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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...

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Detalles Bibliográficos
Autores principales:	Dämmer, Linda Karoline, Ivkić, Angelina, de Nooijer, Lennart, Renema, Willem, Webb, Alice E., Reichart, Gert-Jan
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Public Library of Science 2023
Materias:	Research Article
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

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