Ocean Acidification

Coastal and offshore waters in the South China Sea are warming and becoming acidified due to rising atmospheric levels of carbon dioxide (CO₂), yet the combined effects of these two stressors are poorly known. Here, we carried out shipboard incubations at ambient (398 μatm) and elevated (934 μatm) pCO₂ at in situ and in situ+1.8 °C temperatures and we measured primary productivity at two coastal and two offshore stations. Both warming and increased CO₂ levels individually increased phytoplankton productivity at all stations, but the combination of high temperature and high CO₂ did not, reflecting an antagonistic effect. Warming decreased Chl a concentrations in off-shore waters at ambient CO₂, but had no effect in the coastal waters. The high CO₂ treatment increased night time respiration in the coastal waters at ambient temperatures. Our findings show that phytoplankton assemblage responses to rising temperature and CO₂ levels differ between coastal and offshore waters. While it is difficult to predict how ongoing warming and acidification will influence primary productivity in the South China Sea, our data imply that predicted increases in temperature and pCO₂ will not boost surface phytoplankton primary productivity.