Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU),
Department of Geography and Geosciences, GeoZentrum Nordbayern,
Schlossgarten 5, 91054 Erlangen, Germany
Michael Seewald
Helmholtz Centre for Environmental Research-UFZ, Brueckstrasse 3a,
39114 Magdeburg, Germany
Karsten Rinke
Helmholtz Centre for Environmental Research-UFZ, Brueckstrasse 3a,
39114 Magdeburg, Germany
Kurt Friese
Helmholtz Centre for Environmental Research-UFZ, Brueckstrasse 3a,
39114 Magdeburg, Germany
Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU),
Department of Geography and Geosciences, GeoZentrum Nordbayern,
Schlossgarten 5, 91054 Erlangen, Germany
Jakob Schmidmeier
Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU),
Department of Geography and Geosciences, GeoZentrum Nordbayern,
Schlossgarten 5, 91054 Erlangen, Germany
Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU),
Department of Geography and Geosciences, GeoZentrum Nordbayern,
Schlossgarten 5, 91054 Erlangen, Germany
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Organic matter (OM) turnover into dissolved inorganic carbon (DIC) was investigated by means of carbon isotope mass balances in Germany's largest water reservoir. This includes a metalimnetic oxygen minimum (MOM). Autochthonous particulate organic carbon (POC) was the main contributor to DIC, with rates that were highest for the MOM. Generally low turnover rates outline the environmental fragility of this water body in the case that OM loads increase due to storm events or land use changes.
Organic matter (OM) turnover into dissolved inorganic carbon (DIC) was investigated by means of...
