Palaeontology: Plankton in a greenhouse world
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.
| Published in: | Nature Geoscience |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2013
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| Online Access: | http://eprints.esc.cam.ac.uk/2687/ http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg http://www.nature.com/ngeo/journal/v6/n3/full/ngeo1750.html https://doi.org/10.1038/ngeo1750 |
| Summary: | 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. |
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