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The electronic structure of oxyhemoglobin has been controversial since the discovery of the compound’s diamagnetism in 1936. This study uses partial fluorescence yield Fe L-edge X-ray absorption spectroscopy (XAS) in the 3s→2p fluorescence on oxyhemoglobin solutions, measured using a transition-edge sensor detector, to obtain a quantitative experimental description of the electronic structure of the O2-bound iron site. The spectrum is very different from typical low-spin FeII and FeIII heme spectra, and multiplet simulations indicate a mixed ground configuration with ∼57% low-spin FeIII and ∼43% low-spin FeII character. This is also very different from the FeII character found for the picket-fence porphyrin model complex. The oxyhemoglobin L-edge XAS data further show that the O2 ligand engages in a weak σ- but strong π-bond with the iron ion, leading to the overall strong Fe–O2 bond required for O2 transport.
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Braun et al. (2025) studied this question.
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