Peixe Zircon as a Quality Control Reference Material in U‐Pb Geochronology by <scp>LA</scp> ‐ <scp>ICP</scp> ‐ <scp>MS</scp>

A megacryst zircon from Brazil, referred to here as Peixe#0, was evaluated as a potential reference material for LA‐ICP‐MS U‐Pb dating. Results from multi‐method characterisation – including CA‐ID‐TIMS, SIMS and a long‐term LA‐ICP‐MS data set – enabled us to assess this crystal's suitability as a reference material for routine quality control in age determinations by LA‐ICP‐MS. Using CA‐ID‐TIMS, Peixe#0 yielded mean 206 Pb/ 238 U and 207 Pb/ 235 U ratios of 0.09257 ± 0.1% and 0.7561 ± 0.1%, respectively (precisions expressed as 2RSD), and weighted mean 206 Pb/ 238 U age of 570.85 ± 0.30 Ma (2 s , MSWD = 0.40, n = 4). With the LA‐ICP‐MS compiled database (2063 individual age determinations distributed over 167 sessions spanning eight years) acquired during routine analysis at the Isotope Geology Laboratory (LAGIS) at Unicamp, Brazil, we propose a 206 Pb/ 238 U weighted mean age of 569 ± 13 Ma (2 s ), which includes the long‐term excess variance in the total uncertainty. Oxygen isotopes presented a homogeneous distribution (δ 18 O SMOW = +5.13 ± 0.15‰ (1 s )). The trace element chemical compositions varied substantially depending on the chosen cathodoluminescence zone containing distinct features. Approximately 4 g of Peixe#0 zircon are available for distribution upon request.

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Journal
Geostandards and Geoanalytical Research
Published
2026-02-04
DOI
https://doi.org/10.1111/ggr.70033
Primary Topic
Geological and Geochemical Analysis
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article
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article

Peixe Zircon as a Quality Control Reference Material in U‐Pb Geochronology by LA ‐ ICP ‐ MS

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Geostandards and Geoanalytical Research
Geological and Geochemical Analysis
article

Peixe Zircon as a Quality Control Reference Material in U‐Pb Geochronology by LA ‐ ICP ‐ MS

Jacinta Enzweiler, Érica Martini Tonetto, Margareth Sugano Navarro, Neal J. McNaughton, Michael Wiedenbeck, Elson P. Oliveira, Mauricio Ibañez‐Mejia
article en

Abstract

A megacryst zircon from Brazil, referred to here as Peixe#0, was evaluated as a potential reference material for LA‐ICP‐MS U‐Pb dating. Results from multi‐method characterisation – including CA‐ID‐TIMS, SIMS and a long‐term LA‐ICP‐MS data set – enabled us to assess this crystal's suitability as a reference material for routine quality control in age determinations by LA‐ICP‐MS. Using CA‐ID‐TIMS, Peixe#0 yielded mean 206 Pb/ 238 U and 207 Pb/ 235 U ratios of 0.09257 ± 0.1% and 0.7561 ± 0.1%, respectively (precisions expressed as 2RSD), and weighted mean 206 Pb/ 238 U age of 570.85 ± 0.30 Ma (2 s , MSWD = 0.40, n = 4). With the LA‐ICP‐MS compiled database (2063 individual age determinations distributed over 167 sessions spanning eight years) acquired during routine analysis at the Isotope Geology Laboratory (LAGIS) at Unicamp, Brazil, we propose a 206 Pb/ 238 U weighted mean age of 569 ± 13 Ma (2 s ), which includes the long‐term excess variance in the total uncertainty. Oxygen isotopes presented a homogeneous distribution (δ 18 O SMOW = +5.13 ± 0.15‰ (1 s )). The trace element chemical compositions varied substantially depending on the chosen cathodoluminescence zone containing distinct features. Approximately 4 g of Peixe#0 zircon are available for distribution upon request.

Geostandards and Geoanalytical Research
University of Arizona (US), James Hutton Institute (GB), Universidade Estadual de Campinas (UNICAMP) (BR), Curtin University (AU), GFZ Helmholtz Centre for Geosciences (DE), Massachusetts Institute of Technology (US), University of Edinburgh (GB)
Openalex Percentile: Top 75%
Geological and Geochemical Analysis
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