In situ recovery of bivalve shell characteristics after temporary exposure to elevated pCO
Ocean uptake of carbon dioxide (CO₂) is causing changes in carbonate chemistry that affects calcification in marine organisms. In coastal areas, this CO₂-enriched seawater mixes with waters affected by seasonal degradation of organic material loaded externally from watersheds or produced as a respon...
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Veröffentlicht in: | Limnology and oceanography 2020-10, Vol.65 (10), p.2337-2351 |
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Format: | Artikel |
Sprache: | eng |
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