Response of Marginopora vertebralis (Foraminifera) from Laucala Bay, Fiji, to Changing Ocean pH

Authors

Roselyn Naidu, The University of Fiji
Pamela Hallock, University of South FloridaFollow
Jonathan Erez, The Hebrew University of Jerusalem
Matakite Maata, University of South Pacific

Document Type

Book Chapter

Publication Date

2017

Keywords

benthic foraminifera, climate change, growth, laucala bay, ocean acidification, ph

Digital Object Identifier (DOI)

https://doi.org/10.1007/978-3-319-50094-2_8

Abstract

Increased CO₂ emissions into the atmosphere lead to increased concentrations of dissolved CO₂ in the ocean. A chemical reaction between the dissolved CO₂ and seawater produces HCO₃ ⁻, CO₃ ²⁻ and H⁺ ions. These H⁺ ions increase the acidity of seawater and decrease the pH. Increased acidity and decreased availability of CO₃ ²⁻ ion affect calcite and aragonite production by marine calcifiers in the ocean. To assess potential responses of the larger benthic foraminifer Marginopora vertebralis to ocean acidification, we performed growth experiments at three pH levels [7.5, 7.8, 8.1 (ambient seawater)] for 11 weeks. Specimens were stained with the fluorescent compound Calcein ( ̴40 µmole/l) prior to treatment, allowing identification of calcite added during the treatment period. At pH 8.1, specimens increased their test weight by 8.4%, at pH 7.8 growth was 4.2%, and at pH 7.5, growth was only 3.2%. These differences represent a significant relationship between ocean pH and test growth (i.e., calcification). In addition, several specimens in the pH 8.1 treatment underwent asexual reproduction during the experiment, while no reproduction was observed in the pH 7.8 or 7.5 treatments. These results indicate that ocean acidification predicted to occur by the end of the 21st century will cause a decline in population densities of Marginopora vertebralis in their natural environment, as consequences of both reduced growth rates and rates of reproduction. And because the tests of these foraminifers are important components of carbonate sediments on coral cays and tropical beaches, a decline in their rates of sediment production will exacerbate the consequences of rising sea level.

Citation / Publisher Attribution

Response of Marginopora Vertebralis (Foraminifera) from Laucala Bay, Fiji, to Changing Ocean Ph, in W. Leal Filho (Ed.), Climate Change Adaptation in Pacific Countries, Springer, p. 137-150

Scholar Commons Citation

Naidu, Roselyn; Hallock, Pamela; Erez, Jonathan; and Maata, Matakite, "Response of Marginopora vertebralis (Foraminifera) from Laucala Bay, Fiji, to Changing Ocean pH" (2017). Marine Science Faculty Publications. 902.
https://digitalcommons.usf.edu/msc_facpub/902