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Reconstruction of the recent history of a large deep prealpine lake (Lake Bourget, France) using subfossil chironomids, diatoms, and organic matter analysis: towards the definition of a lake-specific reference state

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Abstract

This paper presents the recent history of a large prealpine lake (Lake Bourget) using chironomids, diatoms and organic matter analysis, and deals with the ability of paleolimnological approach to define an ecological reference state for the lake in the sense of the European Framework Directive. The study at low resolution of subfossil chironomids in a 4-m-long core shows the remarkable stability over the last 2.5 kyrs of the profundal community dominated by a Micropsectra-association until the beginning of the twentieth century, when oxyphilous taxa disappeared. Focusing on this key recent period, a high resolution and multiproxy study of two short cores reveals a progressive evolution of the lake’s ecological state. Until AD 1880, Lake Bourget showed low organic matter content in the deep sediments (TOC less than 1%) and a well-oxygenated hypolimnion that allowed the development of a profundal oxyphilous chironomid fauna (Micropsectra-association). Diatom communities were characteristic of oligotrophic conditions. Around AD 1880, a slight increase in the TOC was the first sign of changes in lake conditions. This was followed by a first limited decline in oligotrophic diatom taxa and the disappearance of two oxyphilous chironomid taxa at the beginning of the twentieth century. The 1940s were a major turning point in recent lake history. Diatom assemblages and accumulation of well preserved planktonic organic matter in the sediment provide evidence of strong eutrophication. The absence of profundal chironomid communities reveals permanent hypolimnetic anoxia. From AD 1995 to 2006, the diatom assemblages suggest a reduction in nutrients, and a return to mesotrophic conditions, a result of improved wastewater management. However, no change in hypolimnion benthic conditions has been shown by either the organic matter or the subfossil chironomid profundal community. Our results emphasize the relevance of the paleolimnological approach for the assessment of reference conditions for modern lakes. Before AD 1900, the profundal Micropsectra-association and the Cyclotella dominated diatom community can be considered as the Lake Bourget reference community, which reflects the reference ecological state of the lake.

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Acknowledgments

The authors express their sincere thanks to Roberto Quinlan, Clément Laplaige, Damien Rius, John Olsen and Bianca Perren for their help in the writing and preparation of the manuscript. The comments of Isabelle Larocque and two anonymous reviewers are gratefully acknowledged.

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Authors and Affiliations

  1. Laboratoire de Chrono-Environnement, UMR 6249 CNRS, UFR Sciences et Techniques, Université de Franche-Comté, 25030, Besançon Cedex, France

    Laurent Millet & Valérie Verneaux

  2. Laboratoire EDYTEM, UMR 5204 CNRS, CISM, Université de Savoie, 73376, Le Bourget du Lac Cedex, France

    Charline Giguet-Covex & Fabien Arnaud

  3. Laboratoire CARRTEL, UMR INRA, Station d’Hydrobiologie Lacustre, 75 avenue de Corzent, BP 511, 74203, Thonon-les-Bains Cedex, France

    Jean-Claude Druart

  4. Institut de Géologie et Paléontologie, Université de Lausanne Anthropôle, CH-1015, Lausanne, Switzerland

    Thierry Adatte

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  1. Laurent Millet
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Correspondence to Laurent Millet.

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Millet, L., Giguet-Covex, C., Verneaux, V. et al. Reconstruction of the recent history of a large deep prealpine lake (Lake Bourget, France) using subfossil chironomids, diatoms, and organic matter analysis: towards the definition of a lake-specific reference state. J Paleolimnol 44, 963–978 (2010). https://doi.org/10.1007/s10933-010-9467-8

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