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Do 15N Variations in Peat Bogs allow Statements of Climatic Changes in the Past?

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Palaeoclimatic Research and Models
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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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References

  1. Senstius, M.W., 1925. The formation of soils in equatorial regions, with special reference to Java. Amer. Soil Survey Assoc. Rpt. Bul. 6,1: 149–161.

    Google Scholar 

  2. Jenny, H., 1928. Relation of climatic Factors to the Amount of Nitrogen in Soils. J. Amer. Soc. Agron. 20: 900–912.

    Article  Google Scholar 

  3. Jenny, H., 1929. Relation of Temperature to the Amount of Nitrogen in Soils. Soils Science 27,3: 169–188.

    Article  Google Scholar 

  4. Aaby, B., 1976. Cyclic climatic variations in climate over the past 5500 yrs reflected in raised bogs. Nature 263: 281–284.

    Article  Google Scholar 

  5. Dansgaard, W., Johnsen, S.J., Reeh, N., Gundestrup, N., Clausen, H.B., Hammer, C.U., 1975. Climatic Changes, Norsemen and modern man. Nature 255: 24–28.

    Article  Google Scholar 

  6. La Marche Jr., V.C., 1974. Palaeoclimatic Inferences from Long Tree-Ring Records. Science 183: 1043–1048.

    Article  Google Scholar 

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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

  • eBook Packages: Springer Book Archive

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