Recycling and deposition of inorganic carbon from calcium carbonate encrustations of charophytes

Author:

Strzałek Małgorzata1ORCID,Kufel Lech1ORCID,Apolinarska Karina2ORCID,Becher Marcin3ORCID,Biardzka Elżbieta1,Brzozowski Michał4ORCID,Kiełczewski Rafał2ORCID,Kowalewski Grzegorz5ORCID,Pukacz Andrzej6ORCID,Woszczyk Michał7ORCID,Pełechaty Mariusz8ORCID

Affiliation:

1. University of Siedlce, Faculty of Sciences, Institute of Biological Sciences Siedlce Poland

2. Adam Mickiewicz University, Institute of Geology Poznań Poland

3. University of Siedlce, Faculty of Agricultural Sciences, Institute of Agriculture and Horticulture Siedlce Poland

4. Department of Ecosystem Research Leibniz Institute of Freshwater Ecology and Inland Fisheries (IGB) Berlin Germany

5. Adam Mickiewicz University, Faculty of Geographical and Geological Sciences, Institute of Geoecology and Geoinformation Poznań Poland

6. Adam Mickiewicz University, Collegium Polonicum Słubice Poland

7. Adam Mickiewicz University, Faculty of Geographical and Geological Sciences, Biogeochemistry Research Unit Poznań Poland

8. Department of Hydrobiology Faculty of Biology, Adam Mickiewicz University Poznań Poland

Abstract

AbstractMany aquatic primary producers can use bicarbonates as a carbon source for photosynthesis. Charophytes of the two genera: Chara and Nitellopsis are quite efficient in this process. Some species of these macroalgae produce carbonate encrustations, mainly calcium carbonate, constituting up to 86% of the summer maximum dry weight of the standing crop. In this study, we analyzed the fate of inorganic carbon accumulated this way in Chara spp. and Nitellopsis obtusa from six Polish lakes located in two regions (warmer W Poland and cooler NE Poland). Our study distinguished two groups of charophyte species that differed in the way of CaCO3 release from their summer standing crops. On average, the corticate Chara rudis and C. tomentosa belonging to the first group were less efficient in depositing CaCO3 from summer to autumn than the less corticate C. contraria and ecorticate N. obtusa of the second group. The latter two species were more efficient in inorganic carbon burial in sediments. On the contrary, dissolution of encrustation was more typical of the first species group and was facilitated by decreasing the pH and saturation index of calcite in lake water. The final output of CaCO3 loss mainly resulted from combined species‐specific features, lake water properties and overwintering patterns. Our study revealed that inorganic carbon cycling through charophytes involves burial and dissolution and is more complex than previously thought.

Publisher

Wiley

Subject

Aquatic Science,Oceanography

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