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  • Hochschulschrift  (2)
  • Amino acids, dissolved hydrolyzable; Arctic Ocean, Central Basin; ARK-XXVII/3; Bacteria; BIOACID; Biological Impacts of Ocean Acidification; Carbon, organic, dissolved; Coomassie stainable particles; CT; DATE/TIME; DEPTH, water; Description; Event label; ICE; Ice station; Ice station #1; Ice station #2; LATITUDE; LONGITUDE; Polarstern; PS80/224-1; PS80/237-1; PS80/3-track; PS80 IceArc; Salinity; Sample code/label; Site; Slope ratio; Transparent exopolymer particles; Underway cruise track measurements; Uronic acids, dissolved  (1)
Document type
Keywords
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Language
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  • 1
    Keywords: Hochschulschrift
    Description / Table of Contents: Bacteria, Organic matter, Extracellular enzymes, Degradation, Carbon cycle, Global Change. - Anthropogenic emissions have increased the concentration of carbon dioxide (CO2) during the last 200 years. Since radiative forcing by greenhouse gases plays an essential role in maintaining the Earth's temperature, increasing emissions resulted in an observed warming of the atmosphere and the ocean. Furthermore, the absorption of excess atmospheric CO2 by the ocean has increased the acidity of seawater at global scale. The experimental simulation of changes in seawater temperature and CO2 projected for the near future led to a substantial acceleration of organic matter degradation. Higher degradation rates were primarily induced by temperature and pH effects on bacterial extracellular enzymes that increased rates of polymer hydrolysis. Effects of changing ocean temperature and pH on bacterial activity and the consequences for the cycling of organic matter are highly relevant for marine organic carbon fluxes and the ocean-atmosphere CO2 exchange.
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 201 S., 2,7 MB)
    DDC: 577.7144
    Language: English
    Note: Bremen, Univ., Diss., 2009
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  • 2
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (102 Blatt = 7 MB) , Illustrationen, Diagramme, Karten
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 3
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    PANGAEA
    In:  Supplement to: Galgani, Luisa; Piontek, Judith; Engel, Anja (2016): Biopolymers form a gelatinous microlayer at the air-sea interface when Arctic sea ice melts. Scientific Reports, 6, 29465, https://doi.org/10.1038/srep29465
    Publication Date: 2023-05-12
    Description: The interface layer between ocean and atmosphere is only a couple of micrometers thick but plays a critical role in climate relevant processes, including the air-sea exchange of gas and heat and the emission of primary organic aerosols (POA). Recent findings suggest that low-level cloud formation above the Arctic Ocean may be linked to organic polymers produced by marine microorganisms. Sea ice harbors high amounts of polymeric substances that are produced by cells growing within the seaice brine. Here, we report from a research cruise to the central Arctic Ocean in 2012. Our study shows that microbial polymers accumulate at the air-sea interface when the sea ice melts. Proteinaceous compounds represented the major fraction of polymers supporting the formation of a gelatinous interface microlayer and providing a hitherto unrecognized potential source of marine POA. Our study indicates a novel link between sea ice-ocean and atmosphere that may be sensitive to climate change.
    Keywords: Amino acids, dissolved hydrolyzable; Arctic Ocean, Central Basin; ARK-XXVII/3; Bacteria; BIOACID; Biological Impacts of Ocean Acidification; Carbon, organic, dissolved; Coomassie stainable particles; CT; DATE/TIME; DEPTH, water; Description; Event label; ICE; Ice station; Ice station #1; Ice station #2; LATITUDE; LONGITUDE; Polarstern; PS80/224-1; PS80/237-1; PS80/3-track; PS80 IceArc; Salinity; Sample code/label; Site; Slope ratio; Transparent exopolymer particles; Underway cruise track measurements; Uronic acids, dissolved
    Type: Dataset
    Format: text/tab-separated-values, 567 data points
    Location Call Number Limitation Availability
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