Differing source water inputs, moderated by evaporative enrichment, determine the contrasting d 18 O CELLULOSE signals in maritime Antarctic moss peat banks (2013)
Attributed to:
Terrestrial Holocene climate variability on the Antarctic Peninsula
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1002/jgrg.20021
Publication URI: http://dx.doi.org/10.1002/jgrg.20021
Type: Journal Article/Review
Parent Publication: Journal of Geophysical Research: Biogeosciences
Issue: 1