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  • 1
    Online Resource
    Online Resource
    Oxford :Oxford University Press, Incorporated,
    Keywords: Ecology -- Polar Regions. ; Natural history -- Polar Regions. ; Electronic books.
    Description / Table of Contents: There is an increased awareness of the importance of polar regions, and their vulnerability to anthropogenic derived change. This book offers a concise but comprehensive introduction to polar ecology. The emphasis is on the organisms that dominate these environments although pollution, conservation and experimental aspects are also considered.
    Type of Medium: Online Resource
    Pages: 1 online resource (409 pages)
    Edition: 2nd ed.
    ISBN: 9780191538261
    Series Statement: Biology of Habitats Series
    DDC: 578.0911
    Language: English
    Note: Intro -- Contents -- Preface -- 1 Introduction to the polar regions -- 1.1 Introduction -- 1.2 The energy balances of the polar regions -- 1.3 Climate -- 1.4 Thermohaline circulation -- 1.5 El Nino Southern Oscillation -- 1.6 Arctic and North Atlantic Oscillations -- 1.7 Magnetic and electrical phenomena -- 2 Stress, adaptation, and survival in polar regions -- 2.1 Introduction -- 2.2 Life at low temperatures -- 2.3 Desiccation -- 2.4 The effects of radiation -- 2.5 Biological rhythms in the polar environment -- 3 Periglacial and terrestrial habitats in polar regions -- 3.1 Introduction -- 3.2 Substrata -- 3.3 Communities -- 3.4 The physiological ecology of polar plants and invertebrates -- 3.5 Specialized communities -- 3.6 Comparison of Arctic and Antarctic terrestrial habitats and communities -- 4 Glacial habitats in polar regions -- 4.1 Introduction -- 4.2 Life in the interior of polar ice sheets and glaciers -- 4.3 Life at the margin -- 4.4 The snow alga community -- 4.5 Wider perspectives -- 5 Inland waters in polar regions -- 5.1 Introduction -- 5.2 Arctic lakes -- 5.3 Antarctic lakes -- 5.4 Streams and rivers -- 5.5 Conclusions -- 6 Open oceans in polar regions -- 6.1 Introduction -- 6.2 Gradients in waters -- 6.3 The plankton -- 6.4 The physiological ecology of polar phytoplankton -- 6.5 The zooplankton -- 6.6 Squid -- 6.7 Fish -- 6.8 The polar marine pelagic systems -- 7 Frozen oceans in polar regions -- 7.1 Introduction -- 7.2 The physical characteristics of sea ice -- 7.3 The biology of sea ice -- 7.4 The ice edge -- 7.5 Polynyas -- 7.6 The wider significance of sea ice biology -- 8 Marine benthos in polar regions -- 8.1 Introduction -- 8.2 The littoral zone -- 8.3 The shallow sublittoral zone -- 8.4 The benthos of deep waters -- 8.5 Benthos under ice shelves -- 8.6 Seasonality and dynamics of benthic communities. , 8.7 Comparisons and conclusions -- 9 Birds and mammals in polar regions -- 9.1 Introduction -- 9.2 Seabirds -- 9.3 Seals -- 9.4 Whales -- 9.5 Bears and foxes -- 10 Climate change in polar regions -- 10.1 Introduction -- 10.2 Changes during geological time: the ice ages -- 10.3 Biological responses to long-term changes -- 10.4 Present-day global climate change and polar regions -- 11 Human impact on polar regions -- 11.1 The first invasions by humans -- 11.2 The ecology of pre-industrial humans in the Arctic -- 11.3 Sealing and whaling -- 11.4 Hunting -- 11.5 Fishing -- 11.6 Pastoral and agriculture development -- 11.7 Introduction of non-native organisms by humans -- 11.8 Mineral and oil extraction -- 11.9 Pollution -- 11.10 Tourism -- 11.11 Military uses of the polar regions -- 11.12 Conservation -- 12 Some conclusions -- Further reading and web resources -- References -- Index -- A -- B -- C -- D -- E -- F -- G -- H -- I -- J -- K -- L -- M -- N -- O -- P -- Q -- R -- S -- T -- U -- V -- W -- X -- Y -- Z.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of neurochemistry 56 (1991), S. 0 
    ISSN: 1471-4159
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Abstract: In vivo microdialysis was used to investigate the regulation of noradrenaline release in rat hippocampus. Idazoxan, an α2-adrenoreceptor antagonist (1–10 mg/kg), increased noradrenaline release in a dose-dependent manner. Inhibition of noradrenaline uptake by desipramine (0.05–20 μM; via the probe) also increased the extracellular content of the transmitter. In the presence of this increased noradrenaline content (desipramine via the probe), the effect of a low dose of idazoxan (1 mg/kg) was potentiated. Local perfusion of idazoxan (1–500 μM) in the hippocampus also increased noradrenaline release but not to the same extent as following systemic administration. In the presence of desipramine, unlike the systemic injection of idazoxan, local perfusion did not potentiate noradrenaline release. The data are consistent with the regulation of extracellular noradrenaline content in the hippocampus by neuronal uptake and to a lesser extent by presynaptic autoreceptors.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 746 (1994), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 123 (1995), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Fifty Thellier palaeointensity determinations were made from the Great Whin Sill (GWS) of northern England and the Midland Valley Sill (MVS) of central Scotland, which form the major part of a late Carboniferous quartz-dolerite complex. Palaeodirectional analysis confirms that the reversed polarity characteristic remanence carried by samples from both sills is consistent with the Permo-Carboniferous reversed superchron. Palaeomagnetic results suggest that the two sills may not be exactly contemporaneous. The MVS was intruded rapidly some time during the emplacement of the GWS, which was itself emplaced over a considerable time period. The MVS may well represent the northernmost expression of the instrusive activity. A mean palaeointensity of 22.9 ± 2.6 μT was calculated for the Great Whin Sill, with a corresponding VDM value of 5.9 ± 1022 A m2. The palaeointensity value calculated from the Midland Valley Sill was much lower, 13.0 ± 0.5 μT, with a corresponding VDM value of 3.3 ± 1022 A m2. Detailed rock magnetic analyses and stepwise thermal demagnetization studies reveal that the remanence carrier in both sills is magnetite of mixed domain state. Multidomain grains are less important in the Midland Valley Sill and thus greater confidence is attached to palaeointensity results from this sill. VDM values from this and other studies of the Permo-Carboniferous reversed superchron (P-CRS) indicate that the dipole strength showed similar variations to that witnessed for the past 5 Ma. There is no conclusive support in favour of either the weak or strong field models that have been suggested for superchrons. More palaeointensity results are needed from the termination of the P-CRS and the late Permian/early Triassic in order to understand how the dipole field evolved during the P-CRS and its relationship to the so-called Mesozoic dipole low.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Water and environment journal 14 (2000), S. 0 
    ISSN: 1747-6593
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Water management can be set within a conceptual framework which emphasises the importance of maximising the usefulness of water as it moves through a catchment area. The framework is based upon a consideration of the thermodynamic property of entropy, i.e. a measure of a system's increasing inability to do work. It is concluded that a consideration of water utility as a determinant is more appropriate than the conventional volume-paradigm applied to water resourcing.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 122 (1995), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An anomalous palaeomagnetic field direction is recognized in a sequence of rapidly extruded subaerial basaltic lava flows within the Mid-Proterozoic (c. 1300 Ma) Gardar lava succession, South Greenland. Thermal demagnetization and component analysis link this direction to a thermoremanent magnetization (TRM) acquired during primary cooling. The direction, which bears no resemblance to any other palaeomagnetic direction witnessed within the Group, is recorded by seven successive flows which appear to have been extruded and magnetized over a short period of time during a geomagnetic polarity transition. Palaeointensity experiments employing the modified Thellier technique indicate that this transitional direction was acquired in a field with only 25 per cent of the magnitude of the stable polarity field. The behaviour of the field direction during and after this transition reflects that witnessed in studies of much younger transitional sequences, whereas that for the field intensity differs fundamentally from consistent observations from younger lava successions. These results provide a significant contribution to our knowledge of the ancient geodynamo and may well document the oldest transitional field identified by a combined palaeomagnetic and palaeointensity study and the only one reported from the Precambrian era.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 11 (1991), S. 329-337 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The light saturated photosynthesis, dark respiration and light independent carbon fixation of macroalgal species endemic to the Antarctic were measured. Five brown algae. Ascoseira mirabilis, Desmarestia anceps, D. antarctica, Phaeurus antarcticus, Himantothallus grandifolius and the red alga Palmaria decipiens were included. Rates of these three parameters at 0°C were very similar to those measured in other studies on temperate algae at higher temperature. This indicates a high degree of physiological adaptation to the Antarctic environment within these species. A comparison was made of polarographic and chemical means of measuring oxygen flux during photosynthesis and dark respiration at low temperature. There was a good correlation between measurements of oxygen evolution and carbon fixation, although apparent photosynthetic quotient values were in most cases high.
    Type of Medium: Electronic Resource
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  • 8
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    INT GLACIOL SOC
    In:  EPIC3Annals of Glaciology, INT GLACIOL SOC, 62(82), ISSN: 0260-3055
    Publication Date: 2021-01-13
    Description: Basal melt of ice shelves is not only an important part of Antarctica’s ice-sheet mass budget, but it is also the origin of one of the most peculiar types of sea ice found in the polar oceans: platelet ice. In many regions around coastal Antarctica, tiny ice crystals form and grow in supercooled plumes of Ice Shelf Water, releasing heat into the surrounding ocean. They usually rise towards the surface, eventually becoming trapped under an ice shelf as marine ice. Frequently, masses of those crystals are advected out of the ice-shelf cavity, and accumulate below a solid sea-ice cover to form a semiconsolidated layer. When the overlying sea ice grows into this so-called sub-ice platelet layer, the loose crystals are consolidated, adding additional thickness to the sea ice. These phenomena are generally referred to as platelet ice, although confusion about the terminology is widespread in the literature. The presence of platelet ice has a profound impact on sea-ice properties and processes in several regions of Antarctica, with numerous implications for the local polar marine biosphere. Most notably, sub-ice platelet layers provide a stable, sheltered, nutrient- and food-rich habitat which usually results in a highly productive and uniquely adapted ecosystem. It has also been hypothesised that platelet ice may be an indicator of the state of an ice shelf, although comprehensive time series are limited to the Ross Sea. This paper clears up the terminology by providing exact definitions of the relevant terms.We review platelet-ice formation, observational methods as well as geographical and seasonal occurrence. The physical properties and ecological implications are merged in a way understandable for physicists and biologists alike, to lay the foundation for the interdisciplinary research that is necessary to tackle the current knowledge gaps.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 9
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    Unknown
    In:  EPIC3"New Challenges for North Sea Research - 20 years after FLEX `76- Meeting“, Hamburg, Germany, Hamburg, Germany, 1996
    Publication Date: 2017-02-09
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 10
    Publication Date: 2017-02-07
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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