Late Quaternary climate-driven environmental change in the Larseman Hills, east Antarctica, multi-proxy evidence from a lake sediment core
Hodgson, Dominic A.; Verleyen, Elie; Sabbe, Koen; Squier, Angela H.; Keely, Brendan J.; Leng, Melanie J.; Saunders, Krystyna M.; Vyverman, Wim. 2005 Late Quaternary climate-driven environmental change in the Larseman Hills, east Antarctica, multi-proxy evidence from a lake sediment core. Quaternary Research, 64 (1). 83-99. 10.1016/j.yqres.2005.04.002Full text not available from this repository. (Request a copy)
Little is known about the response of terrestrial East Antarctica to climate changes during the last glacial–interglacial cycle. Here we present a continuous sediment record from a lake in the Larsemann Hills, situated on a peninsula believed to have been ice-free for at least 40,000 yr. A mutli-proxy data set including geochronology, diatoms, pigments and carbonate stable isotopes indicates warmer and wetter conditions than present in the early part of the record. We interpret this as Marine Isotope Stage 5e after application of a chronological age-depth model and similar ice core evidence. Dry and cold conditions are inferred during the last glacial, with lake-level minima, floristic changes towards a shallow water algal community, and a greater biological receipt of ultraviolet radiation. During the Last Glacial Maximum and Termination I the lake was perennially ice-covered, with minimal snowmelt in the catchment. After ca. 10,500 cal yr B.P., the lake became seasonally moated or ice-free during summer. Despite a low accumulation rate, the sediments document some Holocene environmental changes including neoglacial cooling after ca. 2450 cal yr B.P., and a gradual increase in aridity and salinity to the present.
|Programmes:||BAS Programmes > Antarctic Science in the Global Context (2000-2005) > Signals in Antarctica of Past Global Changes
BGS Programmes > NERC Isotope Geoscience Laboratory
|Date made live:||08 Jun 2012 15:13|
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