Development of in situ sulfur four-isotope analysis with multiple Faraday cup detectors by SIMS and application to pyrite grains in a Paleoproterozoic glaciogenic sandstone

Takayuki Ushikubo, Kenneth H. Williford, James Farquhar, David T. Johnston, Martin Van Kranendonk, John W. Valley

Research output: Contribution to journalArticle

28 Citations (Scopus)

Abstract

An in situ sulfur four-isotope analysis technique with multiple Faraday cup detectors by ion microprobe was developed and applied to detrital pyrite grains in ~2.4Ga glaciogenic sandstone from the Meteorite Bore Member of the Turee Creek Group, Western Australia. Data are standardized with the UWPy-1 pyrite standard (δ34S=16.04±0.18‰, δ33S=-0.003±0.009‰, and δ36S=-0.21±0.24‰, 2 SD) whose sulfur four isotopes were newly determined by gas-source mass spectrometry. Typical reproducibility at two standard deviations (2 SD) of spot-to-spot analyses of standard UWPy-1 pyrite with a primary beam size of ~20μm were ±0.23, ±0.05, and ±0.86‰ for δ34S, δ33S, and δ36S, respectively. The measured 36S/32S ratio [1/(6641±27)] is approximately 19‰ lower than the published ratio for VCDT, and we propose a revision of the 36S abundance in VCDT.Pyrite grains in ~2.4Ga glaciogenic sandstone have wide ranging sulfur isotope ratios (-32.7 to 13.5 for δ34S, -3.03 to 11.66 for δ33S, and -9.7 to 4.6 for δ36S, respectively). Some pyrite grains are zoned in δ34S values within a grain. Sulfur isotope ratios of most pyrite grains are distributed along a line with slope=-0.9 for δ33S vs. δ36S, suggesting that pyrite grains mostly derived from a limited range of source rocks and near-surface sulfur reservoirs. One pyrite aggregate has a distinct texture from other pyrite grains in the same sandstone, and yields a significant mass-independent deficit in 36S with a small excess in 33S (δ36S/δ33S~-4‰). This is used to suggest that this grain authigenically formed by biological activity during or after sedimentation. This work demonstrates that the use of multiple Faraday cup detectors provides improved accuracy and precision for in situ sulfur four-isotope analysis with secondary ion mass spectrometry.

Original languageEnglish
Pages (from-to)86-99
Number of pages14
JournalChemical Geology
Volume383
DOIs
Publication statusPublished - Sep 15 2014
Externally publishedYes

Fingerprint

Secondary ion mass spectrometry
Sandstone
Sulfur
Isotopes
pyrite
sulfur
sandstone
isotope
Detectors
Sulfur Isotopes
sulfur isotope
mass spectrometry
Meteorites
analysis
detector
in situ
ion microprobe
Bioactivity
Sedimentation
meteorite

Keywords

  • Ion microprobe
  • Pyrite
  • S-MIF
  • SIMS
  • Sulfur isotope

ASJC Scopus subject areas

  • Geology
  • Geochemistry and Petrology

Cite this

Development of in situ sulfur four-isotope analysis with multiple Faraday cup detectors by SIMS and application to pyrite grains in a Paleoproterozoic glaciogenic sandstone. / Ushikubo, Takayuki; Williford, Kenneth H.; Farquhar, James; Johnston, David T.; Van Kranendonk, Martin; Valley, John W.

In: Chemical Geology, Vol. 383, 15.09.2014, p. 86-99.

Research output: Contribution to journalArticle

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