John H. Robblee
Lawrence Berkeley National Laboratory
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Featured researches published by John H. Robblee.
Biochimica et Biophysica Acta | 2001
John H. Robblee; Roehl M. Cinco; Vittal K. Yachandra
The mechanism by which the Mn-containing oxygen evolving complex (OEC) produces oxygen from water has been of great interest for over 40 years. This review focuses on how X-ray spectroscopy has provided important information about the structure of this Mn complex and its intermediates, or S-states, in the water oxidation cycle. X-ray absorption near-edge structure spectroscopy and high-resolution Mn Kbeta X-ray emission spectroscopy experiments have identified the oxidation states of the Mn in the OEC in each of the intermediate S-states, while extended X-ray absorption fine structure experiments have shown that 2.7 A Mn-Mn di-mu-oxo and 3.3 A Mn-Mn mono-mu-oxo motifs are present in the OEC. X-ray spectroscopy has also been used to probe the two essential cofactors in the OEC, Ca2+ and Cl-, and has shown that Ca2+ is an integral component of the OEC and is proximal to Mn. In addition, dichroism studies on oriented PS II membranes have provided angular information about the Mn-Mn and Mn-Ca vectors. Based on these X-ray spectroscopy data, refined models for the structure of the OEC and a mechanism for oxygen evolution by the OEC are presented.
Physical Chemistry Chemical Physics | 2004
Shelly A. Pizarro; Pieter Glatzel; Hendrik Visser; John H. Robblee; George Christou; Uwe Bergmann; Vittal K. Yachandra
X-Ray spectroscopy is used to examine the effect of the manganese oxidation state for a series of Mn model compounds. Sensitive to Mn oxidation and structural symmetry, X-ray absorption and emission spectroscopy (XAS and XES) provide complementary insights. However, few benchmark examples of complexes with similar structures but in different oxidation states are available to evaluate data from unknown structures like the oxygen evolving complex (OEC) of Photosystem II (PSII). This study examines two types of compounds prepared in a variety of Mn oxidation states and which possess chemical structures with Mn-Mn interactions (~2.7 Å and ~3.3 Å) that have been observed in the OEC. Model complexes with core compositions Mn3O and Mn4O2 contain combinations of Mn in either a reduced (II) or oxidized (III) state. Within each set of compounds, complexes with higher Mn oxidation states have absorption K-edge energy values that are higher (1.6-2.2 eV) than those of their more reduced counterparts. This trend is accordingly reversed in the Kβ emission spectroscopy where the first moment energy values are lower (0.09-0.12 eV) for compounds with higher Mn oxidation states. We will discuss in detail, how these trends can be quantitatively used to characterize the effects of the Mn oxidation state as well as the surrounding ligand environment on the observed X-ray spectra. The results are discussed with respect to previously obtained data on different S-states of the OEC.
Journal of Synchrotron Radiation | 2001
Emanuele Bellacchio; Karen L. McFarlane; Annette Rompel; John H. Robblee; Roehl M. Cinco; Vittal K. Yachandra
X-ray Absorption Spectroscopy (XAS) is a powerful tool to investigate sulfur in biological molecules. The spectral features are sensitive to the local electronic and geometric environment of the atom; thus, they constitute a fingerprint of the different chemical forms in which the sulfur is present. This allows straightforward detection of the ratio between free thiols and disulfides. Intra- or inter-molecular disulfide bond formation between residues plays an important role in structural and conformational changes in proteins, and such changes can be investigated using sulfur XAS. Also, a thiolate-disulfide equilibrium is involved in the regulation of the redox potential in the cells by means of modulating the concentrations of the reduced (thiolate) and oxidized (disulfide) form of the tripeptide glutathione. Thus, we can monitor the redox state of a cell by means of sulfur XAS. Thiols also exhibit an acid-base equilibrium, and sulfur XAS can be used to determine the local pKa of the -SH group. Here we report examples of how sulfur XAS has been used for these applications.
Archive | 1998
Johannes Messinger; John H. Robblee; Carmen Fernandez; Roehl M. Cinco; Henk Visser; Uwe Bergmann; Pieter Glatzel; Stephen P. Cramer; K. A. Campbell; J. M. Peloquin; R. D. Britt; Kenneth Sauer; Vittal K. Yachandra; Melvin P. Klein
Photosystem II (PS II) catalyzes the light driven oxidation of water to molecular oxygen and the reduction of plastoquinone to plastohydroquinone. Water oxidation occurs in the oxygen evolving complex (OEC) of PS II that is known to cycle through five different redox states, referred to as the S states (S0,..,S4). A cluster of four Mn, one Ca and Cl− is thought to form the central unit of the OEC which stores most of the oxidizing equivalents and binds the substrate water.
Journal of Synchrotron Radiation | 1999
Roehl M. Cinco; John H. Robblee; Annette Rompel; Carmen Fernandez; Kenneth Sauer; Vittal K. Yachandra; Melvin P. Klein
Working on Photosystem II membranes from spinach, we substituted strontium for calcium and probed using Sr EXAFS for any nearby Mn. Sr EXAFS results indicate major differences between the functional (intact) and inactive (hydroxylamine-treated) samples. In intact samples, the Fourier transform of the Sr EXAFS shows a major peak that is missing in inactive samples. This interaction is best simulated by two Mn neighbors at a distance of ~3.5 A.
Archive | 1998
Carmen Fernandez; Roehl M. Cinco; John H. Robblee; Johannes Messinger; Shelly A. Pizarro; Kenneth Sauer; Melvin P. Klein; Vittal K. Yachandra
The oxygen-evolving complex (OEC) of photosystem II (PSII) in green plants and algae contains a cluster of four Mn atoms in the active site, which catalyzes the oxidation of water to dioxygen. Along with Mn, Cl− and Ca2+ are essential cofactors for oxygen evolution (1).
Journal of Synchrotron Radiation | 2001
Annette Rompel; Roehl M. Cinco; John H. Robblee; Matthew J. Latimer; Karen L. McFarlane; Jiong Huang; Marc A. Walters; Vittal K. Yachandra
Mo L-edge and S K-edge X-ray absorption spectroscopy were applied to investigate the charge distribution between Mo and S in a series of Mo thiolate compounds, which serve as amide-sulfur H-bonding models and exhibit different redox potentials arising from polar group effects and ligand hydrogen bonds near the redox center. For all oxidized complexes, the S K-edge spectra exhibit a thiolate-based pre-edge feature centered at 2470.2 eV and the inflection point oCCurs at 2472.0 eV. No intense pre-edge feature is observed in the spectra for the reduced Mo model compounds and the energy shift of the S K-edge position depends on the S-ligand. Correlations between ligand charge density and the redox potential of the Mo-S cores are observed.
Archive | 1998
Roehl M. Cinco; Carmen Fernandez; Johannes Messinger; John H. Robblee; Henk Visser; Karen L. McFarlane; Uwe Bergmann; Pieter Glatzel; Stephen P. Cramer; Kenneth Sauer; Melvin P. Klein; Vittal K. Yachandra
Central to the problem of photosynthetic oxygen evolution is the structure and function of the Mn/Ca/Cl complex that appears to be the locus of charge accumulation and water splitting. In the recent past our group has presented a topological model for the structure of the tetranuclear Mn cluster, the oxidation state assignments of the S-states of the Kok cycle, the orientation of the Mn-Mn vectors relative to the membrane normal, and evidence for the proximity of Ca to the Mn (1–3).
Journal of the American Chemical Society | 2001
Johannes Messinger; John H. Robblee; Uwe Bergmann; Carmen Fernandez; Pieter Glatzel; Hendrik G. Visser; Roehl M. Cinco; Karen L. McFarlane; Emanuele Bellacchio; Shelly A. Pizarro; Stephen P. Cramer; Kenneth Sauer; Melvin P. Klein; Vittal K. Yachandra
Biochimica et Biophysica Acta | 2004
R. David Britt; Kristy A. Campbell; Jeffrey M. Peloquin; M. Lane Gilchrist; Constantino P. Aznar; Michelle M. Dicus; John H. Robblee; Johannes Messinger