The National Institute of Water Resources Alaska division funded this study along with the National Science Foundation (NSF grants: PLR-1417036 and 1417611) and the Bureau of Land Management. We thank Dan Cross-Call, Andrew Weller, Joe Gaglioti, and Louise Farquharson for help in the field. Nick Wiesenburg helped with cross-dating shrub rings. Kim Sparks, Shane Billings, Tim Howe, and Norma Haubenstock contributed greatly to cellulose extractions. We benefitted from discussions with Eric Klein, Jeff Welker, Bruce Finney, Laia Andreu-Hayles, and Lesleigh Anderson. Comments from Trevor Porter and an anonymous reviewer improved this manuscript. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This is LDEO contribution #8113.
Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9w, Palisades, NY, United States; Department of Geosciences, University of Alaska Fairbanks, 900 Yukon Dr., Fairbanks, AK, United States; Water and Environmental Research Center, College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, 306 Tanana Dr., Fairbanks, AK, United States; Alaska Science Center, US Geological Survey, 4210 University Dr., Anchorage, AK, United States; Department of Geology, College of Wooster, 1189 Beall Ave., Wooster, OH, United States; Institute of Arctic Biology, University of Alaska Fairbanks, 902 North Koyukuk Dr., Fairbanks, AK, United States; School of Natural Resources and Extension, University of Alaska Fairbanks, P.O. Box 757140, Fairbanks, AK, United States; Reanier & Associates Inc., 1215 SW 170th St., Seattle, WA, United States
Recommended Citation:
Gaglioti B.V.,Mann D.H.,Wooller M.J.,et al. Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska[J]. Quaternary Science Reviews,2017-01-01,169