Abstract: Holocene hydroclimatic change in south-central Alaska inferred from δ<sup>18</sup>O<sub>diatom</sub> at Sunken Island Lake, Kenai Peninsula lowlands (AGU Fall Meeting 2018)

Holocene hydroclimatic change in south-central Alaska inferred from δ¹⁸O_diatom at Sunken Island Lake, Kenai Peninsula lowlands

Ellie Broadman¹, Darrell S Kaufman¹, Andrew C G Henderson², R Scott Anderson³, Edward Berg⁴, Melanie J Leng⁵ and Nicholas McKay¹, (1)Northern Arizona University, School of Earth and Sustainability, Flagstaff, AZ, United States, (2)Newcastle University, School of Geography, Politics & Sociology, Tyne and Wear, United Kingdom, (3)Northern Arizona University, School of Earth and Sustainability, Flagstaff, United States, (4)US Fish and Wildlife Service, Kenai National Wildlife Refuge, Soldotna, AK, United States, (5)British Geological Survey, NERC Isotope Geoscience Facilities, Nottingham, United Kingdom

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Holocene hydroclimatic change in south-central Alaska inferred from δ18Odiatom at Sunken Island Lake, Kenai Peninsula lowlands

Holocene hydroclimatic change in south-central Alaska inferred from δ¹⁸O_diatom at Sunken Island Lake, Kenai Peninsula lowlands