We obviously agree with Wu et al. that HO might accumulate in the Archean land waters devoid of Fe. We do disagree on the topic of the half-life of HO, as the work cited in support for a longer half-live is not relevant to the conditions in the Archean ocean.
View Article and Find Full Text PDFWe address the chemical/biological history of HO back at the times of the Archean eon (2.5-3.9 billion years ago (Gya)).
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