Competitive fitness of a predominant pelagic calcifier impaired by ocean acidification

• Published in: Nature Geoscience
• Main Authors: Riebesell, U, Bach, LT, Bellerby, RGJ, Monsalve, JRB, Boxhammer, T, Czerny, J, Larsen, A, Ludwig, A, Schulz, KG
• Format: Article in Journal/Newspaper
• Language: English
• Published: Nature Publishing Group 2017
• Subjects: Earth Sciences; Oceanography; Biological Oceanography; Ocean acidification
• Online Access: https://doi.org/10.1038/NGEO2854; http://ecite.utas.edu.au/133657

Coccolithophoressingle-celled calcifying phytoplanktonare an important group of marine primary producers and the dominant builders of calcium carbonate globally. Coccolithophores form extensive blooms and increase the density and sinking speed of organic matter via calcium carbonate ballasting. Thereby, they play a key role in the marine carbon cycle. Coccolithophore physiological responses to experimental ocean acidification have ranged from moderate stimulation to substantial decline in growth and calcification rates, combined with enhanced malformation of their calcite platelets. Here we report on a mesocosm experiment conducted in a Norwegian fjord in which we exposed a natural plankton community to a wide range of CO 2 -induced ocean acidification, to test whether these physiological responses affect the ecological success of coccolithophore populations. Under high-CO 2 treatments, Emiliania huxleyi , the most abundant and productive coccolithophore species, declined in population size during the pre-bloom period and lost the ability to form blooms. As a result, particle sinking velocities declined by up to 30% and sedimented organic matter was reduced by up to 25% relative to controls. There were also strong reductions in seawater concentrations of the climate-active compound dimethylsulfide in CO 2 -enriched mesocosms. We conclude that ocean acidification can lower calcifying phytoplankton productivity, potentially creating a positive feedback to the climate system.