Hillier W, Hendry G, Burnap R L, Wydrzynski T
Department of Chemistry, Michigan State University, East Lansing, MI 48824, USA.
J Biol Chem. 2001 Dec 14;276(50):46917-24. doi: 10.1074/jbc.M102954200. Epub 2001 Oct 10.
The (18)O exchange rates for the substrate water bound in the S(3) state were determined in different photosystem II sample types using time-resolved mass spectrometry. The samples included thylakoid membranes, salt-washed Triton X-100-prepared membrane fragments, and purified core complexes from spinach and cyanobacteria. For each sample type, two kinetically distinct isotopic exchange rates could be resolved, indicating that the biphasic exchange behavior for the substrate water is inherent to the O(2)-evolving catalytic site in the S(3) state. However, the fast phase of exchange became somewhat slower (by a factor of approximately 2) in NaCl-washed membrane fragments and core complexes from spinach in which the 16- and 23-kDa extrinsic proteins have been removed, compared with the corresponding rate for the intact samples. For CaCl(2)-washed membrane fragments in which the 33-kDa manganese stabilizing protein (MSP) has also been removed, the fast phase of exchange slowed down even further (by a factor of approximately 3). Interestingly, the slow phase of exchange was little affected in the samples from spinach. For core complexes prepared from Synechocystis PCC 6803 and Synechococcus elongatus, the fast and slow exchange rates were variously affected. Nevertheless, within the experimental error, nearly the same exchange rates were measured for thylakoid samples made from wild type and an MSP-lacking mutant of Synechocystis PCC 6803. This result could indicate that the MSP has a slightly different function in eukaryotic organisms compared with prokaryotic organisms. In all samples, however, the differences in the exchange rates are relatively small. Such small differences are unlikely to arise from major changes in the metal-ligand structure at the catalytic site. Rather, the observed differences may reflect subtle long range effects in which the exchange reaction coordinates become slightly altered. We discuss the results in terms of solvent penetration into photosystem II and the regional dielectric around the catalytic site.
使用时间分辨质谱法测定了处于S(3)状态的结合底物水的(18)O交换率,该交换率是在不同类型的光系统II样品中测定的。样品包括类囊体膜、盐洗Triton X-100制备的膜片段以及来自菠菜和蓝细菌的纯化核心复合物。对于每种样品类型,都可以分辨出两种动力学上不同的同位素交换率,这表明底物水的双相交换行为是S(3)状态下O(2)进化催化位点所固有的。然而,与完整样品的相应速率相比,在已去除16 kDa和23 kDa外在蛋白的NaCl洗过的膜片段和菠菜核心复合物中,快速交换阶段变得稍慢(约为2倍)。对于也已去除33 kDa锰稳定蛋白(MSP)的CaCl(2)洗过的膜片段,快速交换阶段进一步减慢(约为3倍)。有趣的是,菠菜样品中的慢速交换阶段受影响较小。对于从集胞藻PCC 6803和聚球藻制备的核心复合物,快速和慢速交换率受到不同程度的影响。然而,在实验误差范围内,对野生型和集胞藻PCC 6803的MSP缺失突变体制备的类囊体样品测量到几乎相同的交换率。这一结果可能表明,与原核生物相比,MSP在真核生物中的功能略有不同。然而,在所有样品中,交换率的差异相对较小。如此小的差异不太可能源于催化位点金属-配体结构的重大变化。相反,观察到的差异可能反映了微妙的长程效应,其中交换反应坐标略有改变。我们根据溶剂渗透到光系统II以及催化位点周围的区域介电常数来讨论这些结果。