The deoxy-form of human adult hemoglobin (Hb A) exhibits a distinct negative CD band at 287 nm that disappears in the oxy-form. It has been suggested that the negative CD band is due to the environmental alteration of Tyr-alpha 42 or Trp-beta 37 at the alpha(1)beta(2) contact upon deoxygenation. To evaluate the contributions of the aromatic residues at the alpha(1)beta(2) contact and the penultimate tyrosine residues of the alpha and beta subunits (alpha 140 and beta 145) to the negative CD band, three recombinant (r) Hbs (rHb Ser-alpha 42, rHb His-beta 37, and rHb Thr-beta 145) were produced in Escherichia coli, and we compared the near-uv CD spectra of these three rHbs and Hb Rouen (Tyr-alpha 140-->His) with the spectra of Hb A under the condition in which all mutant Hbs were able to undergo the T-->R transition (Hill's n > 2.0). The contributions of Tyr-alpha 42, Trp-beta 37, Tyr-alpha 140, and Tyr-beta 145 to the negative CD band were estimated from changes in the ellipticity of the negative CD band at 287 nm to be 4, 18, 32, and 27%, respectively. These results indicate that environmental alteration of the penultimate tyrosine residues caused by the formation of salt bridges upon the R-->T transition is primarily responsible for the negative CD band.