Past atmospheric carbon dioxide levels are measured using ice core bubbles and fossilized plant stomata
Past atmospheric carbon dioxide levels are well-established to be reconstructed using geochemical proxies, including ice core trapped gases and plant stomatal traits or carbon isotopes from the fossil record.
The claim states that past atmospheric carbon dioxide levels are measured using ice core bubbles and fossilized plant stomata. Multiple retrieved studies (such as #3, #4, and #9) directly discuss using stomatal traits and plant fossil records to reconstruct paleo-atmospheric CO2 concentrations, thereby supporting the stomatal portion of the claim.
Amanda S. Porter, C. Evans-Fitz.Gerald, C. Yiotis, I. Montañez, J. McElwain. Testing the accuracy of new paleoatmospheric CO2 proxies based on plant stable carbon isotopic composition and stomatal traits in a range of simulated paleoatmospheric O2:CO2 ratios. 2019. https://doi.org/10.1016/J.GCA.2019.05.037
Paper 3 discusses paleoproxy CO2 methods utilizing plant stable carbon isotopic composition and stomatal traits.
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Beerling DJ. Low atmospheric CO(2) levels during the Permo- Carboniferous glaciation inferred from fossil lycopsids.. 2002. https://doi.org/10.1073/pnas.202304999
Paper 4 derives past atmospheric CO2 estimates from the stomatal indices of fossil lycopsids.
Machesky MD, Sheldon ND, Hren MT, Smith SY. The sensitivity of reconstructed carbon dioxide concentrations to stomatal preparation methods using a leaf gas exchange model.. 2025. https://doi.org/10.1002/aps3.11629
Paper 9 evaluates mechanistic models using stomatal traits and leaf carbon isotope ratios to reconstruct past atmospheric carbon dioxide concentrations.
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