Seawater carbonate chemistry and fouling community structure and diversity
1.Increasing levels of CO2 in the atmosphere are affecting ocean chemistry, leading to increased acidification (i.e., decreased pH) and reductions in calcium carbonate saturation state. 2.Many species are likely to respond to acidification, but the direction and magnitude of these responses will be...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.956135 https://doi.org/10.1594/PANGAEA.956135 |