40 research outputs found
Contribution of Groundwater Discharge to the Coastal Dissolved Nutrients and Trace Metal Concentrations in Majorca Island: Karstic vs Detrital Systems
Submarine Groundwater Discharge to a High-Energy Surf Zone at Stinson Beach, California, Estimated Using Radium Isotopes
Setting an Upper Limit on the Myoglobin Iron(IV)Hydroxide p<i>K</i><sub>a</sub>: Insight into Axial Ligand Tuning in Heme Protein Catalysis
To provide insight into the ironÂ(IV)Âhydroxide
p<i>K</i><sub>a</sub> of histidine ligated heme proteins,
we have probed the
active site of myoglobin compound II over the pH range of 3.9–9.5,
using EXAFS, Mössbauer, and resonance Raman spectroscopies.
We find no indication of ferryl protonation over this pH range, allowing
us to set an upper limit of 2.7 on the ironÂ(IV)Âhydroxide p<i>K</i><sub>a</sub> in myoglobin. Together with the recent determination
of an ironÂ(IV)Âhydroxide p<i>K</i><sub>a</sub> ∼ 12
in the thiolate-ligated heme enzyme cytochrome P450, this result provides
insight into Nature’s ability to tune catalytic function through
its choice of axial ligand
A 2.8 Å Fe–Fe Separation in the Fe<sub>2</sub><sup>III/IV</sup> Intermediate, X, from <i>Escherichia coli</i> Ribonucleotide Reductase
A class
Ia ribonucleotide reductase (RNR) employs a μ-oxo-Fe<sub>2</sub><sup>III/III</sup>/tyrosyl radical cofactor in its β
subunit to oxidize a cysteine residue ∼35 Å away in its
α subunit; the resultant cysteine radical initiates substrate
reduction. During self-assembly of the <i>Escherichia coli</i> RNR-β cofactor, reaction of the protein’s Fe<sub>2</sub><sup>II/II</sup> complex with O<sub>2</sub> results in accumulation
of an Fe<sub>2</sub><sup>III/IV</sup> cluster, termed <b>X</b>, which oxidizes the adjacent tyrosine (Y<sub>122</sub>) to the radical
(Y<sub>122</sub><sup>•</sup>) as the cluster is converted to
the μ-oxo-Fe<sub>2</sub><sup>III/III</sup> product. As the first
high-valent non-heme-iron enzyme complex to be identified and the
key activating intermediate of class Ia RNRs, <b>X</b> has been
the focus of intensive efforts to determine its structure. Initial
characterization by extended X-ray absorption fine structure (EXAFS)
spectroscopy yielded a Fe–Fe separation (<i>d</i><sub>Fe–Fe</sub>) of 2.5 Å, which was interpreted to
imply the presence of three single-atom bridges (O<sup>2–</sup>, HO<sup>–</sup>, and/or μ-1,1-carboxylates). This short
distance has been irreconcilable with computational and synthetic
models, which all have <i>d</i><sub>Fe–Fe</sub> ≥
2.7 Ã…. To resolve this conundrum, we revisited the EXAFS characterization
of <b>X</b>. Assuming that samples containing increased concentrations
of the intermediate would yield EXAFS data of improved quality, we
applied our recently developed method of generating O<sub>2</sub> <i>in situ</i> from chlorite using the enzyme chlorite dismutase
to prepare <b>X</b> at ∼2.0 mM, more than 2.5 times the
concentration realized in the previous EXAFS study. The measured <i>d</i><sub>Fe–Fe</sub> = 2.78 Å is fully consistent
with computational models containing a (μ-oxo)<sub>2</sub>-Fe<sub>2</sub><sup>III/IV</sup> core. Correction of the <i>d</i><sub>Fe–Fe</sub> brings the experimental data and computational
models into full conformity and informs analysis of the mechanism
by which <b>X</b> generates Y<sub>122</sub><sup>•</sup>
Spectroscopic Investigations of Catalase Compound II: Characterization of an Iron(IV) Hydroxide Intermediate in a Non-thiolate-Ligated Heme Enzyme
We
report on the protonation state of <i>Helicobacter pylori</i> catalase compound II. UV/visible, Mössbauer, and X-ray absorption
spectroscopies have been used to examine the intermediate from pH
5 to 14. We have determined that HPC-II exists in an ironÂ(IV) hydroxide
state up to pH 11. Above this pH, the ironÂ(IV) hydroxide complex transitions
to a new species (p<i>K</i><sub>a</sub> = 13.1) with Mössbauer
parameters that are indicative of an ironÂ(IV)-oxo intermediate. Recently,
we discussed a role for an elevated compound II p<i>K</i><sub>a</sub> in diminishing the compound I reduction potential. This
has the effect of shifting the thermodynamic landscape toward the
two-electron chemistry that is critical for catalase function. In
catalase, a diminished potential would increase the selectivity for
peroxide disproportionation over off-pathway one-electron chemistry,
reducing the buildup of the inactive compound II state and reducing
the need for energetically expensive electron donor molecules