Lake-Level Fluctuations in the Fryxell Basin, Eastern Taylor Valley, Antarctica
Isotope records (δ180,δ13C, 14C), sedimentology, and diatom assemblages from Lake Fryxell (77°37'S, 163°06'E) sediment cores display evidence of significant changes in depositional environment from > 30 kyr B.P. to the present. These changes reflect variations in meltwater production re...
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DigitalCommons@UMaine
2004
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Online Access: | https://digitalcommons.library.umaine.edu/etd/1190 https://digitalcommons.library.umaine.edu/context/etd/article/2184/viewcontent/WhittakerTE2004.pdf |