Potentially bioavailable ferrous iron nanoparticles in glacial sediments

Iron (Fe) is an essential nutrient for marine phytoplankton, the primary producers of the ocean. Despite it being the fourth most abundant element in the Earth's crust, it is highly insoluble, due in part to its rapid oxidation from ferric (Fe2+) to ferrous phases (Fe3+), which often leads to the formation of nanoparticulate iron oxyhydroxide phases1. The insoluble nature of Fe in oxygenated waters means Fe limitation of primary producers is prevalent in 30-50% of the world's oceans, including areas of high biological productivity proximal to significant glacial activity (e.g., the Southern Ocean). Glaciers and ice sheets are a significant source of nanoparticulate Fe, which may be important in sustaining the high productivity observed in the near coastal regions proximal to glacial coverage. The reactivity of particulate iron is poorly understood, despite its importance in the ocean Fe inventory. Here we combined geochemical extractions, high-resolution imaging and spectroscopy to investigate the abundance, morphology and valence state of reactive iron in glacial sediments. Our results document the widespread occurrence of amorphous and Fe(II)-rich nanoparticles in glacial meltwaters and icebergs. Fe(II) is thought to be highly bioavailable in marine environments. We argue that glaciers and ice sheets are therefore able to supply potentially bioavailable Fe(II)-containing nanoparticulate material for downstream ecosystems, including those in a marine setting. The flux of bioavailable particulate iron from Arctic glaciers may increase as rising air temperatures lead to higher meltwater export.