Sub‐Permil Interlaboratory Consistency for Solution‐Based Boron Isotope Analyses on Marine Carbonates - Archive ouverte HAL
Article Dans Une Revue Geostandards and Geoanalytical Research Année : 2021

Sub‐Permil Interlaboratory Consistency for Solution‐Based Boron Isotope Analyses on Marine Carbonates

Pascale Louvat
Ilia Rodushkin
  • Fonction : Auteur

Résumé

Boron isotopes in marine carbonates are increasingly used to reconstruct seawater pH and atmospheric pCO 2 through Earth's history. While isotope ratio measurements from individual laboratories are often of high quality, it is important that records generated in different laboratories can equally be compared. Within this Boron Isotope Intercomparison Project (BIIP), we characterised the boron isotopic composition (commonly expressed in δ 11 B) of two marine carbonates: Geological Survey of Japan carbonate reference materials JCp-1 (coral Porites) and JCt-1 (giant clam Tridacna gigas). Our study has three foci: (a) to assess the extent to which oxidative pre-treatment, aimed at removing organic material from carbonate, can influence the resulting δ 11 B; (b) to determine to what degree the chosen analytical approach may affect the resultant δ 11 B; and (c) to provide well-constrained consensus δ 11 B values for JCp-1 and JCt-1. The resultant robust mean and associated robust standard deviation (s*) for un-oxidised JCp-1 is 24.36 AE 0.45‰ (2s*), compared with 24.25 AE 0.22‰ (2s*) for the same oxidised material. For un-oxidised JCt-1, respective compositions are 16.39 AE 0.60‰ (2s*; un-oxidised) and 16.24 AE 0.38‰ (2s*; oxidised). The consistency between laboratories is generally better if carbonate powders were oxidatively cleaned prior to purification and measurement.
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hal-03026894 , version 1 (01-04-2021)

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Marcus Gutjahr, Louise Bordier, Éric Douville, Jesse Farmer, Gavin Foster, et al.. Sub‐Permil Interlaboratory Consistency for Solution‐Based Boron Isotope Analyses on Marine Carbonates. Geostandards and Geoanalytical Research, 2021, 45 (1), pp.59 - 75. ⟨10.1111/ggr.12364⟩. ⟨hal-03026894⟩
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