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Impact of dissolved CO(2) on calcification in two large, benthic foraminiferal species
Rising atmospheric CO(2) shifts the marine inorganic carbonate system and decreases seawater pH, a process often abbreviated to ‘ocean acidification’. Since acidification decreases the saturation state for crystalline calcium carbonate (e.g., calcite and aragonite), rising dissolved CO(2) levels wil...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Public Library of Science
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10431644/ https://www.ncbi.nlm.nih.gov/pubmed/37585361 http://dx.doi.org/10.1371/journal.pone.0289122 |