Holocene glacier fluctuations and environmental changes in subantarctic South Georgia inferred from a sediment record from a coastal inlet

• Published in: Quaternary Research
• Main Authors: Berg, Sonja, White, Duanne A., Jivcov, Sandra, Melles, Martin, Leng, Melanie J., Rethemeyer, Janet, Allen, Claire, Perren, Bianca, Bennike, Ole, Viehberg, Finn
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Cambridge University Press (CUP) 2018
• Subjects: Earth-Surface Processes; Arts and Humanities (miscellaneous); General Earth and Planetary Sciences; Antarctic; The Antarctic; Little Jason; Little Jason Lagoon; Antarc*
• Online Access: https://doi.org/10.1017/qua.2018.85; https://nottingham-repository.worktribe.com/file/1350148/1/Holocene%20glacier%20fluctuations; https://nottingham-repository.worktribe.com/output/1350148

© 2018 University of Washington. Published by Cambridge University Press. The subantarctic island of South Georgia provides terrestrial and coastal marine records of climate variability, which are crucial for the understanding of the drivers of Holocene climate changes in the subantarctic region. Here we investigate a sediment core (Co1305) from a coastal inlet on South Georgia using elemental, lipid biomarker, diatom, and stable isotope data to infer changes in environmental conditions and to constrain the timing of late-glacial and Holocene glacier fluctuations. Because of the scarcity of terrestrial macrofossils and the presence of redeposited and relict organic matter in the sediments, age control for the record was obtained by compound-specific radiocarbon dating of mostly marine-derived n-C16 fatty acids. A basal till layer recovered in Little Jason Lagoon was likely deposited during an advance of local glaciers during the Antarctic cold reversal. After glacier retreat, an oligotrophic lake occupied the site, which transitioned to a marine inlet around 8.0±0.9 ka because of relative sea-level rise. From 7.0±0.6 to 4.0±0.4 ka, reduced vegetation coverage in the catchment, as well as high siliciclastic input and deposition of ice-rafted debris, indicates glacier advances in the terrestrial catchment and likely in the adjacent fjord. A second, less extensive period of glacier advances occurred in the late Holocene, after 1.8±0.3 ka.