@article {998,
	title = {Were Rhyolitic Glasses in the Vedde Ash and in the North Atlantic{\textquoteright}s Ash Zone 1 produced by the Same Volcanic Eruption?},
	journal = {Quaternary Science Reviews},
	volume = {20},
	year = {2001},
	note = {id: 253},
	pages = {118-1199},
	abstract = {New evidence from North Atlantic deep-sea sediment cores suggests that rhyolitic glass shards in Ash Zone 1 and in the Vedde Ash may not have been produced by the same eruption as has been widely assumed. Our argument is based on (1) a marine ice-rafted deposit approximately 1000 years older than the Vedde Ash contains rhyolitic shards with the same major element chemistry as the Vedde Ash itself and (2) coincidence of Ash Zone 1 with an abrupt increase in discharge of glacial icebergs into the North Atlantic. Hence, we cannot rule out the possibility that Vedde-like rhyolitic glasses were erupted onto Icelandic glaciers before eruption of the Vedde Ash, stored in the glacial ice, then dispersed by icebergs into the North Atlantic and deposited partly or entirely as Ash Zone 1. While not disproving that Ash Zone 1 and the Vedde Ash came from the same eruption, our findings indicate that further study is needed to establish the exact relation between the two ash deposits.},
	doi = {10.1016/S0277-3791(00)00146-3},
	author = {Bond, G. C. and Mandeville, C. and Hoffmann, S.}
}
@inbook {1388,
	title = {The North Atlantic{\textquoteright}s 1-2 kyr climate rhythm: Relation to Heinrich events, Dansgaard/Oeschger cycles and the Little Ice Age (Book Section)},
	booktitle = {Mechanisms of global climate change at mellennial time scales},
	series = {Geophysical Monograph Series 112},
	year = {1999},
	note = {id: 216},
	month = {1999},
	pages = {35-58},
	author = {Bond, G. C. and Showers, W. and Elliot, M. and Evans, M. and Lotti, R. and Hajdas, I. and Bonani, G. and Johnson, S.},
	editor = {Webb, R. and D, Keigwin L.}
}
@article {754,
	title = {High-Resolution Climate Records from the North-Atlantic during the Last Interglacial},
	journal = {Nature},
	volume = {371},
	year = {1994},
	note = {Ph254Times Cited:313Cited References Count:25},
	month = {Sep 22},
	pages = {326-329},
	abstract = {THE two deep ice cores recovered by the GRIP(1) and GISP(2) projects at Summit, Greenland, agree in detail over the past 100,000 years(3) and demonstrate dramatic climate variability in the North Atlantic region during the last glacial, before the current period of Holocene stability. This glacial climate instability has subsequently been documented in the marine sedimentary record of surface-ocean conditions in the North Atlantic(4). Before 100 kyr ago the two ice core records are discrepant, however, casting doubt on whether the oxygen isotope fluctuations during the last interglacial (Eemian) seen in the GRIP core(1,5) represent a true climate signal. Here we present high-resolution records of foraminiferal assemblages and ice-rafted detritus from two North Atlantic cores for the interval 65 kyr to 135 kyr ago, extending the surface-ocean record back to the Eemian. The correlation between our records and the Greenland ice-core records is good throughout the period in which the two ice cores agree, suggesting a regionally coherent climate response. During the Eemian, our marine records show a more stable climate than that implied by the GRIP ice core, suggesting that localized phenomena may be responsible for the variability in the latter record during the Eemian.},
	issn = {0028-0836},
	doi = {10.1038/371326a0},
	author = {McManus, J. F. and Bond, G. C. and Broecker, W. S. and Johnsen, S. and Labeyrie, L. and Higgins, S.}
}
