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Late Holocene climatic history of northern Germany and Denmark: peat macrofossil investigations at Dosenmoor, Schleswig-Holstein, and Svanemose, Jutland
Authors:KEITH E BARBER  FRANK M CHAMBERS  DARREL MADDY
Institution:(e-mail: ), Palaeoecology Laboratory, Department of Geography, University of Southampton, Southampton SO 17 1BJ, UK;(e-mail: ), Centre for Environmental Change and Quaternary Research, GEMRU, University of Gloucestershire, Francis Close Hall, Swindon Road, Cheltenham GL50 4AZ, UK;(e-mail: ), Department of Geography, University of Newcastle, Newcastle upon Tyne NE1 7RU, UK
Abstract:Plant macrofossil remains have been analysed from two raised peat bogs in northern Germany and Denmark. The quantified vegetation reconstructions of each profile were subjected to multivariate analyses to extract records of changing bog surface wetness (BSW), which are interpreted in these rain-fed bogs as being proxy climate signals. Age/depth models were constructed using radiocarbon dates and a number of drier and wetter phases were defined. The records both register cooler/wetter conditions around 2700, 1800 and 1400 cal. yr BP, and at the beginning of the Little Ice Age around AD 1250–1350. These rising bog water tables must have been reflected in poorer conditions for agriculture, and in particular near Dosenmoor where the profile records a catastrophic change to such conditions culminating at 2750–2600 cal. yr BP.
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