Abstract
The rise of atmospheric oxygen occurred long before the sudden appearance of multicellular eukaryotic organisms in the later Precambrian. Oxygen was necessary but not sufficient for the evolution of multicellular eukaryotes: the rise of modern aerobic eukaryotes (fungi, animals and plants) occurred in a fully oxygenic atmosphere only after the evolution in protists of microtubule-utilising processes (mitosis and meiosis).
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Margulis, L., Walker, J. & Rambler, M. Reassessment of roles of oxygen and ultraviolet light in Precambrian evolution. Nature 264, 620–624 (1976). https://doi.org/10.1038/264620a0
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DOI: https://doi.org/10.1038/264620a0
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