Evidence for the continued existence of Abraxas Lake, Vestfold Hills, East Antarctica during the Last Glacial Maximum

Evidence is provided from a sediment core from saline Abraxas Lake, Vestfold Hills, that indicatesthat the lake existed through the Last Glacial Maximum. It can therefore be concluded that at least part of theVestfold Hills also remained ice-free through the Last Glacial Maximum, or at most was cove...

Full description

Bibliographic Details
Published in:Antarctic Science
Main Authors: Gibson, JAE, Paterson, KS, White, CA, Swadling, KM
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge Univ Press 2009
Subjects:
Online Access:http://www.cambridge.org/online/
https://doi.org/10.1017/S0954102009001801
http://ecite.utas.edu.au/54444