Photo-Assembly of the Catalytic Manganese Cluster
Transcript of Photo-Assembly of the Catalytic Manganese Cluster
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PHOTOSYSTEM II: THE WATER/PLASTOQUINONE OXIDO-
REDUCTASE IN PHOTOSYNTHESIS
T. WYDRZYNSKI AND K. SATOH, EDITORS
CHAPTER 25
PHOTO-ASSEMBLY OF THE CATALYTIC MANGANESE CLUSTER
G. Charles Dismukes*
Department of Chemistry and Princeton Environmental Institute
Princeton University
Princeton, NJ, USA
Gennady M. Ananyev
Department of Environmental Biophysics & Molecular Ecology
Rutgers University, E. Brunswick, NJ, USA
Richard Watt
Department of Chemistry
University of New Mexico, Albuqurque, NM, USA
*correspondence at [email protected], FAX: 609-258-1980
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Table of Contents
Abbreviations ............................................................................................................... 3
I. Introduction .......................................................................................................... 4
II. Function of PSII Subunits in Water Splitting and Photo-assembly ........................ 4
A. The PSII Core Complex. ................................................................................... 5
B. Extrinsic Proteins .............................................................................................. 7
1. The Manganese Stabilizing Protein. The MSP ................................................ 7
2. Other Extrinsic Proteins. ................................................................................ 10
C. Small Subunits ................................................................................................ 10
D. [Mn]4 Core ....................................................................................................... 10
E. The Calcium Effector Site ................................................................................ 11
III. Biogenesis of PSII-WOC ..................................................................................... 12
A. Subunit Assembly ............................................................................................. 12
1. Prokaryotes .................................................................................................... 12
2. Chloroplasts ................................................................................................... 14
B. Mn2+
Uptake Into the Cell ................................................................................. 15
C. Inorganic Core Assembly Involves no Protein Chaperones .............................. 16
IV. Roles of the Inorganic Cofactors from Photo-assembly ...................................... 18
A. Assembly of the Inorganic Core ....................................................................... 18
1. Instrumentation. ............................................................................................. 18
2. Kinetics and Mechanism. ............................................................................... 19
3. Proton Evolution. ........................................................................................... 20
4. Oxo/Hydroxo/Bicarbonate Sites. ................................................................... 21
5. Calcium. ......................................................................................................... 22
6. Protein Subunits Required for Photoactivation .............................................. 24
B. “Inorganic Mutants” of the Manganese and Calcium Sites .............................. 25
1. Manganese Mutants. ...................................................................................... 25
2. Calcium Mutants ............................................................................................ 26
3. Other Metal Ion Sites. .................................................................................... 28
V. Concluding Remarks ..................................................................................... 28
Acknowledgements .................................................................................................... 29
References .................................................................................................................. 38
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Summary
The biogenesis of the photosystem II membrane protein complex is reviewed with emphasis on
the sequence and location of assembly of the subunits within the internal membrane systems of
prokaryotes and chloroplasts. The uptake and distribution of manganese in cyanobacterial cells is
discussed. The role of individual subunits in the isolated photosystem II in light-induced
assembly of the inorganic core of the water splitting complex is discussed (photoactivation
process). The roles of the inorganic cofactors (Mn2+
, Ca2+
, Cl- and bicarbonate) in water splitting
are revealed by examining the effects of their reconstitution with non-native cofactors. Novel
instrumentation for the measurement of O2 concentration and the kinetics and mechanism of
photoactivation are described.
Abbreviations
CA carbonic anhydrase; Chl chlorophyll; EPR electron paramagnetic resonance; MSP
manganese-stabilizing protein; RC reaction center; WOC, water oxidizing complex; XAS x-ray
absorption spectroscopy; XRD x-ray diffraction;.
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I. Introduction
The photosynthetic water splitting enzyme (WOC) located within the Photosystem II reaction
center is responsible for nearly all biological O2 production on Earth. It is remarkable in that,
despite enormous diversification of the classes of oxygenic photoautotrophs, there is but one type
of enzymatic core that performs this chemistry (Dismukes et al. this series). The active site is a
unique mangano-calcium cluster comprised of five constituents plus water,
Mn4Ca1Clx(OHn)y(HCO3)z, that is assembled de novo from elementary ions, water and
bicarbonate by a light-driven photoassembly process within the cofactor-free apo-WOC-PSII
complex. This process is called photoactivation, after the defining works of George Cheniae and
coworkers.(Frasch et al. 2001)
This review covers recent advances dealing with the uptake, distribution, photoassembly and
function of the inorganic cofactors comprising the PSII-WOC from cyanobacteria and higher
plants. It covers aspects of Mn transport, localization and photoassembly, both in vivo during
biogenesis/repair and in vitro during reconstitution of isolated PSII-WOCs. This material
examines processes from the cellular level down to the atomic level.
II. Function of PSII Subunits in Water Splitting and Photo-assembly
A summary of the subunit positioning derived from X-ray diffraction (XRD) analysis can be
found in other chapters. Information derived from XRD is not considered in this review. We
begin with an overview of the composition of the intact PSII protein complex and the associated
inorganic core of the WOC.
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A. The PSII Core Complex
The detergent-solubilized isolated PSII protein core complex from the thermophillic
cyanobacterium Thermosynechococcus elongatus is composed of 19 polypeptide subunits (Zouni
et al. 2001; Ferreira et al. 2004), while 19 or more subunits are present in higher plants like
spinach.(Hankamer et al. 2001). However, these numbers may be underestimates of the
composition in the native membrane based on more sensitive studies using mass spectrometry
and N-terminal amino acid sequencing methods that have identified 31 unique subunits within an
isolated PSII core complex from the cyanobacterium Synechocystis 6803.(Kashino et al. 2002)
This large increase in the number of subunits within the PSII core complex may reflect both
species differences and improvements in purification afforded by polyhistidine tagging of the
CP47 subunit. The native PSII complex exists as a dimer with two-fold symmetry comprised of
two sets of reaction centers and antenna complexes that operate more or less independently in
terms of redox chemistry, but do exchange excitation energy. No reports have indicated any
difference in the properties of the WOC in monomers and dimers, although PSII heterogeneity in
the thermal activation parameters associated with water splitting is known.(Burda et al. 2001)
The D1 (psbA gene) and D2 (psbD gene) proteins are homologous and form a hetero-dimeric
reaction center within each monomeric unit (RC). However, the smallest isolated RC complex
that performs primary charge separation also contains the two subunits of cytochrome b559,
(psbE gene) and (psbF gene) (Nanba et al. 1987; Seibert 1993). The D1, D2, CP47, CP43 and
cytochrome b559 subunits comprise what is called the PSII core, as no complex without these five
subunits had been isolated that evolved oxygen( a number of small subunits that lack cofactors
are also generally present in cores). A stable CP47RC subcore complex assembles within the
thylakoid membrane of cyanobacteria in the deletion mutant lacking the psbC gene for
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CP43.(Rögner et al. 1991) These complexes can be isolated and are active in electron transport
but inactive in O2 evolution, presumably due to an incomplete Mn cluster. A stable CP47RC
subcore complex has been prepared from spinach by removal of CP43 with detergents, called the
CP47RC subcore. Although the CP47RC subcore is devoid of Mn and inactive in O2 evolution, it
is capable of full activity after reconstitution of the Mn cluster by photoactivation in the presence
of the free inorganic cofactors.(Buchel et al. 1999) The successful reconstitution of the CP47RC
subcore together with the subunit positioning data and XRD of the Mn binding site (below)
suggest that a RC subcore lacking CP47, might also be capable of O2 evolution. However, to
date no stable subcore complex lacking CP47 has been isolated to test this hypothesis.
The Mn-cluster is surrounded primarily by the lumenal surface of the D1 trans-membrane
protein of the PSII reaction center, as predicted by previous mutational studies[Diner, 1998
#79;[Debus, 2001 #2216] and model building(Svensson et al. 1996). Nixon and Diner showed
that Asp170 plays a critical role in the binding and oxidation of the first Mn2+
required for the
formation of the Mn cluster.(Nixon et al. 1992) Further spectroscopic analysis confirmed that
deletion of Asp170 significantly alters the EPR signal of the first photooxidized Mn3+
bound to
PSII. (Campbell et al. 2000) Chemical modification studies also confirmed that Asp170 is
required for the binding of Mn2+
at the high affinity site and that D1-His337 may play a role in
ligating the Mn cluster.(Ghirardi et al. 1998)
The YD radical has been found to advance the lowest S-state of the Mn cluster from S0 S1 in
the dark, while in its reduced form it shortens the lifetime of the S2 and S3 states. (Babcock et al.
1975; Styring et al. 1987; Vass et al. 1991) On this basis the YD radical was proposed to function
in vivo to stabilize the Mn cluster against over-reduction and thus possible loss of reduced
Mn2+
.(Rova et al. 1998)
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B. Extrinsic Proteins
In plants three water-soluble extrinsic proteins are attached non-covalently to the lumenal
surface of the PSII complex. Their associated genes and molecular masses are used to identify
these proteins as the 33 kDa (psbO gene), 23 kDa (psbP gene) and 19 kDa (psbQ gene).[Debus,
1992 #683;Debus, 2000 #1766] The 33 kDa protein binds first at the interface of the D1/D2
dimer and the 23 kDa protein binding adjacent to the 33 kDa protein near to the CP43 protein
with the 19 kDa protein binding last.(Nield et al. 2002) The PsbO protein is found universally in
all oxygenic photoautotrophs. The PsbP and PsbQ proteins were until recently not believed to be
present in PSII core complexes from cyanobacteria and the role of these proteins appears to be
substituted by the cytochrome c550 (psbV gene) and to a lesser extent a 12 kDa protein. (psbU
gene).(Shen et al. 1995; Shen et al. 1995; Shen et al. 1998; Ohta et al. 1999; Katoh et al. 2001)
However, recently a smaller protein of 11 kDa with high homology to the psbQ gene product
was found in a PSII core complex isolated from Synechocystis 6803, suggesting a wider
distribution than previously thought.(Kashino et al. 2002)
1. The Manganese Stabilizing Protein. The MSP is so called because removal of this protein
exposes the Mn cluster to exogenous reductants and competition for replacement of manganese
by other metal ions. In vitro photoassembly of spinach apo-WOC-PSII is slowed by the binding
of this protein. This protein is unfolded in solution and only assumes a folded structure when
bound to the intrinsic proteins of PSII.(Lydakis-Simantiris et al. 1999) The isolated spinach MSP
was found not to bind Mn2+
or Ca2+
ions in solution based on low affinity (dissociation constant
KD ~3 mM) and low stoichiometry (0.14 Mn/MSP).(Hunziker et al. 1987) MSP binds to PSII
somewhat more tightly when the Mn cluster is present(Miyao et al. 1989; Kavelaki et al. 1991;
Leuschner et al. 1996) Changes in the oxidation state of the Mn cluster in the PSII core complex
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alter the structure of the MSP making it susceptible to proteolysis.(Hong et al. 2001) PSII does
not require the MSP for oxygen evolution in vitro(Bricker 1992) nor in vivo (Burnap et al. 1991),
but in its absence, the steady-state oxygen evolution rates are decreased.(Miyao et al. 1987;
Burnap et al. 1992) This decrease is attributed to deactivation of the Mn-cluster by endogenous
reductants in the lumen. A deletion mutant of the MSP reveals that it acts as a diffusion barrier in
vivo by suppressing electron donation from Mn2+
and decreasing the quantum yield of
photoactivation in whole cells.(Chu et al. 1994; Burnap et al. 1996) When reductants are added
to PSII membranes in the presence of Ca2+
with the MSP, the Mn2+
ions are trapped and do not
diffuse away, indicating they are trapped in a compartment for later photooxidation and
reassembly of the Mn cluster.(Mei et al. 1992; Riggs-Gelasco et al. 1996) The removal of the
MSP results in the release of two Mn2+
ions from PSII membranes unless high concentrations of
Cl- and Ca
2+ are used.(Miyao et al. 1984; Ono et al. 1984) In the absence of the MSP: the S3
(S4) S0 transition is slowed 5-fold (Miyao et al. 1987; Vass et al. 1987; Burnap et al. 1992),
the S2 state is abnormally stable against dark decay to S1, the reduction kinetics of YZ are
altered(Razeghifard et al. 1997), the substrate water exchange rates are slightly decreased(Hillier
et al. 2001) and the susceptibility to photo-oxidative damage increases.(Mayes et al. 1991;
Philbrick et al. 1991)
PSII appears to possess its own mechanism and biochemical machinery for regulating the
bicarbonate concentration within the lumenal space near the WOC. A low level of carbonic
anhydrase (CA) activity has been found to be intrinsic to oxygen-evolving PSII membranes(Lu
et al. 2002). Careful analysis showed that after washing the membranes with 1 M CaCl2 to
remove the extrinsic polypeptides, the CA activity could be found in both fractions, an intrinsic
CA associated with the membranes that functions in the hydration direction and an extrinsic CA
in the soluble fraction that functions in the dehydration direction. The soluble CA activity was
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found associated with a 33 kDa protein that comigrated with the 33-MSP extrinsic protein of
PSII(PsbO). The authors proposed, and later confirmed that these are the same protein and have
demonstrated that the 33 kDa protein of PSII possesses very low level CA activity (~ 60 s-1
vs
105 s
-1 of typical Zn
2+-CA) that is dependent on the concentration of Mn
2+ and Cl
-(personal
communication A. J. Stemler). The latter results are at variance with earlier work showing that
neither Mn2+
nor Ca2+
have specific binding sites on the spinach 33-MSP when studied as a free
protein.(Hunziker et al. 1987) The discrepancy may be resolved if the Mn-dependent CA activity
represents non-specifically associated Mn2+
arising from electrostatic attraction. These results are
provocative and should be tested further to judge whether this CA activity is found in vivo and
how it may be linked, if at all, to the possible function of bicarbonate as an alternate substrate for
O2 evolution.
In cyanobacterial cells MSP binding to the PSII complex is weakened by genetic mutations to
the lumenal e-loop of CP47 which introduce anionic residues(carboxylates) for positive
residues(arginines). These same mutants also support the highest quantum yields for
photoactivation of O2 evolution. The data point to two consequences of the lumenal surface
charges on the e-loop of CP47. In wild type, two arginine groups of the e-loop of CP47 help to
maintain tight MSP binding which blocks achieving a high quantum yield of photoactivation
(presumably under Mn-limiting conditions?), while the anionic mutants bind less MSP and
exhibit the highest yields of photoactivation. The latter result is consistent with photoactivation
studies showing that absorption of anionic molecules (tetraphenylboron) but not cationic
molecules (tetraphenylphosphonium) into isolated PSII membranes accelerates the rate and
increases the quantum yield of photoactivation under conditions of low Mn2+
concentrations.(Ananyev et al. 1996; Ananyev et al. 2001) Thus, surface-bound anionic groups
in PSII, both native and exogenous in origin, are able to attract/steer Mn2+
ions from solution
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closer to the PSII complex. This role of surface anionic residues at the PSII protein/aqueous
interface is analogous to that played by the surface carboxylates in cation transporter
proteins.(Sansom et al. 2000) This function should not be confused with catalytic residues
involved in the direct coordination of Mn in the native complex.(Ishikawa et al. 2002)
2. Other Extrinsic Proteins. The 23 kDa protein (psbP gene) has been implicated in increasing
the affinity for Ca2+
to the WOC, while the 19 kDa protein (psbQ gene) enhances the Cl- binding
affinity. (Yocum 1991) As with the 33 kDa protein, when all 3 extrinsic proteins are bound, they
form a diffusion barrier that keeps the intrinsic Mn2+
, Ca2+
and Cl- ions sequestered so that the
manganese cluster can be reassembled rapidly upon illumination.(Adelroth et al. 1995;
Wincencjusz et al. 1998) In the absence of the 23- and 19-kDa proteins, oxygen evolution
requires higher concentrations of Ca2+
and Cl- ions, indicating these proteins mediate tighter
binding of these ions.
C. Small Subunits
There are several other intrinsic proteins found in the PSII protein complex, however, their role
in the photo-activation process is not yet clear. PsbI (psbI) 4.2 kDa, PsbTc (psbTc) 3.8 kDa,
PsbW (psbW) 5.9 kDa are intimately associated with the D1/D2 dimer (Debus 2000). The PsbL
(psbL), 4.3 kDa, and PsbK (psbK), 4.3 kDa, proteins are also found with D1/D2. PsbL appears to
aid in electron transfer (YzP680+ Yz
+P680)(Hoshida et al. 1997; Hoshida et al. 1997), while
both have been implicated in plastoquinone binding and are hypothesized to be positioned to
play a role in forming dimeric core units composed of two D1/D2 dimers.(Zheleva et al. 1998)
D. [Mn]4 Core
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The composition and structure of the inorganic core of the intact PSII-WOC has been examined
by a number of techniques in higher plants and cyanobacteria (primarily Synechocystis 6803 and
Thermosynechococcus). There is emerging consensus that the stoichiometry is Mn4Ca1(OHn)xCly
with as few as 1-2 high affinity chlorides in spinach.(Debus 1992; Ananyev et al. 2001; Carrell et
al. 2002) (Vrettos et al. 2001) The number of tightly bound non-exchangeable O2-
/OH-/OH2
molecules has not been directly established and the proton ionization state depends on oxidation
state.
E. The Calcium Effector Site
Calcium is essential for water oxidation in the native enzyme and can be functionally replaced by
Sr2+
.(Boussac et al. 1988) EPR reveals that removal of Ca2+
from the holoenzyme changes the
distribution of unpaired spin density among the four Mn ions. Inhibition by lanthanides reveals
that the affinity for the Ca site in the holoenzyme increases with charge density.(Ono 2000;
Vrettos et al. 2001). However, this finding differs from photoactivation studies showing that Sr2+
,
a lower charge density ion, binds 8-fold tighter to the Ca effector site in PSII membranes
depleted of the 3 extrinsic subunits (Ananyev et al. 2001). EPR reveals that Ca2+
binding to apo-
WOC-PSII selectively templates the folding of the protein complex into a form that exhibits
higher affinity for Mn2+
and binds two Mn2+
ions as a dimanganese(II,II) binuclear site.(Ananyev
et al. 1997) Strontium XAS of Ca-depleted/Sr-reconstituted PSII indicates a close positioning
(~3.5 Å) between Sr and Mn.(Cinco et al. 1998) Calcium XAS of Ca-sufficient PSII also
suggests a heavy atom scatter in the second shell.(Cinco et al. 2002) These and other data
indicate that Ca2+
directly participates in the catalysis of water splitting as an integral cofactor.
The reader is referred to other chapters on the roles of Cl-, Ca
2+ and bicarbonate in the
holoenzyme.
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III. Biogenesis of PSII-WOC
A. Subunit Assembly
1. Prokaryotes. The site of oxygenic photosynthesis in cyanobacteria, green algae and
chloroplasts is a specialized inner membrane called the thylakoid system. Photoactivation of the
inorganic cofactors of the WOC occurs within PSII complexes bound to the thylakoid
membrane.(Cheniae et al. 1971) Biochemical and electron micrographic studies of green algae
and chloroplasts indicates that the chloroplast envelope is a major biogenic structure, from which
thylakoid membranes emerge (Hoober et al. 1994). This function also holds true for
cyanobacteria. Analogous to other gram-negative bacteria, cyanobacteria have an envelope
barrier consisting of an outer membrane, a peptidoglycan layer and an inner (plasma) membrane,
which are physically and functionally distinct from the thylakoid membrane.(Gantt 1994) The
two membrane systems exchange components via vesicle transport. The localization of
photosystem proteins in cyanobacterial cells and chloroplasts has been studied by fractionation
methods. Thylakoid and plasma membranes have been purified from Anacystis nidulans.(Smith
et al. 1993) A number of polypeptides from both photosystems were found in both membranes.
In particular, the D1 and extrinsic 33 kDa proteins were localized in both membranes, but the
latter formed functional complexes only in the thylakoid membrane. Both CP43 and CP47 were
confined to the thylakoid membrane. Two-dimensional fractionation methods combined with
immunoblotting analysis has demonstrated that the purified plasma membrane from
Synechocystis 6803 contains a number of protein components closely associated with the
reaction centers of both photosystems.(Zak et al. 2001) Localization of a functional PSI reaction
center capable of primary charge separation was found, but not a functional PSII reaction center.
However, evidence for localization of D1, D2 and cytb559 subunits in the plasma membrane was
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established, but not CP43 or CP47. The absence of CP47 and CP43 indicates that assembly of a
functioning WOC is highly unlikely in the plasma membrane, based on preliminary observations
that PSII subcomplexes from which both CP43 and CP47 have been dissociated do not assemble
a functional inorganic core during photoactivation.(Buchel et al. 1999)
The newly synthesized D1 protein contains an extension of the carboxyl terminus that is cleaved
by a protease in the mature PSII. The D1 C-terminal extension was shown not to be required for
assembly of functional PSII complexes, nor for growth under optimal conditions in both
Synechocystis 6803(Nixon et al. 1992) and Chlamydomonas.(Lers et al. 1992) However, the
carboxyl extension must be cleaved beyond Ala344 by an soluble protease, called ctpA, prior to
assembly of an active inorganic core.(Nixon et al. 1992; Trost et al. 1997) In Synechocystis 6803
cultures which lack the carboxyl extension or have a genetically engineered two-fold longer
extension no difference in growth rates or O2 evolution rates versus wild type were
detected.(Ivleva et al. 2000) Thus, following cleavage, the carboxyl extension is not involved in
the assembly of an active WOC. Nonetheless, the C-extension in wild-type does provide a
selective advantage, albeit for reason that remain unclear. The timing and location of D1
processing in relation to the sequence of PSII biogenesis has been explored, although much
remains to be understood (Zhang et al. 2000). Translation elongation of newly synthesized D1 is
tightly regulated, as it occurs in vivo only if proper insertion into the thylakoid membrane pre-
exists and a trans-membrane potential is required. However, co- and post-translational assembly
steps of D1 into PSII reaction center and core complexes occur without requirement for
photosynthetic electron transfer or trans-thylakoid proton gradient.
In summary (Table 1), assembly of PSII subunits in prokaryotes begins in the plasma membrane
where the components of the reaction center and 33kDa extrinsic subunit are found in a non-
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functional state. Final assembly, addition of the two inner antenna subunits of the PSII core
complex, uptake of the inorganic cofactors and binding of a functional extrinsic 33 kDa protein
all occur outside of the plasma membrane in the thylakoid system.
2. Chloroplasts. The thylakoid membrane system in chloroplasts has a more complex structure
than the undifferentiated thylakoid membrane of cyanobacteria. SDS-PAGE of the polypeptide
distribution(Wollenberger et al. 1994) and biophysical studies (Wollenberger et al. 1995;
Mamedov et al. 2000) of the light-harvesting antenna attachment and the localization and
specific O2 evolution activity of PSII-WOC complexes found within different regions of the
thylakoid membrane system in chloroplasts indicates that a gradient exists in the number of
subunits and complexity of functional activity. PSII size and functional complexity increases in
going from the individual stroma lamellae, to the periphery of the appressed multi-membrane
grana lamaellae (so-called margins) to the centers of the appressed grana lamaellae (core grana),
as summarized in Table 1. At least two sub-types of PSII, designated PSII-α and PSII-β, are
known that are distinguished by the number of light-harvesting antenna Chl a/b binding proteins
that funnel energy to the reaction center. PSII-α has more LHC II and a larger antenna size
compared to PSII-β.(Wollenberger et al. 1994) The Mn cluster is absent or inactive in the PSII
found in the stroma membrane; a majority fraction of the peripheral grana PSII-WOC are active
but have slow QA QB electron transfer kinetics; while greater than 80-90% of the core grana
PSII-WOC are fully active in O2 evolution and have normal acceptor side kinetics. (Mamedov et
al. 2000) The authors hypothesize that the “photoactivation” process (here meaning both subunit
assembly and inorganic core uptake) is initiated in the stroma lamellae, diffuses into the grana
periphery, and is completed within the appressed regions of the inner grana core.
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In summary, studies of PSII-WOC biogenesis in both cyanobacteria and chloroplasts support an
“assembly line” model for the manufacturing of functional PSII core complexes. Beginning with
insertion into the plasma membrane of PSII reaction center subunits (D1, D2, cytb559,
association unknown) and a non-functional version of the 33-kDa MSP (likely pre-protease
processing?). This is followed by transport to stroma lamaellae where acquisition of inefficient
primary electron transport (slow QA QB) occurs. Some CP43 and CP47 is present,(Mamedov
et al. 2000) although gels reveal that CP43 is present at lower levels than the reaction center
subunits.(Wollenberger et al. 1994) Photoactivation of O2 evolution occurs in some centers (≤
40%), but the activity is unstable in the dark, suggesting that stable binding of the extrinsic 33
kDa protein has not been established in those centers that do photoactivate. PSII core assembly
develops further in the grana margins where gels reveal more prominent staining from CP47 and
CP43 and fluorescence reveals opening of QA- QB transfer. Lastly, diffusion to the core grana
lamaellae occurs where the most stable and active PSII core complex-WOC is found, also in
association with additional LHC II subunits that create the light-efficient PSII-β core complex
(Wollenberger et al. 1994; White et al. 1996). The high stability of the O2 evolution activity in
the latter complexes is associated with the binding of the extrinsic 33 kDa protein.(Burnap et al.
1996) Not all of the details of the assembly steps needed to support this biogenesis model have
been tested. However, we note that deletion of a single gene called VIPP1 (vesicle-inducing
protein in plastids 1) is deleterious to thylakoid membrane formation. VIPP1 is a hydrophilic
protein that is found in both the inner envelope and the thylakoid membranes and is a potential
candidate for facilitating protein transport between the two membrane systems.
B. Mn2+
Uptake Into the Cell
16
The Mn content of cyanobacterial cells is generally well in excess of that needed to supply all
PSII complexes, however intracellular distribution and transport are other determinants not as
well known. The capsular peptidoglycan comprising the cyanobacterial envelope plays a major
role in concentrating free Mn2+
from extracellular solution.(Mohamed 2001) Mature cells of
Synechocystis 6803 take up or exchange free Mn2+
at a rate of about 2 x 106 Mn
2+/cell in a period
of 30 minutes.(Ogawa et al. 2002) There are two pools of intracellular Mn2+
which have been
identified.(Keren et al. 2002) The largest pool, A~ 108 atoms/cell, is found closely associated
with the outer membrane possibly on either the outside or the inner leaflet (periplasm). This pool
can be removed by EDTA, is electrogenically generated under light and can be prevented by
electron transport inhibitors (DCMU) or abolished by proton uncouplers (CCCP). A tightly
associated second pool, B ~ 1.5x106
atoms/cell, is not affected by EDTA, light or proton
uncouplers and has traversed the inner membrane. Under Mn2+
starvation conditions pool B
contains about 105
Mn/cell which is essential for photosynthesis, of which the majority is
targeted to PSII. By comparison, the marine cyanobacterium Synechococcus sp. PCC7002
contains 1.5x106 Mn/cell in pool B, while the non-oxygenic purple bacterium Rhodobacter
capsulatus contains 1% of this amount. A two-component regulatory machinery for sensing of
extracellular Mn2+
concentrations and maintenance of intracellular Mn homeostasis in
cyanobacteria and non-photosynthetic prokaryotes has begun to emerge. (Ogawa et al. 2002)
C. Inorganic Core Assembly Involves no Protein Chaperones
Intracellular transport of transition metal ions used in the enzymatic machinery is typically under
tight control by proteins or small molecule chelators that ensure proper targeting of the metal to
its final destination and also protect the nascent system from unwanted reactions. These
“chaperone” proteins are widely distributed in the case of iron and copper regulator systems. The
17
thermodynamic potentials for aqueous Fe2+
/Fe3+
and Cu+/Cu
2+ metals indicate that these metals
are susceptible to redox changes within cells and thus will undergo major changes in speciation
if not coordinated during transport. Thus it may seem curious that no essential chaperone protein
has yet been identified for delivery of Mn2+
to the apo-WOC-PSII complex during biogenesis.
The explanation is likely due to the inaccessibility of the Mn3+
oxidation state in aqueous media
at neutral pH owing to the large thermodynamic barrier which prevents Mn2+
oxidation (standard
reduction potential 1.2 V at pH 7 vs NHE). Moreover, divalent Mn2+
with its spherical
electronic distribution and half-filled 3d5 electronic configuration (two sigma anti-bonding
electrons) forms relatively weak coordination complexes with all monodentate O, N, S
ligands.(Smith et al. 1976) Thus, free Mn2+
does not generally associate tightly with the internal
machinery of the cell unless there are preorganized chelation sites present with multiple ligand
donors. Generally, the latter sites are specific for ions of a particular size, charge and dehydration
energy so that biosynthetic discrimination is almost always ensured. Surface electrostatics plays
a major role in guiding metal ions to their functional binding sites and this mechanism is
important for steering Mn2+
to the apo-WOC-PSII site.(Ananyev et al. 1996) Binding of aquo-
Mn2+
to the high affinity site in apo-WOC-PSII is influenced by three factors: alkaline pH,
bicarbonate ions and Ca2+
are discussed in the next sections. Although no chaperone for Mn2+
insertion appears to exist, repair of the PSII protein complex caused by light absorption does
involve chaperone-like proteins.(Schroda et al. 2001)
A new and novel protein called Slr0286 was identified in Synechocystis 6803 which has no
homologues in other organisms and is not known to be associated with PSII.(Kufryk et al. 2001)
Deletion of slr0286 did not affect photoautotrophic capacity in wild type, but led to a marked
decrease in the population of Ca2+
bound to the WOC of PSII. A chaperone role for slr0286 in
18
photoactivation was postulated. However, an alternate role in elevating the Ca2+
supply within
the lumenal space of the thylakoid membrane would also be consistent with the data.
IV. Roles of the Inorganic Cofactors from Photo-assembly
A. Assembly of the Inorganic Core
1. Instrumentation. In 1995-96 we constructed a modified Clark-type electrochemical cell for
the detection of dissolved O2 gas in photosynthetic samples (Ananyev et al. 1995; Ananyev et al.
1996; Ananyev et al. 1996). It enabled measurements of O2 concentration with exceptional
sensitivity (50 femtomoles O2), micro-volume sample volume (5 μL) and 10-fold faster time-
resolution than the commercially available Clark electrodes. The electronic layout and novel
material innovations have been described and circuit diagrams are available upon request. It
features a platinum-iridium (Pt:Ir = 75:25) electrode which is 10 times harder than Pt and more
chemically resistant to oxidation, reducing the formation of PtO2 and the resulting photocurrents.
By using a thin (1 m) silicone membrane instead of Teflon, both rapid response (0.1 second rise
time) and substantial reduction in the dark current and loss of membrane fatigue were achieved.
The electrode assembly includes an integral preamplifier, further reducing susceptibility to
transients. This cell is integrated with a versatile LED light source for both red and blue
wavelength excitation, digital control of the pulse-shape and duration (0.5 ms to infinity), and
digital data acquisition system and programming environment (Labview). This instrument
permits measurement of the rate and yield of O2 production in samples containing 1 M PSII
centers and exhibiting as little as 0.5% activity and, by integration, as little as 0.05% of the
activity.
19
2. Kinetics and Mechanism. In the 1960s George Cheniae discovered the photoactivation
process, and together with his coworkers established many of the fundamental properties of the
WOC over the next three decades. This includes determination of the Mn stoichiometry (3-5
Mn/PSII), cooperative nature of the Mn association, and two-step sequence of intermediates
(light-dark-light) required for reconstitution of O2 evolution.(Frasch et al. 2001) The insights
provided by the pioneering results from his laboratory are an enduring legacy made more
remarkable by the fact that they were performed using simple tools: a Petri dish, a commercial
Clark electrode and a light bulb as the photoactivation reactor.
Application of the photoactivation instrument described above has enabled kinetic resolution of
the first two steps prior to the rate-limiting step in the assembly of the inorganic
cofactors.(Ananyev et al. 1996) The steps that follow the rate-limiting step are not individually
resolved, but their Mn stoichiometry needed to restore O2 evolution has been determined.
Photoactivation follows a two-step sequence, as originally discovered by Cheniae and Tamura on
the basis of steady-state O2 yield measurements(Tamura et al. 1987) and confirmed by Miller
and Brudvig.(Miller et al. 1989) Kinetic resolution of these steps revealed a reversible, light-
dependent lag phase where no O2 is produced, followed by a single exponential recovery
phase(Zaltsman et al. 1997). The kinetic resolution provides values of the three rate constants
shown in Figure 1 (k1, k-1 and k2). The sensitivity of the cell permits measurement of these rate
parameters using sub-stoichiometric concentrations and higher of Mn2+
. This permitted
exceptionally accurate titrations of the Mn stoichiometry required for O2 evolution, based on
measuring both an extensive variable (O2 flash yield)(Ananyev et al. 1996) and an intensive
variable (initial rate of recovery of O2 evolution capacity).(Ananyev et al. 2001) The latter
approach provided a particularly accurate assay of Mn stoichiometry because it does not require
determination of the number of apo-WOC centers. The photoactivation of PSII-WOC in whole
20
cells appears to occur similarly to the isolated PSII core complex. The ability to examine the role
of accessory proteins in assembly of the inorganic core under native conditions is possible.
(Burnap et al. 1996; Qian et al. 1997)
Two mild methods have been described for removal of the inorganic cofactors and extrinsic
proteins from PSII complexes (apo-WOC-PSII) that is essential for quantitative work and avoids
the denaturation created by the alkaline TRIS method (Ananyev et al. 1996; Ananyev et al. 1998;
Baranov et al. 2004).
Application of these methods has enabled measurement of the following characteristics of the
photoactivation process, primarily using spinach PSII membranes and PSII core
complexes(Ananyev et al. 1995; Ananyev et al. 1996; Ananyev et al. 1996; Ananyev et al. 1998;
Ananyev et al. 2001): (1) optimization of the total yield of reactivated holo-enzyme capable of
O2 production (70%-100%); (2) a molecularity of 1.0 Mn2+
/PSII on the first photooxidation step;
(3) linear light intensity dependence of the first step reflecting a single turnover that forms Mn3+
;
(4) determination of the proton stoichiometry of the first two steps (1H+ + 1H
+, as described in
the next section).; (5) determination of the rate constant of the subsequent rate-limiting dark step
that is independent of Mn2+
concentration and exhibits a molecularity of approximately 1
Ca2+
/PSII (step IM1 IM2*); (6) the Ca2+
affinity of this site (denoted the Ca2+
effector site)
increases following binding and photoxidation of the high affinity Mn2+
, reflecting mutual
cooperativity in binding; (7) subsequent rapid light and dark steps that are kinetic unresolved and
involve the uptake of 3.0 Mn2+
/PSII; (8) strong cooperativity in the uptake of the Mn ions is seen
in Mn2+
titration of the final O2 evolution flash (25, 50, 75 and > 90% with 1, 2, 3, and 4
Mn/PSII).
3. Proton Evolution. Alkaline pH accelerates the rate of Mn-dependent photoactivation by 10-
fold between pH 5.5 and 7.5, while the final yield of O2 per flash follows closely the known pH
21
dependence of the holo-enzyme. The data indicate that protons are released during the first two
steps of assembly (Ananyev et al. 1996; Ananyev et al. 2001). Direct measurements of proton
release during photoactivation have been described using a commercial ISFET (ion-selective
field-effect transistor) detector.(Ananyev et al. 2001) There are advantages to the ISFET detector
that can help resolve ambiguities obtained with glass electrodes or pH dyes as detectors.
Measurement of the proton concentration in bulk solution during photoactivation by flashes
reveals that a single proton is released upon photooxidation of the initial dark precursor,
attributed to MnII(OH)
+ based on studies of Cesium inhibition (see below). Thus, the first light-
induced assembly intermediate contains one fewer proton and is formulated as, MnIII
(OH)2+, in
which ionization of a water ligand is postulated.
4. Oxo/Hydroxo/Bicarbonate Sites. Bicarbonate ions were shown to efficiently replace alkaline
pH buffers in accelerating the rate of photoactivation, while increasing the yield of reactivated
centers, quite contrary to the reduction seen upon alkalinization. Bicarbonate binds to two sites
within apo-WOC complex as depicted in Figure 2 and described next. A high affinity site
operates at concentrations as low as 10 μM in the presence of stoichiometric Mn2+
/PSII
concentrations where it accelerates the first step of Mn2+
binding and/or photooxidation (Baranov
et al. 2000). The high affinity site is attributed to the ionization of carboxylate residues or
neutralization of cationic residues on the surface of the WOC protein complex, possibly the D1
protein, which electrostatically attract Mn2+
from solution close to the WOC (Baranov et al.
2004). The effect is much like that seen with lipid soluble anions like tetraphenylboron(Ananyev
et al. 1996). In more extensive studies covering 10 and 100 fold higher concentrations of Mn2+
and Ca2+
, respectively, a second bicarbonate binding site to apo-WOC-PSII having lower affinity
that depends upon the Mn2+
concentration has been identified (hence called the ternary site).
Bicarbonate produces a much larger 3-fold rate acceleration at the ternary site. The data suggest
22
that bicarbonate may serve to deliver of oxide/hydroxide needed for Mn-oxo/hydroxo assembly
or, possibly, as an integral cofactor within the WOC (Baranov et al. 2004). Since its conjugate
acid CO2 is highly soluble in the membrane phase, there will be higher concentration of
bicarbonate near the thylakoid membrane than in bulk solution at equilibrium in any system
which gets all of its inorganic carbon from CO2.
At higher (millimolar) concentrations of bicarbonate and Mn2+
the formation of free Mn2+
-
bicarbonate complexes occurs in solution. The formation of these species coincides with a
reduction in the O2 yield and slowing of the rate of photoactivation. These free complexes appear
to serve as a competitive electron donors to the functional site for photoassembly (ie., the ternary
site, Figure 2). Recent EPR studies of the role of calcium have extended the model in Figure 2
by establishing an electronic interaction between MnIII
and Ca2+
in the first photo-intermediate,
IM1 (Baranov et al. 2004).
5. Calcium. The kinetics of photoactivation reveal that Ca2+
binding affinity increases following
photooxidation of the high affinity Mn2+
. Ca2+
binding is coupled to a slow dark process that is
postulated to represent a protein conformational change. This process leads to more rapid uptake
and photooxidation of the remaining 3 Mn2+
.(Zaltsman et al. 1997) EPR spectroscopy reveals
that Ca2+
binding in the dark also induces binding of a dimanganese(II,II) center to apo-WOC-
PSII.(Ananyev et al. 1997) The yield of this Ca-induced dimanganese signal is optimal at a ratio
of 2 Mn/PSII, and saturates with increasing Ca2+
concentration. The calcium concentration for
induction of the Mn2(II,II) signal matches the value observed for both the activation of steady-
state O2 evolution and also the light-induced assembly of the functional WOC by
photoactivation. Formation of the Mn2(II,II) signal is specific for Ca2+
as it does not occur in the
presence of Mg2+
. The spectral features of this signal are indicative of a variety of weakly
23
interacting Mn2(II,II) pairs that have Mn2+
ions coupled by magnetic dipolar forces in the range
of inter-manganese separations of ca. 4.1 ± 0.4 Å.(Khangulov et al. 1995) This Ca-induced
Mn2(II,II) center is a more efficient electron donor to the photooxidized tyrosine radical, Yz ,
than is the mononuclear Mn2+
center present in the absence of Ca2+
, as measured by the Yz▪
radical yield. Formation of the Mn2(II,II) EPR signal by addition of Ca2+
correlates with
reduction of flash-induced catalase activity, indicating that calcium modulates the accessibility or
reactivity of the Mn2(II,II) core with added H2O2. These EPR studies indicates that Ca2+
organizes the binding site for higher affinity cooperative binding of the first two Mn2+
ion to the
apo-WOC protein.
The photoactivation and spectroscopic data noted above provide a self-consistent picture locating
the Ca effector site as an integral part of the Mn4 core, probably via shared bridging ligands to
Mn (aqua/hydroxo/carboxylato/chloro) (Carrell et al. 2002). Binding of the calcium cofactor to
Ca-depleted holoenzyme induces an increase in the energy of the Mn k-shell electron edge by
0.6-1.0 eV in three oxidation states (S1, S2 and S3 states) where Ca-depletion/reconstitution has
been measured by XANES.(reviewed in (Carrell, 2002 #2198). Therefore, a reasonable
interpretation of the role of Ca2+
is that it serves as an electrostatic promoter to raise the Mn
oxidation potential. This increase could be achieved if Ca2+
were to increase the extent of
electron transfer from shared (bridging) ligands (oxo, hydroxo, aquo?) to the empty 4p valence
orbitals on Mn. This interpretation suggests a possible direct role for Ca2+
in increasing the Mn-
ligand covalency and thus activating the Mn-water (substrate) molecule(s) for easier oxidation.
We have postulated that this role may involve Ca-induced ionization of protons from the
substrate water molecules that are bound to the Mn4 cluster(Carrell et al. 2002). This role is also
consistent with the observed correlation between equilibrium binding affinity for divalent metals
bound to the Ca-effector site and their pKa (Vrettos et al. 2001).
24
6. Protein Subunits Required for Photoactivation. Büchel and coworkers demonstrated that the
smallest PSII protein complex that is capable of catalyzing water oxidation is the CP47RC
subcore complex(Büchel et al. 1999). This complex is isolated from thylakoid membranes by
fractionation of a detergent-solubilized complex. It is comprised of only four major subunits (D1,
D2, Cytb559 and CP47) and a number of small subunits, but lacks CP43 and all of the inorganic
cofactors of the WOC. The isolated complex is inactive in O2 evolution, but does photoactivate
at slower rate (lower quantum efficiency) and produces centers having O2 flash yield of 30% vs
PSII membranes. These studies established that CP43 is not an essential subunit for water
splitting, but does provide a functional advantage for both assembly and O2 evolution activity.
YD is the symmetry related photoactive tyrosine in the D2 subunit(tyr-160) that is homologous to
the essential photoactive tyrosine-161 of the D1 subunit of PSII (YZ). It has been implicated in
stabilizing the higher S-states and in photoactivation, (Styring et al. 1987) but is not essential as
mutants lacking YD grow photoautotrophically, although at much slower rates. Diner and
coworkers investigated YD in both wild-type and a mutant strain (D2-Y160F) in which
phenylalanine replaces YD in the cyanobacterium Synechocystis sp. The quantum yield for O2 in
the intact holo-enzyme was found to be identical in the mutant and wild-type PSII cores using
long (saturating) pulses or continuous illumination, confirming earlier work. However, the O2
yield was shown to be appreciably reduced in the mutant using short non-saturating light pulses
(< 50 ms). Evidence was presented that the positive charge associated with the presence of a hole
on the YD-HisH+ radical center may promote the higher quantum yield for O2 production in wild-
type centers via increasing the oxidation potential of P680+, thereby accelerating the rate of
electron transfer from Mn4YZ to P680+. It was also found that the mutant can assemble a
functional WOC from the free inorganic cofactors, but at a 3-fold slower rate and with reduced
25
quantum efficiency vs wild type. The steps responsible for the slower photoactivation kinetics in
the mutant were identified. These features indicate that the YD▪ radical plays at least two
important roles during assembly of a functional WOC, including increasing the probability of
oxidation of Mn2+
in the dark and suppressing decay of the assembly intermediates by charge
recombination at low light flux. They contribute a competitive advantage to organisms that retain
the YD residue and therefore may account for its retention in the genome of all oxygenic
photoautotrophs.
B. “Inorganic Mutants” of the Manganese and Calcium Sites
Inhibitor binding at the high affinity Mn2+
site is characterized by slowing of the rate constant k1
and is competitive with Mn2+
concentrations. Acceleration of the decay of the first photooxidized
MnIII
intermediate is described by rate constant k-1. Inhibition at the Ca-effector site is
characterized by slowing of the rate constant k2 and is competitive with Ca2+
concentration.
1. Manganese Mutants. Mn appears to be unique in catalyzing O2 evolution in all oxygenic
photoautotrophs. No other metals have been found to date that can replace it. We have examined
several metal ions as potential surrogates for Mn2+
in the assembly process of spinach apo-WOC-
PSII.(Ananyev et al. 2001) These studies were conducted by replacing Mn2+
, while keeping all
other components fixed at the optimal concentrations for Mn-dependent photoactivation (Cl-,
Ca2+
and the electron acceptor ferricyanide). The following metal ions were found to inhibit Mn-
dependent photoactivation with varying affinities and none were found capable of supporting O2
evolution in the absence of Mn2+
(Cs+, Ba
2+, VO
2+, V
3+, Cr
3+, Fe
2+, Co
3+, Ni
2+, Cu
2+, Zn
2+,
MoO42-
,Ru3+
, Rh3+
, Re3+
, UO22+
). However, only a very limited range of conditions were studied:
26
fixed pH 6 and concentrations of Ca2+
, Cl- and electron acceptor. Other pH and concentrations
conditions ought to be examined before it is known for sure whether Mn can be replaced.
Cesium (Cs+) is the strongest, competitive, inhibitor of the high affinity Mn
2+ site, while the
smaller alkali metal ions bind with progressively weaker affinity (Cs+> Rb
+> K
+> Na
+> Li
+). The
equilibrium thermodynamic binding affinities were measured for all alkali metal ions and a clear
correlation with charge density was seen. Cs+ binding is highly selective for the Mn site, versus >
104
weaker binding to the Ca effector site. These data and indicate that Cs+ mimics the size and
charge of the functional Mn2+
species that binds to apo-WOC-PSII and initiates the assembly
process. Assignment of this dark precursor to Mn(OH)+ rather than Mn
2+ is implied by these
results. This conclusion is in full accord with the proton evolution results noted above and the
bicarbonate dependence. This proposal is further supported by the observation that metal-oxo
cations like UO22+
and VO2+
are among the strongest competitive inhibitors of the Mn site. These
results enabled the Mn and hydroxide composition of the first two assembly intermediates to be
determined (up to IM1, Figure 1).
2. Calcium Mutants Boussac discovered that Sr2+
can functionally exchange Ca2+
in the intact
holo-enzyme of PSII membranes by restoring O2 evolution activity.(Boussac et al. 1988) Later
we found that there is a kinetic advantage for uptake of Sr2+
versus Ca2+
at the Ca-effector site
during assembly of the apo-WOC enzyme and determined how each of the three rate constants
measured by photoactivation are affected (Table 2). (Ananyev et al. 2001) Sr2+
was shown to be
five times more effective than Ca2+
in accelerating the rate of the first two assembly steps (k1 and
k2) and two times better in retarding the deactivation step (k-1). Sr2+
competes with Ca2+
and thus
occupies the Ca-effector site of the photoassembled PSII. A 65% lower O2 evolution yield per
flash is obtained for the Sr-photoactivated enzyme, which is very close to the decreased steady-
27
state O2 evolution rate in the Sr-exchanged holo-enzyme. This decrease in O2 flash yield is
known to reflect a retardation of the rate of the final step, S3 S0 + O2.(Westphal et al. 2000)
Thus, the data taken together indicate that Ca2+
is clearly involved in accelerating the final step
in the S-state catalytic cycle. This step includes the O-O bond formation reaction. No other metal
ion other than Sr2+
has been found to functionally replace Ca2+
in water splitting.
Another interesting probe of the Ca2+
site is the vanadyl ion. VO2+
stimulates Mn-dependent
photoactivation by accelerating the first step (k1) and increasing the yield of photoactivated
centers when using stoichiometric Mn2+
concentrations or less (Table 2).(Ananyev et al. 2001)
The apparent Michaelis constant at this site is 15 M. By contrast, at higher concentrations
vanadyl slows the first step and reduces the overall yield of photoactivated centers (I50~200 M)
by serving as a competitive electron donor to Yz. The location of the VO2+
binding site appears
to be the Ca-effector site, since Ca2+
blocks the inhibition by VO2+
. Previous studies had
observed stimulation of Mn-dependent O2 evolution by VO2+
in the absence of Ca2+
.(Lockett et
al. 1990) However, by using the photoactivation method we were able to show that this result is
likely due to mobilization of residual Ca2+
by vanadyl ions. The vanadyl stimulation of the rate
constant k1 (Mn site) through binding at the Ca2+
site suggests a cooperative interaction between
the two sites, with binding of VO2+
at the Ca-effector site causing higher affinity binding of Mn2+
at the Mn site. This cooperativity suggests the possibility of either electrostatic or conformational
coupling of the two sites. This interpretation is consistent with equilibrium binding studies
showing that lanthanides of higher charge density bind more strongly to the Ca-depleted holo-
enzyme.(Ono 2000) This cooperativity between the Mn and Ca sites provides a possible
mechanism for the observed correlation in other physico-chemical properties, including XAS and
EPR properties, noted previously. Alternatively, tt is possible that the acceleration of the Mn-
dependent k1 step observed by the VO2+
ion is due to stimulation of proton evolution from MnII
28
or MnIII
, since vanadyl is a weak base (pK1 = 4.3, pK2 = 11.5). In previous studies we found that
organic bases stimulate the rate of the initial step of photoactivation.(Ananyev et al. 2001)
Evidence was presented that the mechanism involves stimulation of proton evolution from (or
hydroxide binding to) Mn (assembly of MnII(OH)
+ and Mn
III(OH)2
+). Distinction between these
alternative proposals for the vanadyl effect on k1 may be resolved by examination of the effect
on photoactivation of lanthanides binding to the Ca-effector site.
3. Other Metal Ion Sites. Recently, Cu2+
was shown to bind to PSII complexes from tobacco at
stoichiometric concentrations and produce stimulation of the electron transfer rate from
water.(Burda et al. 2002) The location of the Cu2+
binding site was not identified, but the authors
speculated a possible site in the WOC. This finding is novel as there is no precedent for an
endogenous functional Cu2+
site in any WOC. An alternative binding site for this novel Cu2+
may
be the acceptor side, based on data showing that a binding site for exogenously added Ni2+
or
Zn2+
has been identified near the QB acceptor in purple bacterial reaction centers and found to
slow the rate of proton transfer into reduced QB2-
.(Utschig et al. 1998; Keller et al. 2001)
V. Concluding Remarks
The universality of the inorganic core of the WOC among all oxygenic phototrophs, its high
efficiency of assembly and the absence of protein chaperones during assembly indicates that the
inorganic core can be assembled spontaneously from elementary ions, light and the apo-WOC
protein. Kinetically, the process is simple. It can be resolved into only two steps in which 1 Mn2+
and 1 Ca2+
are taken up in light and dark steps, respectively, followed by rapid light-dependent
uptake of 3 Mn2+
. This kinetic simplicity indicates minimal control by the protein and thus
implies the core structure may be intrinsically stable relative to other core topologies. Hence, we
can expect it to be among the known Mn4Ox core types previously prepared or accessible by self-
29
assembly (Mukhopadhyay et al. 2002). This sequence of uptake of the cofactors during
photoactivation, depicted in Figure 1, the strong cooperativity in binding of the high affinity
Mn3+
and Ca2+
ions, their coupling to proton release, and the rapid cooperative uptake of the
remaining 3 Mn2+
ions provide support for two of the eight possible Mn4Ox core types proposed
on the basis of EPR/EXAFS spectroscopies (Carrell et al. 2002). The two Mn4Ox core types
deduced by EPR/EXAFS that are consistent with the photoactivation data are depicted in Figure
3. The placement of a Ca2+
ion within each of these structures located along the pseudo three-
fold axis produces core types that are structurally in good agreement with the Mn4Ca1
heterocubane core type proposed on the basis of XRD of a cyanobacterial PSII core complex
(Ferreira et al. 2004). We may conclude that the Mn4Ca heterocubane core topology is
supported not only by the available spectroscopic data from various sources, including XRD,
EPR, and EXAFS, but also with the photoactivation data on assembly.
Acknowledgements
We thank Drs. M. Seibert, H. Pakrasi and J. Barber for preprints. GCD appreciates helpful
discussions with Drs. S. Baranov, A. Tyryshkin and A Stemler.
30
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A B C Dk1 = 0.034
k-1 = 0.01
k2 = 0.0038
dark
k3 ~ 0.006
[MnIIOH]
+
Mn(III)
OH
OHMn
O
Mn
OH
apo-WOC
CahhMn
IM1*IM1
X X
Ca
IM2
Mn4Ca1Ox
HCO3-
nh
2Mn
*Mn
HCO3
light
MnIII
HO
Ca
OH
3+
MnIII
O Ca
3+H2O
Figure 1. The sequence of kinetic intermediates (top) formed during assembly of the inorganic
core of the WOC by photoactivation (A, B, C) (Ananyev et al. 2001). (bottom) proposed
structures of intermediates.
40
COO
XH
R+
HX
COO
X
X
HCO3
A Mn2+Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
D1 D1)R(CO2
3
COO
OH2
HX
Mn2+
COO
X
X
Mn2+
XH
HCO3
HCO3
B
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
Mn2+
R+
D1 D1 Mn2+
)R(CO2
3
H2O
H+
Scheme 2 Baranov et al.
Figure 2. The two proposed sites for bicarbonate stimulation of Mn
2+ assembly during
the photoactivation reaction (Baranov et al. 2004). (A) The high-affinity bicarbonate
site: At low Mn2+
concentrations (< 8 Mn2+/PSII), bicarbonate anions electrostatically
steer Mn2+
ions into the apo-WOC-PSI complex from solution by partitioning or
ionization of protons or through ion-pairing with cationic side chains arginines, R+).
(B) The low-affinity bicarbonate site: At high Mn2+
concentrations ( > 30 Mn2+
/PSII),
bicarbonate binds to the photoactive high-affinity Mn2+
binding site.
41
O
MnMn
O
O
Mn
OMn
( 3-oxo)2( 2-oxo)2
Mn
O
O
Mn
O
Mn
Mn
O
HO OH
( 2-oxo)4( 2-hydroxo)2
Figure 3. Two of the manganese-oxo core types proposed for the PSII-WOC on the
basis of EPR and EXAFS data (Carrell et al. 2002).
42
Table 1. Sequence and location of assembly of PSII core complex protein subunits and inorganic
core cofactors in cyanobacteria and chloroplasts.
Membrane: Plasma Stroma Grana Margin Core Grana
PSII-WOC
Maturation
Unassembled
reaction center
PSII-β
Inner antenna insertion
labile inorganic core
PSII core-β
Completed
polypeptide core
labile inorganic core
PSII core-α
Assembled
polypeptide core
stable inorganic
core + LHC II
Major Subunits RCb,
33-MSP(nf)a RC+CP47 ~CP43 RC+CP43+CP47
All major su +
33-MSP(Boussac et al.)
Electron
Transport
none Slow QAQB
Slow QAQB
Normal PSII
Kinetics
WOC
Photoactivation
none ~40% photoactivatible
labile O2↑
Photoactivation
yield increases
Fully assembled
stable O2↑
a (nf) non-functional; (Boussac et al.) functional
b RC subunits D1, D2, cytb559
Table 2. Activator/inhibitors at the Ca-effector site of Mn-dependent photoactivation of
O2 evolution in spinach apo-WOC-PSII(Ananyev et al. 2001)
Metal Photoactivation
step affected
O2 yield*
At pH 6.5
Michaelis
Const. O2 ?
Ca2+
k1 no effect
k1 accelerated
k2 accelerated
70-100% 1.5mM
Sr2+
k1 no effect
k1 accelerated
k2 accelerated
30% ~30 mM
Mg2+
Weak non-specific
effect
<0.5% >0.1 M
(inhibition)
Ba2+
k1 slowed <0.5% Blocks Mn
Not Ca site
VO2+
k1 accelerated
k1 slowed
<0.5%
15 μM (k1)
200 μM