A quantitative structure-function relationship for the Photosystem II reaction center: supermolecular behavior in natural photosynthesis

Microsecond freeze-hyperquenching: development of a new ultrafast micro-mixing and sampling technology and application to enzyme catalysis

A novel freeze-quench instrument with a characteristic <<dead-time>> of 137 +/- 18 micros is reported. The prototype has several key features that distinguish it from conventional freeze-quench devices and provide a significant improvement in time resolution: (a) high operating pressures (up to 400 bar) result in a sample flow with high linear rates (up to 200 m s(-1)); (b) tangential micro-mixer with an operating volume of approximately 1 nl yields short mixing times (up to 20 micros); (c) fast transport between the mixer and the cryomedium results in short reaction times: the ageing solution exits the mixer as a free-flowing jet, and the chemical reaction occurs "in-flight" on the way to the cryomedium; (d) a small jet diameter (approximately 20 microm) and a high jet velocity (approximately 200 m s(-1)) provide high sample-cooling rates, resulting in a short cryofixation time (up to 30 micros). The dynamic range of the freeze-quench device is between 130 micros and 15 ms. The novel tangential micro-mixer efficiently mixes viscous aqueous solutions, showing more than 95% mixing at eta < or = 4 (equivalent to protein concentrations up to 250 mg ml(-1)), which makes it an excellent tool for the preparation of pre-steady state samples of concentrated protein solutions for spectroscopic structure analysis. The novel freeze-quench device is characterized using the reaction of binding of azide to metmyoglobin from horse heart. Reaction samples are analyzed using 77 K optical absorbance spectroscopy, and X-band EPR spectroscopy. A simple procedure of spectral analysis is reported that allows (a) to perform a quantitative analysis of the reaction kinetics and (b) to identify and characterize novel reaction intermediates. The reduction of dioxygen by the bo3-type quinol oxidase from Escherichia coli is assayed using the MHQ technique. In these pilot experiments, low-temperature optical absorbance measurements show the rapid oxidation of heme o3 in the first 137 micros of the reaction, accompanied by the formation of an oxo-ferryl species. X-band EPR spectroscopy shows that a short-living radical intermediate is formed during the oxidation of heme o3. The radical decays within approximately 1 ms concomitant with the oxidation of heme b, and can be attributed to the PM reaction intermediate converting to the oxoferryl intermediate F. The general field of application of the freeze-quench methodology is discussed.

Architecture of the photosynthetic oxygen-evolving center

Photosynthesis uses light energy to drive the oxidation of water at an oxygen-evolving catalytic site within photosystem II (PSII). We report the structure of PSII of the cyanobacterium Thermosynechococcus elongatus at 3.5 angstrom resolution. We have assigned most of the amino acid residues of this 650-kilodalton dimeric multisubunit complex and refined the structure to reveal its molecular architecture. Consequently, we are able to describe details of the binding sites for cofactors and propose a structure of the oxygen-evolving center (OEC). The data strongly suggest that the OEC contains a cubane-like Mn3CaO4 cluster linked to a fourth Mn by a mono-micro-oxo bridge. The details of the surrounding coordination sphere of the metal cluster and the implications for a possible oxygen-evolving mechanism are discussed.

Engine of life and big bang of evolution: a personal perspective

Photosystem II (PS II) is the engine for essentially all life on our planet and its beginning 2.5 billion years ago was the 'big bang of evolution.' It produces reducing equivalents for making organic compounds on an enormous scale and at the same time provides us with an oxygenic atmosphere and protection against UV radiation (in the form of the ozone layer). In 1967, when I began my career in photosynthesis research, little was known about PS II. The Z-scheme had been formulated [Hill and Bendall (1960) Nature 186: 136-137] and Boardman and Anderson [(1964) Nature 203: 166-167] had isolated PS II as a discrete biochemical entity. PS II was known not only to be the source of oxygen but of variable chlorophyll fluorescence [Duysens and Sweers (1963) In: Studies on Microalgae and Photosynthetic Bacteria, pp. 353-372. University of Tokyo Press, Tokyo] and delayed chlorophyll fluorescence [Arnold and Davidson (1954) J Gen Physiol 37: 677-684]. P680 had just been discovered [Döring et al. (1967) Z Naturforsch 22b: 639-644]. No wonder the 'black box of PS II' was described at that time by Bessel Kok and George Cheniae [Current Topics in Bioenergetics 1: 1-47 (1966)] as the 'inner sanctum of photosynthesis.' What a change in our level of understanding of PS II since then! The contributions of many talented scientists have unraveled the mechanisms and structural basis of PS II function and we are now very close to revealing the molecular details of the remarkable and thermodynamically demanding reaction which it catalyzes, namely the splitting of water into its elemental constituents. It has been a privilege to be involved in this journey.