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  • Weitere Quellen  (5)
  • Nature Publishing Group  (5)
  • American Association for the Advancement of Science
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  • 1
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    Nature Publishing Group
    In:  Nature, 320 (6058). pp. 107-108.
    Publikationsdatum: 2016-03-01
    Materialart: Article , PeerReviewed
    Format: text
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  • 2
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    Nature Publishing Group
    In:  Nature, 288 (5788). pp. 260-263.
    Publikationsdatum: 2016-03-01
    Beschreibung: Organic detritus passing from the sea surface through the water column to the sea floor controls nutrient regeneration, fuels benthic life and affects burial of organic carbon in the sediment record. Particle trap systems have enabled the first quantification of this important process. The results suggest that the dominant mechanism of vertical transport is by rapid settling of rare large particles, most likely of faecal pellets or marine snow of the order of 〉200 μm in diameter, whereas the more frequent small particles have an insignificant role in vertical mass flux4–6. The ultimate source of organic detritus is biological production in surface waters of the oceans. I determine here an empirical relationship that predicts organic carbon flux at any depth in the oceans below the base of the euphotic zone as a function of the mean net primary production rate at the surface and depth-dependent consumption. Such a relationship aids in estimating rates of decay of organic matter in the water column, benthic and water column respiration of oxygen in the deep sea and burial of organic carbon in the sediment record.
    Materialart: Article , PeerReviewed
    Format: text
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  • 3
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    Nature Publishing Group
    In:  Nature, 387 . pp. 31-32.
    Publikationsdatum: 2017-02-28
    Materialart: Article , PeerReviewed
    Format: text
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  • 4
    Publikationsdatum: 2019-01-21
    Beschreibung: Circumpolar surface waters dominate the circulation of the Southern Ocean and sustain one of the ocean's largest standing stocks of biomass thereby producing a significant output of biogenic components, mainly diatoms, to the bottom sediments. Generally transit of biogenic matter from the sea surface to the sea floor affects nutrient regeneration fuels benthic life and transfers signals to the sediment record1–5. Reliable quantification of the relationship between biological production, fractionation of skeletal and tissue components and bottom sediment accumulation depends on direct vertical flux measurements from sediment trap deployments6–9, which have proved to be most scientifically productive10–13. We now present data on vertical mass fluxes from the Southern Ocean and evidence for strong biogeochemical fractionation between organic carbon-, nitrogen- and phosphorus-containing compounds, siliceous and calcareous skeletal remains, and refractory aluminosilicates.
    Materialart: Article , PeerReviewed
    Format: text
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  • 5
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    Nature Publishing Group
    In:  Nature, 333 (6168). pp. 17-18.
    Publikationsdatum: 2019-05-06
    Materialart: Article , PeerReviewed
    Format: text
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