Use of radium isotopes to estimate mixing rates and trace sediment inputs to surface waters in northern Marguerite Bay, Antarctic Peninsula

• Published in: Antarctic Science
• Main Authors: Annett, Amber L., Henley, Sian F., Van Beek, Pieter, Souhaut, Marc, Ganeshram, Raja, Venables, Hugh J., Meredith, Michael P., Geibert, Walter
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2013
• Subjects: Chemistry; Antarctic; Southern Ocean; Antarctic Peninsula; Marguerite; Marguerite Bay; Ryder; Ryder Bay; Antarc*; Antarctic Science
• Online Access: http://nora.nerc.ac.uk/id/eprint/500524/; https://nora.nerc.ac.uk/id/eprint/500524/1/-ANS-ANS25_03-S0954102012000892a.pdf; https://doi.org/10.1017/S0954102012000892

In the western Antarctic Peninsula region, micronutrient injection facilitates strong plankton blooms that support productive food webs, unlike large areas of the low-productivity Southern Ocean.We use naturally occurring radioisotopes of radium to constrain rates of chemical fluxes into Ryder Bay (a small coastal embayment in northern Marguerite Bay), and hence to evaluate possible sources of sediment-derived micronutrients and estimate sediment-ocean mixing rates. We present the first coupled, short-lived radium isotope (223Ra and 224Ra) measurements from Antarctic waters, both present at very low activities (mean 0.155 and 3.21 dpmm-3, respectively), indicating much lower radium inputs than in other coastal environments. Longer-lived 228Ra activity was also lower than existing nearshore values, but higher than open ocean waters, indicating some degree of coastal radium input on timescales exceeding the week-to-month range reflected by 223Ra and 224Ra. Using a simple diffusion model along a shore to mid-bay transect, effective horizontal eddy diffusivity estimates ranged from 0.22–0.83m2 s-1 from 223Ra and 224Ra, respectively, much lower than already-low mixing estimates for the Southern Ocean. Significant radium enrichment and much faster mixing (18m2 s-1) was found near a marine-terminating glacier and consequently any sediment-derived micronutrient inputs in this location are more probably dominated by glacial processes than groundwater, land runoff, or marine sediment sources.