Optical spectra and electronic structure of flavine mononucleotide in flavodoxin crystals

The polarized single-crystal absorption spectra of the oxidized and semiquinone forms of flavodoxin from Clostridium MP have been measured with a double beam recording microspectrophotometer. The spectra establish that the radical species in the crystal is the neutral (blue) falvine semiquinone. Combination of the spectra reported here with polarization data from previous fluorescence and stretched-film studies provides transition moment directions for the first two phi-phi transitions of the oxidized form. Predictions of molecular orbital theory are in good agreement with these experimental directions. The crystal spectra of the semiquinone indicate that the two lowest frequency transitions have the same detailed orbital origin as the corresponding transitions of the oxidized form; in the semiquinone these transitions appear at lower frequency, are closer together, and, as predicted from detailed considerations of transition probabilities, exhibit approximately half the absorption intensity. Our hypothesis of a common orbital origin suggests that semiquinone formation takes place by the addition of an electron to the lowest empty phi orbital of the oxidized form without any gross electronic rearrangement.