Matching Items (36)
Description
Type I H+-PPase encoding genes, such as AVP1 (Arabidopsis thaliana), TsVP (Thellungiella halophilla), TaVP,( Triticum aestivum), and OVP1 (Oryza sativa) are highly conserved and.traditionally known to operate as vacuolar proton translocating pyrophosphatases. It is worth mentioning that Rocha-Facanha and de Meis presented in vitro evidence with tonoplast fractions of maize coleoptiles and seeds consistent with the reverse function of the H+-PPase (1998). These authors suggested that given the appropriate thermodynamic conditions in vivo, the H+-PPase could operate as a system of energy conservation with a role in the maintenance of cytosolic PPi levels. Further evidence in support for a PPi-synthase activity of plant H+-PPases came from work done on tonoplasts from mature oranges where PPi synthesis was demonstrated when a ΔpH of 3 units was imposed (Marsh et al. 2000).
Futher research has shown that transgenics overexpressing type I H+-PPases develop more root and shoot biomass, and have enhanced rhizosphere acidification capacity than wild types. The increased root biomass suggests that previous reports describing the response of these plants to water scarcity as drought tolerance are incomplete. Larger root systems indicate that an important component of the response is drought resistance. The enhanced rhizosphere acidification capacity has also been associated with an increase in nutrient use efficiency, conferring a growth advantage under nitrogen and phosphorous deficient conditions.
While a vacuolar localized H+-PPase easily explains the salt tolerant phenotypes, it does little to provide a mechanism for an increase in root and shoot biomass and/or an augmented rhizosphere acidification capacity. Several groups have argued that higher levels and transport of the growth hormone auxin could be responsible for the above phenotypes. An alternative model focusing on the function of a plasma membrane bound H+-PPase in sieve elements and companion cells links these phenotypes with enhanced phloem sucrose loading and transport.
The following paper reviews publications in which the H+-PPase overexpression technology has been used since 2006 in an attempt to identify cues that could help us test the compatibility of the the proposed models with the actual data.
Futher research has shown that transgenics overexpressing type I H+-PPases develop more root and shoot biomass, and have enhanced rhizosphere acidification capacity than wild types. The increased root biomass suggests that previous reports describing the response of these plants to water scarcity as drought tolerance are incomplete. Larger root systems indicate that an important component of the response is drought resistance. The enhanced rhizosphere acidification capacity has also been associated with an increase in nutrient use efficiency, conferring a growth advantage under nitrogen and phosphorous deficient conditions.
While a vacuolar localized H+-PPase easily explains the salt tolerant phenotypes, it does little to provide a mechanism for an increase in root and shoot biomass and/or an augmented rhizosphere acidification capacity. Several groups have argued that higher levels and transport of the growth hormone auxin could be responsible for the above phenotypes. An alternative model focusing on the function of a plasma membrane bound H+-PPase in sieve elements and companion cells links these phenotypes with enhanced phloem sucrose loading and transport.
The following paper reviews publications in which the H+-PPase overexpression technology has been used since 2006 in an attempt to identify cues that could help us test the compatibility of the the proposed models with the actual data.
ContributorsCoulter, Joshua (Author) / Gaxiola, Roberto (Thesis director) / Wojciechowski, Martin (Committee member) / Pizzio, Gaston (Committee member) / Barrett, The Honors College (Contributor) / School of Life Sciences (Contributor)
Created2014-05
Description
Water is the main driver of net primary productivity (NPP) in arid ecosystems, followed by nitrogen and phosphorous. Precipitation is the primary factor in determining water availability to plants, but other factors such as surface rocks could also have an impact. Surface rocks may positively affect water availability by preventing evaporation from soil, but at higher densities, surface rocks may also have a negative impact on water availability by limiting water infiltration or light availability. However, the direct relationship between rock cover and aboveground net primary productivity (ANPP), a proxy for NPP, is not well understood. In this research we explore the relationship between rock cover, ANPP, and soil nutrient availability. We conducted a rock cover survey on long-term fertilized plots at fifteen sites in the Sonoran Desert and used 4 years of data from annual plant biomass surveys to determine the relationship between peak plant biomass and surface rock cover. We performed factorial ANCOVA to assess the relationship among annual plant biomass, surface rocks, precipitation, and fertilization treatment. Overall we found that precipitation, nutrients, and rock cover influence growth of Sonoran Desert annual plants. Rock cover had an overall negative relationship with annual plant biomass, but did not show a consistent pattern of significance over four years of study and with varying average winter precipitation.
ContributorsShaw, Julea Anne (Author) / Hall, Sharon (Thesis director) / Sala, Osvaldo (Committee member) / Cook, Elizabeth (Committee member) / Barrett, The Honors College (Contributor) / School of Life Sciences (Contributor)
Created2015-05
Description
The distinguishing feature of the filamentous fungi is the hyphae - tube-like microscopic cells that exhibit polarized growth via apical extension and allow the fungus to interact with its environment. Fungi elongate at the hyphal apex, through the localized construction of new plasma membrane and cell wall through the exocytosis of secretory vesicles. One population of these vesicles have been identified as chitosomes, containing chitin synthase isoenzymes, which are responsible for the polymerization of N-acetylglucosamine from UDP N-acetylglucosamine into chitin, the primary fibrillar component of the fungal cell wall. The chitosomes, in addition to other vesicles, can be observed aggregating in the hyphal tip in most filamentous fungi. In the Ascomycota and Basidiomycota, this collection of vesicles exhibits discrete organization and has been termed a Spitzenkörper. Although accumulations of vesicles can be observed in the hyphal tip of many growing filamentous fungi, some debate continues as to what precisely defines a Spitzenkörper. This study reports the details of three separate projects: first, to document the effects of deleting a single chitin synthase, CHS-1 and CHS-6 in Neurospora crassa with regards to hyphal ultrastructure, cytoplasmic organization, and growth in comparison to the wild-type. Given the importance of chitin synthesis in fungal cell growth, deletion of a critical chitin synthase presumably impacts cell wall structure, fungal growth and cytoplasmic organization. Second, an examination of the ultrastructure of four zygomycetous fungi - Coemansia reversa, Mortierella verticillata, Mucor indicus, and Gilbertella persicaria has been conducted. Utilization of cryofixation and freeze-substitution techniques for electron microscopy has produced improved preservation of cytoplasmic ultrastructure, particularly at the hyphal apex, allowing detailed analysis of vesicle size, contents, and organization. Lastly, hyphal tip organization was reviewed in a broad range of fungi. Previous studies had either focused on a few select fungi or representative groups. Vesicle organization, composition and size do appear to vary among the classes of fungi, but some trends, like the vesicle crescent in the zygomycetous fungi have been documented.
ContributorsFisher, Karen Elizabeth (Author) / Roberson, Robert W. (Thesis advisor) / Chandler, Douglas (Committee member) / Riquelme, Meritxell (Committee member) / Stutz, Jeam (Committee member) / Wojciechowski, Martin (Committee member) / Arizona State University (Publisher)
Created2015
Description
Hydrological models in arid and semi-arid ecosystems can be subject to high uncertainties. Spatial variability in soil moisture and evapotranspiration, key components of the water cycle, can contribute to model uncertainty. In particular, an understudied source of spatial variation is the effect of plant-plant interactions on water fluxes. At patch scales (plant and associated soil), plant neighbors can either negatively or positively affect soil water availability via competition or hydraulic redistribution, respectively. The aboveground microclimate can also be altered via canopy shading effects by neighbors. Across longer timescales (years), plants may adjust their physiological (water-use) traits in response to the neighbor-altered microclimate, which subsequently affects transpiration rates. The influence of physiological adjustments and neighbor-altered microclimate on water fluxes was assessed around Larrea tridentata in the Sonoran Desert. Field measurements of Larrea’s stomatal behavior and vertical root distributions were used to examine the effects of neighbors on Larrea’s physiological controls on transpiration. A modeling based approach was implemented to explore the sensitivity of evapotranspiration and soil moisture to neighbor effects. Neighbors significantly altered both above- and belowground physiological controls on evapotranspiration. Compared to Larrea growing alone, neighbors increased Larrea’s annual transpiration by up to 75% and 30% at the patch and stand scales, respectively. Estimates of annual transpiration were highly sensitive to the presence/absence of competition for water, and on seasonal timescales, physiological adjustments significantly influenced transpiration estimates. Plant-plant interactions can be a significant source of spatial variation in ecohydrological models, and both physiological adjustments to neighbors and neighbor effects on microclimate affect small scale (patch to ecosystem) water fluxes.
ContributorsKropp, Heather (Author) / Ogle, Kiona (Thesis advisor) / Hultine, Kevin (Committee member) / Sala, Osvaldo (Committee member) / Vivoni, Enrique (Committee member) / Wojciechowski, Martin (Committee member) / Arizona State University (Publisher)
Created2015
Description
There is a relative lack of basic information about early diverging species of the genus Medicago that, for the most part, were formerly considered to be in the genus Trigonella. Species boundaries are not always clear, for example, the most recent treatment of the genus Medicago submerged four previously recognized species into Medicago monantha, a widely distributed species in the Middle East. These species are recognized on the basis of morphological characters such as fruit number, shape, length and areole shape and size, but species identification is still challenging and further clarification of species boundaries is needed. There is also a lack of cytogenetic information. Some of the relatively few published chromosome numbers, e.g. 2n=28, and 44, differ from those of the rest of the genus, which are mostly 2n=16 or multiples thereof, although seven species are 2n=14. As part of a larger study of the genome and chromosome number evolution in the genus Medicago, we obtained genome size data using flow cytometry for 44 accessions of 14 currently recognized early diverging species, with a focus on Medicago monantha. Chromosome numbers were obtained using standard cytological methods. Our chromosome number data confirm a chromosome number of 2n=16 for M. brachycarpa (genome size of 1.33 pg), and M. monspeliaca (1.88 pg), and 2n=28 for M. polyceratia (2.77 pg) and give new numbers for some species; 2n=16 for M. biflora (2.7 pg), and a previously unknown chromosome number for these early diverging species of 2n=14 for Medicago fischeriana (~1.35 pg). Interestingly, our data support the hypothesis that there are at least two entities within M. monantha as currently recognized that differ in chromosome number and genome size; two accessions had chromosome numbers of 2n=26 and 30 with corresponding genome sizes of 2.68 and 2.85 pg and three other accessions had chromosome numbers 2n=36,44, and another 44 with genome sizes of 3.94, 3.89, and 4.04 pg. There are also some significant morphological differences between these two entities, such as fruit length and areole area. These data lead to both further clarification of the relationships of early diverging Medicago and help build a platform for more in-depth research concerning the evolution of chromosome number and genome size within Medicago.
ContributorsSteier, Julia Elizabeth (Author) / Steele, Kelly (Thesis director) / Wojciechowski, Martin (Committee member) / Fehlberg, Shannon (Committee member) / School of Life Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2016-05
Description
Drylands cover over 40% of the Earth’s surface, account for one third of global carbon cycling, and are hotspots for climate change, with more frequent and severe droughts coupled with deluges of novel magnitude and frequency. Because of their large terrestrial extent, elucidating dryland ecosystem responses to changes in water availability is critical for a comprehensive understanding of controls on global aboveground net primary productivity (ANPP), an important ecosystem service. The focus of this dissertation is to investigate cause-effect mechanisms between altered water availability and ecosystem processes in dryland ecosystems. Across a network of experimental rainfall manipulations within a semiarid Chihuahuan Desert grassland, I examined short- and long-term dynamics of multiple ecosystem processes—from plant phenology to nitrogen cycling—in response to directional precipitation extremes. Aboveground, I found herbaceous plant phenology to be more sensitive in greenup timing compared to deep-rooted, woody shrubs, implying that precipitation extremes will disproportionately affect grass-dominated compared to woody ecosystems. Surprisingly, after 14 years of experimentally adding water and N, I observed no effect on ANPP. Belowground, bulk soil N dynamics remained stable with differing precipitation amounts. However, mineral associated organic N (MAOM-N) significantly increased under chronic N inputs, indicating potential for dryland soil N sequestration. Conversely, the difference between low- and high-N soil N content may increase a drawdown of N from all soil N pools under low-N conditions whereas plants source N from fertilizer input under high-N conditions. Finally, I considered ecosystem-level acclimation to climate change. I found that N availability decreased with annual precipitation in space across continents, but it posed initially increasing trends in response to rainfall extremes at the Jornada that decreased after 14 years. Mechanisms for the acclimation process are thus likely associated with differential lags to changes in precipitation between plants and microorganisms. Overall, my dissertation demonstrates that examining linkages between multiple ecosystem processes, from aboveground phenological cycles to belowground N cycling dynamics, can provide a more integrative understanding of dryland response to climate change. Because dryland range is potentially expanding globally, water limited systems provide a unique and critical focus area for future research that revisit and revise current ecological paradigms.
ContributorsCurrier, Courtney (Author) / Sala, Osvaldo (Thesis advisor) / Collins, Scott (Committee member) / Reed, Sasha (Committee member) / Throop, Heather (Committee member) / Arizona State University (Publisher)
Created2023
Description
Genome-wide, single nucleotide polymorphisms (SNPs) and germination data were analyzed to better understand species delimitation and salt-tolerance within the legume genus Medicago. Molecular phylogenies revealed that the widely-used, genomic model line R108 and two deeply divergent accessions of Medicago truncatula are in fact more closely related to Medicago littoralis than to other accessions representing Medicago truncatula. This result was supported by germination data wherein the two accessions representing deeply divergent Medicago truncatula demonstrated salt-tolerance that was more similar to Medicago littoralis than to other accessions of Medicago truncatula. Molecular phylogenies revealed that two additional accessions representing deeply divergent Medicago truncatula appear to be more closely related to Medicago italica than to other accessions representing Medicago truncatula. The results of the present study elucidate complex evolutionary relationships and contribute to the present understanding of existing salt-tolerance within Medicago.
ContributorsHopkins, Andrew David (Author) / Wojciechowski, Martin (Thesis advisor) / Park, Yujin (Committee member) / Steele, Kelly (Committee member) / Arizona State University (Publisher)
Created2023
Description
Biogeography places the geographical distribution of biodiversity in an evolutionary context. Ants (Hymenoptera: Formicidae), being a group of ubiquitous, ecologically dominant, and diverse insects, are useful model systems to understand the evolutionary origins and mechanisms of biogeographical patterns across spatial scales. On a global scale, ants have been used to test hypotheses on the origin and maintenance of the remarkably consistent latitudinal diversity gradient where biodiversity peaks in the equatorial tropics and decreases towards the poles. Additionally, ants have been used to posit and test theories of island biogeography such as the mechanisms of the species-area relationship, being the increase of biodiversity with cumulative land area. However, there are still unanswered questions about ant biogeography such as how specialized life histories contribute to their global biogeographical patterns. Furthermore, there remain island systems in the world’s biodiversity hotspots that harbor much less ant species than predicted by the species-area relationship, which potentially suggests a place ripe for discovery. In this dissertation, I use natural history, taxonomic, geographic, and phylogenetic data to study ant biodiversity and biogeography across spatial scales. First, I study the global biodiversity and biogeography of a specialized set of symbiotic interactions between ant species, here referred to as myrmecosymbioses, with an emphasis on social parasitism where one species exploits the parental care behavior and social colony environment of another species. In addition to characterizing a new myrmecosymbiosis, I use a global biogeographic and phylogenetic dataset to show that ant social parasitism is distributed along an inverse latitudinal diversity gradient where species richness and independent evolutionary origins of social parasitism peak within the northern hemisphere where the least free-living ant diversity exists. Second, I study the unexplored ant fauna of the Vanuatuan archipelago in the South Pacific. Using approximately 10,000 Vanuatuan ant specimens coupled with phylogenomics, I fill in a historical knowledge gap of South Pacific ant biogeography and demonstrate that the Vanuatuan ant fauna is a novel biodiversity hotspot. With these studies, I provide insights into how specialized life histories and unique island biotas shape the global distribution of biodiversity in different ways, especially in the ants.
ContributorsGray, Kyle William (Author) / Rabeling, Christian (Thesis advisor) / Martins, Emilia (Committee member) / Taylor, Jesse (Committee member) / Pratt, Stephen (Committee member) / Wojciechowski, Martin (Committee member) / Arizona State University (Publisher)
Created2023
Description
The study of organismal adaptations oftentimes focuses on specific, constant conditions, but environmental parameters are characterized by more or less marked levels of variability, rather than constancy. This is important in environments like soils where microbial activity follows pulses of water availability driven by precipitation. Nowhere are these pulses more variable and unpredictable than in arid soils. Pulses constitute stressful conditions for bacteria because they cause direct cellular damage that must be repaired and they force cells to toggle between dormancy and active physiological states, which is energetically taxing. I hypothesize that arid soil microorganisms are adapted to the variability in wet/dry cycles itself, as determined by the frequency and duration of hydration pulses. To test this, I subjected soil microbiomes from the Chihuahuan Desert to controlled incubations for a total common growth period of 60 hours, but separated into treatments in which the total active time was reached with hydration pulses of different length with intervening periods of desiccation, so as to isolate pulse length and frequency as the varying factors in the experiment. Using 16S rRNA amplicon data, I characterized changes in microbiome growth, diversity, and species composition, and tracked the individual responses to treatment intensity in the 447 most common bacterial species (phylotypes) in the soil. Considering knowledge of extremophile microbiology, I hypothesized that growth yield and diversity would decline with shorter pulses. I found that microbial diversity was indeed a direct function of pulse length, but surprisingly, total yield was an inverse function of it. Pulse regime treatments resulted in progressively more significant differences in community composition with increasing pulse length, as differently adapted phylotypes became more prominent. In fact, more than 30% of the most common bacterial phylotypes demonstrated statistically significant population growth responses to pulse length. Most responsive phylotypes were apparently best adapted to short pulse regimes (known in the literature as Nimble Responders or NIRs), while fewer did better under long pulse regimes (known as TORs or Torpid Responders). Examples of extreme NIRs and TORs could be found among bacteria from different phyla, indicating that these adaptations have occurred multiple times during evolution.
ContributorsKut, Patrick John (Author) / Garcia-Pichel, Ferran (Thesis advisor) / Sala, Osvaldo (Committee member) / Zhu, Qiyun (Committee member) / Arizona State University (Publisher)
Created2023
Description
Flowering phenology offers a sensitive and reliable biological indicator of climate change because plants use climatic and other environmental cues to initiate flower production. Drylands are the largest terrestrial biome, but with unpredictable precipitation patterns and infertile soils, they are particularly vulnerable to climate change. There is a need to increase our comprehension of how dryland plants might respond and adapt to environmental changes. I conducted a meta-analysis on the flowering phenology of dryland plants and showed that some species responded to climate change through accelerated flowering, while others delayed their flowering dates. Dryland plants advanced their mean flowering dates by 2.12 days decade-1, 2.83 days °C-1 and 2.91 days mm-1, respectively, responding to time series, temperature, and precipitation. Flowering phenology responses varied across taxonomic and functional groups, with the grass family Poaceae (-3.91 days decade1) and bulb forming Amaryllidaceae (-0.82 days decade1) showing the highest and lowest time series responses respectively, while Brassicaceae was not responsive. Analysis from herbarium specimens collected across Namibian drylands, spanning 26 species and six families, revealed that plants in hyper-arid to arid regions have lower phenological sensitivity to temperature (-9 days °C-1) and greater phenological responsiveness to precipitation (-0.56 days mm-1) than those in arid to semi-arid regions (-17 days °C-1, -0.35 days mm-1). The flowering phenology of serotinous plants showed greater sensitivity to both temperature and precipitation than that of non-serotinous plants. I used rainout shelters to reduce rainfall in a field experiment and showed that drought treatment advanced the vegetative and reproductive phenology of Cleome gynandra, a highly nutritional and medicinal semi-wild vegetable species. The peak leaf length date, peak number of leaves date, and peak flowering date of Cleome gynandra advanced by six, 10 and seven days, respectively. Lastly, I simulated drought and flood in a greenhouse experiment and found that flooding conditions resulted in higher germination percentage of C. gynandra than drought. My study found that the vegetative, and flowering phenology of dryland plants is responsive to climate change, with differential responses across taxonomic and functional groups, and aridity zones, which could alter the structure and function of these systems.
ContributorsKangombe, Fransiska Ndiiteela (Author) / Throop, Heather (Thesis advisor) / Sala, Osvaldo (Committee member) / Vivoni, Enrique (Committee member) / Pigg, Kathleen (Committee member) / Hultine, Kevin (Committee member) / Kwembeya, Ezekeil (Committee member) / Arizona State University (Publisher)
Created2023