Exploratory evaluation of iron and its speciation in surface waters of Admiralty Bay, King George Island, Antarctica

• Published in: Anais da Academia Brasileira de Ciências
• Main Authors: SHEISA F.D. SIERPINSKI, LUIS MIGUEL LAGLERA BAQUER, CÉSAR C. MARTINS, MARCO TADEU GRASSI
• Format: Article in Journal/Newspaper
• Language: English
• Published: Academia Brasileira de Ciências 2023
• Subjects: Ads-CSV; coastal waters; dissolved iron; iron biogeochemistry; Science; Q; Admiralty Bay; Austral; King George Island; Antarc*; Antarctica
• Online Access: https://doi.org/10.1590/0001-3765202320211520; https://doaj.org/article/76a7b0afdf3e4408b2416fa21b7834ce

Abstract The determination of dissolved iron concentrations and speciation was conducted for the first time in surface seawater coastline samples collected during the austral summer of 2020 in Admiralty Bay, King George Island, Antarctica. The technique of competitive ligand exchange/adsorptive cathodic stripping voltammetry with 2,3-dihydroxynaphthalene as the competing ligand was evaluated, showing a sensitivity between 14.25 and 21.05 nA nmol L-1 min-1, with an LOD of 14 pmol L-1 and a mean blank contribution of 0.248 nmol L-1. Physicochemical parameters such as pH (7.85 ± 0.2), salinity (32.7 ± 0.8) and dissolved oxygen (51.3 ± 26.6%) were compatible with those of the literature; however, the average temperature (4.2 ± 0.8 °C) was higher, possibly as a reflection of global warming. The dissolved iron mean value was 18.9 ± 6.1 nmol L-1, with a total ligand concentration of 23.6 ± 12.2 nmol L-1 and a conditional stability complex constant of 12.2 ± 0.2, indicating humic substances as possible ligands. On average, the calculated free iron concentrations were 0.7 ± 0.3 pmol L-1. Relatively high concentrations of iron indicate a possible local source of Fe, likely predominantly from upwelling sediments and secondarily from ice-melting waters, which does not limit the growth of the phytoplankton.