@article {1018,
	title = {Amplitude and timing of temperature and salinity variability in the subpolar North Atlantic over the past 10 k.y.},
	journal = {Geology},
	volume = {35},
	year = {2007},
	note = {id: 983},
	pages = {315-318},
	abstract = {Paired planktic foraminiferal δ18O and Mg/Ca data reveal trends of increasing temperatures (\~{}3 {\textdegree}C) and salinities in the subpolar North Atlantic over the course of the Holocene, which were punctuated by abrupt events. The trends likely reflect an insolation-forced northward retreat of the boundary between polar and North Atlantic subsurface waters. The superimposed variability does not appear to be periodic, but tends to recur within a broad millennial band. The records provide convincing evidence of open-ocean cooling (nearly 2 {\textdegree}C) and freshening during the 8.2 ka event, and suggest similar conditions at 9.3 ka. However, the two largest temperature oscillations in our record (\~{}2 {\textdegree}C) occurred during the past 4 k.y., suggesting a recent increase in temperature variability relative to the mid-Holocene, perhaps in response to neoglaciation, which began at about this time. },
	keywords = {Bj{\"o}rn Drift, Mg/Ca, Neogloboquadrina pachyderma dextral, Ocean Drilling Program Site 984, paleotemperature},
	doi = {10.1130/G23455A.1 },
	author = {Came, R. E. and Oppo, D. W. and McManus, J. F.}
}
@article {2084,
	title = {East Asian monsoon forcing of suborbital variability in the Sulu Sea during Marine Isotope Stage 3: Link to Northern Hemisphere climate},
	journal = {Geochemistry Geophysics Geosystems},
	volume = {4},
	year = {2003},
	note = {631mwTimes Cited:41
Cited References Count:53
},
	month = {Jan 2},
	abstract = {[1] We have generated a new high-resolution record of variations in planktonic foraminiferal oxygen isotopes (delta(18)O) and Mg/Ca from a sediment core (IMAGES 97-2141) in the Sulu Sea located in the Philippine archipelago of western tropical Pacific. This record reveals distinct, suborbital-scale delta(18)O changes, most notably during Marine Isotope Stage 3 (MIS3) (similar to30,000 to 60,000 years B.P.). The amplitudes of these delta(18)O fluctuations (0.4 to 0.7parts per thousand) exceed that which can be attributed to sea level changes and must be due to changes in sea surface conditions. In the same interval, variations in planktonic foraminifera Mg/Ca suggest that suborbital surface ocean temperature variations of 1 to 1.5degreesC in the Sulu Sea were not in phase with delta(18)O. Combined, this evidence indicates that the MIS3 millennial delta(18)O events in the Sulu Sea were primarily the result of changes in surface water salinity, which today is directly related to the East Asian Monsoon (EAM) and its influence on the balance between surface water contributions from the South China Sea and Western Pacific Warm Pool (WPWP). Within dating uncertainties the MIS3 Sulu Sea delta(18)O suborbital variability indicates that times of fresher surface conditions in the Sulu Sea coincide with similar conditions in the WPWP [Stott et al., 2002] and also with intensifications of the summer EAM as recorded in the U-Th dated Chinese (Hulu Cave) speleothem delta(18)O record [Wang et al., 2001] and thus by inference with interstadials in the Greenland Ice core records. Combined, these results indicate that pronounced suborbital variability in the summer EAM and Intertropical Convergence Zone (ITCZ) during MIS3 was tightly coupled with climate conditions in the northern high latitudes.},
	keywords = {1620 global change : climate dynamics (3309), 4267 oceanography : general : paleoceanography, dissolution, equatorial pacific, eurasian snow cover, isotope stage 3, last glacial period, late pleistocene, Mg/Ca, millennial-scale climate change, oxygen isotopes, paleoceanography, planktonic-foraminifera, records, se asian monsoon, south china sea, summer monsoon, surface temperature-variations},
	isbn = {1525-2027},
	doi = {10.1029/2002GC000390},
	author = {Dannenmann, S. and Linsley, B. K. and Oppo, D. W. and Rosenthal, Y. and Beaufort, L.}
}
