Photoreaction Cycle of Photoactive Yellow Protein fromEctothiorhodospira halophilaStudied by Low-Temperature Spectroscopy†

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Vol 35 (45) ◽  
pp. 14047-14053 ◽  
Author(s):  
Yasushi Imamoto ◽  
Mikio Kataoka ◽  
Fumio Tokunaga

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1991 ◽  
Vol 30 (30) ◽  
pp. 7416-7424 ◽  
Author(s):  
Yasushi Imamoto ◽  
Yoshinori Shichida ◽  
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1987 ◽  
Vol 225 (1-2) ◽  
pp. 255-258 ◽  
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Biochemistry ◽  
2006 ◽  
Vol 45 (36) ◽  
pp. 10828-10837 ◽  
Author(s):  
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Tatsuya Iwata ◽  
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Takeshi Todo ◽  
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2008 ◽  
Vol 84 (4) ◽  
pp. 970-976 ◽  
Author(s):  
Yasushi Imamoto ◽  
Miki Harigai ◽  
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Mikio Kataoka


2002 ◽  
Vol 42 (supplement2) ◽  
pp. S153
Author(s):  
N. Shimizu ◽  
H. Kamikubo ◽  
Y. Yamazaki ◽  
Y. Imamoto ◽  
K. Mihara ◽  
...  




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2001 ◽  
Vol 40 (30) ◽  
pp. 8997-9004 ◽  
Author(s):  
Yasushi Imamoto ◽  
Yuji Shirahige ◽  
Fumio Tokunaga ◽  
Takamasa Kinoshita ◽  
Kazuo Yoshihara ◽  
...  


Author(s):  
P.P.K. Smith

Grains of pigeonite, a calcium-poor silicate mineral of the pyroxene group, from the Whin Sill dolerite have been ion-thinned and examined by TEM. The pigeonite is strongly zoned chemically from the composition Wo8En64FS28 in the core to Wo13En34FS53 at the rim. Two phase transformations have occurred during the cooling of this pigeonite:- exsolution of augite, a more calcic pyroxene, and inversion of the pigeonite from the high- temperature C face-centred form to the low-temperature primitive form, with the formation of antiphase boundaries (APB's). Different sequences of these exsolution and inversion reactions, together with different nucleation mechanisms of the augite, have created three distinct microstructures depending on the position in the grain.In the core of the grains small platelets of augite about 0.02μm thick have farmed parallel to the (001) plane (Fig. 1). These are thought to have exsolved by homogeneous nucleation. Subsequently the inversion of the pigeonite has led to the creation of APB's.



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