Abstract

RationaleLi and Mg isotopes are increasingly used as a combined tool within the geosciences. However, established methods require separate sample purification protocols utilising several column separation procedures. This study presents a single‐step cation‐exchange method for quantitative separation of trace levels of Li and Mg from multiple sample matrices.MethodsThe column method utilises the macro‐porous AGMP‐50 resin and a high‐aspect ratio column, allowing quantitative separation of Li and Mg from natural waters, sediments, rocks and carbonate matrices following the same elution protocol. High‐precision isotope determination was conducted by multi‐collector inductively coupled plasma mass spectrometry (MC‐ICPMS) on the Thermo Scientific™ NEPTUNE Plus™ fitted with 1013 Ω amplifiers which allow accurate and precise measurements at ion beams ≤0.51 V.ResultsSub‐nanogram Li samples (0.3–0.5 ng) were regularly separated (yielding Mg masses of 1–70 μg) using the presented column method. The total sample consumption during isotopic analysis is <0.5 ng Li and <115 ng Mg with long‐term external 2σ precisions of ±0.39‰ for δ7Li and ±0.07‰ for δ26Mg. The results for geological reference standards and seawater analysed by our method are in excellent agreement with published values despite the order of magnitude lower sample consumption.ConclusionsThe possibility of eluting small sample masses and the low analytical sample consumption make this method ideal for samples of limited mass or low Li concentration, such as foraminifera, mineral separates or dilute river waters.

Highlights

  • Lithium and magnesium stable isotope geochemistry has the potential to provide insights into low‐ and high‐temperature geological processes such as weathering of the continental and oceanic crust (e.g.1-10), cycling of material through the crust and mantle (e.g.11-15) and cosmochemical processes (e.g.16-18)

  • Significant mass‐dependent isotope fractionations may occur during chemical purification and mass spectrometric measurements

  • Isotope ratio determination of Li and Mg is achieved by multi‐ collector inductively coupled plasma mass spectrometry (MC‐ICPMS)

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Summary

Methods

The column method utilises the macro‐porous AGMP‐50 resin and a high‐aspect ratio column, allowing quantitative separation of Li and Mg from natural waters, sediments, rocks and carbonate matrices following the same elution protocol. High‐precision isotope determination was conducted by multi‐collector inductively coupled plasma mass spectrometry (MC‐ICPMS) on the Thermo ScientificTM NEPTUNE PlusTM fitted with 1013 Ω amplifiers which allow accurate and precise measurements at ion beams ≤0.51 V

Results
| INTRODUCTION
| RESULTS
| DISCUSSION
This study
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