Studies on the slow fluorescence decline in isolated chloroplasts.

Data presented here indicate that the slow fluorescence decline in osmotically disrupted chloroplasts is not associated with the well known divalent cation effect on fluorescence yield. Thus the two phenomena have markedly different magnesium concentration requirements, magnesium addition after the fluorescence decline did not stimulate the dark reversal, and the characteristics of the fluorescence induction kinetics of the two processes are not similar. At pH 7.6 the slow fluorescence decline was stimulated by several uncouplers demonstrated to greatly reduce proton pumping, and at pH 9.2 it was stimulated by all uncouplers tested. Acid-base transition was strongly inhibitory, and this inhibition was relieved by coupling factor is suggested by experiments in which phosphorylation substrates were inhibitory, and this inhibition was prevented by uncoupler. These data are explained in terms of coupling factor structural changes which in an unknown manner influence Photosystem II fluorescence emission. Fluorescence induction curves indicate that the slow quenching decreased only the variable fluorescence. The half rise time was decreased along with the sigmoidicity of the rise curve. These data can be accomodated in terms of a model recently proposed by Butler and Kitajima (Biochim. Biophys Acta (1975) 376, 116-125), involving the transfer of energy from the excited, but closed, reaction centres II to the light harvesting chlorophyll system. The slow fluorescence decline is suggested to represent a decrease of this process.