Cole J, Yachandra V K, Guiles R D, McDermott A E, Britt R D, Dexheimer S L, Sauer K, Klein M P
Biochim Biophys Acta. 1987 Mar 4;890(3):395-8. doi: 10.1016/0005-2728(87)90169-1.
X-ray absorption spectroscopy at the Mn K-edge has been utilized to study the origin of the g = 4.1 EPR signal associated with the Mn-containing photosynthetic O2-evolving complex. Formation of the g = 4.1 signal by illumination of Photosystem II preparations at 140 K is associated with a shift of the Mn edge inflection point to higher energy. This shift is similar to that observed upon formation of the S2 multiline EPR signal by 190 K illumination. The g = 4.1 signal is assigned to the Mn complex in the S2 state.
利用锰K边的X射线吸收光谱来研究与含锰光合放氧复合体相关的g = 4.1电子顺磁共振(EPR)信号的起源。在140 K下光照光系统II制剂形成g = 4.1信号与锰边拐点向更高能量的移动有关。这种移动类似于在190 K光照下形成S2多线EPR信号时观察到的移动。g = 4.1信号被归因于处于S2状态的锰复合体。