@article {339,
	title = {Persistent solar influence on North Atlantic climate during the Holocene},
	journal = {Science},
	volume = {294},
	year = {2001},
	note = {id: 1397; Bond, G Kromer, B Beer, J Muscheler, R Evans, M N Showers, W Hoffmann, S Lotti-Bond, R Hajdas, I Bonani, G New York, N.Y. Science. 2001 Dec 7;294(5549):2130-6. Epub 2001 Nov 15.},
	pages = {2130-6},
	abstract = {Surface winds and surface ocean hydrography in the subpolar North Atlantic appear to have been influenced by variations in solar output through the entire Holocene. The evidence comes from a close correlation between inferred changes in production rates of the cosmogenic nuclides carbon-14 and beryllium-10 and centennial to millennial time scale changes in proxies of drift ice measured in deep-sea sediment cores. A solar forcing mechanism therefore may underlie at least the Holocene segment of the North Atlantic{\textquoteright}s "1500-year" cycle. The surface hydrographic changes may have affected production of North Atlantic Deep Water, potentially providing an additional mechanism for amplifying the solar signals and transmitting them globally.},
	issn = {0036-8075 (Print) 0036-8075 (Linking)},
	doi = {10.1126/science.1065680},
	author = {Bond, G. and Kromer, B. and Beer, J. and Muscheler, R. and Evans, M. N. and Showers, W. and Hoffmann, S. and Lotti-Bond, R. and Hajdas, I. and Bonani, G.}
}
