TY - JOUR A1 - Engel, Anja A1 - Piontek, Judith A1 - Grossart, Hans-Peter A1 - Riebesell, Ulf A1 - Schulz, Kai Georg A1 - Sperling, Martin T1 - Impact of CO2 enrichment on organic matter dynamics during nutrient induced coastal phytoplankton blooms JF - Journal of plankton research N2 - A mesocosm experiment was conducted to investigate the impact of rising fCO(2) on the build-up and decline of organic matter during coastal phytoplankton blooms. Five mesocosms (similar to 38 mA(3) each) were deployed in the Baltic Sea during spring (2009) and enriched with CO2 to yield a gradient of 355-862 A mu atm. Mesocosms were nutrient fertilized initially to induce phytoplankton bloom development. Changes in particulate and dissolved organic matter concentrations, including dissolved high-molecular weight (> 1 kDa) combined carbohydrates, dissolved free and combined amino acids as well as transparent exopolymer particles (TEP), were monitored over 21 days together with bacterial abundance, and hydrolytic extracellular enzyme activities. Overall, organic matter followed well-known bloom dynamics in all CO2 treatments alike. At high fCO(2,) higher Delta POC:Delta PON during bloom rise, and higher TEP concentrations during bloom peak, suggested preferential accumulation of carbon-rich components. TEP concentration at bloom peak was significantly related to subsequent sedimentation of particulate organic matter. Bacterial abundance increased during the bloom and was highest at high fCO(2). We conclude that increasing fCO(2) supports production and exudation of carbon-rich components, enhancing particle aggregation and settling, but also providing substrate and attachment sites for bacteria. More labile organic carbon and higher bacterial abundance can increase rates of oxygen consumption and may intensify the already high risk of oxygen depletion in coastal seas in the future. KW - mesocosm KW - ocean acidification KW - phytoplankton KW - organic matter KW - TEP Y1 - 2014 U6 - https://doi.org/10.1093/plankt/fbt125 SN - 0142-7873 SN - 1464-3774 VL - 36 IS - 3 SP - 641 EP - 657 PB - Oxford Univ. Press CY - Oxford ER -