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Duvensee archaeological sites
The Duvensee archaeological sites ((ドイツ語:Duvenseer Wohnplätze)) are a series of early Mesolithic archaeological sites that are located within the Duvensee bog near Duvensee in Schleswig Holstein, Germany. The bog is one of the oldest and well-researched archaeological settlement areas from the early Holocene in Central Europe. The archaeological sites are renowned for their well-preserved organic remains and are of great importance in understanding the subsistence and settlement strategies of post-glacial hunter-gatherer societies. Recent research has explored the Duvensee societies' diet and land use patterns in relation to the evolution of modern lifestyles and nutrition.〔Holst, D. 2007. ''Subsistenz und Landschaftsnutzung im Frühmesolithikum: Nußröstplätze am Duvensee''. PhD dissertation, Johannes Gutenberg Universität Mainz.〕〔Holst, D. 2009. Eine einzige Nuss rappelt nicht im Sacke. Subsistenzstrategien in der Mittelsteinzeit. ''Mitteilungen der Gesellschaft für Urgeschichte 18'': 11-38.〕〔Holst, D. 2010. Hazelnut economy of early Holocene hunter-gatherers: A case study from Mesolithic Duvensee, northern Germany. ''Journal of Archaeological Science 37'': 2871-2880.〕
==Location and Preservation==
The Duvensee bog is located at the edge of the Duvensee municipality in the Herzogtum Lauenburg district in the southern part of Schleswig-Holstein. The bog formed from a paludifying lake that originated as a kettle hole during the early pre-boreal and once covered an area of more than 4 square kilometres. Siltation set in during the late pre-boreal and the lake was (intentionally) drained in its entirety during the 19th century.〔Funck, H. 1963. Die Entwässerung des Duvensees. ''Schriftenreihe des Heimatbund und Geschichtsvereins Herzogtum Lauenburg 10''. Kommissionsverlag E. Werner, Mölln.〕
The north-western banks of the lake served as areas for human activity during the early Mesolithic. On two peninsulas the remains of small to medium-sized sites in close vicinity to one another were found.
With increasing paludification, which is thought to have set in during the periods of occupation, the sites were covered and protected by thick layers of peat and survive in excellent condition.〔Bokelmann, K. 1971: Duvensee, ein Wohnplatz des Mesolithikums in Schleswig-Holstein und die Duvenseegruppe. ''Offa'' 28: 5-26〕〔Bokelmann, K., F. R. Averdieck and H. Willkomm. 1981: Duvensee, Wohnplatz 8. Neue Aspekte zur Sammelwirtschaft im frühen Mesolithikum. ''Offa'' 38: 21-40〕 Due to increased peat harvesting during the 19th and 20th centuries, the as yet unexcavated portions are now close to the surface and no longer protected by this natural cover.
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