@inbook {1439,
	title = {Analog for Holocene and future Climate?},
	booktitle = {Geophysical Monograph 137, Earth{\textquoteright}s Climate and Orbital Eccentricity: The Marine Isotope State 11 Questions},
	year = {2003},
	note = {id: 1166},
	month = {2003},
	pages = {69-85},
	author = {McManus, J. F. and Oppo, D. W. and Cullen, J. L. and Healey, S. L.},
	editor = {Droxler, A.}
}
@article {634,
	title = {Palaeo-oceanography: Deepwater variability in the Holocene epoch},
	journal = {Nature},
	volume = {422},
	year = {2003},
	note = {Oppo, Delia WMcManus, Jerry FCullen, James LengEngland2003/03/21 04:00Nature. 2003 Mar 20;422(6929):277.},
	month = {Mar 20},
	pages = {277},
	issn = {0028-0836 (Linking)},
	doi = {10.1038/422277b},
	author = {Oppo, D. W. and McManus, J. F. and Cullen, J. L.}
}
@article {2224,
	title = {A 0.5-million-year record of millennial-scale climate variability in the north atlantic},
	journal = {Science},
	volume = {283},
	year = {1999},
	note = {McManusOppo
Cullen
eng
1999/02/12 03:03
Science. 1999 Feb 12;283(5404):971-5.
},
	month = {Feb 12},
	pages = {971-5},
	abstract = {Long, continuous, marine sediment records from the subpolar North Atlantic document the glacial modulation of regional climate instability throughout the past 0.5 million years. Whenever ice sheet size surpasses a critical threshold indicated by the benthic oxygen isotope (delta18O) value of 3.5 per mil during each of the past five glaciation cycles, indicators of iceberg discharge and sea-surface temperature display dramatically larger amplitudes of millennial-scale variability than when ice sheets are small. Sea-surface temperature oscillations of 1 degrees to 2 degreesC increase in size to approximately 4 degrees to 6 degreesC, and catastrophic iceberg discharges begin alternating repeatedly with brief quiescent intervals. The glacial growth associated with this amplification threshold represents a relatively small departure from the modern ice sheet configuration and sea level. Instability characterizes nearly all observed climate states, with the exception of a limited range of baseline conditions that includes the current Holocene interglacial.},
	isbn = {1095-9203 (Electronic)0036-8075 (Linking)},
	doi = {10.1126/science.283.5404.971},
	url = {https://www.ncbi.nlm.nih.gov/pubmed/9974387},
	author = {McManus, J. F. and Oppo, D. W. and Cullen, J. L.}
}
@article {2222,
	title = {Evidence for Late Pleistocene-Holocene Intermediate-Water variability in the North Atlantic},
	journal = {EOS},
	volume = {80},
	year = {1999},
	note = {id: 172},
	month = {1999},
	pages = {S169},
	author = {McManus, J. F. and Oppo, D. W. and Curry, W. and Marchitto, T. and Cullen, J. L.}
}
@article {2223,
	title = {Glacial modulation of rapid climate change during the last 0.5 million years},
	journal = {PAGES newsletter},
	volume = {7},
	year = {1999},
	note = {id: 168},
	month = {1999},
	pages = {12-13},
	author = {McManus, J. F. and Oppo, D. W. and Cullen, J. L.}
}
