Novel δ13C measurement shows high precision in ambient CO2 samples, indicating improved sampling techniques for carbon dynamics.
The carbon isotopic composition (δ13C) of atmospheric carbon dioxide (CO2) is a key tracer for understanding terrestrial carbon dynamics, yet its application in small-volume sampling systems remains constrained by analytical limitations. Here, we present a novel methodology for high-precision δ13C analysis of ambient atmospheric CO2 from 1 mL air samples, tailored to the challenges of growth chamber experiments using microcosm model systems and other volume-limited systems. Our approach emerged from testing the effects of custom vial conditioning, dual-sealing with Terostat®, ultra-low-temperature storage at -80 °C, and cryogenic pre-concentration coupled to continuous-flow isotope-ratio mass spectrometry (IRMS). We demonstrate that vial conditioning and improved dual sealing are critical to ensure analytical precision. Our combined method achieves a precision of ± 0.1 ‰ on δ13C measurements, with negligible isotopic drift for storage durations up to 1-week if ultra-low-temperature storage and zip-lock bags full of CO2-free air were used. Longer storage times reduces measurement precision, emphasising the importance of short-term preservation. This technique offers a significant advance for carbon stable isotope applications in constrained environments, enabling minimally invasive, high-frequency δ13C monitoring with good precision at the millilitre scale.
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Sauze et al. (2025) studied this question.
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