Chemical composition of precipitation at Marion Island (sub-Antarctic)

Over a 1-year period 16.40g Cl⁻m⁻², 10.35 g Na m⁻², 2.11 g SO₄-S m⁻², 1.24g Mg m⁻², 0.39 g K m⁻², 0.37 g Ca m⁻² and 0.21 g inorganic N m⁻² were deposited in precipitation 450 m inland on the eastern coastal plain of sub-Antarctic Marion Island (46°54′S, 37°45′E). Dissolved PO₄-P and organic forms of N were not detected in the precipitation samples. Concentrations of Cl⁻, Na, Mg, Ca and K, as well as the total ionic concentration in the precipitation samples were significantly negatively correlated with the amount of precipitation. The ionic concentration order (Cl > Na > SO₄-S > Mg > K ≈ Ca) in the precipitation was very similar to that in the surrounding ocean. It is likely that most of the inorganic N found in the precipitation originated in penguin rookeries on the nearby shore zone. A comparison is made between precipitation inputs of nutrients at the island and those at other subpolar sites in the S and N Hemispheres.