Ocean acidification effects on calcifying macroalgae
Since the Industrial Revolution, the partial pressure of carbon dioxide (pCO2) has been increasing and global ocean surface waters have absorbed 30% of the anthropogenic CO2 released into the atmosphere. An increase in pCO2 in surface ocean waters causes an increase in bicarbonate ions (HCO3-) and p...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Inter-Research
2014-11-01
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| Series: | Aquatic Biology |
| Online Access: | https://www.int-res.com/abstracts/ab/v22/p261-279/ |