Photosynthetic O2 formation tracked by time-resolved X-ray experiments

被引:375
作者
Haumann, M [1 ]
Liebisch, P [1 ]
Müller, C [1 ]
Barra, M [1 ]
Grabolle, M [1 ]
Dau, H [1 ]
机构
[1] Free Univ Berlin, FB Phys, D-14195 Berlin, Germany
关键词
D O I
10.1126/science.1117551
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Plants and cyanobacteria produce atmospheric dioxygen from water, powered by sunlight and catalyzed by a manganese complex in photosystem II. A classic S-cycle model for oxygen evolution involves five states, but only four have been identified. The missing S-4 state is particularly important because it is directly involved in dioxygen formation. Now progress comes from an x-ray technique that can monitor redox and structural changes in metal centers in real time with 10-microsecond resolution. We show that in the O-2-formation step, an intermediate is formed-the enigmatic S-4 state. Its creation is identified with a deprotonation process rather than the expected electron-transfer mechanism. Subsequent electron transfer would give an additional S-4' state, thus extending the fundamental S-state cycle of dioxygen formation.
引用
收藏
页码:1019 / 1021
页数:3
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