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

Part of: Antarctic Science International Bursary collection: Geosciences

Published online by Cambridge University Press:  29 October 2012

Amber L. Annett ,
Sian F. Henley ,
Pieter Van Beek ,
Marc Souhaut ,
Raja Ganeshram ,
Hugh J. Venables ,
Michael P. Meredith  and
Walter Geibert
Amber L. Annett*
Affiliation:
School of GeoSciences, University of Edinburgh, EdinburghEH9 3JW, UK
Sian F. Henley
Affiliation:
School of GeoSciences, University of Edinburgh, EdinburghEH9 3JW, UK
Pieter Van Beek
Affiliation:
Laboratoire d'Etudes en Geophysique et Oceanographie Spatiales (CNRS/UPS/IRD/CNES), Observatoire Midi Pyrénées, Toulouse, France
Marc Souhaut
Affiliation:
Laboratoire d'Etudes en Geophysique et Oceanographie Spatiales (CNRS/UPS/IRD/CNES), Observatoire Midi Pyrénées, Toulouse, France
Raja Ganeshram
Affiliation:
School of GeoSciences, University of Edinburgh, EdinburghEH9 3JW, UK
Hugh J. Venables
Affiliation:
British Antarctic Survey, NERC, High Cross, Madingley Road, Cambridge CB3 0ET, UK
Michael P. Meredith
Affiliation:
British Antarctic Survey, NERC, High Cross, Madingley Road, Cambridge CB3 0ET, UK
Walter Geibert
Affiliation:
School of GeoSciences, University of Edinburgh, EdinburghEH9 3JW, UK Scottish Association for Marine Science (SAMS), Scottish Marine Institute, Oban, UK
*
[email protected]
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Abstract

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 dpm m-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 0.22–0.83 m2 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 (18 m2 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.

Keywords

actinium-227glacial inputshorizontal eddy diffusivityland-ocean interfaceRadium Delayed Coincidence Counter (RaDeCC)Ryder Bay
Type
Physical Sciences
Information
Antarctic Science , Volume 25 , Issue 3 , June 2013 , pp. 445 - 456
Copyright
Copyright © Antarctic Science Ltd 2012 

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