Adaptation of a globally important coccolithophore to ocean warming and acidification
Although oceanwarming and acidification are recognized as two major anthropogenic perturbations of today’s oceanswe know very little about how marine phytoplankton may respond via evolutionary change. We tested for adaptation to ocean warming in combination with ocean acidification in the globally i...
| Published in: | Nature Climate Change |
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| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2014
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| Subjects: | |
| Online Access: | https://doi.org/10.1038/NCLIMATE2379 https://www.openagrar.de/receive/timport_mods_00037441 https://www.openagrar.de/servlets/MCRFileNodeServlet/timport_derivate_00037441/dn053841.pdf |
| Summary: | Although oceanwarming and acidification are recognized as two major anthropogenic perturbations of today’s oceanswe know very little about how marine phytoplankton may respond via evolutionary change. We tested for adaptation to ocean warming in combination with ocean acidification in the globally important phytoplankton species Emiliania huxleyi. Temperature adaptation occurred independently of ocean acidification levels. Growth rateswere up to 16% higher in populations adapted for one year to warming when assayed at their upper thermal tolerance limit. Particulate inorganic (PIC) and organic (POC) carbon production was restored to values under present-day ocean conditions, owing to adaptive evolution, and were 101% and 55% higher under combined warming and acidification, respectively, than in non-adapted controls. Cells also evolved to a smaller size while they recovered their initial PIC:POC ratio even under elevated CO2. The observed changes in coccolithophore growth, calcite and biomass production, cell size and elemental composition demonstrate the importance of evolutionary processes for phytoplankton performance in a future ocean. |
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