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In this dataset, we measured oyster growth in response to increased temperature and fish thermal plasticity measured as final - initial weight (wet weight) of individuals in a mesocosm experiment conducted in 2019 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured nutrients (PO4, NOs, NH4, chlorophyll-a) in response to increased temperature and fish thermal plasticity. Measured weekly (between 19.05.2017 - 18.08.2017) from water samples taken within each mesocosm at the AWISOM mesocosm facility of the Wadden Sea Station Sylt. Nutrient levels were analyzed with an AutoAnalyzer3 (SEAL Analytical, Norderstedt, Germany). Chlorophyll-a was measured using a bbe AlgaeLabAnalyser (bbe Moldaenke, Schwentinental, Germany)
In this dataset, we measured nutrients (PO4, NOs, NH4, chlorophyll-a) in response to increased temperature and fish thermal plasticity. Measured weekly (between 06.06.2019 - 26.08.2019) from water samples taken within each mesocosm at the AWISOM mesocosm facility of the Wadden Sea Station Sylt. Nutrient levels were analyzed with an AutoAnalyzer3 (SEAL Analytical, Norderstedt, Germany). Chlorophyll-a was measured using a bbe AlgaeLabAnalyser (bbe Moldaenke, Schwentinental, Germany).
In this dataset, we measured epiphyte biomass accumulation in response to increased temperature and fish thermal plasticity measured as total accumulated weight (ash free dry mass) over the course of the mesocosm experiment conducted in 2019 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured epiphyte biomass accumulation in response to increased temperature and fish thermal plasticity measured as total accumulated weight (ash free dry mass) over the course of the mesocosm experiment conducted in 2017 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured copepod abundance in response to increased temperature and fish thermal plasticity estimated as the total number of copepods (count) identified throughout the mesocosm experiment conducted in 2019 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured copepod abundance in response to increased temperature and fish thermal plasticity estimated as the total number of copepods (count) identified throughout the mesocosm experiment conducted in 2017 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured oyster growth in response to increased temperature and fish thermal plasticity measured as final - initial weight (wet weight) of individuals in a mesocosm experiment conducted in 2017 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
In this dataset, we measured mussel growth in response to increased temperature and fish thermal plasticity measured as final - initial weight (wet weight) of individuals in a mesocosm experiment conducted in 2019 at the AWISOM mesocosm facility of the Wadden Sea Station Sylt.
We analyzed concentrations of dissolved and particulate trace metals, including iron (Fe), manganese (Mn), vanadium (V), molybdenum (Mo), thallium (Tl), and rare earth elements (REE), during a mesocosm-based phytoplankton summer bloom mimicking the intertidal zone of the southern North Sea (Jade Bay). The studies aimed to identify key drivers controlling their biogeochemical cycling in dynamic, high-productivity coastal environments. Our results highlight the tidally influenced coastal zone as a critical interface that alters the behavior of supposedly conservative elements such as Mo and Tl (Mori et al., 2021) as well as natural and anthropogenic REE (incl., lanthanum, samarium, and gadolinium) (Mori et al., 2026). Trace metal concentrations and shale-normalized REE patterns, determined by quadrupole inductively coupled plasma–mass spectrometry (ICP-MS) and inductively coupled plasma–optical emission spectrometry (ICP-OES), were combined with biogeochemical bulk parameters and pigment-based assessments of phytoplankton growth and community composition (Mustaffa et al., 2020). Trace metal and REE cycling were evaluated in relation to phytoplankton dynamics, particulate organic matter composition (C, N, P), dissolved organic carbon, total dissolved nitrogen, and macronutrient concentrations (nitrate, ammonium, silicate, and inorganic phosphate). The dataset was obtained during a Planktotron-based mesocosm experiment conducted within the framework of the Coastal Ocean Darkening project (Mustaffa et al., 2020).
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