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Abstract: Magnitude of Warming at the Pleistocene-Holocene Transition in New England (USA) and Atlantic Canada Inferred from Chironomids in a Network of Seven Lakes (AGU25)

Magnitude of Warming at the Pleistocene-Holocene Transition in New England (USA) and Atlantic Canada Inferred from Chironomids in a Network of Seven Lakes

Aidan Warner Burdick1, Kaitlyn Gerstler2, Justin Stroup3, Anne Randall3, W. Wyatt Oswald4,5, Les C. Cwynar6, Ann Dieffenbacher-Krall7, Jamie McFarlin2, Meredith A Kelly3, Nathaniel Kitchel8,9 and Yarrow Axford1, (1)Northwestern University, Earth, Environmental, and Planetary Sciences, Evanston, IL, United States, (2)University of Wyoming, Geology and Geophysics, Laramie, WY, United States, (3)Dartmouth College, Department of Earth Sciences, Hanover, United States, (4)Emerson College, Marlboro Institute for Liberal Arts & Interdisciplinary Studies, Boston, United States, (5)Harvard Forest, Petersham, MA, United States, (6)University of New Brunswick, Fredericton, NB, Canada, (7)University of Maine, School of Biology and Ecology, Orono, ME, United States, (8)Salve Regina University, Cultural and Historic Preservation, Newport, United States, (9)Dartmouth College, Department of Anthropology, Hanover, NH, United States
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