The Carboniferous period featured exceptionally high levels of atmospheric oxygen
Is it true that the Carboniferous period featured exceptionally high levels of atmospheric oxygen?
Yes. Multiple studies and fossil evidence indicate that the Carboniferous period experienced exceptionally high atmospheric oxygen levels (hyperoxia), which is widely linked to the evolution of insect and arthropod gigantism during that era.
Verdict: SUPPORTED · 4 sources for, 0 against · Last checked
The claim states that the Carboniferous period featured exceptionally high levels of atmospheric oxygen. This is a specific, empirical, and well-studied geological/paleontological claim that passes Step 0. Among the retrieved papers, several directly discuss late Paleozoic/Carboniferous hyperoxia and its role in supporting giant arthropods (papers 0, 2, 4, 11). None of the papers refute this premise; they either support it or discuss unrelated topics (such as sulfur isotopes, modern hermetic storage, or early Paleozoic marine extinctions). Therefore, the verdict is SUPPORTED.
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JF, H., A, K., & JM, V. (2010). Atmospheric oxygen level and the evolution of insect body size.. doi.org. https://doi.org/10.1098/rspb.2010.0001
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WC, V. & DT, B. (2011). Can oxygen set thermal limits in an insect and drive gigantism?. doi.org. https://doi.org/10.1371/journal.pone.0022610
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GJ, V. (2016). Gigantism and Its Implications for the History of Life.. doi.org. https://doi.org/10.1371/journal.pone.0146092
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Kurbel, S. (2014). Animal evolution and atmospheric pO2: is there a link between gradual animal adaptation to terrain elevation due to Ural orogeny and survival of subsequent hypoxic periods?. doi.org. https://doi.org/10.1186/1742-4682-11-47
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