Sedimentology and geochemistry of a perennially ice-covered epishelf lake in Bunger Hills Oasis, East Antarctica

A process-oriented study was carried out in White Smoke lake, Bunger Hills, East Antarctica, a perennially ice-covered (1.8 to 2.8 m thick) epishelf ( tidally-forced) lake. The lake water has a low conductivity and is relative ly well mixed. Sediments are transferred from the adjacent glacier to the l ake when glacier ice surrounding the sediment is sublimated at the surface and replaced by accumulating ice from below. The lake bottom at the west en d of the lake is mostly rocky with a scant sediment cover. The east end con tains a thick sediment profile. Grain size and delta(13)C increase with sed iment depth, indicating a more proximal glacier ill the past. Sedimentary P b-210 and Cs-137 signals are exceptionally strong, probably a result of the focusing effect of the large glacial catchment area. The post-bomb and pre -bomb radiocarbon reservoirs are c. 725 C-14 yr and c. 1950 C-14 yr, respec tively. Radiocarbon dating indicates that the east end of the lake is >3 ka sp, while photographic evidence and the absence of sediment cover indicate that the west end has formed only over the last century. Our results indic ate that the southern ice edge of Bunger Hills has been relatively stable w ith only minor fluctuations (on the scale of hundreds of metres) over the l ast 3000 years.