The macronutrient and micronutrient (iron and manganese) signature of icebergs

• Main Authors: Krause, Jana, Carroll, Dustin, Höfer, Juan, Donaire, Jeremy, Achterberg, Eric Pieter, Alarcón, Emilio, Liu, Te, Meire, Lorenz, Zhu, Kechen, Hopwood, Mark James
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications (EGU) 2024
• Subjects: Antarctic; Antarctic Peninsula; Arctic; Greenland; Patagonia; Southern Ocean; Svalbard; The Antarctic; Antarc*; Iceberg*; Iceland
• Online Access: https://oceanrep.geomar.de/id/eprint/59799/; https://oceanrep.geomar.de/id/eprint/59799/1/egusphere-2023-2991.pdf; https://oceanrep.geomar.de/id/eprint/59799/2/egusphere-2023-2991-supplement.zip; https://doi.org/10.5194/egusphere-2023-2991

Ice calved from the Antarctic and Greenland Ice Sheets or tidewater glaciers ultimately melts in the ocean contributing to sea-level rise. Icebergs have also been described as biological hotspots due to their potential roles as platforms for marine mammals and birds, and as micronutrient fertilizing agents. Icebergs may be especially important in the Southern Ocean where availability of the micronutrients iron and manganese extensively limits marine primary production. Whilst icebergs have long been described as a source of iron to the ocean, their nutrient signature is poorly constrained and it is unclear if there are regional differences. Here we show that 589 ice fragments collected from floating ice in contrasting regions spanning the Antarctic Peninsula, Greenland, and smaller tidewater systems in Svalbard, Patagonia and Iceland have similar characteristic (micro)nutrient signatures with limited or no significant differences between regions. Icebergs are a minor or negligible source of macronutrients to the ocean with low concentrations of NOx (NO3 + NO2, median 0.51 µM), PO4 (median 0.04 µM), and dissolved Si (dSi, median 0.02 µM). In contrast, icebergs deliver elevated concentrations of dissolved Fe (dFe; mean 82 nM, median 12 nM) and Mn (dMn; mean 26 nM, median 2.6 nM). A tight correlation between total dissolvable Fe and Mn (R2 = 0.95) and a Mn:Fe ratio of 0.024 suggested a lithogenic origin for the majority of sediment present in ice. Total dissolvable Fe and Mn retained a strong relationship with sediment load (both R2 = 0.43, p<0.001), whereas weaker relationships were observed for dFe, dMn and dSi. Sediment load for Antarctic ice (median 9 mg L-1, n=144) was low compared to prior reported values for the Arctic. A particularly curious incidental finding was that melting samples of ice were observed to rapidly lose their sediment load, even when sediment layers were embedded within the ice and stored in the dark. Our results demonstrated that the nutrient signature of icebergs is consistent with an ...