Abstract
We studied high-resolution stratigraphy of phosphorus (P) forms in the Holocene sediments of large shallow Lake Peipsi (Estonia/Russia) in order to evaluate the lake ecosystem response to environmental changes and track the lake’s eutrophication history. We distinguished four main periods in the history of Lake Peipsi, each having likely different factors responsible for the distribution pattern of P fractions in the sediment record. We suggest that in the oldest period, from ca. 10.4 up to 7.3 cal ka BP, the sediment composition was mainly determined by rising water level, the second period dated 7.3–2.3 cal ka BP was governed mainly by stable hydrology and P loading, while the third period between 2.3 and 0 cal ka BP was primarily influenced by emerging anthropogenic impact. The sediments from the last period since 1950 are subject of ongoing diagenetic processes but still reflect rapid eutrophication of the lake. Comparison of the results with periods derived from other sediment proxies proved the usability of P fractions stratigraphy in reconstruction of the development of lakes.
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Acknowledgements
This research was financially supported by the Estonian Science Foundation (Grants Nos. 6741 and 7888), by the Estonian Ministry of Education and Research through institutional research funding (IUT21-2 and IUT1-8), by European Social Fund through “Mobilitas” postdoctoral grant MJD51, by the Doctoral School of Ecology and Environmental Sciences funded by EU, and by Swiss Grant for Programme “Enhancing public environmental monitoring capacities”.
We acknowledge the contribution from Siim Veski and Jüri Vassiljev at coring, sediment dating and advising during manuscript preparation. We also greatly appreciate the valuable suggestions, comments and corrections made by the editor and the anonymous reviewers of the manuscript.
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Kisand, A., Kirsi, AL., Ehapalu, K. et al. Development of large shallow Lake Peipsi (North-Eastern Europe) over the Holocene based on the stratigraphy of phosphorus fractions. J Paleolimnol 58, 43–56 (2017). https://doi.org/10.1007/s10933-017-9954-2
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DOI: https://doi.org/10.1007/s10933-017-9954-2