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Determination of low-level mercury in coralline aragonite by calcination-isotope dilution-inductively coupled plasma-mass spectrometry and its application to Diploria specimens from Castle Harbour, Bermuda

Carl H. Lamborg·Gretchen J. Swarr·Konrad A. Hughen·Ross J. Jones·Scott Birdwhistell·Kathryn Furby·Sujata A. Murty·Nancy G. Prouty·Chun-Mao Tseng
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Abstract

We have developed a technique that combines a high temperature quartz furnace with inductively coupled plasma-mass spectrometry for the determination of Hg stored in the annual CaCO 3 bands found in coral skeletons. Substantial matrix effects, presumably due to the discontinuous introduction of CO 2 to the gas stream, were corrected for by simultaneously supplying a stream of argon containing highly enriched elemental 202 Hg o and observing peaks in the 200 Hg/ 202 Hg signal as the sample was decomposed. Primary signal calibration for Hg was achieved using gas injections from a saturated vapor standard. The absolute instrument detection limit was low (about 0.2 fmol), with a practical limit of detection (3 σ of blanks) of 2 fmol. Reproducibility of samples was (RSD) 15–27%. We applied this method to the determination of Hg concentrations in two colonies of Diploria labyrinthiformis collected from Castle Harbour, Bermuda, at a site about to be buried under the municipal waste landfill. The temporal reconstructions of Castle Harbour seawater Hg concentrations implied by the coral record show a decline throughout the period of record (1949–2008). The coral archived no apparent signal associated with waste disposal practices in the Harbour (bulk waste land-filling or, since 1994, disposal of waste incinerator ash), and mercury concentrations in the coral did not correlate to growth rate as assessed by linear extension. There was, however, a large and nearly exponential decrease in apparent Hg concentration in the Harbour which circumstantially implicates the dredging and/or landfilling operations associated with the construction of the airport on St. David’s Island.

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Geochimica et Cosmochimica ActaArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 32.3271767410611° to 32.394167471465536° latitude; -64.7317886352539° to -64.63497161865234° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Carl H. Lamborg, Gretchen J. Swarr, Konrad A. Hughen, Ross J. Jones, Scott Birdwhistell, Kathryn Furby, Sujata A. Murty, Nancy G. Prouty, Chun-Mao Tseng. 2013. Determination of low-level mercury in coralline aragonite by calcination-isotope dilution-inductively coupled plasma-mass spectrometry and its application to Diploria specimens from Castle Harbour, Bermuda. https://doi.org/10.1016/j.gca.2013.01.026

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