Late Holocene methane rise caused by orbitally controlled increase in tropical sources. (2011)
Attributed to:
QUEST Deglaciation: Climate and
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1038/nature09739
PubMed Identifier: 21293375
Publication URI: http://europepmc.org/abstract/MED/21293375
Type: Journal Article/Review
Volume: 470
Parent Publication: Nature
Issue: 7332
ISSN: 0028-0836