@article {630,
	title = {Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean},
	journal = {Nature},
	volume = {421},
	year = {2003},
	note = {637uwTimes Cited:483Cited References Count:30},
	month = {Jan 23},
	pages = {354-357},
	abstract = {During the last ice age, the Indian Ocean southwest monsoon exhibited abrupt changes that were closely correlated with millennial-scale climate events in the North Atlantic region(1-3), suggesting a mechanistic link. In the Holocene epoch, which had a more stable climate, the amplitude of abrupt changes in North Atlantic climate was much smaller, and it has been unclear whether these changes are related to monsoon variability. Here we present a continuous record of centennial-scale monsoon variability throughout the Holocene from rapidly accumulating and minimally bioturbated sediments in the anoxic Arabian Sea. Our monsoon proxy record reveals several intervals of weak summer monsoon that coincide with cold periods documented in the North Atlantic region(4)-including the most recent climate changes from the Medieval Warm Period to the Little Ice Age and then to the present. We therefore suggest that the link between North Atlantic climate and the Asian monsoon is a persistent aspect of global climate.},
	issn = {0028-0836},
	doi = {10.1038/nature01340},
	author = {Gupta, A. K. and Anderson, D. M. and Overpeck, J. T.}
}
@article {338,
	title = {Increase in the Asian southwest monsoon during the past four centuries},
	journal = {Science},
	volume = {297},
	year = {2002},
	note = {id: 536; Anderson, David M Overpeck, Jonathan T Gupta, Anil K New York, N.Y. Science. 2002 Jul 26;297(5581):596-9.},
	pages = {596-9},
	abstract = {Climate reconstructions reveal unprecedented warming in the past century; however, little is known about trends in aspects such as the monsoon. We reconstructed the monsoon winds for the past 1000 years using fossil Globigerina bulloides abundance in box cores from the Arabian Sea and found that monsoon wind strength increased during the past four centuries as the Northern Hemisphere warmed. We infer that the observed link between Eurasian snow cover and the southwest monsoon persists on a centennial scale. Alternatively, the forcing implicated in the warming trend (volcanic aerosols, solar output, and greenhouse gases) may directly affect the monsoon. Either interpretation is consistent with the hypothesis that the southwest monsoon strength will increase during the coming century as greenhouse gas concentrations continue to rise and northern latitudes continue to warm.},
	issn = {1095-9203 (Electronic) 0036-8075 (Linking)},
	doi = {10.1126/science.1072881},
	author = {Anderson, D. M. and Overpeck, J. T. and Gupta, A. K.}
}
@article {2215,
	title = {A high resolution ~15,000 year record of El-Nino driven alluviation in southwestern Ecuador},
	journal = {Science},
	volume = {283},
	year = {1999},
	note = {id: 393},
	month = {1999},
	pages = {516-519},
	author = {Rodbell, D. T. and Seltzer, G. O. and Anderson, D. M. and Abbott, M. B. and Enfield, D. B. and Newman, J. H.}
}
@conference {1664,
	title = {The Last Deglaciation in Southern Chile},
	booktitle = {Development of Paleoceanography as a New Field of Science},
	volume = {27},
	year = {1999},
	note = {id: 145},
	month = {1999},
	address = {Stockholm},
	author = {Anderson, D. M. and Archer, R. B.}
}
@article {816,
	title = {Preliminary evidence of early deglaciation in southern Chile},
	journal = {Palaeogeography Palaeoclimatology Palaeoecology},
	volume = {146},
	year = {1999},
	note = {160wbTimes Cited:13Cited References Count:25},
	month = {Feb 15},
	pages = {295-301},
	abstract = {The end of the last ice age in the channels of southern Chile is recorded by resumed sedimentation in formerly ice-filled basins. To identify the timing of initial ice retreat in Southern Chile, we examined ice-proximal sediments from a proglacial lake along the eastern margin of the Magallanes ice sheet, an environment thought to be sensitive to initial melting (Porter, S.C,, Clapperton, C.M., Sugden, D.E., 1992. Chronology and dynamics of deglaciation along and near the Strait of Magellan, southernmost South America. Sver. Geol. Unders. 81, 233-239). AMS-radiocarbon dates of the supra-till deposits in two cores indicate that sedimentation resumed 18 radiocarbon kyr. Deposition in kettle-holes and bogs on the adjacent land surfaces began at the same time or earlier (17-25 radiocarbon kyr) (Clapperton, C.M., Sugden, D.E., Kaufman, D.S., McCulloch, R.D., 1995. The last glaciation in central Magellan Strait, Southernmost Chile. Quat. Res. 44, 133-148). Our preliminary interpretation is that these events indicate initial deglaciation in the region and the formation of a large proglacial lake, followed several thousand years later by the invasion of salt water as sea level rose. Deglaciation in southers Chile occurred too early to be forced by the resumption of North Atlantic Deep Water formation, sea level rise, or northern hemisphere summer insolation, and we suggest instead that southern insolation played a role. The time of initial deglaciation in southern Chile (21-27 calendar kyr) occurred as southern hemisphere annual insolation increased from a minimum at 29 calendar kyr (6 W/m(2) less than today at 80 degrees S). (C) 1999 Elsevier Science B.V. All rights reserved.},
	issn = {0031-0182},
	doi = {10.1016/S0031-0182(98)00146-1},
	author = {Anderson, D. M. and Archer, R. B.}
}
@article {887,
	title = {Plankton Environment and Marine Sediment Record of the Archipelago de Magallanes, Chile},
	journal = {EOS,Transactions,American Geophysical Union},
	volume = {74},
	year = {1993},
	note = {id: 902},
	pages = {372},
	author = {Anderson, D. M. and Archer, R. B.}
}
