The biogenesis of the 2,4,5-trihydroxyphenylalanine quinone (TPQ) cofactor from tyrosine at the active site of copper amine oxidases is believed to proceed along a pathway that includes a conjugate addition of water to the corresponding o-quinone intermediate, followed by autoxidation of the resulting benzenetriol to the hydroxyquinone cofactor. The water addition reaction has been presumed to occur not only in previous model studies reported for cofactor biogenesis starting with either catechol or o-quinone, but also for generation of the neurotoxin 6-hydroxydopamine during autoxidation of dopamine. We here report the surprising finding that water addition does not occur under solution chemistry conditions. The production of hydroxyquinone from catechol arises instead from reaction of the o-quinone with H2O2 generated during autoxidation of catechol. When starting with the o-quinone itself, production of hydroxyquinone still arises from autoxidation of the catechol, generated either by reduction of the o-quinone by its decomposition products at moderate pH, or by a novel base-mediated redox disproportionation of the o-quinone at high pH. These conclusions are supported by the behavior of independently studied o-quinone intermediates, the observed effects of added catalase, and O-18-labeling studies utilizing both [O-18]H2O and [O-18]O-2. The failure to observe water addition to the o-quinone has broad implications for aqueous o-quinone chemistry, and suggests that in TPQ biogenesis, this hydration is being catalyzed at the enzyme active site, possibly by the bound copper.