@article {1941,
	title = {Flooding of Bering Strait and Holocene climate in the Chukchi Sea},
	journal = {Geology},
	volume = {34},
	year = {2006},
	note = {id: 678},
	month = {2006},
	pages = {861-864},
	author = {Keigwin, L. D. and Donnelly, J. P. and Cook, M. S. and Driscoll, N. W. and Brigham-Grette, J.}
}
@article {678,
	title = {Rapid sea-level rise and Holocene climate in the Chukchi Sea},
	journal = {Geology},
	volume = {34},
	year = {2006},
	note = {089zkTimes Cited:67Cited References Count:18},
	month = {Oct},
	pages = {861-864},
	abstract = {Three new sediment cores from the Chukchi Sea preserve a record of local paleoenvironment, sedimentation, and flooding of the Chukchi Shelf (similar to-50 m) by glacial-eustatic sea-level rise. Radiocarbon dates on foraminifera provide the first marine evidence that the sea invaded Hope Valley (southern Chukchi Sea, -53 m) as early as 12 ka. The lack of significant sediment accumulation since ca. 7 ka in Hope Valley, southeastern Chukchi Shelf, is consistent with decreased sediment supply and fluvial discharge to the shelf as deglaciation of Alaska concluded. Abundant benthic foraminifera from a site west of Barrow Canyon indicate that surface waters were more productive 4-6 ka, and this productivity varied on centennial time scales. An offshore companion to this core contains a 20 m record of the Holocene. These results show that carefully selected core sites from the western Arctic Ocean can have a temporal resolution equal to the best cores from other regions, and that these sites can be exploited for high-resolution studies of the paleoenvironment.},
	issn = {0091-7613},
	doi = {10.1130/G22712.1},
	author = {Keigwin, L. D. and Donnelly, J. P. and Cook, M. S. and Driscoll, N. W. and Brigham-Grette, J.}
}
@article {600,
	title = {The deglacial history of surface and intermediate water of the Bering Sea},
	journal = {Deep-Sea Research Part Ii-Topical Studies in Oceanography},
	volume = {52},
	year = {2005},
	note = {995ksTimes Cited:51Cited References Count:52},
	pages = {2163-2173},
	abstract = {The lithology of deglacial sediments from the Bering Sea includes intervals of laminated or dysaerobic sediments. These intervals are contemporaneous with the occurrence of laminated sediments from the California margin and Gulf of California, which suggests widespread low-oxygen conditions at intermediate depths in the North Pacific Ocean. The cause could be reduced intermediate water ventilation, increased organic carbon flux, or a combination of the two. We infer abrupt decreases of planktonic foraminifer delta(18)O at 14,400 and 11,650 yr BP, which may be a combination of both freshening and warming. On the Shirshov Ridge, the abundance of sea-ice diatoms of the genus Nitzschia reach local maxima twice during the deglaciation, the latter of which may be an expression of the Younger Dryas. These findings expand the extent of the expression of deglacial millennial-scale climate events to include the northernmost Pacific. (c) 2005 Elsevier Ltd. All rights reserved.},
	issn = {0967-0645},
	doi = {10.1016/j.dsr2.2005.07.004},
	author = {Cook, M. S. and Keigwin, L. D. and Sancetta, C. A.}
}
