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  • 1
    Online Resource
    Online Resource
    New York, NY :Springer,
    Keywords: Crystals. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (401 pages)
    Edition: 1st ed.
    ISBN: 9781461228127
    Series Statement: Partially Ordered Systems Series
    DDC: 530.41
    Language: English
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Geology, Stratigraphic-Precambrian. ; Paleontology-Precambrian. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (967 pages)
    Edition: 1st ed.
    ISBN: 9780080542591
    DDC: 551.7/1
    Language: English
    Note: Front Cover -- The Precambrian Earth: Tempos and Events -- Copyright Page -- Contents -- Contributing Authors -- PREFACE -- Chapter 1. THE EARLY EARTH -- 1.1. Introduction -- 1.2. Earth's Formation and First Billion Years -- 1.3. The Early Precambrian Stratigraphic Record of Large Extraterrestrial Impacts -- 1.4. Strategies for Finding the Record of Early Precambrian Impact Events -- 1.5. Commentary -- Chapter 2. GENERATION OF CONTINENTAL CRUST -- 2.1. Introduction -- 2.2. Isua Enigmas: Illusive Tectonic, Sedimentary, Volcanic and Organic Features of the > -- 3.7 Ga Isua Greenstone Belt, Southwest Greenland -- 2.3. Geochemical Diversity in Volcanic Rocks of the > -- 3.7 Ga Isua Greenstone Belt, Southern West Greenland: Implications for Mantle Composition and Geodynamic Processes -- 2.4. Abitibi Greenstone Belt Plate Tectonics: The Diachrononous History of Arc Development, Accretion and Collision -- 2.5. Granite Formation and Emplacement as Indicators of Archaean Tectonic Processes -- 2.6. Diapiric Processes in the Formation of Archaean Continental Crust, East Pilbara Granite-Greenstone Terrane, Australia -- 2.7. Early Archaean Crustal Collapse Structures and Sedimentary Basin Dynamics -- 2.8. Crustal Growth Rates -- 2.9. Commentary -- Chapter 3. TECTONISM AND MANTLE PLUMES THROUGH TIME -- 3.1. Introduction -- 3.2. Precambrian Superplume Events -- 3.3. Large Igneous Province Record through Time -- 3.4. Episodic Crustal Growth During Catastrophic Global-Scale Mantle Overturn Events -- 3.5. An Unusual Palaeoproterozoic Magmatic Event, the Ultrapotassic Christopher Island Formation, Baker Lake Group, Nunavut, Canada: Archaean Mantle Metasomatism and Palaeoproterozoic Mantle Reactivation -- 3.6. A Commentary on Precambrian Plate Tectonics -- 3.7. Precambrian Ophiolites. , 3.8. The Limpopo Belt of Southern Africa: A Neoarchaean to Palaeoproterozoic Orogen -- 3.9. Geodynamic Crustal Evolution and Long-Lived Supercontinents During the Palaeoproterozoic: Evidence from Granulite-Gneiss Belts, Collisional and Accretionary Orogens -- 3.10. Formation of a Late Mesoproterozoic Supercontinent: The South Africa-East Antarctica Connection -- 3.11. A Mechanism for Explaining Rapid Continental Motion in the Late Neoproterozoic -- 3.12. Commentary -- Chapter 4. PRECAMBRIAN VOLCANISM: AN INDEPENDENT VARIABLE THROUGH TIME -- 4.1. Introduction -- 4.2. Terminology of Volcaniclastic and Volcanic Rocks -- 4.3. Komatiites: Volcanology, Geochemistry and Textures -- 4.4. Archaean and Proterozoic Greenstone Belts: Setting and Evolution -- 4.5. Explosive Subaqueous Volcanism -- 4.6. Archaean Calderas -- 4.7. Commentary -- Chapter 5. THE EVOLUTION OF THE PRECAMBRIAN ATMOSPHERE: CARBON ISOTOPIC EVIDENCE FROM THE AUSTRALIAN CONTINENT -- 5.1. Introduction -- 5.2. Archaean Atmosphere, Hydrosphere and Biosphere -- 5.3. Evolution of the Precambrian Atmosphere: Carbon Isotopic Evidence from the Australian Continent -- 5.4. Precambrian Iron-Formation -- 5.5. The Precambrian Sulphur Isotope Record of Evolving Atmospheric Oxygen -- 5.6. Earth's Two Great Precambrian Glaciations: Aftermath of the "Snowball Earth" Hypothesis -- 5.7. The Paradox of Proterozoic Glaciomarine Deposition, Open Seas and Strong Seasonality Near the Palaeo-Equator: Global Implications -- 5.8. Neoproterozoic Sedimentation Rates and Timing of Glaciations-A Southern African Perspective -- 5.9. Earth's Precambrian Rotation and the Evolving Lunar Orbit: Implications of Tidal Rhythmite Data for Palaeogeophysics -- 5.10. Ancient Climatic and Tectonic Settings Inferred from Palaeosols Developed on Igneous Rocks -- 5.11. Aggressive Archaean Weathering -- 5.12. Commentary. , Chapter 6. EVOLUTION OF LIFE AND PRECAMBRIAN BIO-GEOLOGY -- 6.1. Introduction -- 6.2. Earth's Earliest Biosphere: Status of the Hunt -- 6.3. Evolving Life and Its Effect on Precambrian Sedimentation -- 6.4. Microbial Origin of Precambrian Carbonates: Lessons from Modern Analogues -- 6.5. Precambrian Stromatolites: Problems in Definition, Classification, Morphology and Stratigraphy -- 6.6. Precambrian Geology and Exobiology -- 6.7. Commentary -- Chapter 7. SEDIMENTATION THROUGH TIME -- 7.1. Introduction -- 7.2. Sedimentary Structures: An Essential Key for Interpreting the Precambrian Rock Record -- 7.3. Archaean Sedimentary Sequences -- 7.4. Discussion of Selected Techniques and Problems in the Field Mapping and Interpretation of Archaean Clastic Metasedimentary Rocks of the Superior Province, Canada -- 7.5. Precambrian Tidalites: Recognition and Significance -- 7.6. Sedimentary Dynamics of Precambrian Aeolianites -- 7.7. Early Precambrian Epeiric Seas -- 7.8. Precambrian Rivers -- 7.9. Microbial Mats in the Siliciclastic Rock Record: A Summary of Diagnostic Features -- 7.10. Microbial Mat Features in Sandstones Illustrated -- 7.11. Sedimentation Rates -- 7.12. Commentary -- Chapter 8. SEQUENCE STRATIGRAPHY AND THE PRECAMBRIAN -- 8.1. Introduction -- 8.2. Concepts of Sequence Stratigraphy -- 8.3. Development and Sequences of the Athabasca Basin, Early Proterozoic, Saskatchewan and Alberta, Canada -- 8.4. Third-Order Sequence Stratigraphy in the Palaeoproterozoic Daspoort Formation (Pretoria Group, Transvaal Supergroup), Kaapvaal Craton -- 8.5. Commentary -- Chapter 9. TOWARDS A SYNTHESIS -- 9.1. Evolution of the Solar System and the Early Earth -- 9.2. Generation of Continental Crust -- 9.3. Tectonism and Mantle Plumes through Time -- 9.4. Precambrian Volcanism, an Independent Variable -- 9.5. Evolution of the Hydrosphere and Atmosphere. , 9.6. Evolution of Precambrian Life and Bio-Geology -- 9.7. Sedimentation Regimes through Time -- 9.8. Sequence Stratigraphy through Time -- 9.9. Tempos and Events in Precambrian Time -- References -- Subject Index.
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of neurochemistry 25 (1975), S. 0 
    ISSN: 1471-4159
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Abstract— The effect of hyperbaric oxygenation on the levels of monoamines and free amino acids in whole mouse brain were found to vary with time of exposure and the pressure system used. Depression of 5-hydroxytryptamine (5-HT), noradrenaline (NA) and dopamine (DA) levels occurred after 40-60 min in 100% oxygen at atmospheric pressure. These effects occurred more rapidly at higher pressures but had disappeared by about 20 min. No significant change in free glutamic acid, glycine, tryptophan, tyrosine or taurine levels was observed following exposure for up to 60 min in oxygen at 4 atm. A progressive decrease in alanine occurred when oxygen replaced air and the pressure and exposure time increased. Other changes, detected in post-convulsant mice only, were increases in the leucine and valine pools. The relationship of these results to other work is discussed.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1095-8649
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Occurrences of 18 scalloped hammerhead sharks tagged with coded ultrasonic transmitters were recorded at seamount El Bajo Espiritu Santo in the Gulf of California over a 10-day period by automated, data-logging monitors. These sharks remained grouped at the seamount during the day and moved separately into the surrounding pelagic environment at night. The temporal pattern of shark occurrences was related to the light-dark cycle: individuals departed prior to dusk and returned near dawn next morning. However, arrivals and departures of more than one shark within short daytime periods indicated group movements to and from the seamount. Sharks returned repeatedly to the tagging site and not to another site centred less than 240 m from the former site.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 691 (1993), 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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  • 6
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] It has long been known that magnetic fields penetrate type II superconductors in the form of quantized superconducting vortices. Most recent research in this area has, however, focused on the collective properties of large numbers of strongly interacting vortices,: the study of vortex physics ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 322 (1986), S. 534-538 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 Map of the Marquesas Islands, an age-progressive volcanic lineament in the south-central Pacific basin, showing the island of Ua Pou. Solid circles (on the enlarged map of the island) mark the location of samples (tholeiites, alkali basalts and differentiates) analysed in the present study. ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 302 (1983), S. 400-403 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Previous Nd isotopic studies1'2 of kimberlites have shown that they generally have initial 143Nd/144Nd ratios corresponding to £Nd 0, implying derivation from a relatively undifferenti ated mantle source with chondritic Sm/Nd. This interpretation is difficult to reconcile with the fact that many ...
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Psychopharmacology 93 (1987), S. 193-200 
    ISSN: 1432-2072
    Keywords: Paroxetine ; 5-Hydroxytryptamine uptake ; Radioligand binding ; Antidepressants ; Rats
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Paroxetine was shown to be a potent (K i =1.1 nM) and specific inhibitor of [3H]-5-hydroxytryptamine (5-HT) uptake into rat cortical and hypothalamic synaptosomes in vitro. Lineweaver-Burk kinetic analysis determined that this inhibition was competitive in nature, implying a direct interaction with the 5-HT uptake transporter complex. Oral administration of paroxetine produced a dose-related inhibition of [3H]-5-HT uptake (ED 50=1.9 mg/kg) into rat hypothalamic synaptosomes ex vivo with little effect on [3H]-l-noradrenaline (NA) uptake (ED 50〉30 mg/kg). This selectivity for 5-HT uptake was maintained after oral dosing for 14 days. Paroxetine (ED 50 1–3 mg/kg PO) prevented the 5-HT depleting effect of p-chloroamphetamine (PCA) in rat brain, demonstrating 5-HT uptake blockade in vivo. Radioligand binding techniques in rat brain in vitro showed that paroxetine has little affinity for α1, α2 or β adrenoceptors, dopamine (D2), 5-HT1, 5-HT2 or histamine (H1) receptors at concentrations below 1000 nM. Paroxetine demonstrated weak affinity for muscarinic receptors (K i =89 nM) but was at least 15 fold weaker than amitriptyline (K i =5.1 nM). Paroxetine, therefore, provides a useful pharmacological tool for investigating 5-HT systems and furthermore should be an antidepressant with reduced tricyclic-like side-effects.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 88 (1984), S. 164-172 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Rocks with boninitic affinities have been recognised in a number of “ophiolites”, including the Cambrian Heathcote and Mt Wellington Greenstone Belts of Victoria. Boninites and high-Mg andesites from the Heathcote Greenstone Belt show a restricted range of initial ɛ Nd values of between +3.3 to +5.8. Extremely refractory boninites from the Mt Wellington Greenstone Belt have ɛ Nd ranging from +1.3 to −9. Ti/Zr is positively correlated with Sm/Nd with the Heathcote lavas generally possessing greater depletion of Ti and enrichment of Zr relative to the middle and heavy REE with increasing LREE/HREE. These data are consistent with the generation of boninites by partial melting of refractory peridotite following invasion by LREE- and Zr-enriched, low ɛ Nd fluids. Tholeiites overlying the boninites in both greenstone belts have flat REE patterns and ɛ Nd∼+5, lower than that anticipated for lavas derived from depleted MORB source reservoirs in the Cambrian, suggesting that their source was also contaminated by a LREE-enriched, low ɛ Nd component similar to that involved in the generation of the Howqua boninites. The added components have characteristics compatible with their derivation from subducted altered oceanic crust and/or from wet subducted sediments. The identification of boninites and other low-Ti lavas in the Victorian greenstone belts is strong evidence for island arc development in southeastern Australia during the Lower Cambrian and provides further support for a subduction-related origin for many ophiolites.
    Type of Medium: Electronic Resource
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