Simple reflectance indices track heat and water stress-induced changes in steady-state chlorophyll fluorescence at the canopy scale
Introduction
Much effort has been devoted to developing non-invasive remote sensing techniques for monitoring plant stress and photosynthetic status. Most remotely sensed vegetation indices are used for characterizing the amount and spatial distribution of vegetation (Baret & Guyot, 1991, Price, 1992). Vegetation indices have also been used to estimate potential levels of canopy photosynthesis and net primary productivity with mixed success (Choudhury, 2001, Gamon et al., 1995, Verma et al., 1993). Nevertheless, the majority of published vegetation indices are not sensitive to rapid changes in plant photosynthetic status brought on by common environmental stressors such as diurnal fluxes in irradiance and heat. This is due to the fact that most vegetation indices have no direct link to photosynthetic functioning beyond their sensitivity to canopy structure (e.g., leaf angle) and pigment concentrations. Consequently, measurements of canopy reflectance have proven less useful for real-time monitoring of plant photosynthesis and/or water status at the whole plant level (Gamon et al., 1990, Peñuelas et al., 1995).
One exception to this involves remote estimates of the xanthophyll cycle captured by the photochemical reflectance index (PRI) (Gamon et al., 1990, Gamon et al., 1992, Gamon et al., 1995, Gamon et al., 1997). The PRI has been linked to the status of the epoxidation state of xanthophyll pigments, one of the components of the non-photochemical de-excitation pathway (Demmig-Adams & Adams, 1992). The PRI is intended for estimating changes in xanthophyll cycle pigments as they vary due to changes in photosynthetic light use efficiency (Gamon et al., 1992, Gamon et al., 1997, Peñuelas et al., 1995, Peñuelas et al., 1997). The PRI is one of the few spectral indices which has been shown to be sensitive to rapid changes in plant photosynthetic status (Gamon et al., 1990, Gamon et al., 1992, Gamon et al., 1997, Peñuelas et al., 1997).
A similar avenue of research gaining both past and recent attention is the study of chlorophyll fluorescence (CF) as a means for the remote estimation of plant physiological status. CF is a protective process by which plants dissipate energy that is in excess of photosynthetic demands. CF is emitted primarily from chlorophyll a of the antennae system of photosystem 2 (PS II). Any physiological process that influences the function of photosystem II and other photosystem de-excitation pathways will have an effect on CF. There are two main controls on the relaxation pathways: (i) the redox state of plastoquinone, the primary stable electron acceptor of PSII, which determines the level of quenching by photochemistry (qP); and (ii) the changes in non-photochemical quenching processes, which are light-induced protective processes that result in the de-excitation of the chlorophyll singlet to the ground state with the production of heat (Johnson et al., 1994, Müller et al., 2001, Pospisil, 1997). CF, qP, and non-photochemical quenching all have rate constants associated with them and any process that increases the rate constants of the other de-excitation pathways will decrease CF intensity (Bjorkman & Demmig-Adams, 1994, Demmig-Adams & Adams, 1992).
CF intensity can vary over time as a function of the photosynthetic activity of the plant tissue being measured. This relationship was initially described by Kautzky (Kautzky & Hirsch, 1931) and has garnered much attention from plant physiologists who have used leaf level CF measurements as a non-invasive plant monitoring tool for many years. More specifically, leaf level CF measurements utilizing a class of instruments known as pulse amplitude modulating fluorometers have been used with varying degrees of success to estimate plant stress, quantum yield, PS II efficiency, and electron transport rates. CF measurement, interpretation, and relation to photosynthesis and plant physiological status have been the subject of several detailed reviews (Larcher, 1994, Lazar, 1999, Lichtenthaler, 1992).
In addition to leaf level measurements, CF can be measured for entire leaves and plants. Fluorescence imaging, as it is commonly referred to, is conducted using laser or flash lamps to induce CF. Concurrently, spectral or imaging sensors are used to measure the CF signal for entire leaves, groups of leaves, or entire plants depending on the sensor type and configuration. These types of measurement systems have been shown to be effective for non-destructive monitoring of plant stress and functioning at near distances and far distances (for reviews, see Buschmann et al., 2000, Lang et al., 1996). Unfortunately, the application of these techniques to larger spatial scales is limited primarily by the small spatial extent of the laser induction pulse as well as incomplete coverage in the spatial domain.
An area of active CF research is exploring the link between steady-state fluorescence (Fs) and plant photosynthetic status. Fs is the fluorescence emitted under constant illumination without saturating flashes. Flexas et al., 1999, Flexas et al., 2000, Flexas et al., 2002a showed that Fs exhibits a strong positive correlation with diurnal variations in H2O stomatal conductance (g), and to a lesser extent, CO2 assimilation (A) influenced by variable irradiance conditions and water stress. Their findings are promising in that Fs can be monitored directly without the use of laser induction pulses or saturation flashes. This provides an avenue for long-term plant stress monitoring using passive remote sensing strategies. Concurrent to these findings, a small but growing body of research has found support for the potential of identifying the Fs signal in reflectance data from passive platforms at near and far distances. This is further expanded below.
Understanding the spectral characteristics of Fs is critical if remote estimates of its properties are attempted. The emission spectra of chlorophyll fluorescence is characterized by two bands spanning the range between 600 nm and 800 nm but with maxima at 690 nm (F690) and 740 nm (F740) (Buschmann et al., 2000). The intensity, shape, and position of these emission bands are affected by a number of factors. Gitelson et al. (1998) showed that a significant portion of the shape of the CF emission spectra of PS II can be explained by re-absorption processes due to chlorophyll pigments. The re-absorption of fluorescence emission is greatest at F690 because this emission peak overlaps the in vivo chlorophyll a, and to a lesser extent, chlorophyll b absorption maxima located in this region of the spectrum. This suggests that the F690 intensity is sensitive to chlorophyll concentration of the leaf tissue as was demonstrated by a number of investigators (Gitelson et al., 1998, Gitelson et al., 1999). In contrast, F740 is minimally affected by chlorophyll concentration, and thus, the ratio F690/ F740 has been shown to be inversely related to chlorophyll content (Gitelson et al., 1998, Lichtenthaler et al., 1998).
The remote detection of Fs in vegetation using passive remote sensing techniques is in a nascent state. Early on, investigators showed that Fs was related to water stress and photosynthetic function using a Fraunhofer line discriminator (Carter et al., 1990, Carter et al., 1996, McFarlane et al., 1980). Buschmann and Lichtenhaler (1988) found evidence for the superposition of a Fs signal on leaf apparent reflectance signatures. Subsequently, Zarco-Tejada et al., 2000a, Zarco-Tejada et al., 2000b demonstrated that the Fs signal could be detected in apparent reflectance data at both the leaf and canopy level using time-decay experiments and induction with long-pass filters in the laboratory. Furthermore, Zarco-Tejada et al. (2003a) showed that the Fs signal could be identified at the canopy scale using spectral subtraction and derivative reflectance-based optical indices under controlled environment conditions. More recently, studies have demonstrated evidence for Fs in-filling of the 760-nm atmospheric oxygen absorption band detectable in the radiance spectra of field instruments (Evain et al., 2004, Moya et al., 2004).
Despite these initial results, little work has been conducted that demonstrates a strong link between reflectance based Fs measurements at the canopy level and plant physiological status. This study explores the link between canopy-level reflectance-derived Fs measurements, and plant physiological status. The goals are (1) outline evidence for a link between Fs and photosynthetic status; (2) identify the Fs signal in passive remote sensing reflectance data; and (3) relate reflectance-derived estimates of Fs to plant photosynthetic status. These steps are critical if Fs measurements are to be used strategically for plant monitoring and if these techniques are scalable to larger stand and landscape levels.
Section snippets
Plant materials and controlled environment
The experiment was conducted on 3-year-old grapevines of Vitis vinifera L. cv. Cabernet Sauvignon potted in 1-L containers. Nine plants were used in the experiment to create a vegetation canopy approximately 1 m × 1 m in size (herein referred to as the ‘canopy’). The plants were grown under favorable conditions in a potting mixture containing 40% peat, 30% sand, and 30% vermiculite, at an outdoor facility under 30% shade cloth prior to the experiment. On the morning the experiment began, the
Gas-exchange and fluorescence measurements
Light response curves for seven fully expanded leaves from separate plants in the experimental canopy are shown in Fig. 1. Assimilation rates approached their maxima at the ambient PPFD value of 700 μmol m− 2 s− 1 and varied between 5 and 10 μmol CO2 m− 2 s− 1. Leaf 3 was chosen for all subsequent gas-exchange and fluorescence measurements given that it showed an average assimilation response for the canopy.
Temperature and water stress effects on photosynthetic functioning are tracked by fluorescence (Fs)
CO2 assimilation (A), stomatal conductance (g), and steady-state fluorescence (Fs) varied
Temperature and water stress effects on photosynthetic functioning are tracked by steady-state fluorescence (Fs) as mediated through photochemical (qP) and non-photochemical quenching
The relationship between Fs and A is complex as mediated through competing de-excitation pathways such as qP and non-photochemical quenching. This was demonstrated under varying temperature and drought conditions while under constant illumination. Early in the diurnal cycle, Fs exhibits an inverse relationship to A and g. This is potentially brought on by an increase in photochemical quenching (qP) under favorable temperature and drought conditions as shown in Fig. 2. Photochemical quenching is
Conclusions
A strong link between plant pigment concentrations and spectral reflectance measurements are well developed in the remote sensing literature (Sims and Gamon, 2002). Barring a few exceptions (e.g., xanthophyll cycle), changes in pools of pigment concentrations are not rapid direct indicators of plant physiological status. Instead, they integrate the cumulative effects of the plant growing environment over longer periods of time (days to weeks) through generalized shifts in pigment concentrations
Acknowledgements
We thank the UC Davis Viticulture and Enology department for providing the plant material used in this study. We also thank employees of the UC Davis Controlled Environment Facility for assistance in configuring the growth chambers for use in the experiment. Financial support to P.J. Zarco-Tejada from the Ramón y Cajal (MCyT) and Averroes (JA) programs is acknowledged. Detailed comments and useful suggestions by the anonymous reviewers are gratefully acknowledged.
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