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Delta 5 advantage ms

Manufactured by Thermo Fisher Scientific
Sourced in Germany

The Delta V Advantage MS is a mass spectrometry instrument designed for high-performance isotope ratio analysis. It provides precise and accurate measurement of stable isotope ratios for a wide range of applications, including environmental research, geochemistry, and food authenticity analysis.

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2 protocols using delta 5 advantage ms

1

Stable Isotope Analysis of Dental Enamel

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Specimens selected all had excellent preservation conditions, and no weathered or fragmented dental specimens were considered. Teeth were cleaned using air-abrasion. Sample of enamel powder (6 mg) was taken from buccal edge using diamond-tipped burr drill. It was washed in 1.5% NaClO for 60 min, rinsed, then centrifuged. It was then washed with acetic acid (0.1 M) for 10 min and rinsed. Residue was lyophilised for 24 h, then set to react with H3PO4 and gases were measured for stable carbon and oxygen ratios using GasBench II (Thermo) coupled with Delta V Advantage MS (Thermo). Values were compared against International Standards: IAEA-603 (δ13C = 2.5; δ18O = −2.4); IAEA-CO-8 (δ13C = −5.8; δ18O = −22.7); USGS44 (δ13C = −42.2), and in-house standard MERCK (δ13C = −41.3; δ18O = −14.4). Measurement error of MERCK standard c was ±0.1‰ for δ13C and ±0.2‰ for δ18O. Overall precision of measurements through repeat extracts from an in-house bovid tooth enamel standard c was ±0.2‰ for δ13C and ±0.3‰. Obligate or non-obligate drinking status was inferred from the range of δ18O as per references72 (link)–74 (link).
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2

Enamel Isotope Analysis Protocol

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Enamel samples were drilled (Balasse et al., 2003) , on the posterior (M2), middle (lower M3) or anterior lobe (upper M3). The archaeological enamel powders were pre-treated for elimination of diagenetic carbonates following Tornero et al. (2013) . Isotope ratios were measured on a DeltaVAdvantage MS interfaced with a Kiel IV device (Thermo Scientific, Bremen, Germany). The analytical precision within each run, estimated from repeated analyses of our laboratory carbonate standard (Marbre LM, normalized to NBS19) was lower than 0.06‰ (n = 8). The modelling procedure was applied to the data sets from KMZ, CTD, CR, HPWN, KH, SKB, PBORD, HVA and ALS (Table 1) following Balasse et al. (2012b) . The data set from Cheia (CHE) (Tornero et al., 2013) was revised in order to correct the estimation of the location of the enamel root junction in teeth where mineralization was incomplete.
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