4.7 Article

High precision measurements of Mg/Ca and Sr/Ca ratios in carbonates by cold plasma inductively coupled plasma quadrupole mass spectrometry

Journal

CHEMICAL GEOLOGY
Volume 236, Issue 3-4, Pages 339-349

Publisher

ELSEVIER
DOI: 10.1016/j.chemgeo.2006.10.010

Keywords

cold ICP-QMS; Mg/Ca; Sr/Ca; carbonate; foraminifera; coral

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We present a new high precision analytical method for the determination of Mg/Ca and Sr/Ca ratios in carbonates using an inductively coupled plasma quadrupole mass spectrometer (ICP-QMS) with a 650-W cold plasma technique and a desolvation introduction system. Signal intensities are detected in pulse-counting mode and Mg/Ca and Sr/Ca ratios are calculated directly from intensity ratios of Mg-24/Ca-43 and Sr-86/Ca-43 using external matrix-matched standards for every 4-5 samples to correct for instrumental mass discrimination and low-frequency ratio drift. Significant matrix effect of Ca content on Mg/Ca determination (-0.018 Mg/Ca (mmol/mol)/[Ca] (ppm)), can be overcome by diluting [Ca] to 6-8 ppm in the sample solution or using an empirical correction. The Sr/Ca ratio affects the Mg/Ca determination, with a factor of -0.32% Mg/Ca per mmol/mol. This is mainly caused by the influence of doubly charged Sr-86, which biases the intensity measurement of the Ca-43(+) ion beam. This effect results in a trivial offset of less than 0.1% on Mg/Ca measurements for Quatemary foraminiferal and coral samples. The internal precision of our method ranges from 0.1 to 0.2%. Replicate measurements made on standards and samples show long-term external uncertainties (2 sigma) of Mg/Ca=0.84% and Sr/Ca=0.49%. The minimum sample size requirement is only 3.5 mu g of carbonate. The application of this newly developed technique on the planktonic foraminifera Globigerinoides ruber from a core recovered in the southern South China Sea yields a glacial-interglacial difference in sea surface temperature (SST) of 3 degrees C. Three-year coral Sr/Ca data suggest that the seasonal SST ranged from 22.6-23.8 degrees C in winter to 26.9-27.9 degrees C in summer in Nanwan, south Taiwan, during 2000-2002. The coral-Sr/Ca inferred SSTs in 2002 match well with instrumental records, which demonstrates the validity of this ICP-QMS method. (c) 2006 Elsevier B.V. All rights reserved.

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