Profile Hidden Markov Models for Analyzing Similarities and Dissimilarities in the Bacterial Reaction Center and Photosystem II

Characterization of the Rate-Limiting Steps in the Dark-To-Light Transitions of Closed Photosystem II: Temperature Dependence and Invariance of Waiting Times during Multiple Light Reactions

Rate-limiting steps in the dark-to-light transition of Photosystem II (PSII) were discovered by measuring the variable chlorophyll-a fluorescence transients elicited by single-turnover saturating flashes (STSFs). It was shown that in diuron-treated samples: (i) the first STSF, despite fully reducing the QA quinone acceptor molecule, generated only an F1(<Fm) fluorescence level; (ii) to produce the maximum (Fm) level, additional excitations were required, which, however, (iii) were effective only with sufficiently long Δτ waiting times between consecutive STSFs. Detailed studies revealed the gradual formation of the light-adapted charge-separated state, PSIIL. The data presented here substantiate this assignment: (i) the Δτ1/2 half-increment rise (or half-waiting) times of the diuron-treated isolated PSII core complexes (CCs) of Thermostichus vulcanus and spinach thylakoid membranes displayed similar temperature dependences between 5 and −80 °C, with substantially increased values at low temperatures; (ii) the Δτ1/2 values in PSII CC were essentially invariant on the Fk−to-Fk+1 (k = 1−4) increments both at 5 and at −80 °C, indicating the involvement of the same physical mechanism during the light-adaptation process of PSIIL. These data are in harmony with the earlier proposed role of dielectric relaxation processes in the formation of the light-adapted charge-separated state and in the variable chlorophyll-a fluorescence of PSII.

Comparison of proton transfer paths to the QA and QB sites of the Rb. sphaeroides photosynthetic reaction centers

The photosynthetic bacterial reaction centers from purple non-sulfur bacteria use light energy to drive the transfer of electrons from cytochrome c to ubiquinone. Ubiquinone bound in the Q_A site cycles between quinone, Q_A, and anionic semiquinone, Q_A^·-, being reduced once and never binding protons. In the Q_B site, ubiquinone is reduced twice by Q_A^·-, binds two protons and is released into the membrane as the quinol, QH₂. The network of hydrogen bonds formed in a molecular dynamics trajectory was drawn to investigate proton transfer pathways from the cytoplasm to each quinone binding site. Q_A is isolated with no path for protons to enter from the surface. In contrast, there is a complex and tangled network requiring residues and waters that can bring protons to Q_B. There are three entries from clusters of surface residues centered around HisH126, GluH224, and HisH68. The network is in good agreement with earlier studies, Mutation of key nodes in the network, such as SerL223, were previously shown to slow proton delivery. Mutational studies had also shown that double mutations of residues such as AspM17 and AspL210 along multiple paths in the network presented here slow the reaction, while single mutations do not. Likewise, mutation of both HisH126 and HisH128, which are at the entry to two paths reduce the rate of proton uptake.

Genomics of a phototrophic nitrite oxidizer: insights into the evolution of photosynthesis and nitrification

Oxygenic photosynthesis evolved from anoxygenic ancestors before the rise of oxygen ~2.32 billion years ago; however, little is known about this transition. A high redox potential reaction center is a prerequisite for the evolution of the water-oxidizing complex of photosystem II. Therefore, it is likely that high-potential phototrophy originally evolved to oxidize alternative electron donors that utilized simpler redox chemistry, such as nitrite or Mn. To determine whether nitrite could have had a role in the transition to high-potential phototrophy, we sequenced and analyzed the genome of Thiocapsa KS1, a Gammaproteobacteria capable of anoxygenic phototrophic nitrite oxidation. The genome revealed a high metabolic flexibility, which likely allows Thiocapsa KS1 to colonize a great variety of habitats and to persist under fluctuating environmental conditions. We demonstrate that Thiocapsa KS1 does not utilize a high-potential reaction center for phototrophic nitrite oxidation, which suggests that this type of phototrophic nitrite oxidation did not drive the evolution of high-potential phototrophy. In addition, phylogenetic and biochemical analyses of the nitrite oxidoreductase (NXR) from Thiocapsa KS1 illuminate a complex evolutionary history of nitrite oxidation. Our results indicate that the NXR in Thiocapsa originates from a different nitrate reductase clade than the NXRs in chemolithotrophic nitrite oxidizers, suggesting that multiple evolutionary trajectories led to modern nitrite-oxidizing bacteria.

Analysis of heterologous regulatory and coding regions in algal chloroplasts

The basic photosynthetic apparatus is highly conserved across all photosynthetic organisms, and this conservation can be seen in both protein composition and amino acid sequence. Conservation of regulatory elements also seems possible in chloroplast genes, as many mRNA untranslated regions (UTRs) appear to have similar structural elements. The D1 protein of Photosystem II (psbA gene) is a highly conserved core reaction center protein that shows very similar regulation from cyanobacteria through higher plants. We engineered full and partial psbA genes from a diverse set of photosynthetic organisms into a psbA deficient strain of Chlamydomonas reinhardtii. Analysis of D1 protein accumulation and photosynthetic growth revealed that coding sequences and promoters are interchangeable even between anciently diverged species. On the other hand functional recognition of 5' UTRs is limited to closely related organisms. Furthermore transformation of heterologous promoters and 5' UTRs from the atpA, tufA and psbD genes conferred psbA mRNA accumulation but not translation. Overall, our results show that heterologous D1 proteins can be expressed and complement Photosystem II function in green algae, while RNA regulatory elements appear to be very specific and function only from closely related species. Nonetheless, there is great potential for the expression of heterologous photosynthetic coding sequences for studying and modifying photosynthesis in C. reinhardtii chloroplasts.

Chemical Evidence for the Dawn of Life on Earth

The dating of the dawn of life on Earth is a difficult task, requiring an accumulation of evidences from many different research fields. Here we shall summarize findings from the molecular scale (proteins) to cells and photosynthesis-related-fossils (stromatolites from the early and the late Archaean Eon), which indicate that life emerged on Earth 4.2–3.8 Ga (i.e. 4.2–3.8 × 109 years) ago. Among the data supporting this age, the isotopic and palaeontological fingerprints of photosynthesis provide some of the strongest evidence. The reason for this is that photosynthesis, carried out in particular by cyanobacteria, was responsible for massive changes to the Earth’s environment, i.e. the oxygenation of the Earth’s atmosphere and seawater, and the fixation of carbon from atmospheric CO2 in organic material. The possibility of a very early (>3.8 Ga ago) appearance of complex autotrophic organisms, such as cyanobacteria, is a major change in our view of life’s origins.

M234Glu is a component of the proton sponge in the reaction center from photosynthetic bacteria

Bacterial reaction centers use light energy to couple the uptake of protons to the successive semi-reduction of two quinones, namely Q(A) and Q(B). These molecules are situated symmetrically in regard to a non-heme iron atom. Four histidines and one glutamic acid, M234Glu, constitute the five ligands of this atom. By flash-induced absorption spectroscopy and delayed fluorescence we have studied in the M234EH and M234EL variants the role played by this acidic residue on the energetic balance between the two quinones as well as in proton uptake. Delayed fluorescence from the P(+)Q(A)(-) state (P is the primary electron donor) and temperature dependence of the rate of P(+)Q(A)(-) charge recombination that are in good agreement show that in the two RC variants, both Q(A)(-) and Q(B)(-) are destabilized by about the same free energy amount: respectively approximately 100 +/- 5 meV and 90 +/- 5 meV for the M234EH and M234EL variants, as compared to the WT. Importantly, in the M234EH and M234EL variants we observe a collapse of the high pH band (present in the wild-type reaction center) of the proton uptake amplitudes associated with formation of Q(A)(-) and Q(B)(-). This band has recently been shown to be a signature of a collective behaviour of an extended, multi-entry, proton uptake network. M234Glu seems to play a central role in the proton sponge-like system formed by the RC protein.

Proton-transfer pathways in photosynthetic reaction centers analyzed by profile hidden markov models and network calculations

In the bacterial reaction center (bRC) of Rhodobacter sphaeroides, the key residues of proton transfer to the secondary quinone (Q(B)) are known. Also, several possible proton entry points and proton-transfer pathways have been proposed. However, the mechanism of the proton transfer to Q(B) remains unclear. The proton transfer to Q(B) in the bRC of Blastochloris viridis is less explored. To analyze whether the bRCs of different species use the same key residues for proton transfer to Q(B), we determined the conservation of these residues. We performed a multiple-sequence alignment based on profile hidden Markov models. Residues involved in proton transfer but not located at the protein surface are conserved or are only exchanged to functionally similar amino acids, whereas potential proton entry points are not conserved to the same extent. The analysis of the hydrogen-bond network of the bRC from R. sphaeroides and that from B. viridis showed that a large network connects Q(B) with the cytoplasmic region in both bRCs. For both species, all non-surface key residues are part of the network. However, not all proton entry points proposed for the bRC of R. sphaeroides are included in the network in the bRC of B. viridis. From our analysis, we could identify possible proton entry points. These proton entry points differ between the two bRCs. Together, the results of the conservation analysis and the hydrogen-bond network analysis make it likely that the proton transfer to Q(B) is not mediated by distinct pathways but by a large hydrogen-bond network.