Relative paleointensity (RPI) in the latest Pleistocene (10-45 ka) and implications for deglacial atmospheric radiocarbon (2018)
Attributed to:
Resolving the ocean's role in deglacial radiocarbon cycling (OCEAN-14)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.17863/cam.30630
Publication URI: https://www.repository.cam.ac.uk/handle/1810/283262
Type: Journal Article/Review