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Delta vs mass spectrometer

Manufactured by Thermo Fisher Scientific
Sourced in Germany

The Delta VS mass spectrometer is a high-performance analytical instrument designed for precise isotope ratio measurements. It features advanced technology to provide accurate and reliable data for a wide range of applications, including environmental analysis, geochemistry, and life science research.

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3 protocols using delta vs mass spectrometer

1

Stable Isotope Analysis of Avian Beaks

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All beaks were dried at 60 °C for 24–48 hours and ground into a fine powder. Powder sub-samples were weighed (to the nearest 0.3 mg) with a micro-balance and sterile-packed in tin containers. Stable isotope values were determined by a Flash EA 1112 Series elemental analyser coupled online via a Finnigan ConFlo II interface to a Delta VS mass spectrometer (Thermo Scientific) and expressed as: δ13C and δ15N = [(Rsample/Rstandard) − 1] * 1000, where R = 13C/12C and 15N/14N, respectively. The carbon and nitrogen isotope ratios were expressed in delta (δ) notation relative to Vienna-PeeDee Belemnite limestone (V-PDB) for δ13C and atmospheric nitrogen (AIR) for δ15N. Replicate measurements of internal laboratory standards (acetanilide STD: Thermo Scientific PN 338 36700) in every batch (n = 14) indicated precision <0.2‰ for both δ13C and δ15N values. Mean mass C:N ratio of all samples was 3.19 ± 0.02.
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2

Sediment Characterization Protocol

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Sediment relative water content (RWC) was determined by drying sediment samples at 60°C until constant weight. Organic matter was determined by the loss on ignition (LOI) method, by burning 1 g of airdried sediment at 550°C for 3 h. Values of pH were measured in the eld in freshly sliced sediment samples using a HANNA pH/mV (HI 9025) probe. Carbon and nitrogen content (%) were determined in dried pulverized sediment samples using a Flash EA 1112 Series elemental analyzer coupled online via Finningan con o III interface to a Thermo delta V S mass spectrometer.
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3

Stable Isotope Analysis of Avian Beaks

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All beak subsections were dried at 60 °C for 24–48 h, weighed (to the closest value to 0.3 mg) with a micro-balance and cracked if needed, and sterile-packed in tin containers. Stable isotopic signatures were determined by a Flash EA 1112 Series elemental analyser (Thermo Scientific Inc., Waltham, MA, USA) coupled online via a Finnigan ConFlo II interface to a Delta vs. mass spectrometer (Thermo Scientific, Bremen, Germany) and expressed as: δ13C and δ15N = [(Rsample/Rstandard) − 1] * 1000, where R = 13C/12C and 15N/14N, respectively. The carbon and nitrogen isotope ratios were expressed in delta (δ) notation relative to Vienna-PeeDee Belemnite limestone (V-PDB) for δ13C and atmospheric nitrogen (AIR) for δ15N. Replicate measurements of internal laboratory standards (acetanilide STD: Thermo Scientific PN 338 36700) in every batch (n = 14) indicated a precision <0.2‰ for both δ13C and δ15N signatures. The mass C:N ratio for each sample, where it was obtained, ranges from 3.05 to 3.86 (Table S2). The analyses were carried out at the Marine and Environmental Science Centre, University of Coimbra (Coimbra, Portugal).
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