The green primary compound of chloroperoxidase was prepared by freeze-quenching the enzyme after rapid mixing with a 5-fold excess of peracetic acid. The electron paramagnetic resonance (EPR) spectra of these preparations consisted of at least three distinct signals that could be assigned to native enzyme, a free radical, and the green compound I as reported earlier. The absorption spectrum of compound I was obtained through subtraction of EPR signals measured under passage conditions. The signal is well approximated by an effective spin Seff = 1/2 model with g = 1.64, 1.73, 2.00 and a highly anisotropic line width. Mössbauer difference spectra of compound I samples minus native enzyme showed well-resolved magnetic splitting at 4.2 K, an isomer shift delta Fe = 0.15 mm/s, and quadrupole splitting delta EQ = 1.02 mm/s. All data are consistent with the model of an exchange-coupled spin S = 1 ferryl iron and a spin S' = 1/2 porphyrin radical. As a result of the large zero field splitting, D, of the ferryl iron and of intermediate antiferromagnetic exchange, S.J.S'.J approximately 1.02 D, the system consists of three Kramers doublets that are widely separated in energy. The model relates the EPR and Mössbauer spectra of the ground doublet to the intrinsic parameters of the ferryl iron, D/k = 52 K, E/D congruent to 0.035, and A perpendicular (gn beta n) = 20 T, and the porphyrin radical.(ABSTRACT TRUNCATED AT 250 WORDS)

Enzymatic synthesis of methyl halides through an S-adenosyl methionine transfer mechanism has been detected in cell extracts of Phellinus promaceus (a white rot fungus), Endocladia muricata (a marine red algae), and Mesembryanthemum crystallium (ice plant). This mechanism represents a novel pathway for the formation of halometabolites. The Michaelis constants for chloride and bromide ion and for S-adenosyl methionine in the reaction have been determined for the enzyme from E. muricata. A recent survey of marine algae indicates that there may be a broad distribution of this enzyme among marine algae.

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We report Mössbauer and EPR measurements on horseradish peroxidase in the native state and the reaction intermediates with peroxide and chlorite. A detailed analysis of the electronic state of the heme iron is given, and comparisons are drawn with related systems. The native enzyme is high-spin ferric and thus has three Kramers doublets. The unusual magnetic properties of the ground doublet and the large energy of the second, (E2-E1)/k approximately equal to 41 K, and third doublet, (E3-E1)/k greater than or equal to 170 K, can be modeled with a quartet admixture of approximately 11% to the spin sextet. All evidence suggests a ferryl, OFeIV, state of the heme iron in compounds I and II and related complexes. The small isomer shift, delta Fe approximately equal to 0.06 mm/s, the (positive) quadrupole splitting, delta EQ approximately equal to 1.4 mm/s, the spin S = 1, and the large positive zero field splitting, D/k approximately equal to 35 K, are all characteristic of the ferryl state. In the green compound I the iron weakly couples to a porphyrin radical with spin S' = 1/2. A phenomenological model with a weak exchange interaction S . J . S', magnitude of less than or equal to 0.1 D, reproduces all Mössbauer and EPR data of compound I, but the structural origin of the exchange and its apparent distribution require further study. Reaction of horseradish peroxidase with chlorite leads to compound X with delta Fe = 0.07 mm/s and delta EQ = 1.53 mm/s, values that are closest to those of compound II. The diamagnetism of compound III and its Mössbauer parameters delta Fe = 0.23 mm/s and delta EQ = -2.31 mm/s at 4.2 K clearly identify it as an oxyheme adduct.

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