Lake sediment records are underrepresented in comprehensive, quantitative, high-resolution (sub-decadal), multi-proxy climate reconstructions for the past millennium. This is largely a consequence of the difficulty of calibrating biogeochemical lake sediment proxies to meteorological time series (calibration-in-time). Thanks to recent methodological advances, it is now possible. This paper outlines a step-by-step, specifically tailored methodology, with practical suggestions for calibrating and validating biogeochemical proxies from lake sediments to meteorological data. This approach includes: (1) regional climate data; (2) site selection; (3) coring and core selection; (4) core chronology; (5) data acquisition; and (6) data analysis and statistical methods. We present three case studies that used non-varved lake sediments from remote areas in the Central Chilean Andes, where little a priori information was available on the local climate and lakes, or their responses to climate variability. These case studies illustrate the potential value and application of a calibration-in-time approach to non-varved lake sediments for developing quantitative, high-resolution climate reconstructions. © 2012 Springer Science+Business Media B.V.
CITATION STYLE
von Gunten, L., Grosjean, M., Kamenik, C., Fujak, M., & Urrutia, R. (2012). Calibrating biogeochemical and physical climate proxies from non-varved lake sediments with meteorological data: Methods and case studies. Journal of Paleolimnology, 47(4), 583–600. https://doi.org/10.1007/s10933-012-9582-9
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