Noguchi Takumi, Sugiura Miwa
Institute of Materials Science, University of Tsukuba, Tsukuba, Ibaraki 305-8573, Japan.
Biochemistry. 2002 Dec 31;41(52):15706-12. doi: 10.1021/bi020603i.
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 hydrated (or deuterated) PS II core films from Synechococcus elongatus were used to obtain the FTIR difference spectra upon the first, second, third, and fourth flash illumination, representing the structural changes in the S(1) --> S(2), S(2) --> S(3), S(3) --> S(0), and S(0) --> S(1) transitions, respectively. In the weakly H-bonded OH region, bands appeared at 3617/3588 cm(-1) as a differential signal in the first-flash spectrum and at 3634, 3621, and 3612 cm(-1) with negative intensities in the second-, third-, and fourth-flash spectra, respectively. These bands shifted down by approximately 940 cm(-1) upon deuteration and by approximately 10 cm(-1) upon H(18)O substitution, indicating that they arise from the OH stretches of water including the substrate and its intermediates. Strongly D-bonded OD bands of water were also identified as broad features in the range of 2600-2200 cm(-1) by taking the double difference between the spectra of D(2)(16)O- and D(2)(18)O-deuterated films. In addition, broad continuum features that probably arise from the large proton polarizability of H-bonds were observed around 3000, 2700, 2550, and 2600 cm(-1) in the first-, second-, third-, and fourth-flash spectra, respectively, of the hydrated PS II film, revealing changes in the H-bond network of the protein. The negative OH intensities upon the second to fourth flashes might be related to proton release from substrate water. The results presented here showed that FTIR detection of water OH(D) bands can be a powerful method for investigating the mechanism of photosynthetic water oxidation.
光合水氧化通过光系统II(PS II)的水氧化复合物(WOC)中的光驱动S态循环进行。为了理解其分子机制,监测每个S态转变中底物水的反应至关重要。我们首次通过使用闪光诱导傅里叶变换红外(FTIR)差示光谱观察水的OH振动,检测了整个S态循环中WOC内水分子的反应。使用来自聚球藻的适度水合(或氘代)PS II核心膜,在第一次、第二次、第三次和第四次闪光照射下获得FTIR差示光谱,分别代表S(1)→S(2)、S(2)→S(3)、S(3)→S(0)和S(0)→S(1)转变中的结构变化。在弱氢键结合的OH区域,在第一次闪光光谱中,3617/3588 cm(-1)处出现带作为差示信号,在第二次、第三次和第四次闪光光谱中,分别在3634、3621和3612 cm(-1)处出现负强度的带。这些带在氘代时向下移动约940 cm(-1),在H(18)O取代时向下移动约10 cm(-1),表明它们来自包括底物及其中间体的水的OH伸缩振动。通过获取D(2)(16)O和D(2)(18)O氘代膜光谱之间的双差,水的强D键结合的OD带也被识别为2600 - 2200 cm(-1)范围内的宽峰。此外,在水合PS II膜的第一次、第二次、第三次和第四次闪光光谱中,分别在3000、2700、2550和2600 cm(-1)附近观察到可能源于氢键大质子极化率的宽连续峰,揭示了蛋白质氢键网络的变化。第二次到第四次闪光时OH的负强度可能与底物水的质子释放有关。这里给出的结果表明,FTIR检测水的OH(D)带可能是研究光合水氧化机制的有力方法。