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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In September-November 1994, the Ocean Drilling Program Leg 158 drilled a series of holes into a large hydrothermally active mound in the TAG hydrothermal field located at a water depth of 3,650 m on the eastern side of the median valley of the Mid-Atlantic Ridge at 26° 08' ...
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 333 (1988), S. 64-66 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The sulphides in the TAG hydrothermal field occur in a mound -220 m by 250 m across and up to 50 m in height. A temperature of 305 °C for discharging hydrothermal field was measured with a temperature probe in one active chimney at the summit of the mound during operations with the research ...
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  • 3
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    Nature Publishing Group
    In:  Nature, 333 (6168). pp. 64-66.
    Publication Date: 2014-04-25
    Type: Article , PeerReviewed
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  • 4
    Publication Date: 2014-02-11
    Description: The concentration of sulphate in today’s oceans—approximately 28,000 μmol l−1—is maintained by a balance between removal by pyrite burial and evaporite deposition and supply by oxidative weathering and the erosion of sulphate minerals from evaporites1. Oceanic sulphate concentrations were much lower before the rise of atmospheric oxygen about 2.4 Gyr ago2. The limited spread of δ34S values in sedimentary sulphides from 3.85 to 2.5 Gyr ago suggests that microbial sulphate reduction, if it played an important role in the Archaean marine sulphur cycle, must have occurred at sulphate concentrations of 200 μmol l−1 or less3. Here we use sulphur isotope systematics of the 2.7 Gyr old volcanogenic massive sulphide ore deposits from Kidd Creek, Ontario, to provide constraints on seawater sulphate concentrations independent of biological considerations. By comparing these values with metal and sulphur budgets from modern hydrothermal settings, we estimate that seawater sulphate concentrations 2.7 Gyr ago were roughly 80 μmol l−1. At these levels, the residence time of sulphate was on the order of 200,000 years, sufficiently long to make sulphate a conservative compound in the open ocean, but still short enough to suggest that hydrothermal sulphur fluxes were accompanied by a globally significant sink associated with microbial sulphate reduction.
    Type: Article , PeerReviewed
    Format: text
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  • 5
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    International Seabed Authority
    In:  In: Polymetallic Massive Sulphides and Cobalt-Rich Ferromanganese Crusts: Status and Prospects. ISA Technical Study, 2 . International Seabed Authority, Kingston, Jamaica, pp. 7-35. ISBN 976-610-467-0
    Publication Date: 2016-06-22
    Description: Since 1979, polymetallic massive sulphide deposits have been found at water depths up to 3,700 m in a variety of tectonic settings at the modern seafloor including mid-ocean ridges, back-arc rifts, and seamounts. Many of the sulphide deposits consist of a black smoker complex on top of a sulphide mound which commonly is underlain by a stockwork zone. It has been widely established that circulating seawater which is modified in a reaction zone close to a subaxial magma chamber is the principal carrier of metals and sulphur which are leached out of the oceanic basement. Precipitation of massive and stockwork sulphides at and beneath the seafloor takes place in response to mixing of the hightemperature (up to 400°C) metal-rich hydrothermal seawater fluid with ambient seawater. Polymetallic seafloor sulphide deposits can reach a considerable size (up to 100 million tonnes) and often carry high concentrations of copper (chalcopyrite), zinc (sphalerite), and lead (galena) in addition to gold and silver. Extremely high concentrations of gold have recently been found in a new type of seafloor mineral deposit previously only known as epithermal (magmatic) gold deposits on the continents. Due to the high concentration of base and precious metals, seafloor polymetallic sulphide deposits have recently attracted the interest of the international mining industry. The recovery of those deposits appears to be both economically and environmentally feasible due to certain advantages over land-based deposits and will likely become reality within this decade. For logistical and technical reasons, future mining operations will largely focus on deposits in national rather than international waters.
    Type: Book chapter , NonPeerReviewed
    Format: text
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