A late Holocene lake sediment sequence from Livingstone Island, South Shetland Islands, with paleo-climatic implications
Island, shows that the lake and its catchment have undergone significant changes during the last 4000 years. Radiocarbon dating (AMS), sediment lithology, and microfossil analyses indicate that the lake was deglaciated over 4000 14C years ago. Distinct peaks in accumulation rates of sediment, Pedius...
Main Authors: | , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1991
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.468.2241 http://www.geol.lu.se/personal/seb/Publ 1991-95/SB et al 1991.pdf |