Preprints
https://doi.org/10.5194/bg-2022-154
https://doi.org/10.5194/bg-2022-154
 
19 Jul 2022
19 Jul 2022
Status: this preprint is currently under review for the journal BG.

Mineralization of autochthonous particulate organic carbon is a fast channel of organic matter turnover in Germany’s largest drinking water reservoir

Marlene Dordoni1, Michael Seewald2, Karsten Rinke2, Robert van Geldern1, Jakob Schmidmeier1, and Johannes A. C. Barth1 Marlene Dordoni et al.
  • 1Friedrich- Alexander-Universität Erlangen-Nürnberg (FAU), Department of Geography and Geosciences, GeoZentrum Nordbayern, Schlossgarten 5, Erlangen, 91054, Germany
  • 2Helmholtz Centre for Environmental Research-UFZ, Brueckstrasse 3a, D-39114, Magdeburg, Germany

Abstract. Turnover of organic matter (OM) is an essential ecological function in inland water bodies and relevant for water quality especially for the potential of dissolved organic carbon (DOC) removal as well as due to emissions of CO2. We investigated various sources of OM including DOC, autochthonous particulate organic carbon (POC), allochthonous particulate organic carbon (ExtPOC), and sedimentary matter (SED) in a temperate drinking water reservoir (Rappbode Reservoir, Germany) with respect to carbon isotope ratios and concentration dynamics. For this purpose, we focused on the metalimnion and the hypolimnion, where respiratory turnover is expected to be dominant and hardly disturbed by atmospheric exchange. The observation period of nine months covered a complete stratification period of the water body. Dissolved inorganic carbon (DIC) concentrations and its isotopes (δ13CDIC) were considered together with isotope data of DOC and POC (δ13CDOC and δ13CPOC) as input parameters for mass balances. DIC concentrations ranged between 0.30 and 0.53 mmol L-1, while δ13CDIC values were between -15.1 and -7.2 ‰ versus the VPDB (Vienna PeeDee Belemnite) standard. Values of δ13CDOC and δ13CPOC ranged between -28.8 and -27.6 ‰ and between -35.2 and -26.8 ‰, respectively. Isotope compositions of sedimentary material and allochthonous POC were inferred from the literature with average values of δ13CSED = -30.7 ‰, and δ13CExtPOC = -31.8 ‰. Comparison of DIC concentration gains and stable isotope mass balances showed that autochthonous POC from primary producers was the main contributor to DIC increases, while contributions from DOC, ExtPOC and SED played a minor role. OM turnover rates, i.e. the conversion of organic carbon towards DIC, calculated with our isotope approach were within the range for oligotrophic water bodies (0.01 to 1.3 µmol L-1 d-1). Some higher values in the metalimnion are likely due the availability of settling POC from the photic zone. Samples from a Metalimnetic Oxygen Minimum (MOM) showed a clear dominance of respiration over photosynthesis through bacterial degradation of autochthonous POC. These high turnover rates further highlight a close link with planktonic biological assemblages. Our work shows that respiration in temperate lentic water bodies largely depends on autochthonous POC production as a major carbon source.

Marlene Dordoni et al.

Status: open (until 30 Aug 2022)

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  • RC1: 'Comment on bg-2022-154', Anonymous Referee #1, 14 Aug 2022 reply

Marlene Dordoni et al.

Marlene Dordoni et al.

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Short summary
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 case OM loads increase by storm events or land use changes.
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