Abstract
Lacustrine sediments have been widely used to investigate past climatic and environmental changes on millennial to seasonal time scales. Sedimentary archives of lakes in mountainous regions may also record non-climatic events such as earthquakes. We argue herein that a set of 64 annual laminae couplets reconciles a stratigraphically inconsistent accelerator mass spectrometry (AMS) 14C chronology in a ~4-m-long sediment core from Lake Mengda, in the north-eastern Tibetan Plateau. The laminations suggest the lake was formed by a large landslide, triggered by the 1927 Gulang earthquake (M = 8.0). The lake sediment sequence can be separated into three units based on lithologic, sedimentary, and isotopic characteristics. Starting from the bottom of the sequence, these are: (1) unweathered, coarse, sandy valley-floor deposits or landslide debris that pre-date the lake, (2) landslide-induced, fine-grained soil or reworked landslide debris with a high organic content, and (3) lacustrine sediments with low organic content and laminations. These annual laminations provide a high-resolution record of anthropogenic and environmental changes during the twentieth century, recording enhanced sediment input associated with two phases of construction activities. The high mean sedimentation rates of up to 4.8 mm year−1 underscore the potential for reconstructing such distinct sediment pulses in remote, forested, and seemingly undisturbed mountain catchments.
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Acknowledgments
The authors thank Bo Yang (Institute of Salt Lakes, CAS, Xi’ning) for his help during fieldwork. Special thanks go to Elisabeth Dietze and Kai Hartmann (Free University Berlin) for providing the unpublished End-Member Modeling script. Benjamin Bekeschus, Christiane Funk, Janina Stapel and Liv Heinecke (AWI-Potsdam & University Potsdam) are acknowledged for their assistances with laboratory analyses. We are grateful to Jan Blöthe (University Potsdam) for his guidance in extracting topographic data. Y. Wang’s doctoral research was funded by the “Helmholtz—China Scholarship Council (CSC) Young Scientist Fellowship” (No. 2008491101). The research was supported by the German Research Foundation (Deutsche Forschungsgemeinschaft DFG). The authors appreciate Steffen Mischke (editor), Mark Brenner (editor-in-chief), Torsten Haberzettl and one anonymous reviewer for their constructive suggestions on our manuscript.
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Wang, Y., Herzschuh, U., Liu, X. et al. A high-resolution sedimentary archive from landslide-dammed Lake Mengda, north-eastern Tibetan Plateau. J Paleolimnol 51, 303–312 (2014). https://doi.org/10.1007/s10933-012-9666-6
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DOI: https://doi.org/10.1007/s10933-012-9666-6