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Nutrient availability affected shallow-lake ecosystem response along the Late-Glacial/Holocene transition

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Abstract

Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.

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Acknowledgements

The authors would like to thank Petr Kuneš, Jan Hošek, Linda Nedbalová and Hana Rajdlová for consultation and important comments. We also thank two anonymous reviewers whose comments substantially improved the manuscript. This project was supported by the Czech Science Foundation (GAČR 17-05935S, GAČR 19-05791S) and the Ministry of Education Youth and Sports of the Czech Republic (Project No. CZ.1.07/2.3.00/20.0289–PAPAVER).

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Tichá, A., Bešta, T., Vondrák, D. et al. Nutrient availability affected shallow-lake ecosystem response along the Late-Glacial/Holocene transition. Hydrobiologia 846, 87–108 (2019). https://doi.org/10.1007/s10750-019-04054-7

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