1 Restoration Strategies for a Native Perennial: Germination and Seedling Physiology of Sphaeralcea Munroana A Thesis Presented in Partial Fulfillment of the Requirements for the Degree of Master of Science with a Major in Forest Resources in the College of Graduate Studies University of Idaho by Olga A. Kildisheva May 4, 2011 Major Professor: Anthony S. Davis 2 AUTHORIZATION TO SUBMIT THESIS This thesis of Olga A. Kildisheva, submitted for the degree of Master of Science with a major in Forest Resources and titled “Restoration Strategies for a Native Perennial: Germination and Seedling Physiology of Sphaeralcea Munroana” has been reviewed in final form. Permission, as indicated by the signatures and dates given below, is now granted to submit final copies to the College of Graduate Studies for approval. Major Professor ______________________________Date______________ Anthony S. Davis Committee Members _______________________________Date______________ R. Kasten Dumroese ________________________________Date______________ James L. Kingery Department Administrator________________________________Date______________ Jo Ellen Force Discipline's College Dean________________________________Date_______________ Kurt S. Pregitzer Final Approval and Acceptance by the College of Graduate Studies _______________________________Date_______________ Nilsa A. Bosque-Pérez 3 Abstract The Great Basin region of the western United States has undergone significant disturbance and fragmentation because of overgrazing for livestock production, disruption of the natural fire regimes, and the introduction of non-native species. At present, habitat loss greatly surpasses the rate of system recovery, making restoration integral to ecosystem function and resilience. To date, restoration research and practice have focused largely on keystone plant species, however, to be effective, restoration must include myriad plant forms and guilds. Munro’s globemallow (Sphaeralcea munroana (Douglas) Spach) is a perennial, cool-season forb, endemic to the Great Basin that serves as an important host for native pollinators, provides soil stabilization, and is a source of food for numerous mammals. For these reasons, as well as its ability to tolerate disturbance, temperature extremes, and drought, it is an important candidate for broad scale ecosystem restoration across its native range. Little information regarding seed germination and seedling establishment is available for Munro’s globemallow, and what does exist is synthesized in the first chapter of this thesis. The second chapter is a detailed examination of the seed dormancy mechanisms. The results of 4 experiments identified physical dormancy, which inhibits water imbibition, to be responsible for poor germination. Seed coat scarification is essential for germination and can be achieved through mechanical or boiling water scarification. The third chapter of this thesis describes an experiment conducted to evaluate a suite of morphological and physiological responses of Munro’s globemallow to a range of temperature and moisture conditions during seedling establishment. Results indicate that seedlings are able to tolerate drought and relative high temperature conditions early in their establishment, however, low temperatures substantially limited seedling development; thus, a later sowing date may optimize plant establishment. Overall, nursery production, seed increase projects, and outplanting success of Munro’s globemallow should be improved through the incorporation of the results of this thesis. 4 Acknowledgements This project would not have been possible without the financial support from the Idaho Transportation Department, the Great Basin Native Plant Selection and Increase Project, the University of Idaho Seed Grant Program, and the University of Idaho Center for Nursery and Seedling Research. In particular, I’m grateful to Cathy Ford and Nancy Shaw, who saw merit in this research direction and worked to facilitate funding. I thank my major professor, Dr. Anthony S. Davis for encouraging me to work independently, pushing me to achieve my goals, and always being only an email away. I extend my thanks to Dr. Kas Dumroese for his editorial support, direction, and practical wisdom. I also thank Dr. Jim Kingery for introducing me to intermountain flora and sharing with me a bounty of stories. I’m grateful to Timothy Johnson for his statistical support, Nalin Suranjith GamaArachchige for his assistance in electron microscopy, as well as Nancy Shaw, Matt Fisk, and Erin Denney for aiding with seed collection. I’m obliged to everyone at the Pitkin Forest Nursery for teaching me the ways of nursery management and for their help during the course of my education at the University of Idaho. I extend my gratitude to Rob Keefe for sparking my interest in seed ecology. I would also like to thank Emily Overton, Bridget McNassar, Sasha Podolak, Jake Kleinknecht, Eric Creeden, Sara Ashkannejhad, Amy Whitcomb, and Jen Lennon for their research involvement, humor, and camaraderie. I offer my sincere gratitude to Matthew Aghai for always being the voice of reason and for his endless support through this process. Finally, I’m grateful to my parents for their whole-hearted encouragement. 5 Table of Contents Title Page i Authorization to Submit Thesis ii Abstract iii Acknowledgements iv Table of Contents v List of Tables vii List of Figures viii Chapter One Sphaeralcea munroana: Restoration Potentials and Challenges General Introduction 1 Species Overview 2 Seed Dormancy 3 Temperature and Moisture as Limiting Factors to Seedling Development 9 Conclusions 12 Literature Cited 13 Chapter Two Seed Coat Morphology, Physical Dormancy, and the Use of Scarification for Dormancy Break in Sphaeralcea munroana Abstract 19 Introduction 20 Materials and Methods 25 Statistical Analysis 27 Results 28 Discussion 31 Conclusions 34 6 Literature Cited Chapter Three 35 Individual and Synergistic Influence of Temperature and Moisture on Sphaeralcea munroana Seedling Growth Abstract 44 Introduction 45 Materials and Methods Plant Establishment 47 Temperature and Moisture Treatments 47 Statistical Analysis 49 Results 49 Discussion 50 Conclusions 53 Literature Cited 54 Appendix A 67 Appendix B 68 7 List of Tables Chapter Two Table 2.1. The effects of mechanical scarification, soaking duration in GA3, or pure water solution on the germination behavior of Sphaeralcea munroana at the end of the 21-d observation period. Parameter values were generated using a non-linear regression model (Equation 2.2), where G (t) is the cumulative germination percentage at time (t) expressed in days (d), Gc is cumulative germination, or the germination asymptote at the end of the testing period (%), GC50 is the time (d) required to reach 50% germination, and Gl is the time (d) until first germination. Multiple comparisons were obtained using Tukey’s HSD (α = 0.05). 38 Table 2.2. The effects of “non-traditional” scarification techniques on the germination behavior of Sphaeralcea munroana at the end of the 21-d observation period. Parameter values were generated using a non-linear regression model (Equation 2.1), where G (t) is the cumulative germination percentage at time (t) expressed in days (d), Gc is cumulative germination, or the germination asymptote at the end of the testing period (%), GC50 is the time (d) required to reach 50% germination, and Gd is the germination rate (% /d). Multiple comparisons were obtained using Tukey’s HSD (α = 0.05). 38 Chapter Three Table 3.1. Sphaeralcea munroana seed collection sites. 56 Table 3.2. Results of the mixed model analysis for the effects of temperature, moisture, and their interaction on the morphological and physiological responses of Sphaeralcea munroana seedlings 35 d after sowing. 56 Appendix B Table 3.3. Sphaeralcea munroana gas exchange responses to 2 temperature and 4 moisture regimes 35 d after sowing. 68 8 List of Figures Chapter One Figure 1.1. General outline of the Great Basin region of the western United States. 18 Chapter Two Figure 2.1. Scanning electron micrographs of a Sphaeralcea munroana seed; (A) top view of the chalazal region of a dormant seed showing the chalazal slit; (B) formation of water gap following dormancy break; (C) the underside of the dislodged cap-like blister covering the water gap; (D) palisade cells of the cap-like structure. Abbreviations: Chsl, chalazal slit; Chsl*, remaining part of the chalazal slit after dormancy break; Ll, light line; Mi, micropyle; Mt, maternal tissue; Pa, palisade; Spl, subpalisade cells; Wg, water gap. 39 Figure 2.2. Mass increase percentage (on a fresh mass basis) of control, mechanically, and boiling water scarified seeds of Sphaeralcea munroana during a 24-hr incubation. Each point scatter represents the mean (±s.e.) of 10 replicates. Different letters indicate significant differences (p < 0.05) at the end of the 24-hr period. 40 Figure 2.3. Cumulative germination percentage of Sphaeralcea munroana seed subject to 4 seed treatments during a 21-d observation period. Each line represents the mean (±s.e.) response of 5 replicates. Different letters indicate significant differences between treatments. 41 Figure 2.4. Germination capacity of Sphaeralcea munroana seeds 21 d following exposure to 8 treatments. Each bar represents the mean (±s.e.) of 5 replicates. Different letters indicate significant differences (α = 0.05). 42 Cumulative germination percentage of Sphaeralcea munroana seeds subject to 6 treatments during a 21-d observation period. Each line represents the mean (±s.e.) response of 5 replicates. Different letters indicate significant differences between treatments. 43 Figure 2.5. Chapter Three Figure 3.1. Number of true leaves (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 57 9 Figure 3.2. Total leaf area (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 58 Figure 3.3. Aboveground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 59 Figure 3.4. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 60 Figure 3.5. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 61 Figure 3.6. Root-to-shoot ratios (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 62 Figure 3.7. Total leaf area (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 63 Figure 3.8. Aboveground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 64 Figure 3.9. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 65 10 Figure 3.10. Root to shoot ratios (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 66 Appendix A Figure 3.11. Light response curves of photosynthetic carbon fixation measured on individual leaves of 5 mature Sphaeralcea munroana plants at the University of Idaho Shattuck Arboretum. Measurements were made between 1000 and 1300 on 02 October 2011 using an LI-6400 Portable Photosynthesis System (Li-Cor, Inc., Lincoln, NE). Constant chamber CO2 (400 μmol mol-1), temperature (20±0.16° C), and relative humidity (79±0.58%) were maintained to avoid confounding the assimilation response. The initial leaf equilibration was set to high photon flux density (2000 μmol quanta m-2s-1), followed by subsequent light decreases in steps of 200 μmol quanta m-2s-1, until a negative photosynthetic rate was reached. Each point represents a mean±s.e. of 5 replicates. 67 11 Chapter 1: Sphaeralcea munroana: Restoration Potentials and Challenges General Introduction The arid-steppe of North America’s Great Basin is delineated by the Colorado and Columbia Plateaus, the Sierra Nevada Mountains, and the Mojave Desert (Figure 1.1.). The region’s unique geomorphology has a considerable effect on the climate, which is dominated by temperature extremes and low, primarily winter, precipitation (Knapp, 1996). The vegetative communities of this area are characterized by the presence of shrubs, perennial bunchgrasses, and forbs (Holmgren, 1972). As an ecological unit, the Great Basin has suffered from substantial disturbance and fragmentation due to overgrazing, shrub removal, and non-native species introduction (Mack, 1981). Decades of natural fire suppression and the aggressive spread of cheatgrass (Bromus tectorum) have been linked to a 4 to 10 fold increase in fire incidence in the course of the last century (D'Antonio and Vitousek, 1992). Frequent fires have promoted an extensive system conversion from sagebrush- to annual grass-dominated communities, which has reduced the available soil moisture, promoted nutrient depletion, and intensified resource competition (Billings, 1990;Whisenant, 1990; D'Antonio and Vitousek, 1992; Obrist, et al., 2003). By recent estimates, the rate of habitat loss greatly surpasses the rate of system recovery, further jeopardizing the populations of sagebrushsteppe obligates, such as pygmy rabbit (Brachylagus idahoensis), greater sage-grouse (Centrocercus urophasianus), and Brewer’s sparrow (Spizella breweri) (Wisdom et al., 12 2005). The predicted rise in CO2 has been projected to enhance biomass production of C3 annual grasses, which could further exacerbate ecosystem conversion (Smith et al., 1987, Smith et al., 2000; Grunzweig and Korner, 2001). Thus, the use of endemic plant species is critical in promoting ecological recovery. Herbaceous perennials comprise a substantial portion of the Great Basin floristic communities and are an integral component of these systems. The use of native species in restoration is optimal because they are evolutionarily adapted to withstand severe climate conditions, provide long-term soil stabilization, and foster habitat biodiversity. Despite the importance of their role, the use of forbs in habitat restoration is relatively novel and largely unexplored (Parkinson, 2008). One such species, Sphaeralcea munroana (Douglas) Spach) (Malvaceae), is a desirable candidate for revegetation; however, its use is constrained by the lack of information regarding the species requirements for successful germination and establishment. Species Overview Munro’s globemallow is a cool-season herbaceous perennial endemic to the Great Basin. Plants initiate growth from a caudex in the form of multiple, unbranched stems, typically reaching 20 to 80 cm in height. Showy, orange inflorescences are produced from May to August. Subsequent seeds are arranged in a schizocarp, composed of 10 to 12 mericarps that form a ring, each containing 1 to 2 pubescent seeds 1.5 mm in length (Rydberg, 1917; Lyons, 1995). S. munroana is able to establish on disturbed sites and survive drought and temperature extremes. In addition to its resilience, this plant is an essential 13 forage source for numerous rodents, lagamorphs, and ungulates (Beale and Smith, 1970; Pendery and Rumbaugh, 1986; Rumbaugh et al,. 1993; Pavek, et al. 2011). Furthermore, it provides nutrition for 20 generalist and 3 specialized (Diadasia diminuta, D. lutzi, and Colletes sphaeralcea) bee species (Cane, 2007). These attributes have made S. munroana an important candidate for broad scale restoration across its native range. Seed dormancy, however, severely limits in and ex situ germination of S. munroana. Few studies explore the dormancy mechanisms and methods for dormancy break in the Sphaeralcea genus (Page, et al. 1966; Roth et al., 1987). Moreover, little is known about seedling tolerance to temperature and moisture stress. Ehleringer and Cooper (1998) suggest that S. ambiuga, native to the Mojave Desert, is “a short-lived, opportunistic species that establishes during wet years but demonstrates higher mortality during dry years due to relatively low water use efficiency”. It is unclear if this life strategy is shared by Sphaeralcea munroana. Plant establishment is the most critical phase in determining future survival and persistence (Harper, 1977); thus, seedling post-germination responses to temperature and moisture stress are important and must be specifically addressed. Seed Dormancy Dormancy is characterized by Vleeshouwers et al. (1995) as “a seed characteristic, the degree of which defines what conditions should be met to make the seed germinate”. This is an evolutionary response to temporal variation in environmental conditions, which allows for different species to be favored over time (Rees, 1996). Several types of dormancy exist and are defined based on the mechanisms that prevent germination. 14 Physical dormancy is common among desert species (including several in the Sphaeralcea genus) and is thought to have developed to prolong seed longevity (Page et al., 1966; Sabo et al., 1979; Roth et al., 1987; Baskin and Baskin, 1998; Smith and Kratsch, 2009). Physically dormant seeds often possess a palisade layer of lignified cells that prevent water entry into the seed (Corner, 1951; Vazquez-Yanes and Perez-Garcia, 1976). Water imbibition is critical because it drives seed expansion (necessary for germination) and is dependent on the interaction between the growth potential of the embryo and the constraints imposed by the seed coat (Kucera et al., 2005). Imbibition in many seeds with physical dormancy is regulated by a specialized anatomical structure, defined as the “water gap”, which is located within the seed coat. The water gap becomes permeable when exposed to temperature flux, drying, or scarification, thus allowing imbibition into an otherwise impermeable seed (Baskin and Baskin, 1998; Baskin et al., 2000; Baskin, 2003). The location, anatomy, and morphology of the water gap demonstrate intra- and extra-family variability (Baskin et al., 2000). The chalazal region is a critical site for water entry in a number of Malvacea species, including Abelmoschus esculentus, Gossypium hirsutum, and Sida spinosa (Christiansen and Moore, 1959; Egley and Paul, 1981; 1982; Serrato-Valenti et al., 1991). In these species the water gap is obstructed by 2 tissue types. Maternal tissue forms a cap that project downward into the chalazal slit and mesophyll tissue projects upward. At the initiation of dormancy break, a section of these tissues that radially surround the chalazal slit) become partially permeable and allow imbibition, which leads to a separation of the palisade and subpalisade layer of cells causing the formation of a blister (Serrato-Valenti et al., 1991). 15 Once water surrounds the entire palisade layer of the seed coat, the mesophyll cracks, allowing the upper portion of the palisade cells to continue swelling. This process eventually causes a detachment of the blister roof, allowing for full imbibition (SerratoValenti et al., 1991). Natural phenomena, such as abrasion by sand and stones (in rapidly moving washes during periods of flooding), temperature fluctuations, fires, and animal digestion are thought to alleviate physical dormancy (Went, 1955; Gutterman, 1993; Baskin and Baskin, 1998). A number of ex situ techniques, primarily chemical and mechanical scarification, have been used to promote germination of physically dormant seeds (Page et al., 1966; Roth et al., 1987; Hoffman et al., 1989; Baskin and Baskin, 1998). For example, Page et al. (1966) observed 30 to 40% germination of S. grossulariifolia following submergence in sulfuric acid, a substantial improvement compared to the control (0%). Similarly, submergence of Sphaeralcea seeds in 18 M sulfuric acid for 10 min improved germination of S. coccinea and 2 accessions of S. grossulariifolia compared with the control (77, 69, 62% versus 5, 14, and 32%, respectively), but failed to do so for S. munroana (8%) relative to the control (2%)(Roth et al., 1987). Additionally, organic solvents have been used to promote germination of physically dormant seeds. A 4-hr submergence in diethyl dioxide improved germination of S. grossulariifolia to 67% compared with 0% reported for untreated seeds (Page et al., 1966). Roth et al. (1987) also found a 3-hr submergence of S. coccinea, S. munroana, and 2 accessions of S. grossulariifolia in diethyl dioxide significantly enhanced germination compared with the control (36, 53, 89, and 68% versus 5, 2, 14, and 32%, respectively). 16 Despite the effectiveness of chemical scarification, chemicals can be hazardous, difficult to obtain, and present serious health risks (Mallinckrodt Baker, 2008 a, b). As a result, alternative methods of seed treatment may be superior. Another technique for improving imbibition of impermeable seeds is immersion in hot water. Boiling water improved seed permeability of several Malvaceae species, presumably by unblocking the water gap (Christiansen and Moore, 1959; Baskin and Baskin, 1997). For example, seeds of Iliamna corei (Malvaceae) germinated to 93% (as compared to 0% germination of the control), following a 5-sec submergence in boiling water (Baskin and Baskin, 1997). Higher germination has also been achieved by mechanical scarification. Seeds of I. corei germinated to 100% following manual scarification with a single edge razor blade (Baskin and Baskin, 1997). The International Seed Testing Association (ISTA, 1976) rules suggest scarification with a file to be a successful measure for relieving dormancy in Althaea officinalis and A. rosea (Malvaceae). Although effective, these techniques are time consuming and unrealistic for use as operational seed treatments. A number of mechanical scarification methods designed for treating large seed quantities exist; however, few have proven to be successful in alleviating dormancy in Sphaeralcea species. Primarily a result of scarification severity, embryo damage often overshadows the dormancy-breaking effects of the treatment. Page et al. (1966) report decreases in germination of S. grossulariaefolia with the duration of scarification time in a sandpaperlined rotating drum, while Roth et al. (1987) suggest that seeds of S. grossulariaefolia, S. 17 coccinea, and S. munroana perished following mechanical scarification, irrelevant of treatment duration. More recently, rotating rock tumblers filled with abrasive media have been used to promote germination of some physically dormant species and provide a potential alternative to traditionally used scarification techniques (Dreesen, 2004). Unfortunately, I found no information regarding the effects of tumbling on the germination behavior of Sphaeralcea munroana. Traditionally used chemical and mechanical scarification techniques are effective, but these methods are hazardous and can result in severe embryonic damage. Thus, other alternatives are needed in order to promote the effective use of S. munroana in restoration. To meet that need, other less traditional techniques, such as fire and heating treatments, may be employed to effectively induce permeability in physically dormant seeds. For example, I. corei demonstrated increased germination following simulated annual summer burning (1 to 2 min), with the highest germination achieved after 6 years (39 ± 6%) compared with the control (0%)(Baskin and Baskin, 1997). Moreover, physically dormant seeds of 8 Fabaceae species germinated to a greater extent after being ignited with a torch (Sugii, 2003). In some cases, dry heat may be a substitute for fire, often achieving better results. For example, Baskin and Baskin (1997) found that several dry heat temperatures and exposure durations optimized the germination of I. corei. Although physical dormancy has been documented in a number of Malvaceae species, reported germination of Sphaeralcea munroana has failed to exceed 53% following scarification, even when dormancy is presumably broken (Roth et al., 1987; Smith and 18 Kratsch, 2009). Thus, it is unclear whether the seeds of this species have additional dormancy types. Physiological dormancy, characterized by the presence of chemical inhibitors that prevent embryonic growth, is commonly found in cold desert herbaceous perennials, and can be relieved by stratification (Baskin and Baskin, 1998). Gibberellic acid (GA3) has successfully served as a proxy for stratification for a number of physiologically dormant species (Timson, 1966; Pinfield et al., 1972). The exogenous application of GA3 is thought to enhance germination by increasing the growth potential of the embryo and by overcoming the mechanical constraints that prevent radical emergence (Karssen et al., 1989; Hilhorst and Karssen, 1992; Hilhorst, 1995; Bewley, 1997; Koornneef et al., 2002; Leubner-Metzger, 2003). In addition, exogenous application of GA3 alone, or in combination with scarification, significantly amplified the germination capacity of several species in the Cactaceae, including Cereus spp., Echinocactus grusonii, Leuchtenbergia principis, Sclerocactus mariposensis, and Harrisia fragrans (Krulik, 1981; Moreno et al., 1991; De La Rosa-Ibarra and Garcia, 1994; Dehgan and Perez, 2005). Although most physically dormant species do not exhibit additional dormancy, some do, including several members of Malvaceae (Baskin and Baskin, 1998). The coupling of physical and physiological dormancy is termed combined dormancy and requires both types to be broken for germination to occur (Nikolaeva, 1969; Baskin and Baskin, 1998). Dunn (2011) reports increased germination of Sphaeralcea ambigua and S. coccinea (to 45.3 and 85.3% relative to the control 18.0 and 4.7%, respectively) following a 30-d stratification of scarified seeds. Similarly, Smith and Kratsch (2009) report that following 19 the mixture of scarification and a 6-wk stratification, seeds of S. grossulariifolia, S. parvifolia, and S. munroana germinated to a greater extent than from either treatment alone, suggesting that seeds of S. munroana may also exhibit combined dormancy. Temperature and Moisture as Limiting Factors to Seedling Development In regions where the growing conditions are restrictive, plant establishment is the most vulnerable stage in vegetative community development (Call and Roundy, 1991). In the arid-steppe ecosystem, wide diurnal temperature fluctuations, episodic precipitation pulses, and extensive droughts impose key restraints to post-germination survival. The maximum temperature and soil moisture changes occur in close proximity to the soil surface, making seedlings more susceptible to environmental fluxes than mature plants (Bazzaz and Mezga, 1973; Raynal and Bazzaz, 1973; Regehr and Bazzaz, 1976). Thus, opportunities for plant establishment in the Great Basin are strongly limited by the environmental conditions. Diurnal temperature can vary by 20 °C, while seasonal differences can be on the order of 40 °C (Smith and Nowak, 1990). These oscillations can be further enhanced throughout the year by the topography-induced nocturnal cold aid drainage (Osmond et al., 1990). The Great Basin-Mojave region is described as the most arid habitat in North America, with annual precipitation averaging 50 to 300 mm. Due to low humidity and abundant irradiance the potential evapotraspiration in this region is high, ranging between 1100 mm in the northern and 2000 mm in the southern portion of the basin (Flaschka et al., 1987). On an inter-annual basis, summer precipitation is highly variable, typically 20 representing only 20 to 30% of total annual precipitation (Bell, 1979). A strong disparity exists between maximum water availability and the ability of plants to use it, because a substantial portion of available moisture is considerably reduced by the time air and soil temperatures become suitable for plants to be fully physiologically active (Caldwell, 1985). The interaction between precipitation and temperature patterns bear considerable implications on the physiological ecology of the native floristic communities. The beginning of the growing season in this region is directly correlated with the amount of winter-spring precipitation and the rise in air and soil temperatures (Turner and Randall, 1987). The seasonal reduction in rainfall amplifies the importance of the spring growing season; as a result, most species initiate growth in March and April, when maximum daily temperatures range from 5 to 15 °C and night temperatures remain near freezing (Thornthwaite, 1948; Comstock and Ehleringer, 1992). Furthermore, maximum temperature and soil moisture changes occur in close proximity to the soil surface, which limit seedling establishment following disturbance (Bazzaz and Mezga, 1973; Raynal and Bazzaz, 1973; Regehr and Bazzaz, 1976). Plant photosynthetic rates demonstrate substantial temperature dependence. At low temperatures photosynthetic rates are reduced due to the decline in the enzyme-catalyzed reaction rates. As temperatures rise, carbon assimilation rises, until a maximum (defined as a “temperature optimum”) is reached, and declines once the optimum has been exceeded (Comstock and Ehleringer, 1992). The maximum photosynthetic rates exhibit considerable variability, and are primarily governed by environmental conditions. At the beginning of the growing season, when day-time temperatures do not exceed 20 °C, the 21 temperature optimum form many Great Basin shrubs is 15 °C, increasing by 5 to 10 °C later in the season (Caldwell, 1985). The maximum CO2 assimilation rates of shrubs native to this region, under natural or irrigated conditions, range from 14 to 19 µmol CO2 m-2 s-1 (Depuit and Caldwell, 1975; Caldwell et al., 1977). At this time, most research has focused on examining the photosynthetic behavior of perennial shrubs, with little attention given to herbaceous species. However, the phenological cycles of herbaceous and woody perennials are different, and may be expresses through variation in photosynthetic behavior. The increasing prominence of native forbs in restoration requires a clear understanding of the physiological ecology of these species. Furthermore, outside agricultural research, knowledge regarding the photosynthetic behavior of members of the Malvaceae family is lacking. In a cultivation setting, Sida spinosa, Gossypium herbaceum, and Gossypium arboreum (Malvaceae), demonstrate relatively high CO2 compensation points that are associated with large net CO2 fixation and faster growth rates (Chen et al., 1970). In the Great Basin, however, rapid growth rates can create severe internal moisture deficits, making the ability of plants to effectively regulate moisture loss imperative. In general, low spring temperatures allow for higher water use efficiency as cold soils reduce leaf conductance, but the freezing night temperatures prevent the full reduction in stomatal opening during the day, when moisture loss is high (Smith and Novak, 1990). As soil moisture deficits increase with seasonal warming, plant water content declines resulting in a lower turgor pressure. Under these conditions, turgor-dependent processes 22 such as leaf expansion and root elongation are suppressed. Decreases in turgor have been linked to reductions in aboveground plant area and overall growth rates (Taiz and Zeiger, 2006). Moisture restrictions cause a greater portion of photosynthates to be distributed to the root system, promoting belowground biomass production. Thus, root-to-shoot ratios (R:S) are a direct result of a dynamic equilibrium between water uptake and photosynthesis (Taiz and Zeiger, 2006). R:S of desert perennials exhibit considerable variability among species, ranging from 0.15 to 6.77, with high R:S values characteristic of plants in the northern Great Basin as compared to a much lower ratios for plants found in the Mojave and Sonoran Deserts (Barbour, 1973; Caldwell et al., 1977). Most research has characterized mature perennial shrub and grass species, while little is known about growth dynamics of forbs, especially shortly following establishment. Conclusions Considering the rate of habitat degradation in the Great Basin, revegetation with native plants is integral to ecosystem function and resilience. Munro’s globemallow is a species with a high restoration potential; but its use is limited by the failure to achieve successful in and ex situ germination as a result of seed dormancy. Furthermore, wide diurnal temperature fluctuations, episodic precipitation pulses, and extensive droughts pose key constraints to post-germination survival. Effective use of S. munroana depends on a clear understanding of dormancy mechanisms and seedling response to environmental stress following germination. 23 Literature Cited Barbour, R. V. and J. C. Petersen. 1973. Desert dogma re-examined: root/shoot ratios, productivity and plant spacing. American Midland Naturalist. 89:41-57. Baskin, C. C. 2003. Breaking physical dormancy in seeds - focussing on the lens. New Phytologist 158:229-232. Baskin, C. C. and J. M. Baskin. 1998. Seeds: Ecology, biogeography and evolution of dormancy and germination. Academic Press, San Diego, California, USA. Baskin, J. M. and C. C. Baskin. 1997. Methods of breaking seed dormancy in endangered species Iliamna corei (Sherff) (Malvaceae), with special attention to heating. Natural Areas Journal 17:313-323. Baskin, J. M. and C. C. Baskin. 2000. Evolutionary considerations of claims for physical dormancy-break by microbial action and abrasion by soil particles. Seed Science Research 10:409-413. Baskin, J. M., C. C. Baskin, and X. Li. 2000. Taxonomy, anatomy and evolution of physical dormancy in seeds. Plant Species Biology 15:139-152. Bazzaz, F. A. and D. M. Mezga. 1973. Primary productivity and microenvironment in an Ambrosia dominated old field. American Midland Naturalist 90:70-78. Beale, D. M. and A. D. Smith. 1970. Forage use, water consumption, and productivity of prongron antelope in western Utah. Journal of Wildlife Management 34:570-578. Bell, F. C. 1979. Precipitation. 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Zeiger. 2006. Plant physiology. 4th edition. Sinauer Associates Inc., Sunderland, Massachusets, USA. Thornthwaite, C. W. 1948. An approach toward a rational classification of climate. Geographical Review 38:55-94. Timson, J. 1966. Germination of Polygonum convolvulus L. New Phytologist 65:423428. Turner, F. B. and D. C. Randall. 1987. The phenology of desert shrubs in Southern Nevada. Journal of Arid Environments 13:119-128. Vazquez-Yanes, C. and B. Perez-Garcia. 1976. Notas sobre la morfologia y la anatomia de la testa de las semillas de Ochroma lagopus Sw. Turrialba 26:310-311. Vleeshouwers, L. M., H. J. Bouwmeester, and C. M. Karssen. 1995. Redefining seed dormancy: An attempt to integrate physiology and ecology. Journal of Ecology 83:1031-1037. Went, F. W. 1955. The ecology of desert plants. Scientific American 192:68-75. Whisenant, S. G. 1990. Posfire population dynamics of Bromus japonicus. American Midland Naturalist 123:301-308. Wisdom, M. J., Rowland, M. M., and Suring, L.H. 2005. Habitat threats in the sagebrush ecosystem: methods of regional assessment and applications in the Great Basin. Allen Press, Lawrence, Kansas, USA. 28 Figure 1.1. General outline of the Great Basin region of the western United States. 29 Chapter Two: Seed Coat Morphology, Physical Dormancy, and the Use of Scarification for Dormancy Break in Sphaeralcea munroana Seeds Abstract The results of a series of experiments involving a variety of dormancy-breaking treatments indicate that Sphaeralcea munroana seeds are physically dormant, possess a water gap responsible for water uptake, and that dormancy is best relieved by mechanical or boiling water scarification. Mechanical scarification resulted in the highest water uptake (86% ) compared to boiling water scarification (22%), and the control (12%), suggesting that boiling resulted in only partial water gap opening. Exogenous application of GA3 and stratification failed to enhance germination compared with scarification alone, indicating an absence of additional dormancy types. These results should improve the usefulness of this cool-season perennial for restoration in the Great Basin, where its effectiveness in soil stabilization, tolerance of disturbed sites, drought, extreme temperatures, and importance as a food source for myriad animals makes it an important species. 30 Introduction Munro’s globemallow (Sphaeralcea munroana (Douglas) Spach) (Malvaceae), a perennial, cool-season forb endemic to the Great Basin, is an important candidate for broad-scale ecosystem restoration across its native range. It serves as an important host for native pollinators, provides soil stabilization, and is a source of food for myriad mammals (Beale and Smith, 1970; Pendery and Rumbaugh, 1986; Rumbaugh et al., 1993; Pavek et al., 2011). In addition, the species is commonly found on disturbed sites and is able to tolerate drought and extreme temperature conditions. Currently, the lack of successful in and ex situ germination due to seed dormancy limits its use in restoration. Few sources explore the dormancy mechanisms and methods that induce germination in the Sphaeralcea genus (Page et al., 1966; Roth et al., 1987). Dormancy is described as “a seed characteristic, the degree of which defines what conditions should be met to make the seed germinate” (Vleeshouwers et al., 1995). Several types of dormancy exist and are characterized based on the mechanisms that prevent germination. Physically dormant seeds have a palisade layer of lignified cells that prevent water imbibition (Corner, 1951; Vazquez-Yanes and Perez-Garcia, 1976). Although a number of species in the Sphaeralcea genus have been observed to benefit from scarification, the cause of dormancy has not been examined directly (Page et al., 1966; Sabo et al., 1979; Roth et al. 1987; Smith and Kratsch, 2009). In these species, imbibition (critical for germination) is regulated by a water gap structure located within the seed coat. The water gap can become permeable following exposure to temperature 31 flux, drying, or scarification, thus allowing imbibition into an otherwise impermeable seed (Baskin and Baskin, 1998; Baskin, 2003; Baskin et al., 2000). Ex situ, chemical and mechanical scarification have been used to improve germination of physically dormant seeds (Page et al., 1966; Roth et al., 1987; Hoffman et al., 1989; Baskin and Baskin, 1998). For example, Page et al. (1966) reported increased germination (30 to 40%) of S. grossulariifolia after submergence in sulfuric acid, a substantial improvement compared to the control (0%). Similarly, submergence of Sphaeralcea seeds in 18 M sulfuric acid for 10 min improved germination of S. coccinea and 2 accessions of S. grossulariifolia relative to the control (77, 69, 62% versus 5, 14, and 32%, respectively), but failed to do so for S. munroana (8%) compared to the control (2%)(Roth et al., 1987). Organic solvents have also been used to promote germination of physically dormant seeds. Page et al. (1966) reported 67% germination of treated S. grossulariifolia seeds following a 4-hr submergence in diethyl dioxide versus 0% germination of untreated seeds. Roth et al. (1987) found a 3-hr submergence of S. coccinea, S. munroana, and 2 accessions of S. grossulariifolia in diethyl dioxide to significantly enhance germination compared with the control (36, 53, 89, and 68% versus 5, 2, 14, and 32%, respectively). Despite the effectiveness of chemical scarification, chemicals can be hazardous, difficult to obtain, and present serious health risks (Mallinckrodt Baker, 2008 a, b). As a result, alternative methods of seed treatment may be superior. 32 Boiling water promoted seed permeability and subsequent germination of several Malvaceae species, presumably through opening of the water gap (Christiansen and Moore, 1959; Baskin and Baskin, 1997). For example, seeds of Iliamna corei (Malvaceae) germinated to 93% (as compared to 0% germination of the control), following a 5-sec submergence in boiling water (Baskin and Baskin, 1997). Mechanical scarification has also been reported to boost germination rates. The International Seed Testing Association recommends scarification with a metal file to break dormancy of Althaea officinalis and A. rosea (Malvaceae) (ISTA, 1976). However, manual seed treatment techniques are time consuming and unrealistic for operational use (Baskin and Baskin, 1998). Mechanized techniques can result in embryo damage due to scarification severity, often overriding the benefits of the treatment. Page et al. (1966) report decreases in germination S. grossulariaefolia with the duration of scarification time in a sandpaper-lined rotating drum, while Roth et al. (1987) suggest that seeds of S. grossulariaefolia, S. coccinea, and S. munroana perished after mechanical scarification irrelevant of treatment duration. Less traditional techniques, such as rock tumbling, fire, and heating have been effectively used to increase seed coat permeability in some physically dormant species. For example, Dreesen (2009) recommends the use of seed abrasion in rotating rock tumbler to improve germination of physically dormant species. I found, however, no information regarding the effects of tumbling on the germination behavior of Sphaeralcea munroana. Abrasion through fire has been observed to benefit germination. For example, I. corei 33 demonstrated increased germination following a 1 to 2 min simulated annual summer burning, with the highest germination achieved after 6 years (39 ± 6% ) compared with the control (0%) (Baskin and Baskin, 1997). Moreover, germination of physically dormant seeds of 8 Fabacea species was substantially amplified after ignition with a torch (Sugii, 2003). Dry heat may be a substitute for fire, often achieving superior results. Baskin and Baskin (1997) found that several dry heat temperatures and exposure durations optimized I. corei germination. Despite evidence for the presence of physical dormancy, reported germination of S. munroana has failed to exceed 53%, even when dormancy was presumably broken (Roth et al., 1987; Smith and Kratsch, 2009). Thus, it is unclear whether these seeds possess additional dormancy types. Physiological dormancy, characterized by the presence of chemical inhibitors that prevent embryonic growth, is commonly found in cold desert herbaceous perennials and can be relieved by stratification (Timson, 1966; Pinfield, et al., 1972; Baskin and Baskin, 1998). Gibberellic acid can serve as a proxy for stratification by alleviating the chemical constraints that prevent radical emergence and increasing embryonic growth (Hilhorst, 1995; Bewley, 1997; Koornneef et al., 2002; LeubnerMetzger, 2003). Although less common, the coupling of physical and physiological dormancy (combined dormancy) requires both types to be broken before germination can occur (Nikolaeva, 1969; Baskin and Baskin, 1998; Emery, 1987). Dunn (2011) reports increased 34 germination of Sphaeralcea ambigua and S. coccinea (to 45.3 and 85.3%, respectively) compared to the control (18.0 and 4.7%, respectively), following a 30-d stratification of scarified seeds. Similarly, Smith and Kratsch (2009) report that following the mixture of scarification and a 6-wk stratification, seeds of S. grossulariifolia, S. parvifolia, and S. munroana germinated to a greater extent than from either treatment alone, suggesting that seeds of S. munroana may also exhibit combined dormancy. Smith and Kratsch (2009) report that pairing scarification with a 6-wk stratification resulted in higher germination of S. grossulariifolia, S. parvifolia, and S. munroana than either treatment alone, suggesting that seeds of S. munroana may exhibit combined dormancy. Successful use of Munro’s globemallow in restoration depends on a clear understanding of the underlying mechanisms governing seed germination. The process of seed imbibition and the site of water entry are critical to our comprehension of the germination dynamics and treatment effects. To address these questions, 4 experiments were initiated. The first experiment compared (a) water uptake of non-treated, scarified, and boiling water scarified seeds and (b) identified the primary site of water uptake. The second experiment, investigated the germination response of fresh S. munroana seeds to mechanical scarification, 6-wk stratification, and their combination. The third experiment evaluated the germination behavior of stored seeds following mechanical scarification, submergence duration in gibberellic acid or plain water, and several combinations of these treatments. The use of native species for restoration is limited by the high seed procurement cost and low establishment rates (when compared to the use of non-native cultivars). Thus, the economically feasible use S. munroana is dependent on the 35 development of large scale seed pre-treatment techniques. In order to address this issue, the final experiment assessed the effectiveness of boiling water, tumbling, burning, heating, and burning + heating scarification on germination. Materials and Methods In general, the experiments were conducted at the University of Idaho, Center for Forest Nursery and Seedling Research, Moscow. Prior to each experiment, seeds were sterilized with a 0.5% NaOCl solution for 15 min and double-rinsed with deionized (DI) water. The general procedure included placing seeds onto germination paper (soaked with DI water) inside randomly arranged Petri dishes, remoistening germination paper with 5 ml of DI water every 3 d to avoid a potential reduction in dormancy break due to substrate desiccation (Flemion, 1931; Stokes, 1965), and monitoring germination (defined by ≥ 5 mm radical length) daily for 21 d. Specifically, for the first 2 experiments, seeds were collected in August 2010 near Payette, Idaho (N 43° 52’ 49.6” W 116° 47’ 01.8”) and kept at 21±1 °C to avoid the possibility of stratification during refrigerated storage. Experiments 3 and 4 used seeds obtained from native stands throughout the Wasatch Mountains of northern Utah (Great Basin Seeds LLC, Ephraim, UT) and stored at 1.5±0.5 °C. All treatments had 5, 50-seed replicates except those in the first experiment, which contained 10, 15-seed replicates. The first experiment, compared water uptake of seeds after exposure to 3 treatments: (1) control, (2) mechanical scarification with a sharp blade in the region opposite the chalaza, and (3) boiling water scarification achieved by a10-sec submergence in 100 °C water. 36 Seeds in each replicate were weighed to the nearest 0.1 mg and re-weighed (after being blotted to reduce the presence of free water) at 1-hr intervals for 10 hr and once at the end of the 24-hr observation period (Gama-Arachchige et al., 2010). Mass increase, expressed as a mean percentage gain on a dry weight basis, was calculated. Subsamples of control and boiling water scarified seeds were sent to the Electron Microscopy Center at the University of Kentucky, Lexington and scanned with a S-3200 Hitachi (Hitachi High Technologies America, Inc. Pleasanton, CA) scanning electron microscope (acceleration voltage of 5.0 kV) (Gama-Arachchige et al. 2010). The chalazal region and the dislodged chalazal cap were observed and photomicrographed. The second experiment assessed the presence of physical, physiological, and combined dormancy by comparing the germination following exposure to a (1) control, (2) mechanical scarification (described above), (3) stratification, and (4) combined scarification + stratification treatments. Seeds were stratified at 4.6±0.02 °C for 6 wk on moistened germination paper inside sealed Petri dishes. Seeds in the combination treatment were scarified first (Smith and Kratsch, 2009). The third experiment evaluated the effects of GA3 on germination. Seeds were subject to 8 treatments: (1) control, a (2) 24- and (3) 48-hr soak in DI water, and a (4) 24- and (5) 48-hr soak in 100 ppm GA3 solution (90% gibberellin A3 basis and DI water). The final 3 treatments were applied to mechanically scarified seeds soaked for (6) 0, (7) 24 or (8) 48 hr in 100 ppm GA3. The final experiment looked at the effects of “non-traditional” scarification, including (1) control, (2) boiling water (described above), (3) tumbling, (4) 37 burning, (5) dry-heating, and (6) burning + heating. Seeds were tumble-scarified in a rotary rock tumbler (Model AR-1) with dry aluminum oxide grit (12 Mesh, Kramer Industries, Inc., Piscataway, New Jersey) for 72 hr. Following tumbling, seeds were separated from grit using a series of sieves (Dreesen, 2004). For burning scarification, seeds were placed in single layer onto a metal mesh screen, submerged uniformly in 95% ethyl alcohol for 1 min. Seeds were removed from the alcohol and placed on a fireresistant surface, ignited with a hand-held butane torch, and allowed to burn for 10 sec before being extinguished with DI water (Sugii, 2003). For dry-heat scarification seeds were placed into a laboratory oven (80 °C) for 60 min (Baskin and Baskin 1997). Seeds subject to burning + heating scarification were burned first. Statistical Analysis Although germination capacity is conventionally used to assess seed performance, other factors (i.e. germination rate and uniformity) are important (Ching, 1959; Thomson and El-Kassaby, 1993; El-Kassaby, 2007). Combining multiple parameters into a single variable (e.g. Czabator, 1962) in an attempt to better describe germination performance has failed to provide a holistic representation of germination. To avoid this, I fit daily germination data to 2 mathematical models, the parameters of which give a detailed description of seed behavior. In experiments 2 and 4, a 3-parameter model was used (Equation 2.1); where G (t) is the cumulative germination percentage at time (t) expressed in days (d), Gc is cumulative germination, or the germination asymptote at the end of the testing period (%), GC50 is the time in days required to reach 50% germination, 38 G (t ) Gc 1 e GC50 t (Equation 2.1) Gd G(t ) Gc 1 e e GC50( t Gl ) (Equation 2.2) and Gd is the germination rate (% /d). Due to differences in germination behavior in experiment 3, an alternative model was used (Equation 2.2); where Gd was replaced with Gl, defined as the time in days to first germination. All remaining parameters were identical to those described above. Parameters (Gc, GC50, Gd, Gl) for each replication were generated by curve-fitting. Expected mean squares, components of variance, and R2 values were estimated for all parameters. In all experiments, specific treatment differences were explored with one-way ANOVA and Tukey’s HSD (α = 0.05) (SAS Institute Inc., Cary, NC). Results In the first experiment (evaluating imbibition), mechanical and boiling water scarification resulted in significant increases (p < 0.0001 and p = 0.0347, respectively) in water uptake compared with the control (Figure 2.2.). The measurements for 3 of the 10 replicates were systematic outliers and were excluded from this analysis. Mechanically scarified 39 seeds exhibited greater (p < 0.0001) mass gain compared to the boiling water scarification at the end of the 24-hr observation period (Figure 2.2.). The photomicrographic evaluation revealed that the chalazal region of the seed possesses a water gap that is covered by a cap-like structure made up of maternal tissues and palisade cells (Figure 2.1. A, B). Boiling water scarification caused a contiguous crack to form around the chalazal region, which lead to the water gap dislodgement and subsequent imbibition (Figure 2.1. B, C, D) (Serrato-Valenti et al., 1992). In the second experiment (investigating presence of physical, physiological, or combined dormancy in fresh seeds), Gc was significantly different among all treatments, while GC50 and Gd were not (p < 0.0001, p = 0.3530, and p = 0.4526, respectively). Most of the variation in Gc (R2 = 0.77) was explained by the differences in treatment. Germination was enhanced (p = 0.0030, p = 0.0002) with scarification (35%) and the combined scarification and stratification (44%) (Figure 2.3.). Combining both treatments failed (p = 0.5191) to improve Gc when compared with scarification alone. The results of experiment 3 (evaluating germination following mechanical scarification, as well as soaking duration in GA3, and water) indicate that Gc, GC50, and Gl were different among all treatments (p < 0.0001, p = 0.0005, and p = 0.0386, respectively). Most of the variation in Gc (R2 = 0.93) was explained by differences in treatment. The correlation was not as strong for GC50 (R2 = 0.53) and Gl (R2 = 0.35) parameters. Results confirm that S. munroana seeds are physically dormant, with scarified seeds exhibiting a higher (p < 0.0001) germination compared to non-scarified seeds (Table 2.1., 2.4.). 40 Exogenous addition of GA3 did not promote germination of the non-scarified seeds. Scarification, scarification + water (24 hr), and scarification + GA3 (24 hr) yielded the greatest Gc (87, 93, and 88%, respectively) at the end of 21 d. Gc was higher (p = 0.0328) for scarification + water (24 hr) than for scarification + water (48 hr) treated seeds. However, a similar relationship did not exist (p = 0.9669) between scarified + GA3 treatments. GC50 was significantly lower for GA3 (48 hr), scarified, and scarified seeds + GA3 (24 and 48 hr) compared with the control (Table 2.1.), suggesting that seeds germinated more succinctly. Seeds in the scarification + GA3 (24 hr) treatment began germination later (p = 0.0497) than their cohorts in the scarification + water (48 hr) treatment. In experiment 4, Gc, GC50, and Gd varied significantly (p < 0.0001, p < 0.0001, and p = 0.0115, respectively) among treatments (Table 2.2.). Most variation in GC50 and Gc (R2 = 0.75, R2 = 0.64) could be explained by differences in treatment, with a weaker correlation for Gd (R2 = 0.44). Gc was highest (49%) after boiling water scarification compared to all other treatments (p < 0.0001) (Table 2.2., Figure. 2.5.). The remaining treatments did not enhance germination (Gc < 20%). Boiling water scarification produced a different germination behavior than the other treatments. For example, until day 7, seed germination was low, demonstrated by the larger (p < 0.0001) GC50 parameter estimate (8.2 d). However, following day 7 (when the Gd of the remaining treatments began to slow), the Gd of boiling water scarified seeds increased (p = 0.0165) without reaching an asymptote within the test duration. 41 Discussion Results suggest that seed coat impermeability in Munro’s globemallow is indicative of physical dormancy. Occurrence of the water gap structure in the chalazal region of the seed, responsible for water uptake following natural dormancy break, is analogous to other Malvaceae species (Christiansen and Moore, 1959; Egley and Paul, 1981; 1982; Egley et al., 1986). Permeability can be achieved artificially (e.g. mechanical scarification) or by stimulating natural dormancy release (e.g. boiling water scarification). Presumably a result of the separation of the palisade and subpalisade layers of cells, boiling water scarification caused the detachment of the cap-like structure in the occlusion of the water gap, allowing imbibition to occur (Serrato-Valenti et al., 1992). Because seed mass increased to 86% following mechanical and to 22% after boiling water scarification, it appears that boiling water scarification only partially opens the water gap. Even so, treatments such as boiling water that induce a natural dormancy break are less likely to damage the embryo and are thus more desirable (Page et al., 1966; Roth et al., 1987). My findings that mechanical scarification amplified Gc coincide with Baskin and Baskin (1997) who observed 100% germination of mechanically scarified seeds of I. corei. However, when large quantities of seeds must be treated, boiling water scarification can be a safe alternative to the use of other chemical scarification treatments, including sulfuric acid and diethyl dioxide (Roth et al., 1987). With boiling water scarification, all 3 germination parameters had large standard errors, which may again indicate an 42 incomplete opening of the water gap, resulting in lower total water uptake (Table 2.2.). Because the germination curve never reached its asymptote within the duration of thestudy, a more accurate assessment of the effects of boiling water scarification would require a longer observation period. Neither heating nor burning yielded significant germination improvements, which is inconsistent with Baskin and Baskin (1997), who found that I. corei germination was optimized following a 60-min dry heat (80 °C) application. Thus, although general patterns of dormancy may be similar across members of the same genus, explicit temperature and moisture requirements seem to be species specific. I found a lack of evidence for the presence of additional dormancy types, with both stratification and GA3 failing to boost Gc compared with scarification alone. The addition of GA3 (24 hr) to scarified seeds amplified Gc over the control, but was not different from water (24 hr), and was likely a result of soaking itself. It is possible that a higher concentration of GA3 was needed to influence germination behavior. For example, in a study comparing the effects of 500 and 1000 ppm of GA3, only the 1000 ppm solution enhanced germination of Harrisia fragrans (Dehgan and Pérez, 2005). Considering, however, that a Gc of 93% was achieved by the scarification + water, gibberellins are unlikely to play an important role in alleviating dormancy of S. munroana. The germination of S. munroana reported for experiment 3 (93 %) was much higher than previously observed (51% for S. munroana and 88% for other Sphaeralcea spp.) (Roth et al., 1987; Smith and Kratsch, 2009). Despite the 95.5 % purity reported for the seed lot 43 used in experiment 3, seeds were additionally cleaned in an air column seed separator (Model B, E.L. Erickson, Brookings, SD) to reduce the presence of empty seeds. The satisfactory level of cleaning was determined by X-ray images (MX-20 Radiography System, Faxitron X-ray Corp., Lincolnshire, IL) which allowed me to monitoring seed fill until a desired level was reached. Through this process a substantial amount of seeds, mostly light brown in color, was removed. It is possible that simply increasing seed lot purity and viability through additional cleaning could improve germination of Sphaeralcea spp., and should be considered in future research and production. While some authors (Smith and Kratsch, 2009; Dunn, 2011) report germination improvements of Sphaeralcea seeds following the combination of scarification and stratification, it is possible that their results a are not a feature of the stratification temperature but of the duration of time seeds spend in moist conditions, which allows for optimal imbibition to occur even in partially permeable seeds. Additionally, after-ripening or a period of dry storage (24±1 °C) of freshly collected seeds, used to promote dormancy release, could play a role in the reported differences in treatment effects. For example, loss of physiological dormancy in Geraniaceae seeds occurs within 2 mo of dry storage (Baskin and Baskin, 1974; Van Assche and Vanderlook, 2006). Furthermore, several cold desert perennials have been reported to benefit from after-ripening (Baskin and Baskin, 1998). This process has been suggested to increase the acceptable germination temperature range, promote the loss of ABA, diminish the GA3 requirement, improve germination rate, and impact seed sensitivity to 44 light (Bewley, 1997; Finch-Savage and Leubner-Metzger, 2006; Kucera et al., 2005). However, seed storage conditions are rarely reported, making comparisons difficult. Additionally, collection timing is strongly coupled with seed maturity and moisture content, which have a strong effect on dormancy strength and germination behavior (Dornobos et al., 1989; Michael et al., 2007). For example, Michael et al. (2007) found that seeds of Malva parviflora (Malvaceae) decreased in moisture content and germination capacity with seed development until complete physiological maturity. Germination declines are associated with the development of physiological dormancy and the enhancement of physical dormancy as a result of declining seed moisture content (Michael et al., 2007). Thus, high temperature and low moisture content during the growing season may contribute to the degree of dormancy development in seeds of S. munroana. Conclusions My findings suggest that seeds of Sphaeralcea munroana exhibit strong physical dormancy due to the impermeability of the seed coat and the presence of a cap-like structure in the occlusion of the water gap, which inhibits water imbibition and prevents germination. Seed coat scarification is essential for germination, following which seeds may benefit from submergence in water. Although mechanical scarification produced the greatest germination, boiling water scarification can be an effective and operationally feasible method for breaking dormancy in large quantities of seeds. 45 Literature Cited Baskin, C. C. 2003. Breaking physical dormancy in seeds - focussing on the lens. New Phytologist 158:229-232. Baskin, C. C. and J. M. Baskin. 1998. Seeds: Ecology, biogeography and evolution of dormancy and germination. Academic Press, San Diego, California, USA. Baskin, J. M. and C. C. Baskin. 1997. Methods of breaking seed dormancy in endangered species Iliamna corei (Sherff) (Malvaceae), with special attention to heating. Natural Areas Journal 17:313-323. Baskin, J. M. and C. C. Baskin. 2000. Evolutionary considerations of claims for physical dormancy-break by microbial action and abrasion by soil particles. Seed Science Research 10:409-413. Baskin, J. M., C. C. Baskin, and X. Li. 2000. Taxonomy, anatomy and evolution of physical dormancy in seeds. Plant Species Biology 15:139–152. Beale, D. M. and A. D. Smith. 1970. Forage use, water consumption, and productivity of prongron antelope in western Utah. Journal of Wildlife Management 34:570-578. Bewley, J. D. 1997. Seed germination and dormancy. Plant Cell 9:1055-1066. Christiansen, M. N. and R. P. Moore. 1959. Seed coat structural differences that influence water uptake and seed quality in hard seed cotton. Agronomy Journal 27:156-160. Corner, E. J. H. 1951. The leguminous seed. Phytomorphology 1:117-150. Dehgan, B. and H. E. Pérez. 2005. Germination of Caribbean applecactus. Native Plants Journal 6:91-96. Dreesen, D. R. 2004. Tumbling for seed cleaning and conditioning. Native Plants Journal 5:52-54. Dunn, B. 2011. Improved germination of two Sphaeralcea A. St.-Hil. (Malvaceae) species with scarification plus stratification treatments. Native Plants Journal 12:13-16. Egley, G. H. and R. N. Paul. 1981. Morphological observations on the early imbibition of water by Sida spinosa (Malvaceae) seeds. American Journal of Botany 68:10561065. Egley, G. H. and R. N. Paul. 1982. Development, structure and function of the subpalisade cells in water impermeable Sida spinosa seeds. American Journal of Botany 69:1402-1409. Egley, G. H., R. N. Paul, and A. R. Lax. 1986. Seed coat imposed dormancyhistochemistry of the region controlling onset of water entry into Sida spinosa. Physiologia Plantarum 67:320-327. Emery, D. E. 1987. Seed propagation of native California plants. Santa Barbara Botanic Garden, Santa Barbara, California, USA. Finch-Savage, W. E. and G. Leubner-Metzger. 2006. Seed dormancy and the control of germination. New Phytologist 171:501-523. Flemion, F. 1931. After-ripening, germination, and vitality of seeds of Sorbus aucuparia L. Contributions of Boyce Thompson Institute 3:413-439. 46 Gama-Arachchige, N. S., J. M. Baskin, R. L. Geneve, and C. C. Baskin. 2010. Identification and characterization of the water gap in physically dormant seeds of Geraniaceae, with special reference to Geranium carolinianum. Annals of Botany 105:977-990. Hilhorst, H. W. M. 1995. A critical update on seed domrnacy. 1. Primary dormancy. Seed Science Research 5:61-73. Hoffman, M. T., R. M. Cowling, C. Douie, and S. M. Pierce. 1989. Seed predation and germination of Acacia eriolob in the Kuiseb River Valley, Namib Desert. South African Journal of Botany 55:103-106. ISTA. 1976. International rules for seed testing. 1976. Seed Science and Technology 4: 3-49. Koornneef, M., L. Bentsink, and H. Hilhorst. 2002. Seed dormancy and germination. Current Opinion in Plant Biology 5:33-36. Kucera, B., M. A. Cohn, and G. Leubner-Metzger. 2005. Plant hormone interactions during seed dormancy release and germination. Seed Science Research 15:281307. Leubner-Metzger, G. 2003. Functions and regulation of beta-1,3-glucanases during seed germination, dormancy release and after-ripening. Seed Science Research 13:1734. Michael, P. J., K. J. Steadman, and J. A. Plummer. 2007. Seed development in Malva parviflora: onset of germinability, dormancy and desiccation tolerance. Australian Journal of Experimental Agriculture 47:683-688. Nikolaeva, M. G. 1969. Physiology of deep dormancy in seeds (Fiziologiya glubokogo pokoya semyan). Israel Program for Scientific Translations [available from the U.S. Dept. of Commerce, Clearinghouse for Federal Scientific and Technical Information, Springfield, Va.], Jerusalem, Israel. Page, R. J., D. L. Goodwin, and N. E. West. 1966. Germination requirements of scarlet globemallow. Journal of Range Management 19:145-146. Pendery, B. M. and M. D. Rumbaugh. 1986. Globemallows: forbs for Utah rangelands. Utah Science 47:41-45. Roth, T. E., J. L. Holechek, and M. Y. Hussain. 1987. Germination response of 3 globemallow species to chemical treatment. Journal of Range Management 40:173-175. Rumbaugh, M. D., H. F. Mayland, B. M. Pendery, and G. E. Shewmaker. 1993. Utalization of globemallow (Sphaeralcea) taxa by sheep. Journal of Range Management 46:103-109. Sabo, D. G., G. U. Johnson, W. C. Martin, and E. F. Aldon. 1979. Germination requirements of 19 species of arid land plants. USDA Forest Severvice Research Paper RM-210. Rocky Mountain Forest and Range Experiment Station, Fort Collins, Colorado, USA. Serrato-Valenti, G., L. Cornara, S. Lotito, and L. Quagliotti. 1992. Seed coat structure and histochemistry of Abelmoschus esculentus. Chalazal region and water entry. Annals of Botany 69:313-321. Smith, A. and H. Kratsch. 2009. Seed propagation of Sphaeralcea (Globemallow). Hortscience 44:1139-1140. 47 Thomson A. J. and Y. A. El-Kassaby. 1993: Interpretation of seed-germination parameters. New Forests. 7: 123- 132. Van Assche, J. A. and F. E. A. Vanderlook. 2006. Germination ecology of eleven species of Geraniaceae and Malvaceae, with special reference to the effects of drying seeds. Seed Science Research 16:283-290. Vazquez-Yanes, C. and B. Perez-Garcia. 1976. Notas sobre la morfologia y la anatomia de la testa de las semillas de Ochroma lagopus Sw. Turrialba 26:310-311. Vleeshouwers, L. M., H. J. Bouwmeester, and C. M. Karssen. 1995. Redefining seed dormancy: an attempt to integrate physiology and ecology. Journal of Ecology 83:1031-1037. 48 Table 2.1. The effects of mechanical scarification, soaking duration in GA3, or pure water solution on the germination behavior of Sphaeralcea munroana at the end of the 21-d observation period. Parameter values were generated using a non-linear regression model (Equation 2.2), where G (t) is the cumulative germination percentage at time (t) expressed in days (d), Gc is cumulative germination, or the germination asymptote at the end of the testing period (%), GC50 is the time (d) required to reach 50% germination, and Gl is the time (d) until first germination. Multiple comparisons were obtained using Tukey’s HSD (α = 0.05). Treatment Gc (%) Control 15.9±4.5 c Mechanical Scarification 87.1±3.8 ab Gibberellic Acid (24 hr) 15.9±2.3 c Gibberellic Acid (48 hr) 15.1±2.4 c Mechanical Scarification + GA3 (24 hr) 88.1±3.9 ab Mechanical Scarification + GA3 (48 hr) 81.7±1.8 ab Mechanical Scarification + Water (24 hr) 93.4±2.9 a Mechanical Scarification + Water (48 hr) 71.9±9.3 b 0.0001 P values Different letters indicate significant differences among treatments GC50 (d) 2.7±0.5 a 0.7±0.2 b 1.7±0.6 ab 0.9±0.3 b 0.6±0.1 b 0.6±0.1 b 1.5±0.3 ab 1.8±0.4 ab 0.0005 Gl (d) 0.1±0.1 ab 0.3±0.1 ab 0.4±0.2 ab 0.2±0.2 ab 0.6±0.1 b 0.4±0.2 ab 0.5±0.1 ab 0.0±0.0 a 0.0386 Table 2.2. The effects of “non-traditional” scarification techniques on the germination behavior of Sphaeralcea munroana at the end of the 21-d observation period. Parameter values were generated using a non-linear regression model (Equation 2.1), where G (t) is the cumulative germination percentage at time (t) expressed in days (d), Gc is cumulative germination, or the germination asymptote at the end of the testing period (%), GC50 is the time (d) required to reach 50% germination, and Gd is the germination rate (% /d). Multiple comparisons were obtained using Tukey’s HSD (α = 0.05). Treatment Gc (%) GC50 (d) Gd (% /d) Control 10.7±1.1 b 1.6±0.2 b 1.4±0.5 b Boiling water 49.0±12.9 a 8.2±1.2 a 4.2±0.8 a Tumbling 20.3±1.3 b 2.1±0.1 b 2.3±0.3 b Burning 17.0±1.6 b 2.0±0.3 b 2.0±0.6 b Heating 10.7±1.3 b 4.4±0.2 b 2.1±0.5 b Burning + Heating 4.2±1.8 b 4.2±0.1 b 1.2±0.5 b 0.0001 0.0001 0.0115 P values Different letters indicate significant differences among treatments. 49 Figure 2.1. Scanning electron micrographs of a Sphaeralcea munroana seed; (A) top view of the chalazal region of a dormant seed showing the chalazal slit; (B) formation of water gap following dormancy break; (C) the underside of the dislodged cap-like blister covering the water gap; (D) palisade cells of the cap-like structure. Abbreviations: Chsl, chalazal slit; Chsl*, remaining part of the chalazal slit after dormancy break; Ll, light line; Mi, micropyle; Mt, maternal tissue; Pa, palisade; Spl, subpalisade cells; Wg, water gap. 50 100 Control Mechanical Boiling water a Mass Increase (%) 80 60 40 b 20 c 0 0 1 2 3 4 5 6 7 8 9 10 24 Time (h) Figure 2.2. Mass increase percentage (on a fresh mass basis) of control, mechanically, and boiling water scarified seeds of Sphaeralcea munroana during a 24-hr incubation. Each point scatter represents the mean (±s.e.) of 10 replicates. Different letters indicate significant differences (p < 0.05) at the end of the 24-hr period. 51 100 Control Scarified Stratified Scarified + Stratified 90 Cumulative Germination (%) 80 70 60 50 b 40 b 30 20 a a 10 0 0 5 10 15 20 Time (d) Figure 2.3. Cumulative germination percentage of Sphaeralcea munroana seed subject to 4 seed treatments during a 21-d observation period. Each line represents the mean (±s.e.) response of 5 replicates. Different letters indicate significant differences (p < 0.05) between treatments. 52 a 100 90 Germination Capacity (%) 80 Control GA3 (24 h) GA3 (48 h) Scarified Scarified + water (24 h) Scarified + water (48 h) Scarified + GA3 (24 h) Scarified + GA3 (48 h) ab ab ab b 70 60 50 40 30 c 20 c c 10 0 Treatment Figure 2.4. Germination capacity of Sphaeralcea munroana seeds 21 d following exposure to 8 treatments. Each bar represents the mean (± s.e.) response of 5 replicates. Different letters indicate significant differences (α = 0.05). 53 50 Control Boiling Tumbling Burning Heating Burning + Heating Cumulative Germination (%) 40 a 30 b b 20 b b 10 b 0 0 5 10 15 20 Time (d) Figure 2.5. Cumulative germination percentage of Sphaeralcea munroana seeds subject to 6 treatments during a 21-d observation period. Each line represents the mean (±s.e.) of 5 replicates. Different letters indicate significant differences (p < 0.05) between treatments. 54 Chapter Three: Individual and Synergistic Influence of Temperature and Moisture on Sphaeralcea munroana Seedling Growth Abstract For Munro’s globemallow (Sphaeralcea munroana) seedlings, temperature affects growth immediately after germination more than available moisture. In a growth chamber study, germinants grown at colder temperatures 17/3 °C had 47% fewer leaves, 21% less leaf area, and less shoot (31%) and root (31%) biomass than their cohorts grown at 23/9 °C. Decreasing irrigation frequency favored biomass allocation to roots and a subsequent increase in root-to-shoot ratio. Neither temperature nor moisture had an effect on gas exchange. These results suggest that although this perennial, cool-season forb shows considerable potential for restoration use on arid sites, it may not be the best candidate for early competition with cool season grasses during its establishment phase. Because growth is hindered by cool temperatures, a later sowing date may improve establishment in nurseries, seed production areas, and restoration sites. 55 Introduction Plant establishment is the most vulnerable stage in plant community development, especially in regions with restrictive growing conditions (Call and Roundy, 1991). Wide diurnal temperature fluctuations, episodic precipitation pulses, and extensive droughts present major limitations to post-germination survival. Seedlings are more susceptible to environmental fluxes than mature plants because the maximum temperature and soil moisture changes occur in close proximity to the soil surface (Bazzaz and Mezga, 1973; Raynal and Bazzaz, 1973; Regehr and Bazzaz, 1976). In the Great Basin, diurnal temperatures can fluctuate by 20 °C (Smith and Nowak, 1990), in part due to topographically-induced formation of large nocturnal cold aid drainage throughout the year (Osmond et al., 1990). The Great Basin-Mojave region has been characterized as the most arid habitat in North America, with precipitation averaging 50 to 300 mm annually. As a result of low humidity and abundant irradiance the potential evapotranspiration in this region is high, ranging between 1100 mm in the northern and 2000 mm in the southern portion of the basin (Flaschka et al., 1987). On an inter-annual basis, summer precipitation is highly variable, typically representing only 20 to 30% of total annual precipitation (Bell, 1979). Thus, strong disparity exists between maximum water availability and the ability of plants to use it because a substantial portion of available moisture is lost by the time air and soil temperatures become suitable for plants to be fully physiologically active (Caldwell, 1985). For example, despite being abundant, winter precipitation may not be used during a considerable portion of the year 56 as a result of cold temperatures, which create a reduction in the physiological plant activity. Moreover, in early spring, moisture loss can still occur via sublimation and evaporation. Therefore, the beginning of the growing season is directly correlated with the amount of winter-spring precipitation and the increase in air and soil temperatures (Turner and Randall, 1987). The seasonal reduction in rainfall enhances the importance of the cool spring growing season. As a result, most species initiate growth in March and April, when maximum daily temperatures range from 5 to 15 °C and night temperatures remain near freezing (Thornthwaite, 1948; Comstock and Ehleringer, 1992). At the soil surface, especially on sites where recent disturbance has considerably reduced the presence of plant cover, diurnal temperature differences are more pronounced. Clearly, the interaction between precipitation and temperature patterns bear considerable implications on the physiological ecology of the native floristic communities. One important component of Great Basin plant communities is Munro’s globemallow (Sphaeralcea munroana (Douglas) Spach). This endemic, perennial forb provides soil stabilization and is a source of nutrition for myriad animals (Beale and Smith, 1970; Pendery and Rumbaugh, 1986; Rumbaugh et al., 1993; Pavek et al., 2011). For these reasons, as well as its ability to tolerate disturbed sites, drought, and extreme temperatures, it is an important candidate for broad scale restoration across its range. While native plants are fundamental in maintaining ecosystem function, the use of forbs in restoration is relatively novel and vastly unexplored (Parkinson, 2008). As a result, little is known about the range of tolerance to environmental conditions that allows for successful establishment and growth of S. munroana. Therefore, the study objective was 57 to evaluate a suite of morphological and physiological characteristics of S. munroana to a range of temperature and moisture conditions during establishment. Materials and Methods Plant Establishment Sphaeralcea munroana seeds were collected from 5 locations throughout Oregon and Idaho (Table 3.1.). All seeds were hand scarified with a scalpel in order to break physical seed dormancy (Kildisheva, 2011) and were sown directly into 66 ml containers (Model RLC4, Ray Leach®, Stuewe and Sons, Inc., Tangent, OR). Containers, augmented with mesh liners to prevent media loss, were filled with autoclaved sand and placed into 4 environmental growth chambers (Model E-30B, Percival Scientific, Inc., IA). A 10-d period was allowed for germination, during which chambers were set to a 24 °C (8 hr)/17 °C (16 hr) diurnal cycle (Sabo et al., 1979). Seedlings were thinned to 1 plant per container 10 d after sowing (DAS) and randomly assigned to a temperature and moisture treatment. At this point, a one-time application of 18-24-16 (N-P-K) solution of MiracleGro® Water Soluble Rose Plant Food (Scotts Co., Marysville, OH) was administered to all containers at a rate of 3.8 mg N per plant. Temperature and Moisture Treatments Because S. munroana typically germinates in April (Parkinson, 2008), climate records for April from 1950 through 2010 were obtained using PRISM Data Explorer (http://prismmap.nacse.org/nn/) for each coordinate and averaged across sites. The 58 resultant temperature regime was 17/3 °C, which I contrasted with a 23/9 °C regime that represented a 6 °C increase in temperature. The diurnal transition followed a 13-h day and an 11-h night. Irradiance was set to 950 µmol m-²s-¹ based on values provided by light response curves developed for field-planted specimens of S. munroana (Appendix A Figure 3.11.). Relative humidity was ambient and ranged between 50 and 60%. Within each chamber, plants were subject to 1 of the 4 moisture availability treatments (3, 6, 9 and 12-d intervals between recharging each container to field capacity). Each temperature × moisture combination was randomly assigned 20 seedlings. Containers were subirrigated by placing them into deionized water for 1 hr. To prevent the effects of environmental heterogeneity within chambers (Lee and Rawlings, 1982), plants were randomized every 3 d. Mortality, physiological, and morphological assessments were made at the end of the 25 d period (35 DAS). For the purpose of uniformity, 5 seedlings from each temperature × moisture regime were randomly selected for physiological and morphological measurements. Gas exchange rates (i.e. photosynthesis, stomatal conductance, and transpiration) were evaluated within 4 hr of light period initiation using an LI-6400 Portable Photosynthesis System (Li-Cor, Inc., Lincoln, NE). Plants were gently removed from containers and separated by tissue type (i.e. root, shoot) from which leaf area and number of true leaves were determined. After drying tissues at 80 °C for 24 hr, the aboveand belowground biomass and the root-to-shoot ratios (R:S) were determined. Cumulative plant mortality for each treatment was recorded upon the termination of the experiment. 59 Statistical Analysis A split-plot design with 2 temperature regimes (whole plot) and 4 moisture levels (subplot) was used. Individual growth chambers were treated as blocks and moisture treatments were completely randomized within chambers. Statistical analysis was conducted with SAS version 9.2 software (SAS Institute Inc., Cary, NC). A mixed effects procedure (PROC MIXED) was used to test the main effects of temperature and moisture by nesting the block (chamber) within temperature. Between-chamber replication was attained by repeating the study during 2 distinct time periods. The testing period was not a significant variable, and was thus eliminated from the analysis. Pair-wise comparisons (a = 0.05) of the least square mean estimates were made for all temperature, moisture, and temperature × moisture interactions. Results Plant mortality, photosynthesis, conductance, and transpiration were unaffected by temperature, moisture, or the temperature × moisture interaction (Table 3.2., Appendix B). Seedlings grown at 17/3 °C produced less true leaves, leaf area, above- and belowground biomass (47, 21, 31, and 31%, respectively) than their cohorts grown at 23/9 °C (Table 3.2., Figure 3.1.-3.4.). Belowground biomass and R:S were the only variables affected by temperature, exhibiting higher values (p = 0.0127 and p = 0.0317) under the most moisture limiting conditions (12-d irrigation interval) (Table 3.2., Figure 3.5., 3.6.). Leaf area, above- and belowground biomass, and R:S were significantly influenced by the temperature × moisture interaction (Table 3.2.). At low temperatures 60 (17/3 °C), these parameters remained constant, irrelevant of moisture availability. However, under the warmest, driest conditions (23/9 °C, 12 d-irrigation interval) leaf area and aboveground biomass decreased relative to more frequent (≤ 9 d) irrigation (Figure 3.7., 3.8.). This trend was not as strong for the aboveground biomass, as plants grown under a 6-d irrigation interval exhibited a similar response as plants subject to the driest regime. Finally, seedlings grown under the warmest, driest conditions had greater (p = 0.0268 and p = 0.0034) belowground biomass and R:S (Figure 3.9., 3.10.). Discussion In general, the imposed average April temperatures and moisture availability regimes applied in this study were sufficient for survival. This suggests that following germination, S. munroana plants are relatively resilient to temperature increases and moisture fluctuations. However, short-term resilience is not necessarily indicative of long-term persistence. It is possible that survivorship may differ during the course of an entire growing season, because development was influenced by temperature differences. Due to the brevity of the period suitable for growth in the Great Basin, plants must establish adequate root systems early in the season as available water shifts downwards in the soil profile in order to ensure survival prior to entering mid-summer dormancy (Fernadez and Caldwell, 1975; Sturges, 1977). Thus, further research, focused on the relation of seedling growth rates early in the season and their relation to subsequent phenology and survival, is necessary. 61 Plants grown under the 17/3 °C regime developed slower, producing roughly half the number of true leaves as those grown at 23/9 °C. This combination of reduced leaf number and leaf area resulted in 29% less biomass production. Moisture availability alone did not elicit substantial effects on plant growth, but the combined influence of warmer temperature and limited moisture caused a predicted decline in leaf area. Decreases in turgor have been linked to reduced aboveground biomass production and overall growth rates in a number of species (Taiz and Zeigler, 2006). For example, Smith and Nobel (1978) report a direct link between leaf size and leaf water potential in a Great Basin perennial, Encelia farionsa. In my study, seedlings exposed to the warmest, driest regime produced less aboveground biomass than plants brought to field capacity every 3 and 9 d. Thus, plants were able to curtail moisture demands by reducing their transpirational surface area, as opposed to decreasing stomatal conductance. However, this response may be a result of low night air temperatures that prevent a full reduction in stomatal opening during the day (Anderson and McNaughton, 1973). I saw a 28% reduction in biomass for seedlings grown at 17/3 °C compared with their warmer cohorts which is analogous to the results reported for the native bunch grass, Agropyron spicatum at temperatures below 8 °C (Harris, 1967; Harris and Wilson, 1970). The capacity to initiate root extension at low temperatures can, however, offer an advantage in the Great Basin. For example, the competitive abilities of the invasive Bromus tectroum have been largely attributed to the species capability to maintain high levels of belowground production at temperatures below 3 °C (Harris, 1967; Harris and 62 Wilson, 1970). Thus, if restoration goals require direct competition with Bromus tectorum early in the growing season, the use of S. munroana alone may not be optimal. The decline in moisture availability encouraged root production in the 2 most waterlimited treatments (9 and 12-d irrigation interval). Higher temperatures amplified the effects of moisture deficit, inducing the highest belowground production under the warmest, driest conditions. When considering water availability alone, the most moisturelimited seedlings produced the highest R:S, reflecting greater resource partitioning to belowground production. R:S ranged from 0.68 to 1.17, which correspond to those reported for a number of mature Great Basin perennials (Barbour, 1973; Caldwell et al., 1977). The imposed environmental conditions did influence the rates of gas exchange. In general, photosynthetic rates ranged from 7.98 to 13.18 mol CO2 m-2s-1 from the warmest, driest to the coolest, wettest conditions. These rates are similar to those observed in several Great Basin woody perennials, suggesting the existence of physiological similarities between the 2 groups (Depuit and Caldwell, 1975; Caldwell, et al., 1977). Conductance conveyed a similar relationship, ranging from 0.096 mol m-2s-1 under the warmest, driest treatment to 0.208 mol m-2s-1 in the coolest most frequently saturated environment. An identical correlation was observed with regard to transpiration, which varied from 0.0019 to 0.0040 (mmol m-2 s-1). Conclusions Under the tested conditions, temperature was the single largest driver of plant behavior. Although moisture limitations are likely to become more pronounced later in the growing 63 season, moisture alone did not strongly influence the physiological and morphological response of S. munroana during initial establishment. Low temperatures impeded plant growth, presumably through the reduction in belowground biomass. Root growth was driven by moisture availability and temperature, but under cool edaphic conditions the temperature influence tended to supersede the role of moisture. The warmest, driest conditions elicited a reduction in aboveground biomass and an increase in belowground production, without affecting gas exchange rates. This implies that seedlings of S. munroana are reasonably drought tolerant even during early development. Further research is needed in order to evaluate in situ plant responses to environmental conditions during early establishment. Because my results indicate that cool night temperatures pose a stricter growth limitation than moisture, a later sowing date (which corresponds more closely with the 23/9 °C regime) may optimize S. munroana establishment. 64 Literature Cited Anderson, J. E. and S. J. McNaught. 1973. Effects of low soil temperature on transpiration, photosynthesis, leaf relative water content, adn grwoth among elevationally diverse plant populations. Ecology 54:1220-1233. Barbour, M. G. 1973. Desert dogma re-examined: root/shoot ratios, productivity and plant spacing. American Midland Naturalist 89:41-57. Bazzaz, F. A. and D. M. Mezga. 1973. Primary productivity and microenvironment in an Ambrosia dominated old field. American Midland Naturalist 90:70-78. Beale, D. M. and A. D. Smith. 1970. Forage use, water consumption, and productivity of prongron antelope in western Utah. Journal of Wildlife Management 34:570-578. Bell, F. C. 1979. Precipitation. Pages 373-392 in D.W. Goodall and R.A. Perry, editors. Arid-land ecosystems: structure, functioning, and managment. Cambridge University Press, London, UK. Caldwell, M. M. 1985. Cold Desert. in B. F. Chabot and H. A. Mooney, editors. Physiological ecology of North American plant communities. Chapman and Hall, New York, New York, USA. Caldwell, M. M., R. S. White, R. T. Moore, and L. B. Camp. 1977. Carbon balance, productivity, and water use of cold-winter desert shrub communities dominatated by C3 and C4 species. Oecologia 29:275-300. Call, C. A. and B. A. Roundy. 1991. Perspectives and processes in revegetation of arid and semiarid rangelands. Journal of Range Management 44:543-549. Comstock, J. P. and J. R. Ehleringer. 1992. Plant adaptation in the Great Basin and Colorado Plateau. Great Basin Naturalist 52:195-215. Depuit, E. J. and M. M. Caldwell. 1973. Seasonal pattern of net photosynthesis of Artemisia tridentata. American Journal of Botany 60:426-435. Fernandez, O. A. and M. M. Caldwell. 1975. Phenology and dynamics of root growth of three cool semi-desert shrubs under field conditions. Journal of Ecology 63:703714. Flaschka, I., C. W. Stockton, and W. R. Boggess. 1987. Climatic variation and surfacewater resources in the Great Basin region. Water Resources Bulletin 23:47-57. Harris, G. A. 1967. Some competitive relationships between Agropyron spicatum and Bromus tectorum. Ecological Monographs 37:89-111. Harris, G. A. and A. M. Wilson. 1970. Competition for moisture among seedlings of annual and perennial grasses as influenced by root elongation at low temperature. Ecology 51:530-534. Kildisheva, O. A. 2011. Restoration strategies for a native perennial: germination and seedling physiology of Sphaeralcea munroana. M. S. Thesis. University of Idaho, Moscow, Idaho, USA. Lee, C. S. and J. O. Rawlings. 1982. Design of experiments in growth chambers uniformity trials in the North Carolina State University Phytotron. Crop Science 22:551-558. Osmond, C. B., L. Pitelka, and G. M. Hidy. 1990. Plant biology of the basin and range. Springer-Verlag, New York, New York, USA. 65 Parkinson, H. A. 2008. Impact of native grasses and cheatgrass on Great Basin forb development. M. S. Thesis. Montana State University, Bozeman, Montana, USA. Pavek, P. L .S., J. H. Cane, O. A. Kildisheva, and A. S. Davis. 2011. Plant guide for Munro’s globemallow (Sphaeralcea munroana). USDA Natural Resources Conservation Service. Pullman, Washington, USA. Pendery, B. M. and M. D. Rumbaugh. 1986. Globemallows: forbs for Utah rangelands. Utah Science 47:41-45. Raynal, D. J. and F. A. Bazzaz. 1973. Establishment of early successional plant populations on forest and prairie soil. Ecology 54:1335-1341. Regehr, D. L. and F. A. Bazzaz. 1976. Low temperature photosynthesis in successional winter annuals. Ecology 57:1297-1303. Rumbaugh, M. D., H. F. Mayland, B. M. Pendery, and G. E. Shewmaker. 1993. Utalization of globemallow (Sphaeralcea) taxa by sheep. Journal of Range Management 46:103-109. Sabo, D. G., G. U. Johnson, W. C. Martin, and E. F. Aldon. 1979. Germination requirements of 19 species of arid land plants. USDA Forest Severvice Research Paper RM-210. Rocky Mountain Forest and Range Experiment Station, Fort Collins, Colorado, USA. Smith, S. D. and R. S. Nowak. 1990. Ecophysiology of plants in the intermountain lowlands. Pages 179-241 in C. B. Osmond, L. F. Pitelka, and G. M. Hidy, editors. Plant biology of the basin and range. Springer-Verlag, New York, New York, USA. Smith, W. K. and P. S. Nobel. 1978. Influence of irradiation, soil-water potential, and leaf temperature on leaf morphology of a desert broadleaf, Encelia farionsa Gray. (Compositae). American Journal of Botany 65:429-432. Sturges, D. L. 1977. Soil-water withdrawal and root characteristics of Big sagebrush. American Midland Naturalist 98:257-274. Taiz, L. and E. Zeiger. 2006. Plant physiology. 4th edition. Sinauer Associates Inc., Sunderland, Massachusets, USA. Thornthwaite, C. W. 1948. An approach toward a rational classification of climate. Geographical Review 38:55-94. Turner, F. B. and D. C. Randall. 1987. The phenology of desert shrubs in southern Nevada. Journal of Arid Environments 13:119-128. 66 Table 3.1. Sphaeralcea munroana seed collection sites. Location Elevation Collection (m) Date N 43° 45.799’ W 117° 07.825’ 779 04 June 2010 N 43° 46.156’ W 117° 19.090’ 749 06 June 2010 N 43° 13.010’ W 119° 00.267’ 1302 20 June 2010 N 43° 47.356’ W 117° 37.859’ 899 22 June 2010 N 43° 52.827’ W 116° 47.030’ 811 08 July 2010 State OR OR OR OR ID Table 3.2. Results of the mixed model analysis for the effects of temperature, moisture, and their interaction on the morphological and physiological responses of Sphaeralcea munroana seedlings 35 d after sowing. Temperature × Moisture Source of Variation Temperature Moisture p p p Mortality True Leaves Leaf Area Aboveground Biomass Belowground Biomass Root:Shoot Photosynthesis Transpiration Conductance α = 0.05 0.2202 0.0052 0.0005 0.0013 0.0062 0.9416 0.0649 0.1450 0.2872 0.2948 0.0817 0.1370 0.2878 0.0127 0.0317 0.5699 0.1041 0.0706 0.6515 0.0915 0.0026 0.0140 0.0268 0.0034 0.8260 0.9977 0.8899 67 5 True Leaves (number) 4 B 3 2 A 1 0 17/9 °C 23/9 °C Diurnal Temperature Regime Figure 3.1. Number of true leaves (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 68 3.0 B 2.5 2 Leaf Area (cm ) 2.0 1.5 1.0 A 0.5 0.0 17/3 °C 23/9 °C Diurnal Temperature Regime Figure 3.2. Total leaf area (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 69 0.020 Aboveground Biomass (g) B 0.015 0.010 A 0.005 0.000 17/3 °C 23/9 °C Diurnal Temperature Regime Figure 3.3. Aboveground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 70 0.020 Belowground Biomass (g) B 0.015 0.010 0.005 A 0.000 17/3 °C 23/9 °C Diurnal Temperature Regime Figure 3.4. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences between treatments. 71 Figure 3.5. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 72 Figure 3.6. Root-to-shoot ratios (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 73 Figure 3.7. Total leaf area (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 74 Figure 3.8. Aboveground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 75 Figure 3.9. Belowground biomass (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 76 Figure 3.10. Root-to-shoot ratios (mean±s.e.) 35 d after sowing, produced by Sphaeralcea munroana seedlings grown under 2 temperature and 4 irrigation regimes. Each bar represents the mean response of 5 replicates. Different letters indicate significant (p < 0.005) differences among treatments. 77 Appendix A -1 -1 Photosynthetic Rate (mol CO2m s ) 25 20 15 10 5 0 -5 0 500 1000 1500 2000 2500 -2 -1 Photon Flux Density (mol quanta m s ) Figure 3.11. Light response curves of photosynthetic carbon fixation measured on individual leaves of 5 mature Sphaeralcea munroana plants at the University of Idaho Shattuck Arboretum. Measurements were made between 1000 and 1300 on 02 October 2011 using an LI-6400 Portable Photosynthesis System (Li-Cor, Inc., Lincoln, NE). Constant chamber CO 2 (400 μmol mol-1), temperature (20±0.16 °C), and relative humidity (79±0.58%) were maintained to avoid confounding the assimilation response. The initial leaf equilibration was set to high photon flux density (2000 μmol quanta m-2s-1), followed by subsequent light decreases in steps of 200 μmol quanta m-2s-1, until a negative photosynthetic rate was reached. Each point represents a mean±s.e. of 5 replicates. 78 Appendix B Table 3.1. Sphaeralcea munroana gas exchange responses to 2 temperature and 4 moisture regimes 35 d after sowing. Photosynthesis Conductance Transpiration (mol CO2 m-2s-1) (mol m-2s-1) (mmol m-2s-1) 17/3 °C 23/9 °C 17/3 °C 23/9 °C 17/3 °C 23/9 °C Moisture 13.12±1.27 8.90±0.65 0.21±0.02 0.18±0.03 0.004±0.0006 0.003±0.0003 3 (d) 13.18±1.75 8.23±0.68 0.19±0.03 0.15±0.02 0.004±0.0007 0.003±0.0003 6 (d) 12.27±1.44 9.07±0.86 0.19±0.03 0.16±0.02 0.004±0.0006 0.003±0.0003 9 (d) 10.95±1.86 7.97±0.85 0.16±0.03 0.10±0.015 0.003±0.0006 0.002±0.0003 12 (d) None of the values are significantly different between or within columns.