Host physiological condition regulates parasitic plant performance: Arceuthobium vaginatum subsp. cryptopodum on Pinus ponderosa
- First Online:
- Cite this article as:
- Bickford, C.P., Kolb, T.E. & Geils, B.W. Oecologia (2005) 146: 179. doi:10.1007/s00442-005-0215-0
- 216 Views
Much research has focused on effects of plant parasites on host-plant physiology and growth, but little is known about effects of host physiological condition on parasite growth. Using the parasitic dwarf mistletoe Arceuthobium vaginatum subsp. cryptopodum (Viscaceae) and its host Pinus ponderosa, we investigated whether changes in host physiological condition influenced mistletoe shoot development in northern Arizona forests. We conducted two studies in two consecutive years and used forest thinning (i.e., competitive release) to manipulate host physiological condition. We removed dwarf mistletoe shoots in April, before the onset of the growing season, and measured the amount of regrowth in the first season after forest thinning (Study I: n=38 trees; Study II: n=35 trees). Thinning increased tree uptake of water and carbon in both studies, but had no effect on leaf N concentration or δ13C. Mistletoe shoot growth was greater on trees with high uptake of water and carbon in thinned stands than trees with low uptake in unthinned stands. These findings show that increased resource uptake by host trees increases resources to these heterotrophic dwarf mistletoes, and links mistletoe performance to changes in host physiological condition.
KeywordsArizonaDwarf mistletoeForest managementHost-parasite physiologyPhotosynthesisWater relations
Dwarf mistletoes (Arceuthobium spp., Viscaceae) are obligate heterotrophic plants that infect numerous conifer species in western North America and around the world (Hawksworth and Weins 1996; Kolb 2002). Species in Arceuthobium are host-specific parasites, with most dwarf mistletoes having primary and secondary host species (Hawksworth and Weins 1996). The dwarf mistletoes are similar to the leafy mistletoes of the Loranthaceae and other families because they acquire all of their water and nutrients from their hosts (Fisher 1983; Lamont 1983). However, dwarf mistletoes differ from many other types of mistletoe because they are essentially leafless and are more heterotrophic (Hull and Leonard 1964b; Miller and Tocher 1975; Logan et al. 2002).
Most research on dwarf mistletoes has focused on negative effects of infection on host performance (e.g., Hawksworth and Shaw 1984; Wanner and Tinnin 1986, 1989; Hawksworth and Geils 1990; Tinnin and Knutson 1999; Sala et al.2001; Godfree et al. 2002; Meinzer et al. 2004), and understanding of their physiological characteristics (e.g., Hull and Leonard 1964a, 1964b; Leonard and Hull 1965; Miller and Tocher 1975; Quarishi et al. 1977; Fisher 1983; Rey et al. 1991; Logan et al. 2002). However, the once dominant view of dwarf mistletoes as detrimental, based on economical impacts on host plant productivity is expanding to include them as keystone-type species that are important to ecosystem food-webs (Mathiasen 1996; Watson 2001; van Ommeren and Whitham 2002; Mooney 2003). For example, forest management in the western U.S. used to emphasize control or sanitation of dwarf mistletoes from conifer stands (Quick 1964; Baranyay and Smith 1972), whereas the value of dwarf mistletoes for animal habitat and structural diversity is increasingly being recognized (Keith 1965; Stevens and Hawksworth 1970; Farentinos 1972; Hawksworth and Geils 1996; Bennetts and Hawksworth 1992; Garnett 2002).
In contrast to the large amount of information on impacts of dwarf mistletoes on their hosts, understanding of factors that regulate the performance of plant parasites such as dwarf mistletoes is sparse (Ayers and Lombardero 2000, Pennings and Callaway 2002). The few studies of this topic have used non-experimental correlative approaches to suggest regulation of mistletoe water use efficiency by the amount of nitrogen (N) contained in the host for partially heterotrophic mistletoes (Schulze and Ehleringer 1984; Schulze et al. 1991), positive relationships between mistletoe abundance and host shoot water potential (Bannister et al. 1999), positive relationships between mistletoe abundance and light intensity in the host canopy (Scharpf 1972; Shaw and Weiss 2000), and linkage between host colonization and chemical composition of host phloem and xylem (Linhart et al. 1994; Snyder et al. 1996). These findings are consistent with the hypothesis that dwarf mistletoe performance is regulated by the physiological condition of the host, analogous to the regulation of the performance of non-parasitic plants by availability of water and mineral nutrients from the soil. In contrast, a descriptive non-experimental study of Arceuthobium divericatum on Pinus edulis found greater dwarf mistletoe infection in trees in high stress sites compared with low stress sites (Mueller 2004). Experimental tests of the hypothesis that host physiological condition regulates mistletoe performance are needed but are limited to effects of N fertilization of hosts on the physiology of Phoradendron juniperinum, which is more autotrophic than the dwarf mistletoes (Marshall et al. 1994). Moreover, few experiments have considered treatments used to improve resource uptake of host trees, such as forest thinning, that are applied widely over forest landscapes (Covington et al. 1997; Latham and Tappeiner 2002; Nyland 2002; Conklin 2003).
We investigated linkages between improved physiological condition of ponderosa pine (Pinus ponderosa Laws. var. scopulorum Engelm), brought about by forest thinning, and performance of Southwestern dwarf mistletoe (Arceuthobium vaginatum [Willd.] Presl subsp. cryptopodum [Engelm.] Hawksw. and Weins) by measuring host tree physiological status in thinned and unthinned stands coupled with measurements of mistletoe shoot growth. Much research has shown that forest thinning increases water and carbon uptake of ponderosa pine (Feeney et al. 1998; Kolb et al. 1998; Latham and Tappeiner 2002; McDowell et al. 2003; Skov et al. 2004). We hypothesized that forest thinning would increase resource uptake by host trees, which in turn would increase resources to the dwarf mistletoes and stimulate mistletoe shoot growth.
We conducted two similar experiments at different sites in consecutive years (2003, 2004). Stands were approximately 40 ha in size and thinned from below (i.e., most small diameter trees were removed) to simulate tree density and structure found in northern Arizona prior to Euro-American settlement in the late nineteenth century (Covington et al. 1997). Both sites were located near Flagstaff, AZ at elevations exceeding 2,000 m in a climate that is characterized by dry weather in May and June, followed by monsoon thunderstorms between mid-July and mid-September (Sheppard et al. 2002). Over the last 50 years an average of 47% of precipitation has occurred in winter (November–March), 34% during the monsoon thunderstorms (July–September), with the remaining 19% falling in other months [Western Regional Climate Center; http://www.wrcc.dri.edu/index.html]. The sites were located in the ponderosa pine forest-type, which is dominated by ponderosa pine interspersed with junipers (Juniperus spp.), Gambel oak (Quercus gambellii), and bunch-grasses.
The 2003 study was located in the Coconino National Forest at an elevation of approximately 2,400 m. Soils on the site were Mollic Eutroboralts derived from mixed igneous parent material (Miller et al. 1995). One half of the study site was assigned a thinning treatment. The two stands (thinned, unthinned) were located next to each other and had the same slope and aspect. In the thinned stand, all competing trees, defined as all trees within a circular perimeter around each subject tree equal to 40× diameter at breast height (DBH), were felled with chainsaws in January 2003; all other thinning was done between May and July 2003 under the auspices of the USDA Forest Service by a logging company. Study trees in unthinned stands for both studies were located more than 20 m from the thinned stand. We measured post-thinning basal area using a random grid design comprising ten 0.1 ha plots spaced 100 m apart in each stand. Tree basal area in the stand before thinning averaged 42.1 m2/ha; thinning reduced basal area by 41% to 24.7 m2/ha in the part of the stand assigned the thinning treatment.
We selected trees for physiological measurements by first identifying nineteen trees infected with dwarf mistletoe in the thinned stand. We then paired these trees with trees of similar DBH (mean=11.6 cm; range=4–44 cm; P=0.50 t-test between stands) and dwarf mistletoe rating (DMR) (Hawksworth 1977) in the unthinned stand. DMR is a measure of mistletoe infection whereby each third of a tree is evaluated for infection (0, 1, 2) and summed to obtain whole-tree infection on a scale from 0 (uninfected) to 6 (heavily infected) (Hawksworth 1977). Mean DMR of trees in the thinned stand was 4.1 and ranged from 1 to 6; mean DMR of trees in the unthinned stand was 4.6, ranged from 3 to 6, and was similar to the DMR of trees in the thinned stand (t-test P= 0.26).
Study II was performed to test the robustness of results from Study I, and was similar to Study I with the following differences. The 2004 study was in a ponderosa pine stand located in the Northern Arizona University Centennial Forest at an elevation of approximately 2,130 m with no significant slope. Soils on the site were Mollic Eutroboralfs derived from benmorite parent material (Miller et al. 1995). One half of the stand was assigned a thinning treatment. Thinning in September 2003 reduced tree basal area by 57% from 32.8 to 14 m2/ha. We measured inter-tree competition as described for the 2003 study and found that CI was higher (ANOVA; P<0.0001) for trees in the control stand (CI=10.7, SE=2.29) compared to trees in the thinned stand (CI=0.08, SE=0.05) after thinning. Eighteen mistletoe-infected ponderosa pines of similar DBH (mean=9.3 cm; range=5–28 cm; P=0.39 t-test between stands) and DMR (mean=3.6; range=2–6; P=0.62 t-test between stands) were selected for study in each of the thinned and unthinned stands. One tree in the thinned stand died and was removed from the study, making n=35.
Mistletoe removal experiment
Host tree physiology
Host physiological status was evaluated by measuring light saturated (PPFD=1,200 μmol m2/s1) net-photosynthetic rate (Pn), stomatal conductance (gs), internal CO2 concentration (Ci), leaf-level N concentration, and leaf 13C/12C isotope discrimination (δ13C). We measured Pn, gs, and Ci of ponderosa pine needles between the hours of 0930 and 1230 using a Li-Cor 6400 portable photosynthesis system (Li-Cor Inc.; Lincoln, NE). We measured one sunlit branch used in the mistletoe removal experiment on each tree in June, August, September, and October 2003 in Study I, and monthly between May and November 2004 in Study II. We measured Pn, gs, and Ci on 1-year-old needles in May (2004) and June (both years), and on fully developed current-year needles for the remainder of both growing seasons. We coupled gas exchange measurements with measurements of leaf xylem predawn water potential (Ψpre) using a Scholander-type pressure bomb (PMS Instrument Co.; Corvallis, OR, USA) in all months except August and September 2004, when up to three days separated gas exchange and predawn water potential measurements due to inclement weather conditions. We used projected leaf area measured with AgImage Plus Ver. 1.08 software (Decagon Devices) to calculate Pn and gs for ponderosa pine and Pn for dwarf mistletoe aerial shoots.
We measured leaf-level N concentration to assess whether differences in carboxylation efficiency existed between trees in the thinned and unthinned stands, as leaf-level N concentration is strongly associated with rubisco concentration, the primary carboxylating enzyme in C3 plants (Field and Mooney 1986). We measured δ13C as an index of Ci over the period of needle development (late May–late July). After cessation of current year needle growth at the end of July in both studies we collected a sample of needles, representative of all needles formed during the current season to avoid intra-seasonal bias, from one branch used in the mistletoe removal experiment on each tree for measurement of δ13C and N concentration. Needle samples were dried for 24 h at 70°C and then ground to a 40-mesh (420 micron) powder using a Wiley Mill (Thomas-Wiley). Samples were analyzed with an Elemental Analyzer-Continuous Flow Isotope Ratio Mass Spectrometer (Finnigan Delta Advantage) at the Colorado Plateau Stable Isotope Laboratory (2005) at Northern Arizona University, Flagstaff, Arizona (http://www4.nau.edu/cpsil/).
Light response curves
We measured photosynthetic light response curves on one branch infected with dwarf mistletoe from each of eight trees, and on the mistletoe shoots growing on those branches. Measurements were made in the first week of September 2004 between the hours of 0800 and 1200 in the unthinned stand at the Study II site, on different but similar-sized trees to those used for the mistletoe regrowth measurements. We measured Pn using a Li-Cor 6400 portable photosynthesis system at the following levels of PPFD (Photosynthetic Photon Flux Density: μmol/m2/s1): 50, 100, 300, 400, 600, 700, 800, 1,000, and 1,200. Leaves and mistletoe shoots acclimated to each level of PPFD for approximately two minutes prior to measurement. Chamber CO2 concentration was maintained at 365 ppm, chamber humidity was maintained within 10% of ambient, and leaf temperature was maintained at 25°C during measurement. We first measured light response curves from pine needles attached to the tree. The branch supporting these needles was excised from the tree, the cut end was immediately placed under water and then re-cut to remove xylem embolisms, and the cut end remained submerged throughout the light response measurements for mistletoe. Measuring light response curves of dwarf mistletoe shoots on cut branches helped prevent breakage of fragile dwarf mistletoe shoots. Additional measurements of the response of mistletoe Pn to PPFD were made in early June 2005 to better understand carbon uptake of mistletoe at low light levels. These measurements were made on five mistletoe plants growing on five different trees at the Study II site using identical techniques to those used in June 2004, except that we focused only on low levels of PPFD (0, 75, 200, 400 μmol/m2/s1) and included a measurement of dark respiration.
Analysis of the data from Study I with repeated measures MANOVA revealed that the original pairing design based on similar tree DBH and DMR had no effect on Ψpre (P=0.20), Pn (P=0.69), gs (P=0.33), or Ci (P=0.49). Consequently, all tree physiological data from Study I and II were analyzed separately without pairing by tree size or DMR with one-way ANOVA or repeated measures MANOVA for measurements repeated over different dates (Study I: n=38; Study II: n=35). Due to a limited number of repeated measurements of tree physiological characteristics (Ψpre, Pn, gs, Ci) our multivariate tests were transformed into univariate tests (Huynh and Feldt 1970; SAS Institute 2002). Effects of date and treatment × date interactions on measurements were evaluated using epsilon-adjusted tests. When significant treatment × date interactions occurred data were analyzed by date using ANOVA with a Bonferroni adjustment for comparisons over multiple dates. If the sphericity chi-square test was significant we evaluated date and treatment interactions using the Geisser and Greenhouse adjusted-univariate test. If the sphericity chi-square test was not significant we evaluated interactions using unadjusted-univariate F tests (SAS Institute 2002). We compared leaf-level N concentration and δ13C between thinned and unthinned stand trees using ANOVA. We pooled mistletoe biomass regrowth data across studies and analyzed these data using ANOVA with study, treatment, and treatment × study as factors and with tree DBH as a covariate.
Host tree physiological response to thinning
Results for Pn, gs, and Ci indicate consistently higher carbon uptake by trees in the thinned stand compared with trees in the unthinned stand. Stomatal conductance (P<0.0001; Fig. 1b) and Ci (P=0.06; Fig. 1c) were higher for trees in the thinned stand. Differences in Pn between trees in thinned and unthinned stands depended on measurement date (treatment × date interaction: P=0.03; Fig. 1d). Bonferonni adjusted ANOVA (P≤0.0125 level) comparisons show significantly higher Pn for trees in the thinned stand in August (P=0.01), September (P=0.001), and October (P<0.0001), but not in June (P=0.02). Leaf N concentration was similar for trees in both stands (P=0.55; mean thinned = 1.21%, SE=0.07; mean unthinned = 1.26%, SE=0.06), suggesting that higher Pn in the thinned stand was due to increased gs and not greater carboxylation efficiency. Leaf-level δ13C for needles formed in 2003 was similar (P=0.73) in both stands (mean thinned = −26.46‰, SE=0.21; mean unthinned = −26.36‰, SE=0.18).
We measured host-tree physiological indicators across more of the growing season in Study II than Study I, and found more variability among months. Differences in gs between thinned and unthinned stands depended on measurement date (treatment × date interaction P=0.002; Fig. 2b). Bonferonni adjusted ANOVA (P≤0.007 level) comparisons showed gs was higher for trees in the thinned stand compared with the unthinned stand from May through September, but not in October (P=0.56) and November (P=0.18), a change we attribute to wet soil conditions and low night time temperatures in both stands in October and November. Differences in Ci between stands also depended on measurement date (treatment × date interaction P=0.001; Fig. 2c). Analyses of individual months (P≤0.007 level) showed higher Ci in trees in the thinned stand than the unthinned stand in May (P=0.003), June (P<0.0001), and September (P<0.0001) with generally, but not significantly, higher Ci in most other months (Fig. 2c). Differences in Pn also depended on measurement date (treatment × date interaction P<0.0001); Pn was higher (P≤0.007 level) in the thinned stand until October (P=0.46) and November (P=0.14) (Fig. 2d). Leaf N concentration was similar between stands (P=0.17; mean thinned: 1.12%, SE=0.04; mean control: 1.19%, SE=0.03), suggesting similar carboxylation efficiency. We also found similar leaf-level δ13C (P=0.79) for thinned and unthinned stands (mean thinned = −24.79‰, SE=0.16; mean control = −24.84‰, SE=0.12) for needles formed in 2004.
Dwarf mistletoe shoot growth
Light response curves
Mistletoe Pn measured in June 2005 was again well below zero at all PPFD levels (Fig. 4). Increasing Pn with increasing PPFD between 0 and 400 μmol/m2/s1 (t-test P=0.007) suggests that mistletoe carbon balance in June included a small amount of CO2 assimilation from the atmosphere at low PPFD. For example, the mean Pn of −4.2 μmol/m2/s1 at PPFD=400 μmol/m2/s1 consisted of 1.2 μmol/m2/s1 of gross photosynthesis that offset a dark respiration rate of 5.4 μmol m2/s1 (Fig. 4). An additional finding from the June 2005 measurements was large temporal variation in CO2 exchange of mistletoe shoots. Mistletoe Pn was more negative in June 2005 than in September 2004 (Fig. 4) at similar PPFD levels (e.g., t-test P=0.008 for PPFD=400 μmol/m2/s1).
Thinning increased host-tree Ψpre, and hence water uptake, in both studies (Figs. 1a, 2a). Increases in Ψpre in both studies were consistent with increases in thinned and thinned and burned ponderosa pine stands compared with unthinned stands on other study sites in northern Arizona (Feeney et al. 1998; Kolb et al. 1998; Skov et al. 2004). Differences in Ψpre between thinned and unthinned stands were more pronounced in Study II than Study I (Figs. 1a, 2a), probably due to lower tree basal area after thinning and greater competitive release in Study II. Peak water stress in unthinned stands was more severe in Study II (minimum Ψpre = −1.9 MPa) than Study I (minimum Ψpre = −1.3 MPa). The lowest Ψpre reported for ponderosa pine in northern Arizona is about −2.0 MPa (Simonin et al. 2005, Skov et al. 2004). Thus, water stress in the Study II unthinned stand was severe for this region. Consistent with our results, the lowest Ψpre in northern Arizona usually occur in early July, after dry spring weather and before the onset of monsoon rains (Kolb and Stone 2000).
Increased water availability in thinned stands increased tree carbon uptake. Tree light-saturated Pn was higher in trees in thinned than unthinned stands throughout most of both studies (Figs. 1d, 2d). Higher water availability likely contributed to higher gs in trees in the thinned stand (Figs. 1b, 2b), which increased Pn as leaf-level N concentration was similar between stands in both studies, implying similar carboxylation efficiency. Leaf gs has been reported to be strongly correlated with Pn in other studies of ponderosa pine, and for other plant species (Wong et al. 1979; Feeney et al. 1998; Skov et al. 2004). The higher Ci measured in trees in the thinned stand in most months further supports higher CO2 availability as the dominant mechanism of higher Pn in the thinned compared with the unthinned stand (Figs. 1c, 2c). Ci was higher in the unthinned stand compared with the thinned stand only in July of Study II, probably due to a limitation on carboxylation potential from severe water stress in the unthinned stand, as mid-day light-saturated Pn was close to zero in this stand in July. The only dates in both studies when leaf gas exchange was similar between thinned and unthinned stands were in October and November of Study II when Ψpre was high (e.g., low water stress) and similar for the thinned and unthinned stand (Fig. 2). Our findings are consistent with previous research that effects of thinning on Pn and gs of ponderosa pine are greatest when Ψpre is lowest (Feeney et al. 1998; Kolb et al. 1998; Skov et al. 2004).
δ13C, a time-integrated measurement of the ratio between Ci and ambient CO2 concentration and hence the ratio between Pn and gs (Farquhar et al. 1989), was not affected by thinning in either year. Similar findings have been reported by other studies of ponderosa pine in northern Arizona, even when thinning increased Pn and gs (Skov et al. 2004; Wallin et al. 2004). Significant increases in ponderosa pine leaf δ13C in northern Arizona have been reported only during extreme droughts that dramatically reduce gs (Adams and Kolb 2004; Wallin et al. 2004). Similar leaf δ13C in thinned and unthinned stands may have been caused by increased soil respiration in the thinned stand (Kaye and Hart 1998) resulting in higher atmospheric 13CO2 concentration in the lower canopy layer where our leaf samples were collected (Brooks et al. 1997; Buchmann et al. 1997; Flanagan and Ehleringer 1998; Fessenden and Ehleringer 2003), or an effect of irradiance on leaf δ13C (Waring and Silvester 1994), as thinning increased irradiance on the lower crown branches used in our study. Another explanation supported by our results in Study I is that thinning increased Pn and gs similarly so that Ci did not change enough during the period of needle development to influence δ13C of the whole leaf tissue.
Our light response curves show that Southwestern dwarf mistletoe provides for little of its carbohydrate needs by direct photosynthesis, and has large seasonal changes in CO2 exchange (Fig. 4). Release of CO2 from mistletoe respiration was much greater than uptake from photosynthesis over a wide range of PPFD levels, resulting in large negative values of Pn. Mistletoe dark respiration rate was 19 to 5 fold greater than gross photosynthesis at low to moderate PPFD (75–400 μmol/m2/s1) in June measurements. Photoinhibition of mistletoe photosynthesis by high PPFD is suggested by higher Pn at 400 PPFD than at 1,200 PPFD in September. More negative Pn of mistletoe in June compared with September suggest considerable seasonal variation in respiration driven by the phenology of mistletoe growth or reproduction. In contrast to the domination of mistletoe shoot carbon balance by respiration, Pn of ponderosa pine was positive at all light levels (Fig. 4), with a light saturation point of 600–800 μmol/m2/s1 PPFD similar to other reports for this species (Kolb and Robberecht 1996; Bond et al. 1999).
Increased uptake of water and carbon by host ponderosa pine trees, caused by forest thinning, stimulated dwarf mistletoe shoot growth. Thinning increased mistletoe shoot growth by an average of 35% (Fig. 3). The interface between the xylem of the dwarf mistletoe endophytic system and host xylem and phloem regulates mistletoe acquisition of resources, as considerable resistance to the movement of solute from host to mistletoe occurs at this interface (Srivastava and Esau 1961; Alosi and Calvin 1985; Davidson et al. 1989). Despite this resistance, supply of growth-limiting resources from host xylem and phloem to mistletoe xylem apparently increased in response to thinning. The identity of these resources from the host is not clear in our study but probably includes carbon-containing compounds such as cyclitols, amino acids, organic acids, and cytokinins that are known to be utilized by mistletoes from the host (Stewart and Press 1990; Kolb 2002).
One possible confounding factor in elucidating the mechanism behind increased dwarf mistletoe growth in the thinned stands is mistletoe carbohydrate storage prior to thinning. Carbohydrate storage in the dwarf mistletoe endophytic system before thinning could reduce dependence of mistletoe on resources from the host tree supplied after thinning. Early studies suggested that carbohydrate acquired by dwarf mistletoes from host xylem sap accumulated primarily in the endophytic system (Rediske and Shea 1961; Hull and Leonard 1964b). However, more recent evidence from A. oxycedri indicated accumulation of most compounds, including carbohydrates, in the aerial shoots of dwarf mistletoe with little accumulation in the endophytic system (Rey et al. 1991). We attempted to eliminate possible effects of mistletoe carbohydrate storage on dwarf mistletoe growth by removing dwarf mistletoe aerial shoots and measuring regrowth from the endophytic system, and by using trees of similar size and DMR and using tree DBH as a covariate in analysis of mistletoe regrowth. This experimental approach clearly showed greater dwarf mistletoe growth on trees in thinned compared with unthinned stands.
Another possible explanation for increased mistletoe shoot growth in the thinned stands is a difference in temperature between thinned and unthinned stands, as tree removal could alter microclimate. The stimulation of mistletoe growth in the thinned stand may have occurred because of warmer temperatures that increased rates of synthesis and expansion of cells of dwarf mistletoe aerial shoots. However, this explanation is unlikely considering the fact that restoration thinning projects similar to those in our study have had little effect on air temperature within a stand (Meyer et al. 2001). It is also possible that mistletoes grew more in the thinned than the unthinned stands because thinning increased tissue water potential of both mistletoe and its host, and thus reduced constraints on mistletoe growth from water stress.
Our findings show that dwarf mistletoes exhibit substantial plasticity in short-term growth which is linked to host physiological condition and resource uptake. We found that increases in water availability and carbon uptake by host trees stimulated mistletoe growth in the lower portion of the tree canopy. Our findings are limited to the lower portion of the canopy as we did not measure mistletoe growth in the mid- and upper-levels of tree canopies. However, our results are similar to a report from New Mexico for the same species used in our study that stand thinning increased dwarf mistletoe infection over the entire canopy of individual trees compared with an unthinned stand (Conklin 2003). The effects of thinning on resource availability to host trees are probably greatest in the first year or two after thinning, as dominance and resource use by herbaceous species and other understory plants increases in subsequent years (Covington et al. 1997; Moore et al. 2005). Long-term effects of changes in host-tree physiological condition by thinning on dwarf mistletoe growth and reproduction are unknown. Increased resources immediately after thinning may stimulate growth of the mistletoe endophytic system in the short term and increase resource acquisition from host trees in the future. Increased competition with understory plants and remaining trees several years after thinning could diminish resources available to host trees and mistletoes for future growth. Or, tree height growth and crown expansion may be stimulated by thinning more than dwarf mistletoe expansion, resulting in a decrease in long-term tree- and stand-level infection (e.g., Roth and Barrett 1985).
Our finding of increased parasitic plant growth on more vigorous host trees shown by an experiment approach is contrary to a report of greater occurrence of A.divericatum on P. edulis growing on high stress compared with low stress sites in Arizona shown using a descriptive, non-experimental approach (Mueller 2004). These seemingly contradictory results may be due to differences in the measured mistletoe responses. Greater mistletoe occurrence in a stand implies greater mistletoe establishment and survival, which is different than greater mistletoe growth per branch, the variable we measured. Consistent with our results, biomass of Melampyrum pretense, a root parasite, increased on host Pinus sylvestris trees grown with ectomycorrhizal fungi that increase tree nutrient uptake (Allen 1991) compared with trees grown without ectomycorrhizae (Salonen et al. 2000). Similarly, growth of Rhinanthus minor, a hemiparasitic plant, was greater when its host, Lolium perenne, was colonized with arbuscular mycorrhizal fungi (Davies and Graves 1998). These parallel findings suggest that growth of many parasitic plants may be linked to changes in host physiological condition induced by a variety of factors that affect host resource uptake such as competition and mycorrhizae.
In conclusion, growth of the parasitic plant dwarf mistletoe (A. vaginatum subsp. cryptopodum) is responsive to the physiological condition of the host tree (P. ponderosa) similar to the stimulation of growth of a non-parasitic plant by an increase in the supply of a limiting soil resource. The linkage between host-tree physiological condition and dwarf mistletoe performance in our study suggests that changes in resource uptake of host trees by anthropogenic activities (e.g., forest management, air pollution) or by more natural disturbances (e.g., wildfire, insect outbreaks) may have secondary effects on obligate parasitic plants which may ripple through the ecosystem given the keystone status of mistletoes in many forests and woodlands (Watson 2001).
Funding was provided by Mission Research Program, School of Forestry, Northern Arizona University (McIntire-Stennis/AZ Bureau of Forestry) and the USDA Rocky Mountain Research Station JVA (RJVA 00-JV-11221006-210) between B. Geils and T. Kolb. We thank Shawn Faiella, Megan Van Horne, Michelle Schaffer, Natacha Guerard, and Dan Koepke for help in conducting the study, Becky Mueller, Kitty Gehring and two anonymous reviewers for their comments on the manuscript, and the NAU Centennial Forest and Coconino National Forest for use of study sites. The experiments described in this paper comply with the current laws of the United States, where the experiments were performed.