1. Introduction
Photosynthesis is a fundamental process that converts light energy into chemical energy. Oxygenic phototrophs use two photosystems (PSI and PSII) that constitute the Z-scheme and the associated generation of assimilatory power. Photosystems are multisubunit complexes in the thylakoid membrane and PSII absorbs and transforms light energy into chemical energy resulting in water splitting and oxygen evolution. PsbA (D1) and PsbD (D2) are the core subunits of PSII that exhibit photooxidoreductase activities and convert plastoquinone and water into plastoquinol (QH
2) and dioxygen (O
2). The Mn
4CaO
5 cluster is the oxygen evolution centre of PSII and is directly coordinated with multiple conserved residues of D1 and PsbC (CP43)-glutamic acid-354 (E354), further stabilised through second coordination spheres supported by conserved residues of D1, D2, and CP43 [1-3]. The tyrosine-161 (Y161) and histidine-190 (H190) residues of D1 work in tandem to transfer electrons to the reaction centre Chl
a (P
680), wherein Y161 transfers electrons and H190 acts as a proton acceptor [
4,
5]. Charge separation involves the transfer of an electron from P
680, which then forms P
680+, to primary acceptor (plastoquinone, Q) via an intermediary acceptor, pheophytin (Pheo
a).
Amino acids residues surrounding the Mn
4CaO
5 cluster affect the PSII oxygen evolving capacity [
6,
7]. For example, a N181A/S mutation of the D1 protein results in slower O-O bond formation during water-splitting reaction in
Synechocystis sp. PCC 6803 [
8].
A D170A/S substitution of D1 poisons oxygen evolving capacity, while D170E mutation is complementary with little effect on the activity [9]. Additionally, the substitutions N87A/S, F117L, D170AES, and E189D in D1 results in impaired water-splitting activity and possibly reduced PSII stability [5].
Cyanobacteria typically possess multiple
psbA gene copies with different expression levels that mostly reflect varying environmental conditions [1,10-12]. For example,
Synechocystis sp. PCC 6803 has three
psbA genes with
psbA1 upregulated in high light,
psbA2 constitutively expressed [
13], and
psbA3 expressed during low oxygen “microaerophilic” conditions. A general name of
psbA’ is given to “microaerophilic”
psbA genes since other cyanobacteria have a comparable strategy [
14].
Dark expression of sentinel
psbA (belonging to the “rogue” D1 group) blocked oxygen-evolving PSII activity through an uncleavable C-terminus and altered amino acid residues surrounding the Mn
4CaO
5 cluster in nitrogen-fixing cyanobacterium
Cyanothece [
1,
15,
16]. Recently, a D1 variant was renamed “chlorophyll
f synthase (ChlF)”. It is a far-red light (FRL) induced paralog of D1 in Chl
f-producing cyanobacteria [
17]. The ChlF encoding gene participates in the far-red light-induced photoacclimation (FaRLiP) gene cluster and it is only transcribed under FRL conditions. It is unknown how ChlF catalyses the formation of chlorophyll
f (Chl
f) from Chl
a, although molecular oxygen is required [
18]. The ChlF-encoding gene from
Chroococcidiopsis thermalis PCC 7203 (AFY86562) was used to replace the D1 subunit-encoding gene in the PSII complex of
Synechocystis sp. PCC 6803 that resulted in up to ~0.1% Chl
f of total chlorophyll when the transformant was grown photoheterotrophically with 5 mM glucose at a light intensity of 10–30 μmol photons m
-2 s
-1 [
19]. ChlF is a D1 paralog that lacks many of the conserved amino acid residues surrounding the Mn
4CaO
5 cluster [
1]. Those conserved amino acids in ChlF may play important roles in control of assembling an unconventional oxygen-evolving centre if ChlF substitutes for D1 in PSII complexes.
Chl
f has a 2-formyl in the C2-position of Chl
a responsible for the bulk red shifted absorption and possesses the most red-shifted absorption in chlorophylls [
20]. Chl
f enables cyanobacteria to utilize habitats in low white light (WL) and high FRL conditions [21-26]. The far-red light acclimation is also reported in endolithic cyanobacteria [22, 27,28]. Chl
f is present in PSI and PSII when ChlF is heterologously expressed in
Synechocystis sp. PCC 6803 and
Synechococcus sp. PCC 7002 [
19,
29]. Chl
f is detected in isolated PSI and PSII systems induced by FRL conditions in the following Chl
f-producing cyanobacteria:
Chroococcidiopsis thermalis,
Synechococcus sp. PCC 7335, and
Halomicronema hongdechloris [19,29-32] although there are quite few other cyanobacteria reported to produce Chl
f [22-26]. Absorption spectra of naturally occurring Chl
f-containing photosystems are more red-shifted than heterologously produced Chl
f-containing PS complexes owing to a relatively higher Chl
f content [
29,
32].
There are five
psbA genes in the
H. hongdechloris genome. In particular,
psbA2 (
XM38_018880) codes for WL-D1 (or typical D1) protein in
H. hongdechloris in WL conditions [
33]. In turn,
psbA3 (
XM38_020870) and
psbA4 (
XM38_037330) are expressed in WL conditions but at a lower level than
psbA2 [
33].
H. hongdechloris has paralogous genes encoding FRL-D2 (
XM38_010820), FRL-CP47 (
XM38_010800), FRL-CP43 (
XM38_010810), FRL-PsbH (
XM38_010780), FRL-PsbO (
XM38_010880), and FRL-PsbV (
XM38_010890) subunits of PSII in FRL grown cells. In addition, FRL-D1 (
XM38_010770) and ChlF (
XM38_010900) encoding genes in the FaRLiP gene cluster are up-regulated in FRL conditions [
33].
The Mn
4CaO
5 cluster is the centre of water-splitting catalytic region and is directly coordinated with D1 and CP43 in PSII [
34]. Cells grown in FRL conditions have a lower O
2-evolving rate than that of the cells grown under WL conditions [
35]. ChlF from
H. hongdechloris has over 70% conserved residues compared with typical D1 proteins. This supports an idea that ChlF may replace the WL-D1 subunit and exhibit a similar stability in the PSII complexes (33). A specific Q127 and D128 substitutions in ChlF (QD motif) is critical for activity and might be involved in binding the newly synthesised Chl
f [
19]. However, it is unclear whether these amino acid residues are directly involved in Chl
f biosynthesis.
This report used published data on cyanobacterial PSII structure to characterize the functional motifs of ChlF from H. hongdechloris at the primary and 3D-structural modelling levels. As a whole, the new insights into the functional mechanisms of ChlF and Chl f biosynthesis should allow for a better understanding of the various functions of D1 paralogs.
4. Discussion
The genes encoding FRL-D1 and ChlF are in the FaRLiP cluster under the same regulatory mechanism [
33]. The different functions of D1 paralogs (FRL-D1 and ChlF) support the hypothesis of two different forms of PSII complexes assembled under FRL conditions. One of the substituted FRL-PSII of such complexes contains FRL-D1 and other FRL-PSII subunits. FRL-D1 proteins possess all essential conserved motifs of the D1 protein and agree well with published FRL-PSII cryo-EM structure [
50], although the alignment of 18 FRL-D1 sequence showed variations at the positions of L124 with A/S/C and L206 with 3 species having F206 at the position (
Figure 2). Presence of the critical residues coupling of oxygen evolving Mn
4CaO
5 cluster in FRL-D1 suggests a functional Chl
a/
f-binding PSII under FRL conditions as PSII-FRL-D1 complexes (
Figure 2). Therefore, the FRL-PSII complex conducts PSII-performing charge separation and water-splitting reactions under FRL conditions, which is consistent with recent structure of PSII complexes acclimated to FRL conditions [50-52]. Meanwhile FRL-PSII complex (PSII-ChlF) containing the ChlF subunit instead of D1 proteins (FRL-D1 or WL-D1) plays a certain role in Chl
f biosynthesis. PSII-ChlF contains the previously described QD motif [
19] and presences of conserved L117, Q127, D128, S144, L145, F147, Q 252, and S285 in the 18 ChlF sequences. Six out of eight specific amino acid residues surrounding Mn4CaO5 are not shared with typical D1 and FRL-D1 although some changes are various between ChlF sequences (
Figure 8). H332 from typical D1 changed as H332D, H332E, H332N, H332R, H332S, H332Q, and H332K in ChlF (
Figure 3) and experimental data indicated most mutants abolished oxygen evolution capability and only mutants of H335S and H335Q gave 10-15% oxygen evolution rate [
49]. The PSII-ChlF structural model supports a new function of ChlF although it shares >70% homology with D1.
4.1. Proposed uncoupled Mn4CaO5 cluster in PSII-ChlF complexes
The centre of oxygen evolving complex is the Mn
4CaO
5 cluster. It is stabilized with reaction centre proteins D1 and D2 and is surrounded by inner antenna proteins CP47 (near D2), and CP43 (near D1) [
53]. Water-splitting proceeds in a multi-step process whereby the carefully positioned antenna chlorophylls of CP43 and CP47 transfer their excitation energy to reaction centre chlorophylls (P
D1 and P
D2) of D1 and D2, respectively. Excited P
680 donates electron to primary acceptor Pheo
a which transmits it to Q
A and Q
B. Oxidized P
680+ is reduced by an electron donated
via Y161 (Y
Z, D1) by the chemical splitting of water into oxygen. This occurs because the Mn
4CaO
5 cluster undergoes a series of redox reactions known as Kok’s “oxygen clock” [half-reactions: 2H
2O → 4H
+ + 4e
- + O
2, and 2Q
B + 4H
+ + 4e
- →2Q
BH
2]. Y
Z is an electron donor for P
680+ of PSII and an electron carrier from the Mn
4CaO
5 cluster to the electron acceptor P
680+.
ChlF synthase is a paralog of the reaction centre protein D1, however, structural modelling (
Figure 3 and 7) confirmed the differences between ChlF and FRL-D1 and proposed an uncoupled Mn
4CaO
5 cluster in the PSII-ChlF complex. The proposed unconventional Mn
4CaO
5 cluster is supported by noticeable variations from ChlF sequences in the region of the 241-DEEE motif (
Figure 3), the position to coordinating the bicarbonate in the typical D1 [
1]. This is consistent with the hypothesis of “super-rogue” D1 proteins [
1,
11]. Additionally, N298 on D1 protein is required for oxygen evolution and mutants of N298D and N298E will impair oxygen evolving activity [
54]. The substitution D298 and E298 occurs in 15 ChlF sequences (
Figure 3).
P
680+ is a powerful oxidant that facilitates the extraction of electrons from the Mn
4CaO
5 cluster via redox active Y
Z. Hence, reduction of P
680+ might occur via cytochrome
b559 and Chl
a, or via Y
Z and Y
D in the absence of coordinated active Mn
4CaO
5 cluster. Electron donation to P
680+ via Y
Z is still possible with the aid of Y
D at a higher pH environment; that is, Y
D can outcompete Y
Z in the reduction of P
680+ at a higher pH [
55]. The altered electron transfer in the PSII-ChlF complex may enable the reduction of P
680+ by the oxygenation of Chl
a at the C-2 position to produce Chl
f.
4.2. The changed electron transfer pathways in dysfunctional PSII-ChlF complexes
ChlF has an unconventional coordinated Mn
4CaO
5 cluster (
Figure 8). According to experimental data, the significant changes surrounding the Mn
4CaO
5 cluster could not support water oxidation and oxygen evolution even if it presents in PSII-ChlF complexes [4-7,49,54]. In additional, the changes at the D1 conserved sites N87, F117, D170, and E189 in ChlF (
Figure 3) reduced PSII stability including the impaired water-splitting activities
[5]. Another noticed changes around Pheo a including the feature substitution Q128D129 motif in ChlF (Figure 7). The conserved site of F147 in ChlF could shift the Em(Pheo a/Pheo a-) to more positive values and decrease the recombination rate of 1[P680+/Pheo a] to P*680 [56]. However, ChlF has conserved Y
Z and Y
D together with H-bond partners H190 (D1) and H189 (D2) at similar modelled distances to that of D1. On the whole, this suggests that there is an altered electron transport efficiency from P
680+ to primary and secondary acceptors. The presumed non-functional uncoupled Mn
4CaO
5 cluster in PSII-ChlF complexes suggests that Y
Z and Y
D supply the electrons required for the completion of redox reactions. Y160 of ChlF is conserved compared to other D1 sequences; however, this residue is not needed for the catalytic formation of Chl
f [
57]. Interestingly, the F147Y substitution in ChlF could cause the undelivered (or slower) electron at the level of Pheo
a. Additionally, electron transfer within PSII is possible from a photooxidized reaction centre to Pheo
a, Q
A, and Q
B. DCMU (3-(3,4-dichlorophenyl)-1,1-dimethylurea) is an inhibitor of the Q
B binding site and inhibits Chl
f synthesis [
57]. Therefore, the light-driven redox chemistry of PSII without the coupled Mn
4CaO
5 cluster would play an active role in Chl
f biosynthesis.
PSII electron transfer follows the resonance energy migration within the light-harvesting antenna with the resulting excitation of the reaction centre primary donor (chlorophyll dimer P
680, or P
D1 and P
D2) while the primary acceptor (Pheo
a) reduces the primary quinone (Q
A). This causes a reduction of oxidized P
680+• by Y
Z of D1 due to water oxidation by the coordinated Mn
4CaO
5 cluster. Impairment of the Mn
4CaO
5 cluster suggests that there is a longer-lived P
680+• radical [
58], and superoxide or H
2O
2 may be released as a long-lifetime free radical [
59,
60]. The expression of a ChlF encoding gene in a PSII-less mutant (D1/D2 double mutant) yielded Chl
f, and its production was regulated by light-driven electron transfer [
57]. Hence, a longer-lived P
680+• radical is required for Chl
f biosynthesis.
4.3. Reaction mechanism of Chl f biosynthesis pathway
Oxidation of a methyl group to a formyl group is a difficult task because CH
3 is a chemically stable side-group. Free radical formation can be specifically involved [61-63]. Pheo
a on the acceptor side of PSII may form singlet oxygen or hydroxyl free radical.
Figure 4 suggests that the specific substituted residues of F147 in ChlF cause a loss of the H-bond at C17
3-Pheo
a and a potential slower electron transfer rate, although there were no available experimental data, such as a constructed mutant of Y147F (
Figure 4). The non-heme iron may also contribute to the formation of singlet oxygen or hydroxide radicals in the presence of light and aerobic conditions [64-67]. The inhibition of Chl
f synthesis by DCMU implied that electron transports by primary and secondary acceptors Pheo
a, Q
A, and Q
B were involved in the reaction chemistry [
57]. As is known in PSII, the dominant pathway of charge recombination goes through the radical pair of [P
680+/Pheo
a-] and an additional non-radiative pathway could proceed through repopulation of P*
680 from
1[P
680+/Pheo
a-], which was observed in D1 mutant Q130E in
Synechocystis PCC 6803 [
56]. We proposed the reaction scheme of Chl(Chlide)
f synthesis from Chl(Chlide)
a via free radical chemistry (
Figure 9). Pheo
a excitation in an oxygenated environment produces an anion radical (D
-•) via singlet and triplet excited state coupled to electron donation by Chl
a. The cation-radical of the Chl
a methyl group is produced via deprotonation. This cation-radical reacted with dioxygen to form a peroxide further oxidized to superoxide or hydroxyl radical (
Figure 9, step 4a) via reductants Pheo
a (-610 mV) or Q
A- (-80 mV) [
68,
69].
Peroxide radical can decompose to a hydroxymethyl-Chl derivative, and further react to form the formyl group in an unknown pathway (
Figure 9, step 4b). Therefore, the altered electron pathway from P
680+ to Pheo
a, Q
A, and Q
B in the PSII-ChlF complex drives Chl
f synthesis. The non-heme iron of PSII might not be involved in this oxygenation in the proposed mechanism; this differs from the biosynthetic mechanism of Chl
b [
70].
Chemical synthesis involving the oxidation of aromatic molecules with a methyl sidechain is often accomplished by free-radical chemistry using water as proton source under elevated temperatures; over-oxidation to the carboxylic acid is prevented by addition of a catalyst such as copper [
71]. More recently, a radical-free mechanism was more specific for the synthesis of formyl groups [
72]. ChlF has a likely impaired oxygen evolving cluster; therefore, there is an increased potential of light-induced photoinhibition (even under low visible light) [
73]. Two important photoinhibition sites in PSII include charge separation between P
680+ and Q
A-, and electron transfer from Y
Z to P
680+ [
74]. Photoinhibition can cause carotenoid and chlorophyll radicals (from photopigments adjacent to P
680 and accessory Chls) following the loss of Y
Z and Y
D radicals [
75]. Accessory Chls and carotenoids in PSII have been proven to represent sites of photoinhibition damage following a hydroxylamine treatment [
76]. It is unclear if ChlF is degraded during photoinhibition since detailed studies are unavailable. The A345, S345, or F345 substitutions in the functional domain of D1 resulted in comparable hydrolysis rates following carboxyl-terminal processing protease (CtpA), while G345 and V345 substitutions showed lower hydrolysis rates [
77]. However, the P345 substitution resulted in complete inhibition [
77].
ChlF has two unique S motifs in addition to the QD motif (
Figure 3) that are likely hydrolysis sites with potentially lower hydrolysis rates. The H-bond between Y
Z and H190 of ChlF is potentially retained, although there may be H-bonds with other amino acids when the Mn
4CaO
5 cluster is depleted or uncoupled. Hence, electron transfer from Y
Z to P
680+ is possible without the coupled functional Mn
4CaO
5 cluster although it could be slower [
2,
78,
79]. Therefore, a long-lived P
680+ may exist in PSII-ChlF complex that functions as a powerful oxidant with a redox potential of approximately 1.13 mV [
78].
Replacement of an MG motif in D1 to a unique QD motif in ChlF facilitates the production of Chl
f in vivo. This suggests that the QD motif is the most probable active site of the enzyme, although it is unknown whether close proximity of D128 is critical [
19]. Further work is required to determine whether photoinhibition (or free radical formation) in the PSII-ChlF complex in fact catalyzes Chl
f production.