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Testing the timing of radiocarbon-dated events between proxy archives

M. Blaauw

Centro de Investigación en Matemáticas, A.P. 402, 36000 Guanajuato, Mexico, Palaeobiology, Uppsala University, Geocentrum, Villavägen 16, SE-75236 Uppasala, Sweden, drieteenmeeuw{at}hotmail.com

J. A. Christen

Centro de Investigación en Matemáticas, A.P. 402, 36000 Guanajuato, Mexico

D. Mauquoy

Department of Geography and Environment, University of Aberdeen, Elphinstone Road, AB24 3UF Aberdeen, UK

J. van der Plicht

Centre for Isotope Research, University of Groningen, Nijenborgh 4, 9747 AG Groningen, The Netherlands

K. D. Bennett

Palaeobiology, Uppsala University, Geocentrum, Villavägen 16, SE-75236 Uppsala, Sweden, School of Geography, Archaeology and Palaeoecology, Queen’s University Belfast, Belfast BT7 1NN, UK

For interpreting past changes on a regional or global scale, the timings of proxy-inferred events are usually aligned with data from other locations. However, too often chronological uncertainties are ignored in proxy diagrams and multisite comparisons, making it possible for researchers to fall into the trap of sucking separate events into one illusionary event (or vice versa). Here we largely solve this ‘suck in and smear syndrome’ for radiocarbon (14C) dated sequences. In a Bayesian framework, millions of plausible age-models are constructed to quantify the chronological uncertainties within and between proxy archives. We test the technique on replicated high-resolution 14C-dated peat cores deposited during the ‘Little Ice Age’ (c. AD 1400-1900), a period characterized by abrupt climate changes and severe 14C calibration problems. Owing to internal variability in proxy data and uncertainties in age-models, these (and possibly many more) archives are not consistent in recording decadal climate change. Through explicit statistical tests of palaeoenvironmental hypotheses, we can move forward to systematic interpretations of proxy data. However, chronological uncertainties of non-annually resolved palaeoclimate records are too large for answering decadal timescale questions.

Key Words: Bayesian age-modelling • radiocarbon • chronological uncertainty • meta-analysis • synchronicity of events • ‘Little Ice Age’

The Holocene, Vol. 17, No. 2, 283-288 (2007)
DOI: 10.1177/0959683607075857


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