Decrease in volume and density of foraminiferal shells with progressing ocean acidification

Rapid increases in anthropogenic atmospheric CO(2) partial pressure have led to a decrease in the pH of seawater. Calcifying organisms generally respond negatively to ocean acidification. Foraminifera are one of the major carbonate producers in the ocean; however, whether calcification reduction by...

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Detalles Bibliográficos
Autores principales: Kuroyanagi, Azumi, Irie, Takahiro, Kinoshita, Shunichi, Kawahata, Hodaka, Suzuki, Atsushi, Nishi, Hiroshi, Sasaki, Osamu, Takashima, Reishi, Fujita, Kazuhiko
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8497592/
https://www.ncbi.nlm.nih.gov/pubmed/34620940
http://dx.doi.org/10.1038/s41598-021-99427-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8497592/
https://www.ncbi.nlm.nih.gov/pubmed/34620940
http://dx.doi.org/10.1038/s41598-021-99427-1

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