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Abrupt Climate Change around 2,650 BP in North-West Europe: Evidence for Climatic Teleconnections and a Tentative Explanation

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Water, Environment and Society in Times of Climatic Change

Part of the book series: Water Science and Technology Library ((WSTL,volume 31))

Abstract

Natural variations in atmospheric 14C, which are expressed as wiggles in the radiocarbon calibration curve (Stuiver et al, 1993) severely limit the possibilities for fine-resolution dating of changes in vegetation and climate as recorded in lake deposits and raised bogs (e.g van Geel, 1978; Magny, 1993a; Barber et al, 1994). Van Geel and Mook (1989) stressed the importance of 14C Wiggle-Match Dating (WMD) of organic deposits, given that WMD can reveal relationships between 14C variations and short-term climatic fluctuations caused by solar and/or geomagnetic variations. Kilian et al (1995) have shown that, by using this strategy, raised-bog deposits in particular can be dated more precisely. Hence the raised-bog archive can be compared effectively with other proxy data archives, the more so because WMD has shown that an unexpected 14C reservoir effect plays a role in dating raised-bog deposits (individual conventional radiocarbon dates appear to be 100 to 250 years too old). Wiggle-matching is an elegant way of identifying this effect, and of estimating its magnitude.

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van Geel, B., Renssen, H. (1998). Abrupt Climate Change around 2,650 BP in North-West Europe: Evidence for Climatic Teleconnections and a Tentative Explanation. In: Issar, A.S., Brown, N. (eds) Water, Environment and Society in Times of Climatic Change. Water Science and Technology Library, vol 31. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3659-6_2

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