Y. Rosenthal et al., Precise determination of element/calcium ratios in calcareous samples using sector field inductively coupled plasma mass spectrometry, ANALYT CHEM, 71(15), 1999, pp. 3248-3253
A new method was developed for rapid and precise simultaneous determination
of Mg/Ca, Sr/Ca, Mn/Ca, Cd/Ca, Ba/Ca and U/Ca ratios in foraminiferal shel
ls using sector field inductively coupled plasma mass spectrometry (ICPMS).
Element/calcium ratios were determined directly from intensity ratios usin
g external, matrix-matched standard to correct for instrumental mass discri
mination, Because of large differences in the abundance of chemical constit
uents of the foraminiferal shell, major elemental ratios were determined in
analog mode (using Mg-24, Ca-43, Ca-44, Mn-55, and Sr-88) whereas trace el
emental ratios were determined in pulse-counting mode (using Cd-111, Ba-138
, U-238, and the low-abundance Ca-46 isotope). Matrix-induced variations in
mass discrimination over a calcium concentration range of 2.0-24.5 mM were
observed only for Mg/Ca and Cd/Ca ratios. However, these effects are negli
gible if the samples and standard calcium concentration are within a factor
of 2-3. Multi-ratio method reproducibility was better than previously repo
rted for other ICPMS methods yielding precision (1 sigma) of Sr/Ca = 0.45%;
Mg/Ca = 0.45%, Mn/Ca = 0.8%, Cd/Ca = 1.7%, Ba/Ca = 0.7%, and U/Ca = 1.4% f
or foraminifera samples as small as 25 mu g. Using this approach for a sing
le-ratio analysis, Sr/Ca ratios were determined with precision of 0.06% (1
sigma) on carbonate samples as small as a single foraminifera shell (<10 mu
g). The new method is more sensitive, more precise, and simpler to use tha
n previously available ICPMS techniques. It provides an efficient tool for
simultaneous determination of several elemental ratios of paleoceanographic
interest in a single foraminiferal sample, thereby reducing overall sample
size requirement and analysis time.