Abstract
The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals.
Cite
CITATION STYLE
APA
Langer, G. (2013). Plankton in a greenhouse world. Nature Geoscience, 6(3), 164–165. https://doi.org/10.1038/ngeo1750
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free