A nutrient control on expanded anoxia and global cooling during the Late Ordovician mass extinction (2022)
Attributed to:
How did the evolution of plants, microbial symbionts and terrestrial nutrient cycles change Earth's long-term climate?
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1038/s43247-022-00412-x
Publication URI: http://dx.doi.org/10.1038/s43247-022-00412-x
Type: Journal Article/Review
Parent Publication: Communications Earth & Environment
Issue: 1