4.1 Article

RESPONSE OF THE MILIOLID ARCHAIAS ANGULATUS TO SIMULATED OCEAN ACIDIFICATION

Journal

JOURNAL OF FORAMINIFERAL RESEARCH
Volume 45, Issue 2, Pages 109-127

Publisher

CUSHMAN FOUNDATION FORAMINIFERAL RESEARCH
DOI: 10.2113/gsjfr.45.2.109

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Funding

  1. USGS Coastal and Marine Geology Program
  2. Geological Society of America
  3. USF Department of Geology

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A common, but not universal, effect of ocean acidification on benthic foraminifera is a reduction in the growth rate. The miliolid Archaias angulatus is a high-Mg (>4 mole% MgCO3), symbiont-bearing, soritid benthic foraminifer that contributes to Caribbean reef carbonate sediments. A laboratory culture study assessed the effects of reduced pH on the growth of A. angulatus. We observed a statistically significant 50% reduction in the growth rate (p < 0.01), calculated from changes in maximum diameter, from 160 mu m/28 days in the pH 8.0/p CO2air 480 ppm control group to 80 mu m/28 days at a treatment level of pH 7.6/p CO2air 1328 ppm. Additionally, pseudopore area, delta O-18 values, and Mg/Ca ratio all increased, albeit slightly in the latter two variables. The reduction in growth rate indicates that under a high-CO2 setting, future A. angulatus populations will consist of smaller adults. A model using the results of this study estimates that at pH 7.6 A. angulatus carbonate production in the South Florida reef tract and Florida Bay decreases by 85%, from 0.27 Mt/yr to 0.04 Mt/yr, over an area of 9,000 km(2).

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