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  • Abundance; Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biological sample; BIOS; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; DATE/TIME; Day of experiment; Entire community; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gullmar_fjord_2013; Gullmar Fjord, Skagerrak, Sweden; Identification; Mesocosm or benthocosm; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate; Salinity; Silicate; Stereomicroscopy (Leica); Temperate; Temperature, water; Treatment; Type  (1)
  • Aphanizomenon flos-aquae, biomass as carbon; Aphanizophyll; BIOACID; Biological Impacts of Ocean Acidification; Chaetoceros sp., biomass as carbon; DATE/TIME; Day of experiment; KOSMOS_2012_Tvaerminne; MESO; Mesocosm experiment; Mesocosm label; Nitrogen fixation rate; Phase; Skeletonema marinoi; δ15N  (1)
  • Hochschulschrift  (1)
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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (76 Seiten = 4 MB) , Illustration, Graphen, Karte
    Edition: 2020
    Language: German
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Paul, Allanah Joy; Achterberg, Eric Pieter; Bach, Lennart Thomas; Boxhammer, Tim; Czerny, Jan; Haunost, Mathias; Schulz, Kai Georg; Stuhr, Annegret; Riebesell, Ulf (2016): No observed effect of ocean acidification on nitrogen biogeochemistry in a summer Baltic Sea plankton community. Biogeosciences, 13(13), 3901-3913, https://doi.org/10.5194/bg-13-3901-2016
    Publication Date: 2024-03-06
    Description: Nitrogen fixation by filamentous cyanobacteria supplies significant amounts of new nitrogen (N) to the Baltic Sea. This balances N loss processes such as denitrification and anammox, and forms an important N source supporting primary and secondary production in N-limited post-spring bloom plankton communities. Laboratory studies suggest that filamentous diazotrophic cyanobacteria growth and N2-fixation rates are sensitive to ocean acidification, with potential implications for new N supply to the Baltic Sea. In this study, our aim was to assess the effect of ocean acidification on diazotroph growth and activity as well as the contribution of diazotrophically fixed N to N supply in a natural plankton assemblage. We enclosed a natural plankton community in a summer season in the Baltic Sea near the entrance to the Gulf of Finland in six large-scale mesocosms (volume ∼ 55m3) and manipulated fCO2 over a range relevant for projected ocean acidification by the end of this century (average treatment fCO2: 365–1231µatm).
    Keywords: Aphanizomenon flos-aquae, biomass as carbon; Aphanizophyll; BIOACID; Biological Impacts of Ocean Acidification; Chaetoceros sp., biomass as carbon; DATE/TIME; Day of experiment; KOSMOS_2012_Tvaerminne; MESO; Mesocosm experiment; Mesocosm label; Nitrogen fixation rate; Phase; Skeletonema marinoi; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 1870 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-03-15
    Description: Ocean acidification is considered as a crucial stressor for marine communities. In this study, we tested the effects of the IPCC RPC6.0 end-of-century acidification scenario on a natural plankton community in the Gullmar Fjord, Sweden, during a long-term mesocosm experiment from a spring bloom to a mid-summer situation. The focus of this study was on microzooplankton and its interactions with phytoplankton and mesozooplankton. The microzooplankton community was dominated by ciliates, especially small Strombidium sp., with the exception of the last days when heterotrophic dinoflagellates increased in abundance. We did not observe any effects of high CO2 on the community composition and diversity of microzooplankton. While ciliate abundance, biomass and growth rate were not affected by elevated CO2, we observed a positive effect of elevated CO2 on dinoflagellate abundances. Additionally, growth rates of dinoflagellates were significantly higher in the high CO2 treatments. Given the higher Chlorophyll a content measured under high CO2, our results point at mainly indirect effects of CO2 on microzooplankton caused by changes in phytoplankton standing stocks, in this case most likely an increase in small-sized phytoplankton of 〈8 μm. Overall, the results from the present study covering the most important part of the growing season indicate that coastal microzooplankton communities are rather robust towards realistic acidification scenarios.
    Keywords: Abundance; Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Biological sample; BIOS; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; DATE/TIME; Day of experiment; Entire community; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gullmar_fjord_2013; Gullmar Fjord, Skagerrak, Sweden; Identification; Mesocosm or benthocosm; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate; Salinity; Silicate; Stereomicroscopy (Leica); Temperate; Temperature, water; Treatment; Type
    Type: Dataset
    Format: text/tab-separated-values, 9769 data points
    Location Call Number Limitation Availability
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