Articles | Volume 72, issue 2
https://doi.org/10.5194/egqsj-72-219-2023
https://doi.org/10.5194/egqsj-72-219-2023
Research article
 | 
14 Nov 2023
Research article |  | 14 Nov 2023

A 1100-year multi-proxy palaeoenvironmental record from Lake Höglwörth, Bavaria, Germany

Sudip Acharya, Maximilian Prochnow, Thomas Kasper, Linda Langhans, Peter Frenzel, Paul Strobel, Marcel Bliedtner, Gerhard Daut, Christopher Berndt, Sönke Szidat, Gary Salazar, Antje Schwalb, and Roland Zech

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Latest update: 12 Oct 2024
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Short summary
This study presents a palaeoenvironmental record from Lake Höglwörth, Bavaria, Germany. Before 870 CE peat deposits existed. Erosion increased from 1240 to 1380 CE, followed by aquatic productivity and anoxia from 1310 to 1470 CE. Increased allochthonous input and a substantial shift in the aquatic community in 1701 were caused by construction of a mill. Recent anoxia has been observed since the 1960s.