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will likely further supplement this expansion of high-resolution records, providing
records with more robust low-frequency characteristics that can be combined with
proxies that are exceptionally good at capturing high-frequency climate variability
(e.g., Moberg et al. 2005 ) . In this way, the next decade of high-resolution paleo-
climatology will likely see paleoclimatic reconstructions with far less uncertainty,
covering more geographical regions, and providing meaningful estimates of climate
sensitivity before the 'Anthropocene'.
Acknowledgements I gratefully acknowledge the support of my research by the National Oceanic
and Atmospheric Administration (NOAA, NA050AR4311106), the National Science Foundation
(NSF, ATM-0402421), and the U.S. Department of Energy (DOE, DE-FG02-98ER62604).
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