[1] To characterize the concentrations and size distributions of water-soluble organic and inorganic aerosol species, including Na + , non-sea-salt sulfate (nss SO 4 2À ), methane sulfonate (MSA), oxalate, and succinate, over the Southern Ocean (SO) and coastal East Antarctica (CEA), bulk and size-segregated aerosols were collected from 40°S, 100°E to 69°S, 76°E and between 69°S, 76°E and 66°S, 110°E during a cruise from November 2010 to March 2011. Results show that sea salt was the major component of the total aerosol mass, accounting for 72% over the SO and 56% over CEA. The average concentrations of nss SO 4 2À varied from 420 ng m À3 over the SO to 480 ng m À3 over CEA. The concentrations of MSA ranged from 63 to 87 ng m À3 over the SO and from 46 to 170 ng m À3 in CEA. The average concentrations of oxalate were 3.8 ng m À3 over the SO and 2.2 ng m À3 over CEA. The concentrations of formate, acetate, and succinate were lower than those of oxalate. A bimodal size distribution of aerosol mass existed over CEA, peaking at 0.32-0.56 μm and 3.2-5.6 μm. MSA was accumulated in particles of 0.32-0.56 μm over CEA. High chloride depletion was associated with fine-mode particles enriched with nss SO 4 2À , MSA, and oxalate. Higher cation-to-anion and NH 4 + /nss SO 4 2À ratios in aerosols over CEA compared to that over the SO imply the higher neutralization capacity of the marine atmosphere over CEA.