Centennial-to-millennial hydrologic trends and variability along the North Atlantic Coast, USA, during the Holocene

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Note: this date was deemed unreliable and not used to establish Nora sediment ages
Note: This is the uppermost date shown in the paper

Wolfe, Brent B. and Edwards, Thomas W. D. and Hall, Roland I. and Johnston, John W.

A 5200-year record of freshwater availability for regions in western North America fed by high-elevation runoff

Chipman, Melissa L. and Clarke, Gina H. and Clegg, Benjamin F. and Gregory-Eaves, Irene and Hu, Feng Sheng

A 2000 year record of climatic change at Ongoke Lake, southwest Alaska

Ersek, Vasile and Clark, Peter U. and Mix, Alan C. and Cheng, Hai and Lawrence Edwards, R.

Holocene winter climate variability in mid-latitude western North America

Neil, Karen and Gajewski, Konrad and Betts, Matthew

Human-ecosystem interactions in relation to Holocene environmental change in Port Joli Harbour, southwestern Nova Scotia, Canada

Curtis, J.H.; Hodell, D.A.;  Brenner, M.

Lake Peten-Itza Ostracod and Gastropod Stable Isotopic Data

Curtis, Jason H. and Brenner, Mark and Hodell, David A. and Balser, Richard A. and Islebe, Gerald A. and Hooghiemstra, Henry

Previous work in Neotropical, closed-basin lakes has shown that, during the Holocene, changes in the 18O of shell material were controlled primarily by the ratio of E/P (Hodell et al., 1991; Hodell et al., 1995; Curtis et al., 1996) because of relatively stable temperatures and lack of large variations in 18O of source water (Curtis & Hodell, 1993).

Curtis, Jason H. and Hodell, David A. and Brenner, Mark

Climate Variability on the Yucatan Peninsula (Mexico) during the Past 3500 Years, and Implications for Maya Cultural Evolution

oxygen isotopes from Cytheridella ilosvayi

Note added by NAm2k hydroclimate authors: In closed-basin tropical to subtropical lakes with a season- ally dry climate, the d18O of lake water is controlled mainly by the ratio of evaporation to precipitation

oxygen isotopes from Pyrgophorus coronatus