Abstract
Recent geophysical and geochemical data and theoretical modeling indicate high levels of atmospheric O2 (up to 35 %) during the Carboniferous-Permian. I suggest that this O2 pulse had a substantial impact on global accumulations of petroleum source rocks and coal during this geological period.
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APA
Premović, P. I. (2006). The late Paleozoic oxygen pulse and accumulations of petroleum source rocks and coal. Journal of the Serbian Chemical Society, 71(2), 143–147. https://doi.org/10.2298/JSC0602143P
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