Impact of dissolved CO2 on calcification in two large, benthic foraminiferal species

Rising atmospheric CO2 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 CO2 levels will ei...

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Bibliographic Details
Main Authors: Linda Karoline Dämmer, Angelina Ivkić, Lennart de Nooijer, Willem Renema, Alice E. Webb, Gert-Jan Reichart
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2023-01-01
Series:PLoS ONE
Online Access:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10431644/?tool=EBI