Estuarine organisms are exposed to periodic strong fluctuations in seawater pH driven by biological carbon dioxide (CO 2 ) production, which may in the future be further exacerbated by the ocean acidification associated with the global rise in CO 2 . Calcium carbonate-producing marine species such as mollusks are expected to be vulnerable to acidification of estuarine waters, since elevated CO 2 concentration and lower pH lead to a decrease in the degree of saturation of water with respect to calcium carbonate, potentially affecting biomineralization. Our study demonstrates that the increase in CO 2 partial pressure (pCO 2 ) in seawater and associated decrease in pH within the environmentally relevant range for estuaries have negative effects on physiology, rates of shell deposition and mechanical properties of the shells of eastern oysters Crassostrea virginica (Gmelin). High CO 2 levels (pH~7.5, pCO 2~3 500 µatm) caused significant increases in juvenile mortality rates and inhibited both shell and soft-body growth compared to the control conditions (pH ~8.2, pCO 2 380 µatm). Furthermore, elevated CO 2 concentrations resulted in higher standard metabolic rates in oyster juveniles, likely due to the higher energy cost of homeostasis. The high CO 2 conditions also led to changes in the ultrastructure and mechanical properties of shells, including increased thickness of the calcite laths within the hypostracum and reduced hardness and fracture toughness of the shells, indicating that elevated CO 2 levels have negative effects on the biomineralization process. These data strongly suggest that the rise in CO 2 can impact physiology and biomineralization in marine calcifiers such as eastern oysters, threatening their survival and potentially leading to profound ecological and economic impacts in estuarine ecosystems.KEY WORDS: Hypercapnia · Ocean acidification · Calcification · Shell structure · Energy metabolism · Oxygen consumption · Mollusks
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 419: [95][96][97][98][99][100][101][102][103][104][105][106][107][108] 2010 between 4 and 5 mo in summer and early fall (Cochran & Burnett 1996; see also long-term water pH data for eastern US estuaries at http://cdmo.baruch.sc.edu/). Given that pH is measured on a log scale, even relatively small changes in pH result in a considerable change in concentrations of hydrogen and hydroxide ions, which may have important physiological consequences for the resident biota.The effects of seasonal and diurnal hypercapnia experienced by estuarine organisms are likely to become exacerbated in the coming years due to global climate change and ocean acidification driven by anthropogenically released CO 2 (Caldeira & Wickett 2003. The uptake of atmospheric CO 2 is especially pronounced in surface ocean waters (< 250 m depth), where nearly 50% of anthropogenic CO 2 is absorbed, making near-shore habitats including estuaries vulnerable to ocean acidification (Feely et al. 2008, Doney e...