Annals of Botany 78 : 591–598, 1996 Interactive Effects of Soil Nutrients, Moisture and Sand Burial on the Development, Physiology, Biomass and Fitness of Cakile edentula J I A N H U A Z H A N G* Department of Biology, McGill Uniersity, 1205 Ae. Dr. Penfield, Montreal, Que., H3A 1B1, Canada Received : 14 August 1995 Accepted : 9 May 1996 The relative importance and interactive effects of nutrient supply, soil moisture content and sand burial on the development, physiology, biomass allocation and fitness of Cakile edentula were examined under controlled greenhouse conditions. Plant traits were more frequently affected by nutrient supply than by soil moisture content or sand burial. Measurements on most plant traits also varied depending on the two or three way interactions among the three environmental factors. Plants partially buried by sand had higher leaf chlorophyll concentration than those unburied at the early stages of development, especially under low soil moisture content. High nutrient supply tended to lower the leaf chlorophyll concentration of mature plants, and this effect was more pronounced under high as compared to low soil moisture content. High nutrient supply enhanced the photosynthetic capacity of plants when they were water stressed. With adequate soil moisture, high nutrient supply increased}decreased the photosynthetic capacity of plants with}without previous experience of water stress. High nutrient supply increased the biomass allocation to the root system of plants, especially at low soil moisture content. Partial sand burial also promoted biomass allocation to the root system of plants grown at low soil moisture content. # 1996 Annals of Botany Company Key words : Soil nutrition, water supply, sand accretion, multiple stresses, biomass allocation, Cakile edentula. INTRODUCTION Plants inhabiting lacustrine or coastal sand dune systems usually encounter substantial variations in soil nutrients, moisture content and sand accretion (Barbour, de Jong and Pavlik, 1985 ; Maun, 1985 ; Tyndall, Teramura and Douglass, 1986 ; Hawake and Maun, 1988). Such variations may occur at small spatial as well as temporal scales. Normally, sand dune systems are poor in nutrient supply. The reported nitrogen concentration of dune soils ranges from 0±006–0±02 % by weight in Britain (Willis et al., 1959 ; Hassouna and Wareing, 1964), 0±001–0±003 % along the Pacific coast (Holton, 1980) and only trace amounts in the sand dune along Lake Huron (Maun, 1985) as compared to 0±02–0±5 % in cultivated soils (Brady, 1974). Often, dune plants are flexible in their requirements for essential nutrients as the result of adaptation to low soil fertility (Hawake and Maun, 1988 ; Zhang, 1995). However, deposition of organic debris through wave action may periodically raise the soil nutrient content to higher levels (van der Valk, 1974), resulting in increased biomass and shoot}root ratio of dune plants (Pemadasa and Lovell, 1974 ; Holton, 1980 ; Hawake and Maun, 1988). These responses of plants were observed even with the addition of very small amounts of N, P and K (Hawake and Maun, 1988). The degree of fluctuation in nutrient level of dune soils depends on daily and seasonal variations in wind speed, wind direction and rainfall (van der Valk, 1974 ; Maun, 1985). * Present address : Research Center, Agriculture and Agri-Food Canada, Harrow, ON, Canada N0R 1G0. 0305-7364}96}11059108 $25.00}0 Although the moisture content of dune soils remains relatively stable at depths greater than 20 cm (van der Valk, 1974), substantial variation occurs at shallow depths depending on wind direction and velocity, and the distance from the wave line (Tyndall et al., 1986). The variation can be rather high so that it was reported that the sand at some locations on the foredune along Currituck Bank, North Carolina, USA, became completely dry to a depth of at least 20 cm by late June (Tyndall et al., 1986). The surface sand dries out quickly even after rainfalls due to the low water holding capacity of sand. The drying out of surface sand affects the survivorship of seedlings of dune plants (Payne and Maun, 1984 ; Tyndall et al., 1986). The growth of established plants may also be affected as low soil water potential reduces the leaf water potential, stomatal conductance, and nutrient uptake of dune plants (Tyndall et al., 1986), which in turn lower the productivities of plants. Sand movement represents another frequent environmental stress faced by dune plants. Maun (1985) monitored sand accretion at three locations about 30–50 m apart on the foredune along Lake Huron and observed about 6–10 cm difference in depth of sand accretion between locations on various dates of observation during a growth season. Differences in sand accretion are more distinct between dune systems. The annual sand accretion was 8±7 cm along Lake Huron (Maun, 1985), 30 cm along Lake Michigan (Olson, 1958) and 30 cm along the Atlantic coast of North Carolina (van der Valk, 1974). Most dune plants show increased growth when partially buried by sand (Maun and Lapierre, 1984 ; Zhang and Maun, 1990, 1992 ; Yuan, Maun and Hopkins, 1993 ; Zhang, 1995). For example, sand # 1996 Annals of Botany Company 592 Zhang—Enironmental Response of Cakile edentula accretion has been shown to increase the total chlorophyll content of newly emerged leaves (Disraeli, 1984), number of bundle sheath cells and photosynthetic rate (Yuan et al., 1993), biomass (Wallen, 1980 ; Maun and Lapierre, 1984), and seed production (Zhang and Maun, 1992) of various dune species. In an artificial burial experiment, Zhang and Maun (1992) observed enhanced shoot growth of young seedlings of Cakile edentula (Bigel.) Hook within 1 week after burial with both unwashed and washed sand. However, the growth advantage of buried plants was maintained and resulted in increased biomass and seed production for plants buried with unwashed sand only. This result supports the idea that the improved growth of buried plants is most likely to result from a collective effect of sand burial and improved soil nutrient and moisture status associated with sand accretion (Olson, 1958 ; Marshall, 1965). The effects of variations in the above three environmental factors on the growth of dune plants have each been investigated extensively, but few studies have examined their integrative impact on plants. The lack of integration in ecological studies has drawn criticisms from plant physiologists. Green, Mitchell and Gjerstad (1994) emphasized that results from a study examining the response of plants to any environmental factor in isolation may not be adaptable to a field situation because they only partially reflect the norms of reaction of the plants in multiple dimensions. Given that natural environments vary both temporally and spatially at small as well as large scales (Bell et al., 1986 ; Bell and Lechowicz, 1994), it would be more relevant to study the response of plants to a set of major environmental factors at varying levels. It is thus the purpose of this study to investigate the relative importance and combined effect of nutrient supply, soil moisture content, and sand accretion on Cakile edentula, an annual commonly found in the sand dune systems along the Great Lakes (Maun, Boyd and Olson, 1990), with special emphasis on the development, physiology, biomass allocation and final fitness of the plant. MATERIALS AND METHODS Fruit of Cakile edentula were collected from plants growing in a foredune area along Lake Huron at the Pinery Provincial Park (43°15« N, 81°50« W) in southwestern Ontario, Canada and stratified at 4 °C for 2 months before being set to germinate in a greenhouse. On 27 Jan. 1993, 160 germinated seeds (all germinated on that day) were individually transplanted into 15 cm plastic pots filled with washed commercial sand. The pots were randomly assigned to ten blocks on two greenhouse benches with 16 plants within each block. One or two weeks after transplanting (depending on the treatment), eight different treatments were applied at random to the 16 plants within each block (2 plants per treatment). The eight treatments were a factorial combination of low and high levels of moisture, nutrient supply, and sand burial. The low and high moisture treatments were maintained by delivering 80 and 150 ml tap water per pot (1 week after transplanting), respectively, at 2-d intervals throughout the experiment. The low and high nutrient treatments were maintained by weekly addition of 80 ml and 150 ml of 20-20-20 (N-P-K) solution per pot (1 week after transplanting) at 5 and 50 % of the recommended doses, respectively. The low and high sand burial treatments were maintained by burying the plants (2 weeks after transplanting) with washed sand to 0 and 6 cm, respectively. Zhang (1996) provided detailed information on the experimental procedures and ecological relevance of the treatments. Each plant was measured at weekly intervals for the number of leaves, chlorophyll content and width of the fifth newly emerged leaf, and the number of lateral branches. The fifth newly emerged leaf was chosen for chlorophyll measurement because it was well developed in plants across treatments. Leaf chlorophyll content was determined using the Minolta dual-wavelength chlorophyll meter (SPAD502, Minolta 1989). The SPAD values were then converted to chlorophyll concentration following Monje and Bugbee (1992). When plants had attained the maximum height 6 weeks after transplanting, the photosynthetic rate and water use efficiency (WUE) of plants were measured twice for each plant using a Li-cor 6200 (Li-Cor Inc, Lincoln, Nebraska, USA) system. The first measurement was taken within 12–24 h after watering and was referred to as normal photosynthetic rate and WUE. The second measurement was taken after various periods following watering when a plant started to show slight water stress (onset of wilting of the first leaf) and was thus referred to as stressed photosynthetic rate and WUE. Each plant was harvested when there was no sign of further growth and the youngest fruit was well developed. At harvest, the total number of T 1. Summary (F alues) of repeated-measures analysis of ariance for the number of leaes, leaf chlorophyll content, leaf width and number of lateral branches of plants measured at weekly interals. Within subject effects are not presented as time of obseration and its interaction with the three enironmental factors are all significant Source Nutrient (N) Moisture (M) Burial (B) N¬M N¬B M¬B N¬M¬B Number of leaves 1661±67*** 57±98*** 0±01NS 7±11** 0±15NS 0±54NS 0±02NS Chlorophyll content 10±27** 33±09*** 16±46*** 5±99* 4±00* 4±97* 0±13NS Leaf width 1007±89*** 112±13*** 1±88NS 4±53* 0±01NS 4±27* 0±63NS Number of branches 170±78*** 54±56*** 2±87NS 0±96NS 0±56NS 0±80NS 0±08NS *** Significant at P ! 0±001, ** significant at P ! 0±01, * significant at P ! 0±05 and NS not significant (P " 0±05). Zhang—Enironmental Response of Cakile edentula Number of leaves 200 A B C D E F G H 150 100 50 Chlorophyll (mg m–2) 0 600 525 450 375 300 30 Leaf width (mm) fruits (lowerupper) were counted and the dry weight (50 °C for 52 h) of fruits, shootleaves, roots and total biomass were measured. Dry matter allocation to each component and root}shoot ratio were then calculated. The mean fruit mass was estimated by dividing the total fruit weight by fruit number. The abortion rate of flowers was calculated based on measurements on the total number of flowers and fruit segments. The collected data were screened for outliers by identifying data points that were apparently isolated from the main cluster(s) of measurements on a given variable. The identified outliers were double checked for potential mistakes made during measurement or data entry. Uncorrectable data points were then considered as outliers and eliminated from analysis. Six measures on stressed photosynthesis and WUE were excluded (Table 1). The six excluded measurements on stressed photosynthesis and WUE were randomly distributed among different treatments. Each plant variable was transformed (angular for proportional data and natural log for the others) and then analysed using a three way ANOVA (Proc GLM, SAS Institute Inc., 1985). The weekly measurement data were analysed using repeated measures analysis of variance (Proc GLM, SAS Institute Inc., 1985). 593 24 18 12 RESULTS Deelopment Seedlings used in this study had the same number of leaves during the first 2 weeks after transplanting (Fig. 1). The effect of treatments was seen 3 weeks after transplanting or 1–2 weeks after treatment. Plants grown at high nutrient supply produced significantly more leaves than those at low nutrient supply under both moisture rich and poor conditions (Table 1, Fig. 1). When plants reached their maximum size about 6 weeks after transplanting, the difference in leaf number between plants grown at high and low nutrient supply could be three to four-fold. Higher soil moisture content also corresponded to more leaves per plant. However, its effect depends on the level of nutrient supply (Table 1). Under nutrient rich conditions, plants produced more leaves at high than low soil moisture content. Under nutrient poor conditions, there was little difference in the number of leaves between plants grown under high and low soil moisture content. The number of leaves per plant was not affected by sand accretion alone or its interaction with the other two factors throughout the experiment (Table 1, Fig. 1). Although the burial treatment 2 weeks after transplanting buried about 70 % of the above ground part (including some older leaves) of the plants, there was little difference in leaf number between the unburied and buried plants 1 week later (3 weeks after transplanting) apparently due to enhanced leaf production of the latter. The chlorophyll concentration of leaves varied significantly depending on the three environmental factors and their two-way interactions (Table 1). Under moisture rich conditions, unburied plants had a slightly higher leaf chlorophyll concentration than buried ones in the first 4 weeks after transplanting (Fig. 1). Thereafter, there was a Number of branches 6 14 11 8 5 2 0 1 2 3 4 5 6 7 0 1 2 3 Weeks after planting 4 5 6 7 F. 1. Number of leaves (A, B), chlorophyll content (C, D), leaf width (E, F) and number of lateral branches (G, H) of Cakile edentula under moisture rich (A, C, E, G) and moisture poor (B, D, F, H) treatments on different dates of observation. (E) Nutrient rich ; (D) nutrient poor ; (——), buried ; (– –) unburied. substantial increase in leaf chlorophyll concentration of plants grown at low nutrient supply so that they maintained greater leaf chlorophyll concentrations than those grown at high nutrient supply across burial depths. Under moisture poor conditions, high leaf chlorophyll concentration was observed in unburied plants during the first 5 weeks after transplanting. Plants grown at high nutrient supply began to show a lower leaf chlorophyll concentration than those at low nutrient supply 6 weeks after transplanting as observed in moisture rich conditions. Plants at given levels of nutrient supply and sand burial had higher leaf chlorophyll concentrations under moisture poor than moisture rich conditions at the early stages (e.g. the first 5 weeks after planting) of development (Fig. 1). Leaf width depended significantly on nutrient supply and soil moisture content (Table 1) with plants grown at high nutrient supply and soil moisture content having wider leaves for both the buried and unburied plants (Fig. 1). The effect of soil moisture content on leaf width was more 594 Zhang—Enironmental Response of Cakile edentula T 2. Summary (F alues) of ANOVA for physiological traits of Cakile edentula measured 6 weeks after planting Variable Nutrient (N) Normal photosynthesis Normal WUE Stressed photosynthesis Stressed WUE 0±01NS 6±56* 97±87*** 5±93* Moisture (M) Burial (B) N¬M N¬B M¬B N¬M¬B 0±79NS 0±30NS 5±84* 0±43NS 1±17NS 0±58NS 5±76* 0±71NS 6±34* 2±17NS 5±09* 0±35NS 1±18NS 0±08NS 0±01NS 4±20* 0±01NS 3±26NS 7±60** 0±41NS 0±89NS 0±01NS 0±20NS 1±18NS *** Significant at P ! 0±001, ** significant at P ! 0±01, * significant at P ! 0±05 and NS not significant (P " 0±05). A B Normal WUE (µmol mmol–1) Normal photosynthesis (µmol m–2 s–1) 22 19 16 13 10 E F 11 8 5 2 C D G H 2.4 2.0 1.6 1.2 Stressed WUE (µmol mmol–1) Stressed photosynthesis (µmol m–2 s–1) 14 2.8 0 6 0 6 5 4 3 2 0 6 Depth of sand accretion (cm) 6 0 6 F. 2. Bar charts showing the effect of nutrient supply (+, nutrient rich ; *, nutrient poor), soil moisture content (moisture rich, A, C, E, G and moisture poor, B, D, F, H) and sand burial on normal photosynthesis (A, B), normal WUE (C, D), stressed photosynthesis (E, F) and stressed WUE (G, H) of Cakile edentula. Vertical bars indicate the standard errors. pronounced at high than low nutrient supply. Sand burial alone did not affect plant leaf width significantly. Although there was a significant interaction between sand burial and soil moisture content (Table 1), the magnitude was too small because it is difficult to depict any general trend (Fig. 1). Plants grown at high nutrient supply or soil moisture content produced significantly more lateral branches regardless of sand accretion (Table 1, Fig. 1). Physiology The photosynthetic rate of plants shortly after watering (normal photosynthetic rate) depended on the joint effect of nutrient supply and soil moisture content (Table 2). Plants that had been continuously grown in moisture rich conditions had higher photosynthetic rates at high than low nutrient supply (Fig. 2). Conversely, plants that had been grown continuously in moisture poor conditions had a higher photosynthetic rate at low than high nutrient supply. The water use efficiency of plants shortly after watering (normal WUE) varied with nutrient supply only (Table 2) with those under nutrient rich conditions being significantly more efficient in using water for photosynthesis than those under nutrient poor conditions, especially when soil moisture content is low (Fig. 2). The three environmental factors and their interactions affected the photosynthetic rate of plants more when there was a water stress (Table 2). In general, plants had a significantly higher rate of photosynthesis (stressed photosynthetic rate) under nutrient rich than poor conditions (Fig. 2). However, the difference between plants grown at high s. low nutrient supply was smaller under moisture poor than moisture rich conditions. This is because plants that had been grown under moisture poor conditions were able to maintain higher rates of photosynthesis at low nutrient supply than plants that had been grown under moisture rich conditions. Sand burial reduced the photo- Zhang—Enironmental Response of Cakile edentula 595 T 3. Summary (F alues) of ANOVA for biomass and fitness traits of Cakile edentula measured at harest Variable Nutrient (N) Total biomass Allocation to shoot Allocation to root Root}shoot ratio Allocation to fruits Number of fruits Abortion rate Weight of fruits Mean fruit weight Moisture (M) 8875±61*** 3±26NS 8±34** 11±82*** 1±27NS 7083±71*** 2±75NS 8016±22*** 5±58* 27±14*** 7±74** 0±34NS 0±49NS 3±09NS 30±28*** 8±03** 23±38*** 3±23NS Burial (B) 6±74** 12±46*** 29±36*** 1±51NS 4±94* 5±63* 10±55** 0±29NS 2±41NS N¬M N¬B M¬B N¬M¬B 23±96*** 0±12NS 2±69NS 2±57NS 4±68NS 84±17*** 0±34NS 39±78*** 13±02*** 2±63NS 0±27NS 1±69NS 0±09NS 0±36NS 18±94*** 0±08NS 0±89NS 28±46*** 6±87** 0±27NS 7±93** 7±81* 10±73** 1±87NS 0±02NS 0±01NS 1±61NS 5±79* 10±56** 0±22NS 0±51NS 4±91* 0±01NS 0±01NS 0±51*** 0±63NS A B 0.22 Root/shoot ratio 12 8 4 G H 17 14 11 8 M N 525 350 175 0 0.16 0.13 50 I J 47 44 41 0 6 0 6 6.0 O P 4.5 3.0 1.5 0 44 E F K L Q R 41 38 35 32 38 Total weight of fruits (g) Number of fruits 700 0.19 0 6 0 6 Depth of sand accretion (cm) Abortion rate of flowers (%) 20 D 0.10 Allocation to fruits (%) Allocation to roots (%) 0 C Mean fruit weight (mg) Plant biomass (g) 16 Allocation to shoot (%) *** Significant at P ! 0±001, ** significant at P ! 0±01, * significant at P ! 0±05 and NS not significant (P " 0±05). 44 38 32 26 20 12 9 6 3 0 0 6 0 6 F. 3. Bar charts showing the effect of nutrient supply (+, nutrient rich ; *, nutrient poor), soil moisture content (moisture rich, A, C, E, G, I, K, M, O, Q and moisture poor, B, D, F, H, J, L, N, P, R) and sand burial on biomass and fitness traits of Cakile edentula. Vertical bars indicate the standard errors. synthetic rate of plants under moisture poor but not moisture rich conditions. The stressed water use efficiency of plants varied significantly with soil nutrition and the level of sand burial (Table 2). High soil nutrient supply significantly enhanced the stressed water use efficiency of unburied but not buried plants under both low and high moisture conditions (Fig. 2). Biomass and fitness Measurements on the biomass and fitness of plants varied significantly with the three environmental factors and their interactions (Table 3). In general, the total biomass of plants increased significantly with nutrient supply under both moisture rich and moisture poor conditions (Fig. 3). At high nutrient supply, plants under moisture rich conditions also had significantly greater biomass than those under moisture poor conditions. Sand burial did not have apparent effects on plant biomass except at low soil nutrient level under moisture poor conditions, where a slight increase was observed in the buried plants. Plants grown at high nutrient supply had greater root}shoot ratios than those at 596 Zhang—Enironmental Response of Cakile edentula low nutrient supply only under moisture poor conditions. Buried plants, at a given level of soil nutrients, also had significantly greater root}shoot ratio, than unburied ones under moisture poor but not moisture rich conditions (Fig. 3). Dry matter allocation to shoots and fruits of plants did not show any clear trend of variation with any of the three environmental factors. A substantial increase in the amount of dry matter allocated to the root systems was observed in plants grown at a given level of soil nutrients under moisture poor conditions as a result of sand burial (Fig. 3). Under moisture poor conditions, the abortion rate of flowers was significantly higher for unburied plants or those grown at high soil nutrient level (Fig. 3). Under moisture rich conditions, variations in the abortion rate of flowers appeared to be independent of the three environmental factors. The number of fruits produced by a plant increased significantly with nutrient supply under both moisture rich and poor conditions. While plants grown under nutrient poor conditions had a similar number of fruit regardless of soil moisture content and sand burial, those grown in nutrient rich conditions produced more fruit at high rather than low levels of soil moisture or sand burial. The total weight of fruits increased with soil nutrient level under both moisture rich and poor conditions, and with soil moisture level under nutrient rich conditions. Sand burial did not have any significant effect on the total weight of fruits. Plants tended to produce small fruits when buried under nutrient rich conditions within a given soil moisture regime, or grown at moisture rich conditions at a given depth of sand burial. Buried plants grown at low soil nutrient levels, however, tended to produce larger fruits than unburied ones under both moisture rich and poor conditions (Fig. 3). DISCUSSION Temporal and spatial environmental variations are expected to occur in almost any ecosystem (Bell et al., 1986). To understand the impact of a given environmental factor on plants, it would be most relevant to study its effects relative to other abiotic or biotic factors. Although sand dune systems undergo drastic environmental changes even on a daily basis (Barbour et al., 1985 ; Maun, 1985), and it has been recognized that plant growth may be affected by a group of interacting factors (Olson, 1958 ; Marshall, 1965 ; Zhang and Maun, 1992), few studies have examined the relative importance and integrative effect of these environmental factors on dune plants. Among the 17 (a total of traits listed in Tables 1, 2, and 3) plant variables measured in this study, 13 were significantly affected by nutrient supply, ten by soil moisture content and eight by sand accretion as main factors. At P ¯ 0±05, the chance of mistakenly identifying a non-significant response of plant is about 1 out of 17 variables. Thus, the differences between 13 out of 17 and 10 or 8 out of 17 variables are not likely to result from chance alone, suggesting that nutrient supply is a significantly more important factor than soil moisture content or sand burial on the growth of Cakile edentula under field conditions where variations in multiple factors occur. Two or three way interactions between the three environmental factors are often observed (14 out of 17) and some of the results are useful to explain divided opinions between researchers. For example, it was reported by Disraeli (1984) that the concentration of chlorophyll in leaves of Ammophila breiligulata increased exponentially with increased sand accretion. Using the same species, Yuan (1991) observed a decrease in leaf chlorophyll concentration with increasing depth of sand burial. According to the current study, both increased and decreased leaf chlorophyll may occur as one of the possible responses of plants to sand accretion under different regimes of environmental conditions (Fig. 1). It is thus reasonable to assume that differences in the combination of environmental factors may be responsible for the contradicting results obtained in these two previous studies. Buried plants of C. edentula generally had lower leaf chlorophyll concentrations than unburied ones at earlier stages of development of the plants (Fig. 1), which may be a direct effect of compensatory growth commonly found in plants. Increased biomass and fitness of plants in response to moderate defoliation are typical examples of compensatory growth (Belskey, 1986, 1987 ; Oba, 1994). Sand burial also reduces the total amount of photosynthetic area or the above ground part of plants and thus may practically have a similar effect as defoliation that initiates a process of compensatory growth of the target plants. Zhang and Maun (1992) provided indirect support for this hypothesis by showing that the improved shoot growth within one week after the burial of C. edentula seedlings was not triggered by nutrient addition or the response of plants to the dark condition imposed by the deposited sand. While the compensatory growth of plants may make up the reduced photosynthetic area and balance the carbon and nutrition requirements of plants, overcompensation in some species or under a certain set of circumstances (Oba, 1994) may result in deficient supply in growth materials and, in the case of buried plants of C. edentula, low chlorophyll concentration of the newly developed leaves. The majority of the evidence showing improved growth of buried plants is based on biomass and final fitness, while far fewer studies have examined the physiological response of plants to sand burial. A recent study by Yuan et al. (1993) showed that buried plants of A. breiligulata and Calamoilfa longifolia generally had higher net photosynthetic rates than unburied ones. This result is probably not due to improved moisture conditions in the root zones because the water potential of leaves of both buried and unburied plants did not differ significantly. Yuan et al. (1993) attributed the increased photosynthetic rate of buried plants to thicker leaves and a great total area of mesophyll cells exposed to intercellular spaces per unit leaf area (Ames}A). A larger Ames}A value has been observed to increase CO absorbtion (Nobel and Walker, 1985). This # hypothesis is relevant because Yuan et al. (1993) used established adult plants in their study. The well developed root system of established plants may minimize the limiting effect of soil nutrients and moisture on photosynthesis. For young seedlings or annual plants, however, the nutrition and moisture status of the microhabitat may be crucial to Zhang—Enironmental Response of Cakile edentula their photosynthetic abilities. In the current study, the photosynthetic rate of plants was measured shortly after watering, which mimics the soil conditions after rainfall or big wave action, and when plants had just started to show a sign of water stress, which mimics the soil conditions on dry and hot summer days. The results showed that the photosynthetic capacity of a plant depended on sand burial, soil nutrition, and the current as well as the history of soil moisture conditions. Sand burial affected the photosynthesis of plants mainly under conditions where water stress was a recurrent event (stressed photosynthesis). This may occur during the summer or before the majority of the root system of a plant reaches the 20 cm depth. In these cases, however, buried plants tend to have a lower rather than higher photosynthetic rate than unburied ones (Fig. 2). It then follows that sand burial alone is not likely to enhance the photosynthetic capacity of plants. Zhang and Maun (1992) also suggested that sand burial generally did not stimulate long term positive responses of plants unless the deposited sand contained a certain amount of nutrients. Even so, variations may occur depending on soil moisture status. Nutrient addition increases the photosynthetic capacity of water stressed plants no matter if they have or have not experienced any water stress previously (stressed photosynthesis in Fig. 2). Provided with adequate water (e.g. after rainfall or big waves), nutrient addition tends to increase or decrease the photosynthetic capacity of plants that have not or have experienced water stress previously (normal photosynthesis in Fig. 2). Therefore, nutrient addition due to sand accretion or deposition of organic debris may affect the growth of dune plants to various degrees depending not only on the current but also the history of soil moisture status. The pattern of biomass allocation of plants is one of the major focuses of contemporary ecological studies. Evidence from a large body of literature shows that plants under nutrient or moisture poor conditions often have a large root to shoot ratio (Sultan and Bazzaz, 1993 a, b ; Green et al., 1994). The response of C. edentula to soil nutrient and moisture content contradicted this generalization in that plants tended to have a greater root to shoot ratio in nutrient rich than in nutrient poor conditions, especially when soil moisture content had been continuously low (Fig. 3). It is recognized that the root-bound growth of plants that commonly occurs in greenhouse experiments may have caused abnormal distribution of biomass between the above and below ground parts of the plants in this study. If this was really the case then plants grown under nutrient rich conditions would be more likely to be root-bound and thus tend to have a small root to shoot ratio, especially at high soil moisture content without sand accretion. This is not supported by the results from this study. According to Zhang (1993), the root to shoot ratio of C. edentula grown under a single testing environment is negatively related to overall biomass regardless of the age of plants. This correlation does not explain the results of the current study either because high nutrient supply resulted in large plants associated with higher root to shoot ratios. Green et al. (1994) reported that nitrogen nutrition and drought interacted to determine the root to shoot ratio of Pinus 597 taeda L. seedlings. While high nitrogen supply decreased the root to shoot ratio of P. taeda seedlings, the effect of nitrogen decreased with the length of drought treatment and was no longer observable after 10 d water stress (Green et al., 1994). It was also observed that starch metabolism to support growth was fast in water stressed plants under high nitrogen supply, but was limited under low nitrogen supply (Green et al., 1994). Perhaps efficient starch metabolism of C. edentula plants at high nutrient supply may have enabled them to maintain a greater root biomass than plants at low nutrient supply under water stressed condition. Biomass allocation to roots was also observed to increase with sand burial under moisture poor but not moisture rich conditions (Fig. 3). Although the underlying mechanisms are as yet unknown, the result demonstrates that the effect of an environmental factor on biomass allocation of plants may be altered by variation in another factor. In fact, the interaction between environmental factors on plant biomass allocation is an important but poorly addressed question (Green et al., 1994). Although sand accretion affected the total biomass of plants (P ! 0±01) according to the analysis of variance, the effect was perhaps not substantial biologically (Fig. 3). However, buried plants did produce significantly more fruits than unburied ones, especially at high soil nutrition. A similar result has also been reported by Zhang and Maun (1992). This was partially achieved through a more economical reproductive strategy of the buried plants, as they tended to have a lower abortion rate of flowers than the unburied ones, and through a trade off between fruit number and weight (Fig. 3). Compensatory growth following sand burial would be another option, as it is commonly observed that defoliated plants tend to increase their final fitness (Belskey, 1986, 1987). Because plants are generally subjected to multiple stresses under field conditions, they would possess the ability (as the result of natural selection) to adjust their growth according to the levels of all the major environmental factors involved. Interactions between abiotic and}or biotic factors may activate plant responses that are not normally observed under a single testing environment. These responses perhaps have significant ecological and evolutionary values and should receive more attention. A C K N O W L E D G E M E N TS I thank the Natural Sciences and Engineering Research Council of Canada for a post-doctoral fellowship and Dr M. J. Lechowicz at the Department of Biology, McGill University for helpful discussions on the project. Comments by Dr I. A. Ungar and an anonymous reviewer on an early draft of the manuscript are highly appreciated. LITERATURE CITED Barbour MG, de Jong TM, Pavlik BM. 1985. Marine beach and dune plant communities. In : Chabot BF, Mooney HA, eds. Physiological ecology of North American plant communities. New York : Chapman and Hall, 296–322. 598 Zhang—Enironmental Response of Cakile edentula Bell G, Lechowicz MJ. 1994. The flips side : manifestations of how plants perceie patchiness and different heterogeneity by plants. Ecophysiological processes aboe and below ground. New York : Academic Press. Bell G, Lechowicz MJ, Appenzeller A, Chandler M, DeBlois E, Jackson L, Mackenzie B, Preziosi R, Belskey AJ. 1986. Does herbivory benefit plants ? A review of the evidence. The American Naturalist 126 : 870–892. Belskey AJ. 1987. The effect of grazing : confounding of ecosystem : community and organism scales. The American Naturalist 129 : 777–783. Brady NC. 1974. The nature and properties of soils. New York : Macmillian Publishing Co. Inc. Disraeli DJ. 1984. The effect of sand deposits on the growth and morphology of Ammophila breiligulata. Journal of Ecology 72 : 145–154. Green TH, Mitchell RJ, Gjerstad DH. 1994. Effects of nitrogen on the response of loblolly pine to drought. New Phytologist 128 : 145–152. Hassouna MG, Wareing PF. 1964. Possible role of rhizosphere bacteria in the nutrition of Ammophila arenaria. Nature (London) 202 : 467–469. Hawake MA, Maun MA. 1988. Some aspects of nitrogen, phosphorus, and potassium nutrition of three colonizing beach species. Canadian Journal of Botany 66 : 1490–1496. Holton B. Jr. 1980. Some aspects of the nitrogen cycle in a northern California costal dune-beach ecosystem, with emphasis on Cakile maritima. Ph. D. Thesis, University of California, Davis. Marshall JK. 1965. Corynephorus canescens (L.) P. Beauv. as a model for the Ammophila problem. Journal of Ecology 53 : 447–463. Maun MA. 1985. Population biology of Ammophila breiligulata and Calamoilfa longifolia on Lake Huron sand dunes. I. Habitat, growth form, reproduction, and establishment. Canadian Journal of Botany 63 : 113–124. Maun MA, Boyd RS, Olson L. 1990. The biological flora of coastal dunes and wetlands. 1. Cakile edentula (Bigel.) Hook. Journal of Coastal Research 6 : 137–156. Maun MA, Lapierre J. 1984. The effect of burial by sand on Ammophila breiligulata. Journal of Ecology 72 : 827–839. Minolta. 1989. SPAD-502 owner’s manual. Ramsey, NJ : Industrial meter division, Minolta Corp. Monje OA, Bugbee B. 1992. Inherent limitations of nondestructive chlorophyll meters : a comparison of two types of meters. HortScience 27 : 69–71. Nobel PS, Walker DB. 1985. Structure of leaf photosynthetic tissue. In : Barber J, Baker NR, eds. Photosynthetic mechanisms and the enironment. New York : Elsevier (Biomedical Division), 501–536. Oba G. 1994. Responses of Indigofera spinosa to simulated herbivory in a semidesert of North-West Kenya. Acta Œcologica 15 : 105–117. Olson JS. 1958. Lake Michigan dune development. II. Plants as agents and tools in geomorphology. Journal of Geology 66 : 345–351. Payne AM, Maun MA. 1984. Reproduction and survivorship of Cakile edentula var. lacustris along the Lake Huron shoreline. American Midland Naturalist 111 : 86–95. Pemadasa MA, Lovell PH. 1974. The mineral nutrition of some dune annuals. Journal of Ecology 62 : 647–657. SAS Institute Inc. 1985. SAS user’s guide : statistics. Version 5. Cary, North Carolina, USA : SAS Institute Inc. Sultan SE, Bazzaz FA. 1993 a. Phenotypic plasticity in Polygonum persicaria. II. Norms of reaction to soil moisture and the maintenance of genetic diversity. Eolution 47 : 1032–1049. Sultan SE, Bazzaz FA. 1993 b. Phenotypic plasticity in Polygonum persicaria. III. the evolution of ecological breadth for nutrient environment. Eolution 47 : 1050–1071. Tyndall RW, Teramura A, Douglass LW. 1986. Potential role of soil moisture deficit in the distribution of Cakile edentula. Canadian Journal of Botany 64 : 2789–2791. van der Valk AG. 1974. Environmental factors controlling the distribution of forbs on costal foredunes in Cape Hatteras National Seashore. Canadian Journal of Botany 52 : 1057–1073. Wallen B. 1980. Changes in structure and function of Ammophila during primary succession. Oikos 34 : 227–238. Willis AJ, Folkes BF, Hope-Simpson JF, Yemm EW. 1959. Braunton Burrows : the dune systems and its vegetation. Journal of Ecology 47 : 1–24. Yuan T. 1991. Relationship between sand accretion and photosynthesis of Ammophila breviligulata (C ) and Calamovilfa longifolia (C ) $ % under field, greenhouse and growth chamber conditions. Master Thesis, University of Western Ontario. Yuan T, Maun MA, Hopkins WG. 1993. Effects of sand accretion on photosynthesis, leaf-water potential and morphology of two dune grasses. Functional Ecology 7 : 676–682. Zhang J. 1993. Seed dimorphism in relation to germination and growth of Cakile edentula. Canadian Journal of Botany 71 : 1231–1235. Zhang J. 1995. Differences in phenotypic plasticity between plants from dimorphic seeds of Cakile edentula. Oecologia 102 : 353–360. Zhang J. 1996. Seed mass effects across environments in an annual dune plant. Annals of Botany 77 : 555–563. Zhang J, Maun MA. 1990. Effects of sand burial on seed germination, seedling emergence, survival, and growth of Agropyron psammophilum. Canadian Journal of Botany 68 : 304–310. Zhang J, Maun MA. 1992. Effects of burial in sand on the growth and reproduction of Cakile edentula. Ecography 15 : 296–302.
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