Moss stable isotopes (carbon-13, oxygen-18) and testate amoebae reflect environmental inputs and microclimate along a latitudinal gradient on the Antarctic Peninsula. (2016)
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/10.17863/cam.10283
Publication URI: https://www.repository.cam.ac.uk/handle/1810/266100
Type: Journal Article/Review