Abstract
Heme and non-heme iron in biology mediate the storage/release
of NO• from S-nitrosothiols as a means to control the
biological concentration of NO•. Despite their importance in many
physiological processes, the mechanisms of N-S bond formation/cleavage at Fe
centers have been controversial. Herein, we report
the interconversion of NO• and S-nitrosothiols mediated
by FeII/FeIII chloride complexes. The reaction of two
equivalents of S-nitrosothiol (Ph3CSNO) with [Cl6FeII2]2-
results in facile release of NO• and formation of iron(III)
halothiolate. Detailed spectroscopic studies, including in situ UV-vis, IR, and
Mössbauer spectroscopy, support the interaction of the S−atom with the FeII center. This is in
contrast to the proposed mechanism of NO• release from the
well-studied “red product” k1-N
bound S-nitrosothiol FeII complex,
[(CN)5Fe(k1-N-RSNO)]3-.
Additionally, FeIII chloride can mediate NO• storage
through the formation of S-nitrosothiols. Treatment of iron(III)
halothiolate with two equivalents of NO• regenerates Ph3CSNO
with the FeII source
trapped as the S = 3/2 {FeNO}7 species [Cl3FeNO]-,
which is inert towards further coordination and activation of S-nitrosothiols.
Our work demonstrates how labile iron can mediate the interconversion of NO•/thiolate
and S-nitrosothiol, which has important implications for how Nature
manages the biological concentration of free NO•.