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Based upon fourteen field surveys conducted between 2003 and 2008, we showed that the seasonal pattern of sea surface partial pressure of CO2 (pCO2) and air-sea CO2 fluxes differed among four different physical-biogeochemical domains in the South China Sea (SCS) proper. The four domains were located between 4 and 23 °N and 109 and 121 °E, covering ~38% of the surface area of the entire SCS. In the area off the Pearl River Estuary, relatively low pCO2 values of 320 to 390 µatm were observed in all four seasons and both the biological productivity and CO2 uptake were enhanced in summer in the Pearl River plume waters. In the northern SCS slope/basin area, a typical seasonal cycle of relatively high pCO2 in the warmer seasons and relatively low pCO2 in the cold seasons was revealed. In the central/southern SCS area, moderately high sea surface pCO2 values of 360 to 425 µatm were observed throughout the year. In the area west of the Luzon Strait, a major exchange pathway between the SCS and the Pacific Ocean, pCO2 was particularly dynamic in winter, when northeast monsoon induced upwelling events and strong outgassing of CO2. These episodic events might have dominated the annual air-sea CO2 flux in this particular area. The estimate of annual sea-air CO2fluxes showed that, most areas of the SCS proper served as weak sources to the atmospheric CO2, with sea-air CO2 flux values of 0.46±0.43 molm-2 yr-1 in the northern SCS slope/basin, 1.37±0.55 molm-2 yr-1 in the central/southern SCS, and 1.21±1.47 molm-2 yr-1 in the area west of the Lu- zon Strait. However, the annual sea-air CO2 exchange was nearly in equilibrium (-0.44±0.65 molm-2 yr-1) in the area off the Pearl River Estuary. Overall the four domains released (18±10)x1012 gCyr-1 into the atmosphere. The CO2 release rate of the South China Sea essentially exceeded the average CO2 emission level of most tropical oceans [ABSTRACT FROM AUTHOR]