Takumi Noguchi

Differently hydrated films of photosystem II (PSII) core complexes from Synechococcus elongatus were prepared in a humidity-controlled infrared cell. The relative humidity was changed by a simple method of placing a different ratio of glycerol/water solution in the sealed cell. The extent of hydration of the PSII film was lowered as the glycerol ratio increased. FTIR difference spectra of the water oxidizing complex upon the first to sixth flashes were measured at 10 degrees C using these hydrat

Flash-induced Fourier transform infrared (FTIR) difference spectroscopy has been used to study the water-oxidizing reactions in the oxygen-evolving centre of photosystem II. Reactions of water molecules were directly monitored by detecting the OH stretching bands of weakly H-bonded OH of water in the 3700–3500 cm −1 region in FTIR difference spectra during S-state cycling. In the S 1 →S 2 transition, a band shift from 3588 to 3617 cm −1 was observed, indicative of a weakened H-bond. Decoupling e

Fourier transform infrared (FTIR) signals of a histidine side chain were identified in flash-induced S(2)/S(1) difference spectra of the oxygen-evolving complex (OEC) of photosystem II (PS II) using PS II membranes from globally (15)N-labeled spinach and PS II core complexes from Synechocystis cells in which both the imidazole nitrogens of histidine were selectively labeled with (15)N. A negative band at 1113-1114 cm(-1) was downshifted by 7 cm(-1) upon both global (15)N-labeling and selective [

Protein bands in flash-induced Fourier transform infrared (FTIR) difference spectra of the S-state cycle of photosynthetic water oxidation were analyzed by uniform (15)N and (13)C isotopic labeling of photosystem II (PS II). The difference spectra upon first- to fourth-flash illumination were obtained with hydrated (for the 1800-1200 cm(-)(1) region) or deuterated (for the 3500-3100 cm(-)(1) region) films of unlabeled, (15)N-labeled, and (13)C-labeled PS II core complexes from Thermosynechococcu

Photosynthetic water oxidation is performed via the light-driven S-state cycle in the water-oxidizing complex (WOC) of photosystem II (PS II). To understand its molecular mechanism, monitoring the reaction of substrate water in each S-state transition is essential. We have for the first time detected the reactions of water molecules in WOC throughout the S-state cycle by observing the OH vibrations of water using flash-induced Fourier transform infrared (FTIR) difference spectroscopy. Moderately

The flash-induced Fourier transform infrared (FTIR) difference spectrum of the oxygen-evolving Mn cluster upon S1-to-S2 transition (S2/S1 spectrum) was measured using photosystem II (PS II) core complexes of Synechocystis 6803 in which tyrosine residues were specifically labeled with 13C at the ring-4 position. The double-difference spectrum between the unlabeled and labeled S2/S1 spectra showed that the bands at 1254 and 1521 cm-1 downshifted by 25 and 15 cm-1, respectively, upon ring-4-13C-Tyr

Nitrile hydratase (NHase) from Rhodococcus sp. N-771 is a photosensitive enzyme that catalyzes hydration of nitriles to the corresponding amides. Light-induced Fourier transform infrared difference spectra between the inactive and active forms of NHase were measured with both the natural (14N) and 15N-labeled NHases. The results showed, for the first time, that NHase intrinsically possesses nitric oxide (NO) molecules bound to the non-heme iron center. The possible role of NO in the photoactivat

The vibrations of a water molecule in the water-oxidizing complex (WOC) of photosystem II were detected for the first time using Fourier transform infrared (FTIR) spectroscopy. In a flash-induced FTIR difference spectrum upon the S(1)-to-S(2) transition, a pair of positive and negative bands was observed at 3618 and 3585 cm(-1), respectively, and both bands exhibited downshifts by 12 cm(-1) upon replacement of H(2)(16)O by H(2)(18)O. Upon D(2)O substitution, the bands largely shifted down to 268

Photosynthetic oxygen evolution by plants and cyanobacteria is performed by water oxidation at the Mn(4)CaO(5) cluster in photosystem II. The reaction is known to proceed via a light-driven cycle of five intermediates called S(i) states (i = 0-4). However, the detailed reaction processes during the intermediate transitions remain unresolved. In this study, we have directly detected the proton and protein dynamics during the oxygen-evolving reactions using time-resolved infrared spectroscopy. The

The structure and molecular interactions of the primary donor (P680) in the reaction center (D1-D2-cytochrome b-559 complex) of photosystem II (PS II) have been investigated by detecting light-induced FT-IR difference spectra upon the formation of its triplet state (3P680). The 3P680/P680 spectrum obtained was analyzed by comparing it with difference spectra between the ground and lowest triplet states of purified chlorophyll a (Chl) in organic solvents. The negative peaks at 1669 and 1707 cm-1

A Fourier transform infrared (FTIR) difference spectrum of the primary electron donor (P680) of photosystem II upon its photooxidation (P680+/P680) was obtained in the frequency region of 1000-3000 cm-1. The reaction center (RC) complex (D1-D2-Cytb559) was used for the measurements in the presence of ferricyanide as an exogenous electron acceptor. Control measurements of electronic absorption (300-1200 nm) showed that illumination of the RC complex at 150 K induced major oxidation of P680 concom