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  • Institut für Meereskunde Kiel  (2)
  • Nature Research  (1)
  • 1
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    Institut für Meereskunde Kiel
    Publikationsdatum: 2022-06-07
    Beschreibung: Denitrification rates were measured by the acetylene blockage method in the various sediment types occurring in Kiel Bight, namely sand, muddy sand, and mud, during the course of almost two years. Nitrate concentration in the sediments was found to be the major factor controlling denitrification. The source of the nitrate is nitrification in the sediments themselves. Nitrification there is mainly controlled by oxygen supply. In this way, the anaerobic process of denitrification indirectly requires oxygen. Anoxic muds have hence the lowest, oxic sands the highest denitrification rates. Effects of eutrophication like increased supply of nitrogen and organic matter to the sediments and the increased incidence of anoxia in the bottom water tend to reduce denitrification in such a situation.
    Materialart: Article , NonPeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    Institut für Meereskunde Kiel
    In:  Kieler Meeresforschungen - Sonderheft, 56 (S8). pp. 112-116.
    Publikationsdatum: 2018-07-24
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
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    Nature Research
    In:  Nature Communications, 10 (1). Art.Nr. 2805.
    Publikationsdatum: 2022-01-31
    Beschreibung: Oceanic anoxic events have been associated with warm climates in Earth history, and there are concerns that current ocean deoxygenation may eventually lead to anoxia. Here we show results of a multi-millennial global-warming simulation that reveal, after a transitory deoxygenation, a marine oxygen inventory 6% higher than preindustrial despite an average 3 °C ocean warming. An interior-ocean oxygen source unaccounted for in previous studies explains two thirds of the oxygen excess reached after a few thousand years. It results from enhanced denitrification replacing part of today’s ocean’s aerobic respiration in expanding oxygen-deficient regions: The resulting loss of fixed nitrogen is equivalent to an oceanic oxygen gain and depends on an incomplete compensation of denitrification by nitrogen fixation. Elevated total oxygen in a warmer ocean with larger oxygen-deficient regions poses a new challenge for explaining global oceanic anoxic events and calls for an improved understanding of environmental controls on nitrogen fixation.
    Materialart: Article , PeerReviewed
    Format: text
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    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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