Acid rock drainage and rock weathering in antarctica: Important sources for iron cycling in the southern ocean

• Published in: Environmental Science & Technology
• Main Authors: Dold B., González-Toril, Elena, Aguilera, Ángeles, López Pamo, Enrique, Cisternas, M. E., Bucchi, F., Amils, Ricardo
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Chemical Society 2013
• Subjects: Antarctic; Antarctic Ocean; South Shetland Islands; Southern Ocean; The Antarctic; Antarc*; Antarctica; Sea ice
• Online Access: http://hdl.handle.net/10261/95265; https://doi.org/10.1021/es305141b

Here we describe biogeochemical processes that lead to the generation of acid rock drainage (ARD) and rock weathering on the Antarctic landmass and describe why they are important sources of iron into the Antarctic Ocean. During three expeditions, 2009-2011, we examined three sites on the South Shetland Islands in Antarctica. Two of them displayed intensive sulfide mineralization and generated acidic (pH 3.2-4.5), iron-rich drainage waters (up to 1.78 mM Fe), which infiltrated as groundwater (as Fe2+) and as superficial runoff (as Fe3+) into the sea, the latter with the formation of schwertmannite in the sea-ice. The formation of ARD in the Antarctic was catalyzed by acid mine drainage microorganisms found in cold climates, including Acidithiobacillus ferrivorans and Thiobacillus plumbophilus. The dissolved iron (DFe) flux from rock weathering (nonmineralized control site) was calculated to be 0.45 × 109 g DFe yr-1 for the nowadays 5468 km of ice-free Antarctic rock coastline which is of the same order of magnitude as glacial or aeolian input to the Southern Ocean. Additionally, the two ARD sites alone liberate 0.026 and 0.057 × 109 g DFe yr-1 as point sources to the sea. The increased iron input correlates with increased phytoplankton production close to the source. This might even be enhanced in the future by a global warming scenario, and could be a process counterbalancing global warming. © 2013 American Chemical Society. MINECO (CGL2011/22540 and CTM2011-1477-E) Peer Reviewed