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...

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Bibliographic Details
Main Authors: Svante Bjorck, Hannelore Hskansson, Rolf Zale, Wibjorn Karlen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1991
Subjects:
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