Early life stages of the Arctic copepod Calanus glacialis are unaffected by increased seawater pCO2

• Published in: ICES Journal of Marine Science
• Main Authors: Bailey, Allison, Thor, Peter, Browman, Howard I., Fields, David M., Runge, Jeffrey, Vermont, Alexander, Bjelland, Reidun, Thompson, Cameron, Shema, Steven, Durif, Caroline M. F., Hop, Haakon
• Other Authors: Norkko, Joanna, Research Council of Norway, Institute of Marine Research, National Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Oxford University Press (OUP) 2016
• Subjects: Arctic; Svalbard; Norway; Arctic copepod; Calanus glacialis; Ocean acidification; Sea ice
• Online Access: http://dx.doi.org/10.1093/icesjms/fsw066; http://academic.oup.com/icesjms/article-pdf/74/4/996/31245946/fsw066.pdf

As the world's oceans continue to absorb anthropogenic CO2 from the atmosphere, the carbonate chemistry of seawater will change. This process, termed ocean acidification, may affect the physiology of marine organisms. Arctic seas are expected to experience the greatest decreases in pH in the future, as changing sea ice dynamics and naturally cold, brackish water, will accelerate ocean acidification. In this study, we investigated the effect of increased pCO2 on the early developmental stages of the key Arctic copepod Calanus glacialis. Eggs from wild-caught C. glacialis females from Svalbard, Norway (80°N), were cultured for 2 months to copepodite stage C1 in 2°C seawater under four pCO2 treatments (320, 530, 800, and 1700 μatm). Developmental rate, dry weight, and carbon and nitrogen mass were measured every other day throughout the experiment, and oxygen consumption rate was measured at stages N3, N6, and C1. All endpoints were unaffected by pCO2 levels projected for the year 2300. These results indicate that naupliar development in wild populations of C. glacialis is unlikely to be detrimentally affected in a future high CO2 ocean.