and Snake Pit) is higher as compared with shrimps from the same hydrothermal vent fields. Fauna inhibiting shrimp swarms lack almost any taxa specific for particular assemblages: almost all the taxa are also present in the mussel beds. Structure of the shrimp assemblage is less homogeneous as compared with that of the mussel assemblage. Population prevalence of one taxon (Copepoda) in the shrimp assemblage is most likely connected with extreme and unstable conditions of the biotope occupied by the shrimps in a hydrothermal field. Taxonomic similarity between the mussel and shrimp assemblages within one hydrothermal vent field is higher as compared with similarity between the mussel (or shrimp) assemblages from different fields.
    Keywords: Akademik Mstislav Keldysh; AMK47; AMK47-4327-1; AMK47-4330-1; AMK47-4330-2; AMK47-4332-2; AMK47-4349-1; AMK47-4358-1; AMK47-4392-2; AMK47-4393-1; AMK47-4393-2; AMK47-4393-3; AMK47-4399-1; AMK47-4402-1; AMK47-4749-2; AMK49; AMK49-4611-1; AMK49-4611-2; AMK49-4611-3; AMK49-4611-4; AMK49-4611-5; AMK50; AMK50-4793-1; AMK50-4797-1; AMK50-4797-4; AMK50-4797-5; AMK50-4797-6; AMK50-4812-1; AMK50-4812-4; AMK50-4819-10; AMK50-4819-12; AMK50-4819-17; AMK50-4819-8; Archive of Ocean Data; ARCOD; Broken Spur Hydrothermal Field; Broken Srur Hydrothermal Field; Broken Srur Hydrothermal Field, K point mound; MIR; MIR deep-sea manned submersible; Rainbow Hydrothermal Field; Snake Pit Hydrothermal Field; Snake Pit Hydrothermal Field, Beehive mound
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  • 7
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    PANGAEA
    In:  Supplement to: Nemirovskaya, Inna A; Chemyavskii, N G (2011): Studies of hydrocarbons in the waters and snow-ice cover of the southeast sector of the Antarctic. Translated from Okeanologiya, 2011, 51(1), 5-15, Oceanology, 51(1), 4-14, https://doi.org/10.1134/S0001437011010139
    Publication Date: 2023-03-16
    Description: Data are presented on concentration of hydrocarbons (HC) relative to concentrations of suspended matter, lipids, organic carbon, and chlorophyll a in surface waters and snow-ice cover of the East Antarctic coastal areas. It was shown that growth of concentrations of aliphatic HC (AHC) to 30 µg/l in surface waters takes place in frontal zones and under young ice formation. AHC concentration in snow increases with growth of aerosol concentration in the atmosphere. In the lower part of ice, at the boundary with seawater, despite low temperatures, autochthonous processes may provide high AHC concentrations (up to 289 µg/l). Within the snow-ice cover on fast ice, concentration co-variations of all the compounds considered take place.
    Keywords: AF2008-NLS; Akademik Mstislav Keldysh; AMK50; Archive of Ocean Data; ARCOD; DruzhnSt-2008; MirnySt-2008; Mirny Station; MULT; Multiple investigations; ProgrSt-2008; Prydz Bay, Collaboration Sea; Southern Ocean - Atlantic Sector
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  • 8
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    PANGAEA
    In:  Supplement to: Kosyan, A R; Kucheruk, Nikita V; Flint, Mikhail V (2012): Role of bivalve mollusks in the sediment balance of the Anapa Bay Bar. Translated from Okeanologiya, 2012, 52(1), 78-84, Oceanology, 52(1), 72-78, https://doi.org/10.1134/S0001437012010122
    Publication Date: 2023-03-16
    Description: Sandy beaches of the Anapa Bay Bar are a unique natural resource, but they are gradually being degrade under both natural and anthropogenic factors. Emissions of sand and shelly ground from the adjacent sea bottom partly compensate for this process. Concentration of carbonates may reach up to 50% in beach sands, and most of these carbonates are of mollusk origin. The major deposit formation role belongs to the key bivalve species: Chamelea gallina (Linnaeus, 1758). Average biomass of this mollusk species reaches up to 450 g/m**2 at depths 5-10 m. The other two subdominating mollusk species, bivalve Donax trunculus (Linnaeus, 1758) and gastropod Rapana venosa (Valenciennes, 1846), may impact as 16 g/m**2 and 6 g/m**2, respectively. Annually, 350 kg of shelly ground per running meter are newly deposited on the Anapa beach.
    Keywords: Archive of Ocean Data; ARCOD; Black Sea; KKF12-1; KKF12-2; KKF12-3; KKF12-4; KKF12-5; KKF12-6; KKF12-7; KKF12-8
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Lukashin, Vyacheslav N; Demina, Lyudmila L; Gordeev, Viacheslav V; Gordeev, Vladimir Yu (2012): The geochemistry of deepwater particulate matter over the hydrothermal field at 9°50'N (the East Pacific Rise). Translated from Okeanologiya, 2012, 52(2), 292-305, Oceanology, 52(2), 271-283, https://doi.org/10.1134/S0001437012010146
    Publication Date: 2023-03-16
    Description: Results of geochemical studies of suspended matter from the water mass over the hydrothermal field at 9°50'N on the East Pacific Rise are reported. The suspended matter was sampled in background waters, in the buoyant plume, and in the near-bottom waters. Contents of Si, Al, P, Corg, Fe, Mn, Cu, Zn, Ni, Co, As, Cr, Cd, Pb, Ag, and Hg were determined. No definite correlations were found between the elements in the background waters. Many of the chemical elements correlated with Fe and associated with its oxyhydroxides in the buoyant plume. In the near-bottom waters trace elements are associated with Fe, Zn, and Cu (probably, with their sulfides formed during mixing of hydrothermal fluids with seawater). Chemical composition of sediment matter precipitated in a sediment trap was similar to the near-bottom suspended matter.
    Keywords: Archive of Ocean Data; ARCOD
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Lein, Alla Yu; Kravchishina, Marina D; Politova, Nadezhda V; Savvichev, Alexander S; Veslopolova, E F; Mitskevich, Irina N; Ul'yanova, Nina V; Shevchenko, Vladimir P; Ivanov, Mikhail V (2012): Transformation of particulate organic matter at the water-bottom boundary in the Russian Arctic seas: Evidence from isotope and radioisotope data. Translated from Litologiya i Poleznye Iskopaemye, 2012, 2, 115-145, Lithology and Mineral Resources, 47(2), 99-128, https://doi.org/10.1134/S0024490212020034
    Publication Date: 2023-03-16
    Description: Comprehensive biogeochemical studies including determination of isotopic composition of organic carbon in both suspended matter and surface layer (0-1 cm) bottom sediments (more than 260 determinations of d13C-Corg) were carried out for five Arctic shelf seas: White, Barents, Kara, East Siberian, and Chukchi Seas. The aim of this study is to elucidate causes that change isotopic composition of particulate organic carbon at the water-sediment boundary. It is shown that isotopic composition of organic carbon in sediments from seas with high river run-off (White, Kara, and East Siberian Seas) does not inherit isotopic composition of organic carbon in particles precipitating from the water column, but is enriched in 13C. Seas with low river run-off (Barents and Chukchi Seas) show insignificant difference between d13C-Corg values in both suspended load and sediments because of low content of isotopically light allochthonous organic matter in suspended matter. Biogeochemical studies with radioisotope tracers (14CO2, 35S, and 14CH4) revealed existence of specific microbial filter formed from heterotrophic and autotrophic organisms at the water-sediment boundary. This filter prevents mass influx of products of organic matter decomposition into the water column, as well as reduces influx of OM contained in suspended matter from water into sediments.
    Keywords: Archive of Ocean Data; ARCOD
    Type: Dataset
    Format: application/zip, 23 datasets
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