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Effect of elevated CO2 on the community metabolism of an experimental coral reef.
Langdon, Chris1, Broecker, Wallace S.2, Hammond, Douglas E.3, Glenn, Edward4, Fitzsimmons, Kevin4, Nelson, Steven G.4, Peng, Tsung-Hung5, Hajdas, Irka6, 1 Biosphere 2 Center of Columbia University, Oracle, AZ2 Lamont-Doherty Earth Obs. of Columbia University, Palisades, NY3 Dept. of Earth Sciences, Uni. of S. California, Los Angeles, CA4 Environmental Research Laboratory, Uni. of Arizona, Tucson, AZ5 NOAA-AOML, Miami, FL6 IPP ETH Hoenggerberg, Zurich, Switzerland
ABSTRACT- The effect of elevated pCO2 on the metabolism of a coral reef community dominated by macroalgae has been investigated utilizing the large 2650 m3 coral reef mesocosm at the Biosphere-2 facility near Tucson, Arizona. The carbonate chemistry of the water was manipulated to simulate present day and a doubled CO2 future condition. Each experiment consisted of a 1-2 month preconditioning period followed by a 7-9 day observational period. The pCO2 was 404±63 atm during the present day pCO2 experiment and 658±59 atm during the elevated pCO2 experiment. Nutrient levels were low and typical of natural reefs waters (NO3- 0.5-0.9 M, NH4+ 0.4 M, PO43- 0.07-0.09 M). As previously observed, the increase in pCO2 resulted in a decrease in calcification from 0.041±0.007 to 0.006±0.003 mol CaCO3 m-2 d-1. Net community production (NCP) and dark respiration did not change in response to elevated pCO2. Light respiration measured by a new radiocarbon isotope dilution method exceeded dark respiration by a factor of 1.2±0.3 to 2.1±0.4 on a daily basis. The 1.8-fold increase with increasing pCO2 indicates that the enhanced respiration in the light was not due to photorespiration. Gross production (GPP) computed as the sum of NCP plus daily respiration (light+dark) increased significantly (0.24±0.03 vs. 0.32±0.04 mol C m-2 d-1). However, the conventional calculation of GPP based on the assumption that respiration in the light proceeds at the same rate as the dark underestimated the true rate of GPP by 41-100% and completely missed the increased rate of carbon cycling due to elevated pCO2. We conclude that under natural, undisturbed, nutrient-limited conditions elevated CO2 depresses calcification, stimulates the rate of turnover of organic carbon, particularly in the light, but has no effect on net organic production.
Key words: gross primary production, calcification, carbon cycling, light respiration