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Oxygen-isotope (d18O) evidence of Holocene hydrological changes at Signy Island, maritime Antarctica (2003)

First Author: Noon P

Attributed to: National Environmental Isotope Facility (NEIF) funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1191/0959683603hl611rp

Publication URI: http://dx.doi.org/10.1191/0959683603hl611rp

Type: Journal Article/Review

Parent Publication: The Holocene

Issue: 2