Calcification

This study aims to provide historical information on key environmental parameters and describe the current trends of coral growth in Bonaire. In particular, we aim to reconstruct changes in terrestrial runoff and bleaching stress events and establish their effects on the calcification rates for Siderastrea spp corals around Bonaire over multiple decades. For this coral cores of Siderastrea sppcorals will be used to reconstruct the changes in calcification and environmental parameters along a gradient of terrestrial influence and anthropogenic activity. During March 2023 15 coral cores were collected from Siderastrea spp colonies at four locations around the west coast of Bonaire.

Abstract Ocean acidification studies in the past decade have greatly improved our knowledge of how calcifying organisms respond to increased surface ocean CO2 levels. It has become evident that, for many organisms, nutri- ent availability is an important factor that influences their physiological responses and competitive interactions with other species. Therefore, we tested how simulated ocean acidification and eutrophication (nitrate and phosphate enrichment) interact to affect the physiology and ecology of a calcifying chlorophyte macroalga (Halimeda opuntia(L.) J.V. Lamouroux) and its common noncalcifying epi- phyte (Dictyota sp.) in a 4-week fully crossed multifacto- rial experiment. Inorganic nutrient enrichment (+NP) had a strong influence on all responses measured with the excep- tion of net calcification. Elevated CO2 alone significantly decreased electron transport rates of the photosynthetic apparatus and resulted in phosphorus limitation in both spe- cies, but had no effect on oxygen production or respiration. The combination of CO2 and +NP significantly increased electron transport rates in both species. While +NP alone stimulated H. opuntia growth rates, Dictyota growth was significantly stimulated by nutrient enrichment only at elevated CO2, which led to the highest biomass ratios of Dictyota to Halimeda. Our results suggest that inorganic nutrient enrichment alone stimulates several aspects of H. opuntia physiology, but nutrient enrichment at a CO2 con- centration predicted for the end of the century benefits Dic- tyota sp. and hinders its calcifying basibiont H. opuntia.