Interactive Effects of Ocean Acidification, Elevated Temperature, and Reduced Salinity on Early-Life Stages of the Pacific Oyster

• Published in: Environmental science & technology Vol. 48; no. 17; pp. 10079 - 10088
• Main Authors: Ko, Ginger W. K, Dineshram, R, Campanati, Camilla, Chan, Vera B. S, Havenhand, Jon, Thiyagarajan, Vengatesen
• Format: Journal Article
• Language: English
• Published: United States American Chemical Society 02.09.2014
• Subjects: Acidification; Acids - chemistry; Analysis of Variance; Animals; Carbonates - chemistry; Crassostrea - growth & development; Crassostrea gigas; Herbivores; Hydrogen-Ion Concentration; Larva - growth & development; Life Cycle Stages; Lipids; Marine; Microscopy, Fluorescence; Oysters; Pacific Ocean; Salinity; Seawater - chemistry; Temperature; Pacific Ocean; United States > US; INW, Huanghai Sea; INW, Asia; INE, USA, Pacific Northwest
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/es501611u

Ocean acidification (OA) effects on larvae are partially attributed for the rapidly declining oyster production in the Pacific Northwest region of the United States. This OA effect is a serious concern in SE Asia, which produces >80% of the world’s oysters. Because climate-related stressors rarely act alone, we need to consider OA effects on oysters in combination with warming and reduced salinity. Here, the interactive effects of these three climate-related stressors on the larval growth of the Pacific oyster, Crassostrea gigas, were examined. Larvae were cultured in combinations of temperature (24 and 30 °C), pH (8.1 and 7.4), and salinity (15 psu and 25 psu) for 58 days to the early juvenile stage. Decreased pH (pH 7.4), elevated temperature (30 °C), and reduced salinity (15 psu) significantly delayed pre- and post-settlement growth. Elevated temperature lowered the larval lipid index, a proxy for physiological quality, and negated the negative effects of decreased pH on attachment and metamorphosis only in a salinity of 25 psu. The negative effects of multiple stressors on larval metamorphosis were not due to reduced size or depleted lipid reserves at the time of metamorphosis. Our results supported the hypothesis that the C. gigas larvae are vulnerable to the interactions of OA with reduced salinity and warming in Yellow Sea coastal waters now and in the future.