Address for correspondence:
Susan L. Ustin
Department of Land, Air, and Water Resources
University of California
Davis, CA 95616
(530) 752-0621
This study was specifically formulated to examine the changes in the spectral reflectance of needles from mature Loblolly pine (Pinus taeda L.) trees in response to exposure to controlled levels of ozone. The exposure study was carried out at the University of Georgia by the research group headed by Dr. R. Teskey. Ozone treatment of mature tissue was achieved using branch exposure chambers or BECs (Figure 1). "Branches of mature trees growing in the field are contained inside chambers in which the ambient air can be controlled" (1). Figure 2 shows the layout of the study site. Six branches from each of six trees were exposed to varying levels of ozone within the BECs. Several reflectance spectra (usually 3) were measured for each needle age class, from up to two branch tips from each branch chamber. Because of the need to measure the spectra nondestructively, the branches were not clipped from the trees but measured in situ and were measured at night so that illumination could be controlled. Needles from each age class, while still attached to the branch, were attached to a frame so that the viewing and illumination geometry could be held constant between all spectra. This apparatus made it difficult to have access and measure the reflectance of branches in some of the chambers.
Ozone is a strong oxidant and produces several symptomatic physiological effects in coniferous forests. Ambient ozone concentrations of 40 to 70 ppb are common over much of the United states, concentrations well above the 10 to 40 ppb concentrations seen in clean air. There is considerable variation in the response of different genotypes of trees to ozone. Some genotypes of loblolly pine have shown response at concentrations as low as 50 ppb (2). Thus, ozone is suspected to be a contributing cause, and in many areas may be one of the leading causes, of forest damage in most of the world's industrialized countries.
Studies have indicated that cell membranes, including chloroplast membranes, suffer the most injury. The granulation of the chloroplast stroma are the first observed cellular anatomical changes following fumigation in beans. General disruption of chloroplast function, including loss of grana and thylakoid membranes, may proceed other anatomical cellular changes. Because chlorophyll is one of the major light absorbing compounds, these changes are directly observable in the reflectance spectra of the plant canopy.
The cellular damage that results from exposure to ozone or other pollutants result in an increase in the allocation of metabolic energy for repair. At some exposure threshold, the cellular damage becomes greater than the plants ability to respond through increased repair and maintenance respiration. At this stage it often becomes inefficient to maintain older tissue and senescence ensues. In the case of conifers, this results in the retention of fewer needle flushes. Once this threshold is exceeded, visible damage, in the form of chlorosis and foliar loss, becomes evident.
Numerous changes occur in photosynthetic pigment concentrations during stress. Losses of chlorophyll a and b often are not proportional and the chlorophyll a/b ratio tends to increase with stress. The ratio of chlorophyll a/b is generally greater in photosystem I than photosystem II. The damage produced as a result of ozone exposure disrupts the PS II - PS I pathway and causes increased fluorescence and photo-oxidation of PS II which may produce a shift in chlorophyll a/b ratios. Such effects have been noted in response to environmental stresses and to pollution effects (3,4). Another possible explanation for the increase in the chlorophyll a/b ratio is the large developmentally controlled difference between the a/b ratio for young and old foliar tissue. Repair associated with increased pollutant induced damage will result in a higher proportion of young foliage growth, thus the higher chlorophyll a/b ratio.
The concentration of accessory pigments also change under ozone exposure.
The concentrations, and possibly the species, of carotenoids and xanthophylls,
having absorption features in the 400-500 nm wavelength region, increase
with stress. Increased accessory pigments provide a mechanism for protecting
photosynthetic reaction centers from photo-oxidation. Although specific
roles for accessory pigment shifts remains uncertain, Gamon et al. reported
spectral changes due to a xanthophyll conversion under high irradiance
conditions that are related to photosynthetic oxidation state(5). Such
spectral changes may be important factors for monitoring physiological
states in foliage and canopies. Coincident with accessory pigment changes
is a corresponding linear increase in fluorescence from photosystem II
as energy for carbon fixation is lost. Such changes indicate the extent
of altered light harvesting capability in chloroplasts and the affect on
carbon assimilation. Gamon et al. found fluorescence quenching occurred
when the xanthophyll cycle pigment was converted from violaxanthin to zeaxanthin.
Quantification of such accessory pigment responses to pollutant stress
could provide a means to link mechanistic carbon balance models to spectral
measurements.
Measurements required non-destructive spectral sampling of the foliage within the ozone exposure chambers. We needed constant lighting and sample geometry for measurements so we constructed a foliage sample holder attached to the terminus of the fiberoptic cable that also held a 1000 watt power-regulated lamp in constant orientation (Figure 3). The sample holder was U-shaped, approximately three inches square with Velcro strips along the sides. This permitted us to rapidly place the foliage across the field-of-view of the sensor, and to hold it in place, without damage during measurement. Measurements were made at night to reduce extraneous light that might have been reflected from adjacent surfaces within the chamber during the day, and to keep solar lighting conditions constant, while at the same time keeping the entire measurement apparatus small enough to fit easily into the ozone chambers without damage to the branches. The lamp was attached to the sample holder at a 25° angle between the sample and sensor. The sample was oriented nadir to the sensor at 10 cm from the terminus of the fiber optic probe producing a field of view about 1 cm2. Spectra were measured using a Personal Spectrometer II model Analytical Spectral Devices Spectrometer and recorded to disk using a Zenith laptop computer. Data were acquired during the nights between Aug. 2-5,1989.
Spectral measurements were made on foliage from accessible branches
within the chambers. Foliage was divided into age classes, with the most
recent growth (second flush, 1989) = age class 1; first flush, 1989 = age
class 2; and second flush 1988 = age class 3. Not all chambers had 1988
foliage represented on the branches. Three replicate spectra of each age
class from two branches per chamber were measured in each chamber unless
otherwise noted. Foliage was oriented horizontally and held in place to
fully cover the field of view. Different amounts of foliage were present,
depending on treatment and the specific orientation of the branches within
the chambers.
The foliage spectra from the trees were divided into two groups: irrigated and non-irrigated. Because of the level of rainfall during the summer, no significant physiological differences were observed in the two groups (R. Teskey, University of Georgia, pers. comm.). Based on an initial examination of the reflectance spectra, no significant spectral differences attributable to irrigation treatment were observed either. For this reason, the spectra from all trees were combined for data analyses presented here.
Because of the difficulty of nondestructively measuring the reflectance of individual whorls, the amount of foliage within the field-of-view varies between samples independent of the treatment. While much of the total foliage biomass variability is associated with reduced needle retention in the older whorls, there was also random variance associated with the measurement procedure. Because this random variance would obscure the variance associated with ozone exposure, the data was normalized to constant reflectance in the region of 840 nanometers. The 840 nm region was selected because both chlorophyll and water have small absorption coefficients at this wavelength. These normalized mean spectral plots are shown in Appendix A.
The spectra in Appendix A were grouped both by ozone treatment and by whorl. The "by treatment" plot shown in Figure 4 for the high ozone exposures (2.5 times ambient) clearly shows increased reflectance in the chlorophyll absorption region (650-700 nm) with increasing needle age. This increased reflectance, or decreased absorptance, can be attributed to foliar chlorophyll loss as the needles age.
The relationships seen in the "by Whorl" (i.e., by age-class) plots
are less clear. The "by Whorl" youngest needle-age averages (whorl 1) for
all trees is plotted in Figures 5 and 6. While increases in reflectance
with ozone treatment level are expected, this relationship is not consistently
observed in all cases (see Table 1). In particular, the non-filtered air
treatment (NFA) does not fit the trend defined by the other exposure treatments:
it has higher reflectance across the spectrum than is expected for nonozone
exposed foliage. This albedo offset possibly relates to differences between
chamber conditions and ambient air conditions. For this reason, the non-filtered
air treatment has not been included in further analysis and the carbon-filtered
air treatments were used for comparisons with the ozone treatments.
While the first eigenvector from the analysis of mean corrected data is comparable to the second eigenvector from the analysis of non-mean corrected data, it is not necessarily identical. Eigenvalues in the analysis of mean corrected data represent the variance about the mean, rather than about the origin, their relative values give a clear indication of the importance of the spectral trends defined by the eigenvectors. As before, the data was analyzed using two different groupings: by treatment and by needle age. The analysis of the data grouped by treatment reveals spectral changes associated with increasing needle age. While the analysis of the data grouped by needle age was used to identify spectral changes associated with the various ozone treatments.
For all but the "non-filtered air" (NFA) treatment, the first principal component of the "by treatment" grouped data accounts for more than 90% of the variance (see Table 4). As was discussed earlier, the data for the NFA treatment does not follow the trends defined from the other treatments. The results from the NFA treatment were not used in further analysis and were not included in the "by needle age class" grouped analysis.
The dominant spectral trends defined in the PCA "by ozone treatment" is plotted in Figure 10 and can be primarily attributed to changes in needle chlorophyll concentration. As chlorophyll absorption increases (reflectance decreases) the features get broader. This type of band broadening (over the region between 550-750 nary), occurs with increased chlorophyll absorption, that is with increased band depth, and is consistent with a pattern of chlorophyll concentration increasing with needle age (this study included only three age classes: the two whorls from the current seasons growth and the second whorl from last years growth). Chlorosis generally produces a decrease in chlorophyll absorption well depth and a narrowing of the chlorophyll well, but in this case, it produces a more rapid loss of absorption in the 560 to 640nm portion of the chlorophyll absorption well than at 680nm and longer wavelengths. This asymmetry appears to result from chloroplast damage or alterations that accompanies the chlorophyll loss. To visualize the changes in reflectance properties as foliage ages we show the mean spectrum modified by adding or subtracting the first principal component for age classes one and three. In general, the reflectance spectra from older needles have a spectrum which corresponds to the mean reflectance spectrum plus the first eigenvector spectrum multiplied by a constant (the thin line in Figure 10). Those spectra from younger needles correspond to the mean spectrum minus the first eigenvector spectrum multiplied by a constant (the thick line in Figure 10). This presentation allows comparison of how foliar aging effects differ from the mean spectrum. Although the PCA modified spectra are similar, the effects of ozone treatment on foliage of differing ages is not identical. In general for a given ozone exposure, younger foliage exhibits less asymmetry in the 575 nm to 680 nm region than do older needles. The region about 550 nm shows the least discrimination in response to ozone exposure between foliage of differing ages.
The dominant spectral trends in the reflectance spectra grouped "by needle age" are plotted in Figure 11 and can be also attributed chlorosis and chloroplast membrane damage. In this case, the feature also gets broader, but this change occurs as chlorophyll absorption decreases (reflectance increases). This type of band broadening, coupled with a decrease in chlorophyll absorption, is consistent with a combination of decreasing chlorophyll concentration and chloroplast membrane damage. These spectral changes have been observed in previous studies of the effects of ozone on the spectra of Ponderosa pine (6) where the band broadening was attributed to membrane changes and/or chloroplast damage. For both the first and third whorl, the level of ozone exposure is highly correlated to the weighting of this first component. In general, The reflectance spectra of needles exposed to low levels of ozone have a spectrum that corresponds to the mean spectrum plus the first eigenvector spectrum multiplied by a constant (the thin line in Figure 11). Those spectra from needles exposed to high levels of ozone exhibit spectra that correspond to the mean spectrum minus the first eigenvector spectrum multiplied by a constant (the thick line in Figure 11).
The ozone exposure effects of greatest magnitude, as identified in the
PCA, are in the wavelength regions centered around 680 nm and 550 nm. Foliage
exposed to low ozone concentrations compared to foliage exposed to higher
ozone concentrations, have a more steeply negative slope in the 550-680
nm chlorophyll absorption region compared to the flatter slope for foliage
exposed to higher ozone concentrations, consistent with greater absorption
of photosynthetically active radiation in foliage having less ozone exposure.
Such patterns would result if ozone exposures in differing proportions
of chlorophyll a and b, and changes in the pool sizes of carotein and xanthophyll
accessory pigments. An additional difference is the apparent shift in the
wavelength position of the "red edge," the inflection point for chlorophyll
absorption on the 700 nm side of the feature. The shift in this inflection
point to longer wavelengths has been attributed to higher chlorophyll concentrations
(7), however, the effect of ozone in this study was to broaden the chlorophyll
well at lower chlorophyll concentrations. Close inspection of Figures 10
and 11 reveal that the spectral trends defined by the first principal components
are not the same between foliar aging and ozone exposure, despite the fact
that both result in chlorosis due to loss of foliar chlorophyll, changes
in relative proportions and pool sizes of other accessory pigments, and
to membrane damage or other changes. This is an important observation as
it provides a basis to separate both biologically important changes in
plant spectra due to aging and ozone exposure.
It is not clear whether the relatively small spectral effects of chloroplast alteration observed in this study on foliage could be seen as clearly at the canopy level. Nonetheless, trees exposed to high levels of ozone retain fewer whorls of needles than those growing in areas of lower ozone concentration. Because of the large effect of needle age on reflectance, this change in needle retention and mean canopy needle age, will assist in the detection of ozone exposure at the canopy scale.
Because of the limited range of spectral changes observed, and the fact
that airborne sensors would be subject to greater levels of extraneous
measurement error, it is unclear whether such canopy scale measurements
could be successful. It is important to keep in mind that the responses
reported here are from a single growing season of ozone exposure and the
maximum dose, 2.5 times ambient, represents a relatively moderate exposure.
Under natural conditions cumulative effects may be greater, and at least
in some regions of the United States, ozone concentrations may currently
exceed the levels used in this study. In an examination of image data,
images can be compared for changes over time, allowing control over some
external sources of variation. Both the mean and the variance of spectral
properties are expected to change under chronic canopy ozone exposures,
and where spatially coherent patterns occur, detecting small absolute changes
in reflectance may not be impossible. At the field level, spectral measures
such as those reported here, offer a non-destructive sampling technique
to monitor canopy physiological properties and cumulative responses to
environmental stress agents such as ozone exposure.
(2) Response of Loblolly Pine Seedlings to Ozone Over Three Growing Seasons," NCASI Tech. Bull. No. 576 (November 1989).
(3) Salisbury, F. B. and Ross, C. W., "Plant Physiology," Ed. 3., Wadsworth Publishing Co. Belmont, CA. p. 540 (1985).
(4) Rock, B. N., T. Hoshizaki, and J. R. Miller. "Comparison of in situ and airborne spectral measurements of the blue shift associated with forest decline.", Remote Sens. of Environ. 24: 109-127 (1988).
(5) Gamon, J. A., Field, C. B., Bilger, W., Bjorkman, O., Fredeen, A. L., and Penuelas, J. "Remote sensing of the xanthophyll cycle and chlorophyll fluorescence in sunflower leaves and canopies", Oecol. 85: 1-7 (1990).
(6) Curtiss, B. and Ustin, S. L., "Parameters affecting reflectance of coniferous forests in the region of chlorophyll pigment absorption", IGARSS '89 Int. Geosci. and Remote Sens. Symp. Vancouver, B. C., p. 2633-2636 (July, 1989).
(7) Collins, W., "Remote sensing of crop type and maturity", Photogramm. Eng. and Remote Sens. 44: 43-55 (1978).