Abstract
A peat bog from the northern part of Germany (near Stade) has been investigated down to a depth of 440 cm. The 15N content of the organic material exhibits distinct variations ranging from about -4.5 to +4.5 %o. The results suggest that a correlation exists between these 15N variations and the climatic conditions which prevailed above the peat area during the formation of its organic material. A statistical analysis yields cyclic variations with periodicities of about 170, 280 and 1000 years over the past 4500 years, indicating that similar climatic conditions occurend within these intervals.
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© 1983 ECSC, EEC, EAEC, Brussels and Luxembourg
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Schleser, G.H. (1983). Do 15N Variations in Peat Bogs allow Statements of Climatic Changes in the Past?. In: Ghazi, A. (eds) Palaeoclimatic Research and Models. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7236-0_15
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DOI: https://doi.org/10.1007/978-94-009-7236-0_15
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-009-7238-4
Online ISBN: 978-94-009-7236-0
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