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Microbiology and Molecular Biology Reviews, September 1998, p. 667-683, Vol. 62, No. 3
Department of Biology, Mount Allison
University, Sackville, New Brunswick E4L 1G7,
Canada,1 and
Department of Plant
Physiology, University of Umeå, S901-87 Umeå,
Sweden2
1092-2172/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Chlorophyll Fluorescence Analysis of Cyanobacterial
Photosynthesis and Acclimation
SUMMARY
INTRODUCTION
INTERPRETING CYANOBACTERIAL FLUORESCENCE SIGNALS
A Distinct Photosynthetic System Yields Distinct
Fluorescence Signals
FO,
FV/FM, and
FO' in Cyanobacteria versus Plants
PHOTOCHEMICAL QUENCHING AND EXCITATION PRESSURE
PREDICTING LIGHT ACCLIMATION STATUS
State Transitions Dominate Nonphotochemical Quenching of
Cyanobacterial Fluorescence
Predicting the Acclimated Light Intensity from
qN Light Response
Inorganic Carbon Accumulation and Fluorescence Quenching
State Transitions Can Be Measured Nondestructively
PREDICTING PHOTOSYNTHESIS FROM FLUORESCENCE
APPLYING FLUORESCENCE ANALYSIS TO DIFFERENT CYANOBACTERIA
CONCLUSIONS AND PROSPECTS
Tracking Acclimation Status in the Laboratory and Field
Conclusions
APPENDIX
ACKNOWLEDGMENTS
REFERENCES
SUMMARY
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Cyanobacteria are ecologically important photosynthetic prokaryotes that also serve as popular model organisms for studies of photosynthesis and gene regulation. Both molecular and ecological studies of cyanobacteria benefit from real-time information on photosynthesis and acclimation. Monitoring in vivo chlorophyll fluorescence can provide noninvasive measures of photosynthetic physiology in a wide range of cyanobacteria and cyanolichens and requires only small samples. Cyanobacterial fluorescence patterns are distinct from those of plants, because of key structural and functional properties of cyanobacteria. These include significant fluorescence emission from the light-harvesting phycobiliproteins; large and rapid changes in fluorescence yield (state transitions) which depend on metabolic and environmental conditions; and flexible, overlapping respiratory and photosynthetic electron transport chains. The fluorescence parameters FV/FM, FV'/FM',qp,qN, NPQ, and
PS II were originally developed to extract information from the fluorescence signals of higher plants. In this review, we consider how the special properties of cyanobacteria can be accommodated and used to extract biologically useful information from cyanobacterial in vivo chlorophyll fluorescence signals. We describe how the pattern of fluorescence yield versus light intensity can be used to predict the acclimated light level for a cyanobacterial population, giving information valuable for both laboratory and field studies of acclimation processes. The size of the change in fluorescence yield during dark-to-light transitions can provide information on respiration and the iron status of the cyanobacteria. Finally, fluorescence parameters can be used to estimate the electron transport rate at the acclimated growth light intensity.
INTRODUCTION
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Principles of Modulated Fluorescence Analysis
Chlorophyll fluorescence analysis allows noninvasive, near-instantaneous measurement of key aspects of photosynthetic light capture and electron transport. For natural samples, fluorescence signals are specific to photobionts and allow in situ measurements of small (61) or dilute (65, 130) mixed natural populations. For molecular studies, fluorescence signals can be used for rapid screening of mutant or transgenic colonies and cultures and for tracking physiological processes during gene regulation experiments. Rapid screening has become increasingly important with the advent of genomic sequencing and saturation mutagenesis. Therefore, applications of chlorophyll fluorescence are expanding in both field and laboratory settings.
In cyanobacteria, the photosynthetic system is tightly connected to the other principal metabolic paths and is in itself a major metabolic sink for iron, nitrogen, and carbon skeletons. Therefore, chlorophyll fluorescence signals can provide rapid, real-time information on both photosynthesis and the overall acclimation status of cyanobacteria. We and other groups have been adapting to cyanobacteria techniques of in vivo fluorescence analysis originally developed for plants (5, 20-28, 58, 61, 69, 74, 80, 87-91, 112, 116, 128, 133, 138, 141, 142, 150).
Fluorescence analysis depends on the phenomenon that when a pigment absorbs the energy of a photon and enters an excited electronic state, there are essentially four routes for the return to ground state: (i) photochemical reactions in which the excited electron leaves the pigment molecule and enters an electron transport chain, as occur in specific chlorophylls in photosynthetic reaction centers; (ii) heat dissipation, in which the excited electron returns to ground state by releasing heat; (iii) transfer of the excitation energy to an adjacent pigment, as occurs in the light-harvesting antenna systems of photosynthetic organisms; and (iv) emission of a fluorescence photon, of a wavelength longer than that of the photon initially absorbed. These four processes are in competition, and for a given excited molecule, the path with the largest first-order rate constant predominates. For biological systems, the overall chlorophyll fluorescence yield is usually low, and in vivo chlorophyll fluorescence from photosystem II (PS II) predominates (38, 66, 112). In cyanobacteria, phycobiliproteins also contribute fluorescence, which overlaps with the spectrum of chlorophyll emission.
Although PS II fluorescence is a minor pathway for excitation dissipation, it competes with the quantitatively more important energy dissipation routes of PS II photochemistry, exciton transfer to other pigment systems (such as PS I), and heat dissipation. Therefore, changes in photochemistry or in the two nonphotochemical routes (energy transfer and heat emission) cause changes in the fluorescence yield from PS II (13, 66, 112). When the potentials for photochemistry and nonphotochemical dissipation are minimal, the fluorescence yield is maximal. Quenching or lowering of the fluorescence yield below its maximum occurs when excitation flow increases to the competing photochemical or nonphotochemical pathways.
To deduce information on photosynthesis from analysis of fluorescence
quenching, one assumes that changes in fluorescence yield reflect
proportional changes in the competing deexcitation pathways of
photochemistry, exciton transfer, and heat dissipation. This basic
assumption is not strictly valid (53, 56, 144). Nevertheless, the fluorescence signal is rich in information, and in
plants the parameters FV/FM,
FV'/FM', qP,
qN, NPQ, and
PS II are empirically verifiable
indices of photosynthetic performance and acclimation status (12,
36, 45, 66, 67, 82, 99, 102-104, 106, 107, 127, 129, 134, 145,
153).
For any pigment, the level of fluorescence emission depends on the pigment concentration, the excitation light intensity, and the fluorescence yield or efficiency of fluorescence emission. For fluorescence quenching analysis, the excitation intensity and pigment concentration must be constant, so that changes in fluorescence reflect the changes in fluorescence yield which result from the competing photochemical and nonphotochemical deexcitation pathways. Changes in pigment concentration are generally not a concern over the brief periods of fluorescence measurements.
Modulated fluorometers are currently widely used to measure in vivo chlorophyll fluorescence from plants and increasingly from cyanobacteria in both the laboratory and the field (128, 130). This review concentrates on data obtained with modulated fluorometers, although other approaches are also used (40). Modulated fluorometers specifically detect and amplify only the fluorescence excited by a weak, constant measuring beam consisting of a train of low light pulses at a frequency of 1 to 100 kHz. Therefore, the excitation intensity is constant and changes in the fluorometer signal reflect changes in fluorescence yield. The modulated measuring beam is sufficiently weak that it drives essentially no photosynthesis, allowing determination of the fluorescence yield of dark-adapted samples. Furthermore, since the detection system ignores fluorescence excited by other light, it is possible to change the actinic light and provide multiple saturating pulses of light over the course of one measurement (Table 1; see Fig. 2). The fluorescence yield can therefore be measured under different levels of actinic light, and saturating flashes can be used at any point to momentarily close all PS II centers and drive photochemical quenching to zero (see Fig. 2).
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Goals and Scope
In this review, we discuss pulse-amplitude modulated fluorescence
as a rapid, noninvasive monitor of acclimation and photosynthesis in
cyanobacteria and cyanolichens. We do not cover the biophysical mechanisms underlying chlorophyll fluorescence emission, which are well
reviewed elsewhere (31, 38, 66, 112, 127, 137, 141, 144).
Rather, we summarize some of the potentials and limitations of
fluorescence analysis for extracting physiologically and ecologically useful information from cyanobacteria, whose photosynthetic physiology (see Fig. 1) and fluorescence patterns (see Fig. 2) differ in important
respects from those of plants (20, 22, 91, 112, 128, 141).
In particular, we demonstrate how characteristic changes in
nonphotochemical quenching of fluorescence can be used to estimate the
light level to which the sample is acclimated. This information can
then be used in conjunction with the
PS II parameter to estimate
electron transport under acclimated conditions.
INTERPRETING CYANOBACTERIAL FLUORESCENCE SIGNALS
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A Distinct Photosynthetic System Yields Distinct Fluorescence Signals
The central PS II and PS I photosynthetic complexes are very similar in plants and cyanobacteria, as are many elements of the light capture, electron transport, and carbon dioxide fixation systems. Nevertheless, cyanobacteria are metabolically flexible prokaryotic organisms, with several key structural and metabolic distinctions which strongly influence the nature and interpretation of their fluorescence signals (Fig. 1).
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In cyanobacteria, the principal light-harvesting complexes are phycobilisomes peripheral to the thylakoid membranes, rather than the integral membrane chlorophyll-a/b binding proteins which capture light in plants. Cyanobacterial phycobilisomes diffuse along the surface of the thylakoids, at a rate sufficient to allow movement from PS II to PS I within 100 ms (96). This distinction in light capture structures between plants and cyanobacteria has many metabolic and functional consequences (7). In particular, the cellular phycobiliprotein content influences cellular fluorescence yield. Furthermore, cyanobacteria have high and variable ratios between PS I and PS II complexes (98, 112), so that in comparison with plants, PS II accounts for relatively little of the cellular chlorophyll. This can also influence the interpretation of fluorescence signals, since the variable fluorescence component arises from PS II while the constant or F0 fluorescence component contains emissions from PS II, phycobiliproteins, and possibly also PS I chlorophyll (112).
Photosynthetic and respiratory electron flow both occur in cyanobacterial thylakoid membranes (62, 121), sometimes simultaneously, and they share numerous electron transport intermediates (Fig. 1). Under illumination, there is net input of electrons into the transport system from the water-splitting activity of PS II. Under light or dark conditions, there are variable electron fluxes from NAD(P)H, which is oxidized by one or more thylakoid-bound dehydrogenases (11, 54, 85, 86, 121, 139). Electrons from ferredoxin can also enter the transport system, possibly passing via the same complex(es) that catalyze NAD(P)H oxidation (86). In a photoautotroph, electrons derived from NAD(P)H or ferredoxin are clearly not a net input of reductant into the system; rather, they represent some form of cyclic flow, since the electrons used to reduce NAD(P)H or ferredoxin derive ultimately from the water-splitting activity of PS II. Typically, cyclic electron flow is used to describe flow from PS I via ferredoxin and/or NADPH (54, 86) directly back to the intersystem transport chain. This cyclic flow can drive proton translocation through localized reductions of plastoquinone at the cytosolic side of the thylakoid, with concomitant proton uptake, and plastoquinol oxidation near the luminal side, with proton release to the lumen (55) (Fig. 1). More generally, electrons derived from the oxidation of carbohydrates or other reserve molecules can be carried by NAD(P)H into the thylakoid intersystem transport chain via the thylakoid-bound dehydrogenase(s). These electrons from the reserve molecules are derived ultimately from PS II water splitting and, upon reentry to the thylakoid system, can pass to oxygen under light or dark or to PS I (139) under illumination. The reserves thus act as an electron bank so that the flow into the thylakoid system can be offset in time from the original photosynthetic production of reductant, with important regulatory consequences (34, 84, 94).
In all known cases, electrons from these various inputs come together at the cytochrome bf complex, which is a plastoquinol oxidoreductase (68) (Fig. 1). There are two plastoquinone binding sites in the complex, which allow for a Q cycle, in which some of the electrons removed from plastoquinol at the luminal side of the membrane are cycled within the complex and passed back to plastoquinone bound near the cytoplasmic side of the membrane. This branch of the transport chain allows the cyanobacteria to increase the number of protons translocated per net electron passing through the transport chain. Since the reduction involves proton uptake from the cytosol and the oxidation releases protons to the lumen, electron flux through the Q cycle must respond sensitively to the magnitude of the proton gradient across the membrane.
The primary electron flux through the cytochrome bf complex is from plastoquinone to luminal electron carriers, primarily plastocyanin or cytochrome c553 (81, 113), which transport the electrons either to PS I or to a cytochrome oxidase complex which may include cytochrome c(m) (81). Plastocyanin and cytochrome c553 can each fulfill transport roles to PS I or the cytochrome oxidase (81). Double-inactivation mutants mutated in both proteins are inviable in some (81) but not all (155) strains, so that some strains must have an alternate route for electron flow away from cytochrome bf. Although single-inactivation mutants mutated in one or the other protein are viable (26, 71, 81), the loss of one protein can lower the capacity for electron flux away from PS II, particularly under conditions of excess excitation (26). Conversely, overexpression of heterologous plastocyanin in Synechococcus can increase the electron transport capacity (44). Thus, although partially complementary, the two proteins may play somewhat distinct functional roles. Furthermore, plastocyanin contains a copper redox cofactor while cytochrome c553 contains an iron redox cofactor, and in some strains they are differentially regulated in response to copper and iron availability (15, 16, 119, 120, 154). Another example of alternate electron carriers is the iron-sulfur protein ferredoxin, which accepts electrons from PS I but which can be replaced under conditions of iron stress by flavodoxin (70, 75).
The flow of electrons to oxygen as a final acceptor responds rapidly to environmental and metabolic conditions and can be an important element in preventing overreduction of PS II and the intersystem transport chain under excess illumination (22a, 88, 147). This flow to oxygen can be mediated by cytochrome oxidase activity (131) or by photoreduction of oxygen by electrons from PS I, either directly (3, 79) or via ferredoxin (43, 50).
Carbon metabolism and nitrogen metabolism in the prokaryotic cyanobacteria occur in close proximity to the cytosolic surface of the thylakoids and so have strong and direct influences on electron transport and hence on fluorescence (63, 83, 84, 92, 116, 122), both as sinks for ATP and electrons and as sources of electrons extracted from reserve molecules.
In summary, this system forms a web of electron sources and sinks, linked by interconnected redox intermediates, that allows for flexible and rapid shifts in electron fluxes in response to environmental or metabolic changes (5, 54, 55, 74, 80, 81, 85, 86, 131, 135, 147). Furthermore, through shared electron transport carriers, respiration directly influences the photosynthetic regulatory status and vice versa (34, 84, 94). Several of the characteristic properties of cyanobacterial fluorescence signals result from these respiration/photosynthesis interactions, including their distinct patterns of photochemical and nonphotochemical quenching.
In plants, a cycle of conversions of xanthophyll carotenoids is driven
by the trans-thylakoid
pH gradient and is implicated in
regulating nonphotochemical dissipation of excess light energy (1,
46, 47, 57). Cyanobacteria lack this cycle (33) but
have alternate strategies to cope with excess excitation (105, 147). Finally, cyanobacteria show changes in the functional
organization of the light capture system, termed state transitions,
which can result in large changes in the PS II fluorescence yield
depending upon the level of illumination (7, 14, 97, 111,
112). In contrast, in higher plants, state transitions have
relatively minor influences on PS II fluorescence (66). This
review deals now with how the distinct organization and function of
cyanobacterial photosynthesis lead to opportunities and limitations for
chlorophyll fluorescence analysis of cyanobacteria.
FO, FV/FM, and FO' in Cyanobacteria versus Plants
Ting and Owens (141) have shown that for any chlorophyll-containing suspension, the values of FO, FM and FV/FM measured with a modulated fluorometer vary somewhat with pigment concentration. Therefore, within a set of experiments, the chlorophyll concentration should be standardized if precision is required or, alternately, a small correction could be introduced to compensate for variation in the chlorophyll concentration. In our experiments, chlorophyll concentrations from 1 to 3 µg/ml gave results sufficiently consistent for quenching analysis. The use of alternate cuvettes and detectors can greatly extend this concentration range (125).
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A more fundamental problem with the measurement of FO in cyanobacteria is that FO fluorescence varies considerably depending on the cellular phycobiliprotein concentration. Figure 3 illustrates that as the phycocyanin/chlorophyll ratio of wild-type Synechococcus sp. strain PCC 7942 rises, FO fluorescence also increases, particularly once the phycocyanin content is increased above a threshold level. This phycobiliprotein contribution to FO fluorescence is not influenced by changes in the redox state of PS II (51, 72, 111). It could be a low-yield fluorescence emission from coupled phycobilisomes or a high-yield emission from a small population of uncoupled phycobilisomes (96) or free phycobiliproteins. The exact source(s) of this phycobiliprotein fluorescence could be addressed by studies using cyanobacteria with a range of phycobiliprotein contents analyzed with the range of different color light-emitting diodes now available as modulated fluorescence excitation sources (65). In a Synechococcus sp. strain PCC 7942 mutant lacking phycocyanin, FO is low (Fig. 3), which confirms the FO/phycobiliprotein correlation observed in the wild type. Furthermore, in this mutant strain, FV/FM under acclimated growth is about 0.75 (157), as opposed to values of 0.4 to 0.6, typical of wild-type Synechococcus grown under the same conditions.
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In plants FV/FM
[(FM
FO)/FM] (Fig. 2) is well
verified as an index of the maximal photochemical efficiency of PS II
(12), but this interpretation depends on both
FO and FV originating predominantly from PS II. This assumption is not valid for
cyanobacteria (20, 111, 112, 128), since phycobiliprotein
fluorescence contributes to FO and PS II
accounts for only a small proportion of total chlorophyll. In higher
plants under ideal conditions, FV/FM
is near 0.8 and lower values reflect inhibition of PS II function
(12). In cyanobacteria, changes in
FV/FM under conditions of constant
pigment content correlate well with changes in independent measurements
of PS II function such as oxygen evolution (24, 27, 28, 80),
but the absolute level of FV/FM is
not a reliable indicator of PS II function. The distortion of
FO fluorescence is pronounced only at high
cellular concentrations of phycocyanin (Fig. 3), which may be achieved
primarily under nutrient-rich artificial culture conditions, as used in
our experiments to date. When interpreted with caution,
FV/FM is still a useful parameter, particularly if the same sample is monitored repeatedly over time and
if the cellular pigment content is constant. As expected, the
prochlorophyte Prochloron shows a high value of
FV/FM (126), consistent
with the lack of phycobilisomes and the chlorophyll-based antenna
system in this group of cyanobacterial relatives.
FO' is the minimal fluorescence level with all PS II reaction centers open. It is measured with cells under a given light acclimation status but transferred briefly to darkness or far-red light. The determination of FO' is a problematic aspect of quenching analysis in cyanobacteria, since under moderate light intensities FO' is often very close to the steady-state FS fluorescence level (Fig. 2). Furthermore, unlike in plants, FO' in cyanobacteria is usually higher than the FO fluorescence as a result of the dark-to-light increase in PS II fluorescence yield, i.e., the state transition (see below). It is therefore difficult to distinguish the initial small but rapid drop in fluorescence yield as PS II centers open, from the slower state transition-dependent decline to the dark FO fluorescence level. Computerized data logging might alleviate this problem by resolving the fluorescence relaxation kinetic phases.
In higher plants, FV'/FM', defined
as (FM'
FO')/FM' (Fig. 2),
reflects the photochemical efficiency of open PS II centers under a
given light acclimation status (45).
FV'/FM' generally varies inversely
with qN (see below), since nonphotochemical
energy dissipation lowers the photochemical efficiency of PS II below the maximum levels reflected by
FV/FM. A drop in
FV/FM, as occurs during
photoinhibition of PS II activity, also feeds through and results in a
drop in FV'/FM'. Thus, in a plant,
changes in the FV'/FM' parameter
reflect the combined regulation of PS II through both reversible
nonphotochemical quenching and photoinhibitory inactivation of PS II.
In cyanobacteria, changes in FV'/FM' also combine nonphotochemical influences on PS II function and photoinhibitory inactivation of PS II. As described below, nonphotochemical quenching of cyanobacterial PS II fluorescence results primarily from changes in excitation distribution between the two photosystems rather than from excitation dissipation. Therefore, in a cyanobacterium, a drop in FV'/FM' can result from a photoinhibitory drop in FV/FM or from a regulatory redistribution of excitation from PS II to PS I. In plant fluorescence analysis, a common implicit assumption is that down-regulation of PS II reflects overall down-regulation of photosynthetic electron transport. This assumption is not applicable to cyanobacteria, which have more flexible excitation distribution and electron transport systems. Furthermore, cyanobacterial FV'/FM' suffers the same limitations as described above for FV/FM, which are further compounded by the difficulty of measuring the FO' fluorescence level. Nevertheless, as shown in Fig. 4, changes in measured FV'/FM' correlate well with changes in oxygen evolution during a photoinhibitory treatment (24, 27). Cyanobacterial FV'/FM' is a useful integrated measure of PS II activity, even though various mechanisms may underlie the changes in PS II function.
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PHOTOCHEMICAL QUENCHING AND EXCITATION PRESSURE
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Photochemical and nonphotochemical quenching measure changes in variable fluorescence, which derives from PS II; they are therefore less susceptible to distortion from non-PS II contributions to FO fluorescence. They involve minimal mechanistic assumptions (145), although the terms qP and qN often carry mechanistic associations which are not applicable to cyanobacteria.
Photochemical quenching reflects a lowering of fluorescence below maximal levels through photochemical competition with fluorescence emission. Thus, when all PS II reaction centers are open and the potential for photochemistry is maximal, photochemical quenching of fluorescence is also maximal and fluorescence yield is low (FO or FO'). Conversely, when all PS II centers are closed and no photochemistry can occur, photochemical quenching is zero and the fluorescence yield is maximal (FM or FM'). In practice, photochemical quenching is quantified by the photochemical quenching coefficient (145):
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FO', under a given
condition.
qP reflects the balance between excitation of PS II centers, which closes them, and removal of electrons from PS II by the electron transport chain, which reopens the centers. This balance, or excitation pressure on PS II, responds not only to incident light intensity (27) but also to factors influencing electron flow away from PS II, such as temperature (24, 59, 82, 101, 102, 106, 107) and the availability of terminal electron acceptors such as CO2 or O2 (88, 147). Indeed, the pivotal position of PS II in photosynthetic electron transport means that environmental and metabolic signals are integrated into qP, which is thus a general index of the balance between energy capture and consumption.
As shown in Fig. 5, in cyanobacteria and cyanolichens, qP typically stays high over a broad range of incident light intensity, up to 10 times higher than the growth light intensity (21, 23, 27, 28, 80, 138). This contrasts sharply with the pattern typical of higher plants, where qP falls progressively as the light intensity exceeds the growth light. This cyanobacterial capacity to maintain PS II centers open under excess light reflects a complex and flexible electron transport system (5, 44, 55, 85, 86, 131, 135), as well as a generally high PS I/PS II ratio (23, 42, 98, 112). In particular, cyanobacteria have a very high and flexible capacity to remove electrons from PS II, with oxygen as a terminal acceptor for electron flow from water (21a, 88, 91, 128, 147). This flow is low under low light, variable but significant at the growth light intensity, and large under excess light (see below). It thus serves to buffer PS II from excess excitation by removing electrons as required. At least part of this flow is sensitive to cyanide inhibition, suggesting a contribution from respiratory electron flow through cytochrome oxidase (131).
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In spite of the different patterns of qP in cyanobacteria and plants, the parameter does successfully measure PS II closure in cyanobacteria, as shown by titration with 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). This inhibitor binds to the QB binding site of PS II, blocking electron flow and causing reaction center closure. Figure 6 shows that in Synechococcus sp. strain PCC 7942, as expected, qP and oxygen evolution drop in parallel upon progressive DCMU inhibition of PS II. Furthermore, our work on Synechococcus sp. strain PCC 7942 showed that although this strain has a strong capacity to maintain PS II open, even fractional closure of the reaction centers can lead to photoinhibition and large changes in gene expression, indicative of active acclimation processes (24, 27, 28) in response to relatively small drops in the proportion of open reaction centers.
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PREDICTING LIGHT ACCLIMATION STATUS
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State Transitions Dominate Nonphotochemical Quenching of Cyanobacterial Fluorescence
Nonphotochemical quenching reflects any process other than photochemistry which lowers the yield of variable fluorescence. It can be quantified by using the coefficient qN (145):
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FO'), with the
maximum potential variable fluorescence, FV = (FM
FO) (Fig. 2). In
cyanobacteria, variable fluorescence appears to arise essentially from
PS II, while as discussed, the FO' and
FO fluorescence levels arise only partly from PS
II. The cyanobacterial FO' and
FO signals detected by a modulated fluorometer
with a red-modulated light-emitting diode (LED) each contain a
contribution from phycocyanin fluorescence, which we believe is fairly
constant over the course of a measurement. This underlying background
fluorescence is subtracted out as an equivalent component of both
FO' and FO and so does
not seriously distort the calculation of qN.
Significant drops in FO fluorescence during illumination can distort qN in higher plants. This FO quenching is quantified as follows (9):
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An alternate quantification of nonphotochemical fluorescence quenching is as follows (67):
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Figure 7 presents typical light response curves of nonphotochemical quenching in the cyanobacterium Synechococcus sp. strain PCC 7942, along with a curve from a rye plant for comparison. In the cyanobacterium, qN (or NPQ) is high in the dark and drops to a minimum near the growth light intensity. In the plant, qN climbs steadily as the light intensity surpasses the growth level. These differing patterns reflect a fundamental difference in the predominant processes contributing to nonphotochemical quenching. In plants nonphotochemical quenching is dominated by a mechanism(s) for excitation-dependent thermal dissipation of energy from PS II and its antennae, in competition with fluorescence and photochemistry (1, 46, 47, 57, 66, 67, 153).
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In contrast, nonphotochemical quenching in cyanobacteria largely reflects changes in the PS II fluorescence yield as a result of the state transition mechanism (7, 14, 17, 18, 21, 22, 33, 97, 111, 112), which regulates the distribution of excitation energy between PS II and PS I. The biophysical basis of the energy redistributions remains incompletely understood (2, 17, 18, 118, 156), but it is clear that the relative distribution of excitation energy from the phycobilisome to the two photosystems changes (7, 42, 136). An allophycocyanin-B protein in the phycobilisome core serves as a regulated secondary terminal emitter, which receives about 25% of the excitation energy captured by the phycobilisome. Under state I, this portion of the captured excitation is directed largely to PS II, but under state II, most of it is redirected to PS I, thereby lowering the yield of PS II fluorescence and photochemistry (48, 49, 112, 156). A recent model proposes that reversible changes in the oligomerization of PS II and PS I underpins the state transition mechanism (7). Furthermore, the phycobilisomes diffuse along the surface of the thylakoids (96) sufficiently rapidly that movement of phycobilisomes could be involved in the state transitions.
State transitions in cyanobacteria are regulated by the redox status of the electron transport chain joining PS II and PS I (34, 41, 94, 95, 97, 128, 149). If the chain is reduced, cells tend to state II, with a low yield of PS II fluorescence and a distribution of excitation energy to PS I, which extracts electrons from the chain. If the chain becomes more oxidized the cells shift toward state I, with a higher yield of PS II fluorescence and more distribution of excitation energy to PS II. Although the evidence for redox control of state transitions is quite strong, it is possible to observe conditions of low qP, indicating PS II reduction, while cells maintain low qN, presumed to reflect state I and an oxidized intersystem transport chain (86a). To accommodate these observations within the framework of redox regulation of state transitions, there must be partial decoupling of PS II and the intersystem redox status under some conditions, or some as yet unknown subtlety to the redox sensing mechanism(s).
Respiratory and photosynthetic electron flow occur via the same electron transport intermediates in cyanobacteria (5, 44, 55, 85, 86, 131, 135, 147) (Fig. 1). Respiratory electron flow in the dark generally poises the electron transport chain toward a reduced state; therefore, in the dark or under very low light, cyanobacteria are in state II (41, 94, 95). This is reflected in low variable fluorescence and high nonphotochemical quenching, as shown in Fig. 7. As light is applied, PS I activity partially oxidizes the electron transport chain and the cells shift toward state I, with higher PS II fluorescence yield (Fig. 2) and lower nonphotochemical quenching (Fig. 7). As light exceeds the growth level, the PS II variable fluorescence yield remains high or drops somewhat (Fig. 2) and nonphotochemical quenching may increase, although not to the levels achieved in darkness (Fig. 7). Finally, if DCMU is added (Fig. 2), PS II centers close, resulting in a rapid rise in fluorescence as photochemical quenching is lost. This rapid rise is equivalent to the fluorescence peak under a brief saturating light pulse, which also closes reaction centers (Fig. 2). The DCMU inhibition of PS II substantially lowers electron input to the transport chain, and the electron transport chain becomes oxidized by continuing PS I activity. This results in a second, slower fluorescence rise phase (Fig. 2) as the cells enter a full state I with maximum PS II fluorescence (FM) (Fig. 2) and minimal nonphotochemical quenching. This redox dependence of the state transition is illustrated in Fig. 8. Titration with the inhibitor DCMU (143) under the growth light intensity progressively blocks PS II activity (Fig. 6), resulting in net oxidation of the transport chain and state I with low qN (Fig. 8A). Titration with DBMIB (143) also inhibits electron transport, but PS II itself remains active, resulting in reduction of the portion of the transport chain preceding the DBMIB binding site on the cytochrome bf complex. The state transition mechanism senses this change as an apparent overexcitation of PS II, and the cells enter state II with high qN (Fig. 8B).
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The origin of cyanobacterial nonphotochemical quenching in the state transition mechanism is illustrated in Fig. 9, which compares the 77K fluorescence emission spectra and qN values of a cyanobacterial sample in the darkness, under growth light intensity, and after addition of DCMU. The 77K emission spectra, measured with excitation of the phycobilisome at 574 nm, show the changing distribution of energy. In the dark, PS II fluorescence is low, reflecting the high nonphotochemical quenching. Upon illumination, qN drops as the excitation energy is redistributed in favour of PS II. This process continues to an extreme upon addition of DCMU.
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In plants, excitation-dependent quenching driven by the
trans-thylakoid
pH gradient is the major component of
qN (1, 46, 47, 57), with only minor
contributions from state transitions and other mechanisms
(66). In plants, nonphotochemical quenching drops upon
collapse of the trans-thylakoid pH gradient (67, 153). In cyanobacteria, nonphotochemical quenching does not
collapse upon addition of carbonyl cyanide
p-trifluoromethoxyphenylhydrazone (FCCP), an ionophore
uncoupler (22, 86a). We therefore concluded that
energy-dependent quenching is not a significant contributor to
qN in cyanobacteria. Interestingly, Delphin et
al. (32) present evidence that in red algae, whose
chloroplasts also contain phycobilisomes, a plant-type
pH-dependent
nonphotochemical quenching occurs even under low light levels, in
contrast to the state transitions observed in cyanobacteria, which do
not depend on
pH.
Nonphotochemical quenching reflects changes in PS II photochemistry but not necessarily net energy dissipation from the photosynthetic system, if energy is redirected from PS II to PS I. In cyanobacteria, therefore, a high qN does not necessarily mean a low overall photosynthetic efficiency (21, 138). Indeed, redistribution of energy from the PS II-phycobilisome supracomplex to PS I is an important regulatory mechanism in cyanobacteria, to accommodate changing excitation (21, 132, 133) or requirements for ATP to accumulate CO2 and nutrients (5, 91, 116). In contrast to this work, nonphotochemical quenching in a Microcystis strain has been interpreted as reflecting thermal energy dissipation of excitation. These cyanobacteria had a sustained content of the carotenoid zeaxanthin (60). Furthermore, some cyanobacterial strains such as Synechocystis sp. strain PCC 6803 do not display high nonphotochemical quenching after dark adaptation, indicating that they do not enter state II in the dark (51).
The diversity of cyanobacterial pigment and photosynthetic systems requires further characterization of the various origins and regulation of nonphotochemical quenching, particularly under natural growth conditions and limiting nutrient conditions, which can also lead to the loss or alteration of the state transition response (29, 39).
Recent evidence suggests that state II in dark-adapted cyanobacteria might involve an inactivation of the water-splitting complex (83). This limits the electron supply to the P680 chl of PSII and favors recombination in the reaction center, lowering the fluorescence yield (112a). This interpretation suggests that state transitions involve several different mechanisms, since there is clear evidence that under some conditions redirection of excitation energy is responsible for the changes in fluorescence yield observed as state transitions (see, e.g., reference 21).
A methodological problem in measuring light response curves of qN is the potential photoinhibitory loss of variable fluorescence as the actinic light is increased above the acclimated growth level. This can be detected if the FM level measured with DCMU is lower than a previous FM' level, usually that measured around the growth light intensity. In this case, the uninhibited FM level for the sample is unknown, and therefore absolute values of qN cannot be determined. Nevertheless, if a relative qN is calculated by using the highest FM' level achieved, the pattern with respect to light intensity is valid. Photoinhibition during measurement can be avoided by minimizing saturating flashes, keeping exposure to high actinic light brief, and terminating light response curves at 5 to 10 times the growth light intensity.
Predicting the Acclimated Light Intensity from qN Light Response
Figure 10 shows that in a wide range of cyanobacteria with different pigment contents and morphologies, grown under different conditions and light histories, qN reaches a minimum near the acclimated growth light intensity (22). Therefore, the light intensity to which the population is photosynthetically acclimated can be predicted from a readily measured light response curve of qN (or NPQ). Although ambient light is readily measured under many circumstances, this relation between qN and growth light shows the range of the overall light regime which is exploited for acclimated growth. In many cases, the natural light regime is highly variable and cyanobacteria must integrate light information over time to regulate synthesis of the abundant proteins of the photosynthetic system. We hope that the qN light response curve will prove useful with samples where the past light regime is unknown or samples from variable light regimes in which the optimal light intensities for acclimated growth are unknown (132, 133). For controlled light acclimation studies, tracking the qN minimum over time may show the point at which a population completes acclimation after a light shift. Furthermore, for prediction of electron transport in cyanobacteria from fluorescence parameters, it is essential to measure fluorescence under approximately the acclimated growth light intensity (see below).
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Note that this relation does not involve the absolute levels of qN or NPQ but simply their pattern in response to light intensity. Determination of actual qN or NPQ levels requires the measurement of FM by destructive DCMU treatment. If a nondestructive measurement is required and the absolute levels of the parameters are not critical, a simple plot of FM' or FV'/FM' against light intensity will suffice; the light intensity at which maximum values are achieved coincides approximately with the acclimated light intensity.
Inorganic Carbon Accumulation and Fluorescence Quenching
Cyanobacteria and some algae accumulate an intracellular pool of inorganic carbon to limit photorespiration (4, 109). The size of the pool influences both photochemical and nonphotochemical fluorescence quenching (5, 87-91). These fluorescence effects can be used to monitor the transport and accumulation of inorganic carbon noninvasively and in real time (30, 90). One mechanism for the fluorescence effects appears to be a bicarbonate-dependent stimulation of linear electron flow from PS I to O2, CO2, or nitrite in some strains, which increases photochemical quenching (5, 51, 77, 78, 88, 91, 92).
Carbon accumulation can also influence nonphotochemical quenching, possibly by driving a transition to state II to increase PS I cyclic electron transport to fulfill the need for ATP (93) to drive the accumulation pump.
Miller et al. (89) also describe a form of nonphotochemical quenching which depends on inorganic carbon accumulation in Synechococcus sp. strain PCC 7942 cells grown at high light intensities but which does not occur in cells grown at low light intensities. The modulated fluorescence trace from the cells grown at high light intensities resembles a transition to state II upon carbon accumulation, with a drop in FM' fluorescence yield and an increase in qN. This increase in qN was not, however, reflected in a comparable change in the cellular fluorescence emission spectra at 77K. This is in contrast to a large drop in 77K PS II fluorescence emission upon dark adaptation of the same cells, similar to that presented in Fig. 9. This component of carbon accumulation-dependent nonphotochemical quenching in cells grown at high light intensities thus appears distinct from the state transition mechanism. It might ultimately relate to bicarbonate-dependent changes in the PS II water splitting-complex (112a).
State Transitions Can Be Measured Nondestructively
The change in fluorescence yield during state transitions is strongly influenced by the excitation light, the rate of respiration, the cellular iron supply (39), and the circadian status of the cell (83). Therefore, determining the size of state transitions can provide information about these factors. The magnitude of state transitions can be measured by comparing qN or NPQ values under different conditions, but explicit calculation of these parameters requires a lethal DCMU treatment to determine FM. This precludes repeated measures on a single sample over time. Alternately, changes in qN between different conditions, for example cells in the dark and under illumination, can be quantified by a nondestructive method that does not require explicit measurement of FM:
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PREDICTING PHOTOSYNTHESIS FROM FLUORESCENCE
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For field measurements, a fluorescence-based estimate of electron transport and carbon dioxide fixation is very valuable (104, 134). Fluorescence measurements are possible with dilute samples; unlike gas exchange, they are specific to photobionts and so do not detect interference from heterotrophic respiratory activity in mixed samples or lichens. The fluorescence transients arise largely from PS II, and so calculations based on fluorescence reflect PS II activity and electron transport through PS II. In extrapolating from fluorescence signals to photosynthesis, we therefore rely on a congruence between PS II activity, net electron transport, and overall photosynthesis. Cyanobacteria and cyanolichens have carbon-concentrating mechanisms which suppress the oxygenase reaction of the ribulose-1,5-bisphospate oxygenase-carboxylase enzyme (4, 5, 87, 90, 91, 108, 110). This simplifies the empirical relation between PS II activity, reflected in fluorescence signals, and gas exchange, as is also the case in C4 plants (36).
Sundberg et al. (138) have simultaneously measured fluorescence quenching parameters and CO2 exchange in cyano-lichens to develop a model to predict gross photosynthesis from fluorescence parameters. They found the empirical relation
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PS II = (FM'
FS)/FM' = (FV'/FM')qP
(a fluorescence estimate of the photochemical yield of PS II),
Ii = number of incident photons per square meter
per hour, and 1 CO2 fixed/10 photons is an empirical
conversion factor.
This predictor gave good estimates of actual CO2 fixation near the acclimated growth light intensity. Under higher light, the predictor, which is based on light-driven electron flow through PS II, progressively overestimated actual CO2 fixation. The overestimation probably reflects electron flow back to O2 under excess light (22a, 88, 131, 147), which maintains PS II centers open but does not contribute to CO2 CO2 fixation. Other workers have found that this flexible electron transport to O2 interferes with estimates of CO2 fixation from fluorescence measures (74). In our experiments, we could estimate the acclimated growth light intensity from the light response curve of nonphotochemical quenching. With this light intensity, we made reasonable predictions of the acclimated rate of CO2 fixation from fluorescence parameters. The general applicability of this approach must, however, be further tested. The 1 CO2 fixed/10 photons is an empirical conversion factor that reflects the (unknown) quantum yield of CO2 fixation and also compensates for the downward distortion of FV'/FM' by phycobilisome fluorescence.
We developed a similar empirical relation to predict gross oxygen
evolution from
PS II in liquid cyanobacterial cultures:
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PS II = (FM'
FS)/FM' = (FV'/FM')qP,
Ii = number of micromoles of photons incident
per hour; 1 O2/12 photons is an empirical conversion
factor, and chl is the chlorophyll content in milligrams.
Figure 11 shows that this relation gives a good approximation of measured oxygen evolution at or near the growth light intensity. At higher light intensities, the predictor increasingly overestimates measured oxygen evolution, again because of pseudocyclic electron flow, with electrons extracted from water by PS II ultimately reaching oxygen as a terminal acceptor. The empirical conversion factor of 1 O2/12 photons again combines the unknown quantum yield of O2 evolution and compensation for the low FV'/FM' values in cyanobacteria.
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In summary, a two-step process gives reasonable estimates of oxygen
evolution or carbon fixation under the acclimated growth light
intensity. First, a light response curve of nonphotochemical quenching
shows the acclimated light intensity. Then oxygen evolution or carbon
fixation is estimated from the fluorescence parameter
PS II, the
acclimated light level, and an empirical conversion factor calibrated
against gas exchange measurements. Failure to measure near the
growth light intensity, or an inappropriate empirical calibration
factor, can lead to a significant overestimation of actual
photosynthesis.
APPLYING FLUORESCENCE ANALYSIS TO DIFFERENT CYANOBACTERIA
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We have tested the methods described in nine strains of cyanobacteria representing a wide range of pigment contents, phycobilisome structures, and physiological properties, as well as six strains of cyanobacterial lichens, as outlined in Table 2. The methods have been extensively validated with Synechococcus sp. strain PCC 7942 (Anacystis nidulans R2) grown under a range of light intensities, CO2 levels, and temperatures (22-24, 26-28; see above). Furthermore, a mutant of this strain lacking phycobilisome rods and containing no PC proved amenable to quenching analysis (Fig. 3) (158). The closely related strain Synechococcus sp. strain PCC 6301 (Anacystis nidulans) displays very similar fluorescence properties (21a). Both these strains have a somewhat unusual phycobilisome with a core composed of only two cylinders.
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