Matching Items (42)
Description
Cyanobacteria and algae living inside carbonate rocks (endoliths) have long been considered major contributors to bioerosion. Some bore into carbonates actively (euendoliths); others simply inhabit pre-existing pore spaces (cryptoendoliths). While naturalistic descriptions based on morphological identification have traditionally driven the field, modern microbial ecology has shown that this approach is insufficient to assess microbial diversity or make functional inferences. I examined endolithic microbiomes using 16S rRNA genes and lipid-soluble photosynthetic pigments as biomarkers, with the goal of reassessing endolith diversity by contrasting traditional and molecular approaches. This led to the unexpected finding that in all 41 littoral carbonate microbiomes investigated around Isla de Mona (Puerto Rico) and Menorca (Spain) populations of anoxygenic phototrophic bacteria (APBs) in the phyla Chloroflexi and Proteobacteria, were abundant, even sometimes dominant over cyanobacteria. This was not only novel, but it suggested that APBs may have been previously misidentified as morphologically similar cyanobacteria, and opened questions about their potential role as euendoliths. To test the euendolithic role of photosynthetic microbes, I set a time-course experiment exposing virgin non-porous carbonate substrate in situ, under the hypothesis that only euendoliths would be able to initially colonize it. This revealed that endolithic microbiomes, similar in biomass to those of mature natural communities, developed within nine months of exposure. And yet, APB populations were still marginal after this period, suggesting that they are secondary colonizers and not euendolithic. However, elucidating colonization dynamics to a sufficiently accurate level of molecular identification among cyanobacteria required the development of a curated cyanobacterial 16S rRNA gene reference database and web tool, Cydrasil. I could then detect that the pioneer euendoliths were in a novel cyanobacterial clade (named UBC), immediately followed by cyanobacteria assignable to known euendoliths. However, as bioerosion proceeded, a diverse set of likely cryptoendolithic cyanobacteria colonized the resulting pore spaces, displacing euendoliths. Endolithic colonization dynamics are thus swift but complex, and involve functionally diverse agents, only some of which are euendoliths. My work contributes a phylogenetically sound, functionally more defined understanding of the carbonate endolithic microbiome, and more specifically, Cydrasil provides a user-friendly framework to routinely move beyond morphology-based cyanobacterial systematics.
ContributorsRoush, Daniel (Author) / Garcia-Pichel, Ferran (Thesis advisor) / Anbar, Ariel (Committee member) / Cadillo-Quiroz, Hinsby (Committee member) / Cao, Huansheng (Committee member) / Arizona State University (Publisher)
Created2020
Description
Modern agriculture faces multiple challenges: it must produce more food for a growing global population, adopt more efficient and sustainable management strategies, and adapt to climate change. One potential component of a sustainable management strategy is the application of biochar to agricultural soils. Biochar is the carbon-rich product of biomass pyrolysis, which contains large proportions of aromatic compounds that influence its stability in soil. Concomitant with carbon sequestration, biochar has the potential to increase soil fertility through increasing soil pH, moisture and nutrient retention. Changes in the soil physical and chemical properties can result in shifts in the soil microbiome, which are the proximate drivers of soil processes. This dissertation aims to determine the compositional and functional changes in the soil microbial community in response to the addition of a low-volatile matter biochar. First, the impact of biochar on the bacterial community was investigated in two important agricultural soils (Oxisol and Mollisol) with contrasting fertility under two different cropping systems (conventional sweet corn and zero-tillage napiergrass) one month and one year after the initial addition. This study revealed that the effects of biochar on the bacterial community were most pronounced in the Oxisol under napiergrass cultivation, however soil type was the strongest determinant of the bacterial community. A follow-up study was conducted using shotgun metagenomics to probe the functional community of soil microcosms, which contained Oxisol soil under napiergrass two years after the initial addition of biochar. Biochar significantly increased total carbon in the soils but had little impact on other soil properties. Theses analyses showed that biochar-amended soil microcosms exhibited significant shifts in the functional community and key metabolic pathways related to carbon turnover and denitrification. Given the distinct alterations to the biochar-amended community, deoxyribose nucleic acid (DNA) stable isotope probing was used to target the active populations. These analyses revealed that biochar did not significantly shift the active community in soil microcosms. Overall, these results indicate that the impact of biochar on the active soil community is transient in nature. Yet, biochar may still be a promising strategy for long-term carbon sequestration in agricultural soils.
ContributorsYu, Julian (Author) / Penton, C. Ryan (Thesis advisor) / Cadillo-Quiroz, Hinsby (Thesis advisor) / Garcia-Pichel, Ferran (Committee member) / Hall, Sharon (Committee member) / Arizona State University (Publisher)
Created2020
Description
I studied the molecular mechanisms of ultraviolet radiation mitigation (UVR) in the terrestrial cyanobacterium Nostoc punctiforme ATCC 29133, which produces the indole-alkaloid sunscreen scytonemin and differentiates into motile filaments (hormogonia). While the early stages of scytonemin biosynthesis were known, the late stages were not. Gene deletion mutants were interrogated by metabolite analyses and confocal microscopy, demonstrating that the ebo gene cluster, was not only required for scytonemin biosynthesis, but was involved in the export of scytonemin monomers to the periplasm. Further, the product of gene scyE was also exported to the periplasm where it was responsible for terminal oxidative dimerization of the monomers. These results opened questions regarding the functional universality of the ebo cluster. To probe if it could play a similar role in organisms other than scytonemin producing cyanobacteria, I developed a bioinformatic pipeline (Functional Landscape And Neighbor Determining gEnomic Region Search; FLANDERS) and used it to scrutinize the neighboring regions of the ebo gene cluster in 90 different bacterial genomes for potentially informational features. Aside from the scytonemin operon and the edb cluster of Pseudomonas spp., responsible for nematode repellence, no known clusters were identified in genomic ebo neighbors, but many of the ebo adjacent regions were enriched in signal peptides for export, indicating a general functional connection between the ebo cluster and biosynthetic compartmentalization. Lastly, I investigated the regulatory span of the two-component regulator of the scytonemin operon (scyTCR) using RNAseq of scyTCR deletion mutants under UV induction. Surprisingly, the knockouts had decreased expression levels in many of the genes involved in hormogonia differentiation and in a putative multigene regulatory element, hcyA-D. This suggested that UV could be a cue for developmental motility responses in Nostoc, which I could confirm phenotypically. In fact, UV-A simultaneously elicited hormogonia differentiation and scytonemin production throughout a genetically homogenous population. I show through mutant analyses that the partner-switching mechanism coded for by hcyA-D acts as a hinge between the scytonemin and hormogonia based responses. Collectively, this dissertation contributes to the understanding of microbial adaptive responses to environmental stressors at the genetic and regulatory level, highlighting their phenomenological and mechanistic complexity.
ContributorsKlicki, Kevin (Author) / Garcia-Pichel, Ferran (Thesis advisor) / Wilson, Melissa (Committee member) / Mukhopadhyay, Aindrila (Committee member) / Misra, Rajeev (Committee member) / Arizona State University (Publisher)
Created2021
Description
The ability to find evidence of life on early Earth and other planets is constrained by the current understanding of biosignatures and our ability to differentiate fossils from abiotic mimics. When organisms transition from the living realm to the fossil record, their morphological and chemical characteristics are modified, usually resulting in the loss of information. These modifications can happen during early and late diagenesis and differ depending on local geochemical properties. These post-depositional modifications need to be understood to better interpret the fossil record. Siliceous hot spring deposits (sinters) are of particular interest for biosignature research as they are early Earth analog environments and targets for investigating the presence of fossil life on Mars. As silica-supersaturated fluids flow from the vent to the distal apron, they precipitate non-crystalline opal-A that fossilizes microbial communities at a range in scales (μm-cm). Therefore, many studies have documented the ties between the active microbial communities and the morphological and chemical biosignatures in hot springs. However, far less attention has been placed on understanding preservation in systems with complex mineralogy or how post-depositional alteration affects the retention of biosignatures. Without this context, it can be challenging to recognize biosignatures in ancient rocks. This dissertation research aims to refine our current understanding of biosignature preservation and retention in sinters. Biosignatures of interest include organic matter, microfossils, and biofabrics. The complex nature of hot springs requires a comprehensive understanding of biosignature preservation that is representative of variable chemistries and post-depositional alterations. For this reason, this dissertation research chapters are field site-based. Chapter 2 investigates biosignature preservation in an unusual spring with mixed opal-A-calcite mineralogy at Lýsuhóll, Iceland. Chapter 3 tracks how silica diagenesis modifies microfossil morphology and associated organic matter at Puchuldiza, Chile. Chapter 4 studies the effects of acid fumarolic overprinting on biosignatures in Gunnuhver, Iceland. To accomplish this, traditional geologic methods (mapping, petrography, X-ray diffraction, bulk elemental analyses) were combined with high-spatial-resolution elemental mapping to better understand diagenetic effects in these systems. Preservation models were developed to predict the types and styles of biosignatures that can be present depending on the depositional and geochemical context. Recommendations are also made for the types of deposits that are most likely to preserve biosignatures.
ContributorsJuarez Rivera, Marisol (Author) / Farmer, Jack D (Thesis advisor) / Hartnett, Hilairy E (Committee member) / Shock, Everett (Committee member) / Garcia-Pichel, Ferran (Committee member) / Trembath-Reichert, Elizabeth (Committee member) / Arizona State University (Publisher)
Created2021
Description
Biological soil crusts (BSCs) dominate the soil surface of drylands in the western United States and possess properties thought to influence local hydrology. Little agreement exists, however, on the effects of BSCs on runoff, infiltration, and evaporative rates. This study aims to improve the predictive capability of an ecohydrology model in order to understand how BSCs affect the storage, retention, and infiltration of water into soils characteristic of the Colorado Plateau. A set of soil moisture measurements obtained at a climate manipulation experiment near Moab, Utah, are used for model development and testing. Over five years, different rainfall treatments over experimental plots resulted in the development of BSC cover with different properties that influence soil moisture differently. This study used numerical simulations to isolate the relative roles of different BSC properties on the hydrologic response at the plot-scale. On-site meteorological, soil texture and vegetation property datasets are utilized as inputs into a ecohydrology model, modified to include local processes: (1) temperature-dependent precipitation partitioning, snow accumulation and melt, (2) seasonally-variable potential evapotranspiration, (3) plant species-specific transpiration factors, and (4) a new module to account for the water balance of the BSC. Soil, BSC and vegetation parameters were determined from field measurements or through model calibration to the soil moisture observations using the Shuffled Complex Evolution algorithm. Model performance is assessed against five years of soil moisture measurements at each experimental site, representing a wide range of crust cover properties. Simulation experiments were then carried out using the calibrated ecohydrology model in which BSC parameters were varied according to the level of development of the BSC, as represented by the BSC roughness. These results indicate that BSCs act to both buffer against evaporative soil moisture losses by enhancing BSC moisture evaporation and significantly alter the rates of soil water infiltration by reducing moisture storage and increasing conductivity in the BSC. The simulation results for soil water infiltration, storage and retention across a wide range of meteorological events help explain the conflicting hydrologic outcomes present in the literature on BSCs. In addition, identifying how BSCs mediate infiltration and evaporation processes has implications for dryland ecosystem function in the western United States.
ContributorsWhitney, Kristen M (Author) / Vivoni, Enrique R (Thesis advisor) / Farmer, Jack D (Committee member) / Garcia-Pichel, Ferran (Committee member) / Arizona State University (Publisher)
Created2015
Description
Biological Soil Crusts (BSCs) are organosedimentary assemblages comprised of microbes and minerals in topsoil of terrestrial environments. BSCs strongly impact soil quality in dryland ecosystems (e.g., soil structure and nutrient yields) due to pioneer species such as Microcoleus vaginatus; phototrophs that produce filaments that bind the soil together, and support an array of heterotrophic microorganisms. These microorganisms in turn contribute to soil stability and biogeochemistry of BSCs. Non-cyanobacterial populations of BSCs are less well known than cyanobacterial populations. Therefore, we attempted to isolate a broad range of numerically significant and phylogenetically representative BSC aerobic heterotrophs. Combining simple pre-treatments (hydration of BSCs under dark and light) and isolation strategies (media with varying nutrient availability and protection from oxidative stress) we recovered 402 bacterial and one fungal isolate in axenic culture, which comprised 116 phylotypes (at 97% 16S rRNA gene sequence homology), 115 bacterial and one fungal. Each medium enriched a mostly distinct subset of phylotypes, and cultivated phylotypes varied due to the BSC pre-treatment. The fraction of the total phylotype diversity isolated, weighted by relative abundance in the community, was determined by the overlap between isolate sequences and OTUs reconstructed from metagenome or metatranscriptome reads. Together, more than 8% of relative abundance of OTUs in the metagenome was represented by our isolates, a cultivation efficiency much larger than typically expected from most soils. We conclude that simple cultivation procedures combined with specific pre-treatment of samples afford a significant reduction in the culturability gap, enabling physiological and metabolic assays that rely on ecologically relevant axenic cultures.
ContributorsNunes Da Rocha, Ulisses (Author) / Cadillo-Quiroz, Hinsby (Author) / Karaoz, Ulas (Author) / Rajeev, Lara (Author) / Klitgord, Niels (Author) / Dunn, Sean (Author) / Truong, Viet (Author) / Buenrostro, Mayra (Author) / Bowen, Benjamin P. (Author) / Garcia-Pichel, Ferran (Author) / Mukhopadhyay, Aindrila (Author) / Northen, Trent R. (Author) / Brodie, Eoin L. (Author) / College of Liberal Arts and Sciences (Contributor)
Created2015-03-19
Description
The experiments conducted in this report supported previous evidence (Bethany et al., 2019) that a newly identified predatory bacterium causes a higher rate of mortality in the biological soil crust cyanobacterium M. vaginatus when in hot soils than in cold soils. I predicted that the extracellular propagules of this predatory bacterium were inactivated at seasonally low temperatures, rendering them non-viable when introduced to M. vaginatus at room temperature. However, I found that the predatory bacterium became only transiently inactive at low temperatures, recovering its pathogenicity when later exposed to warmer temperatures. By contrast, inactivation of infectivity was complete by exposure in both liquid and dry conditions for five days at 40 °C. I also expected that its infectivity towards M. vaginatus was temperature dependent. Indeed, infection was hampered and did not cause high mortality when predator and prey were incubated at or below 10 °C, which could have been due to slowed metabolisms of M. vaginatus or to an inability of the predatory bacterium to attack in cold conditions. Above 10 °C, when M. vaginatus grew faster, time to full death of predator/prey incubations correlated with the rate of growth of healthy cultures.
The experiments in this study observed a correlation between the growth rate of uninfected cultures and the decay rate of infected cultures, meaning that temperatures that cultures that displayed a higher growth rate for uninfected M. vaginatus would die faster when infected with the predatory bacterium. Infected cultures that were incubated at temperatures 4 and 10 °C did not display death and this could have been due to lower activity of M. vaginatus at lower temperatures or the inability for the predatory bacterium to attack at lower temperatures.
The experiments in this study observed a correlation between the growth rate of uninfected cultures and the decay rate of infected cultures, meaning that temperatures that cultures that displayed a higher growth rate for uninfected M. vaginatus would die faster when infected with the predatory bacterium. Infected cultures that were incubated at temperatures 4 and 10 °C did not display death and this could have been due to lower activity of M. vaginatus at lower temperatures or the inability for the predatory bacterium to attack at lower temperatures.
ContributorsAhamed, Anisa Nour (Author) / Garcia-Pichel, Ferran (Thesis director) / Giraldo Silva, Ana Maria (Committee member) / Bethany Rakes, Julie (Committee member) / School of Molecular Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2020-05
Description
With the development and successful landing of the NASA Perseverance rover, there has been growing interest in identifying how evidence of ancient life may be preserved and recognized in the geologic record. Environments that enable fossilization of biological remains are termed, “taphonomic windows”, wherein signatures of past life may be detected. In this dissertation, I have sought to identify taphonomic windows in planetary-analog environments with an eye towards the exploration of Mars. In the first chapter, I describe how evidence of past microbial life may be preserved within serpentinizing systems. Owing to energetic rock-water reactions, these systems are known to host lithotrophic and organotrophic microbial communities. By investigating drill cores from the Samail Ophiolite in Oman, I report morphological and associated chemical biosignatures preserved in these systems as a result of subsurface carbonation. As serpentinites are known to occur on Mars and potentially other planetary bodies, these deposits potentially represent high-priority targets in the exploration for past microbial life. Next, I investigated samples from Atacama Desert, Chile, to understand how evidence of life may be preserved in ancient sediments formed originally in evaporative playa lakes. Here, I describe organic geochemical and morphological evidence of life preserved within sulfate-dominated evaporite rocks from the Jurassic-Cretaceous Tonel Formation and Oligocene San Pedro Formation. Because evaporative lakes are considered to have been potentially widespread on Mars, these deposits may represent additional key targets to search for evidence of past life. In the final chapter, I describe the fossilization potential of surficial carbonates by investigating Crystal Geyser, an active cold spring environment. Here, carbonate minerals precipitate rapidly in the presence of photosynthetic microbial mat communities. I describe how potential biosignatures are initially captured by mineralization, including cell-like structures and microdigitate stromatolites. However, these morphological signatures quickly degrade owing to diagenetic dissolution and recrystallization reactions, as well as textural coarsening that homogenizes the carbonate fabric. Overall, my dissertation underscores the complexity of microbial fossilization and highlights chemically-precipitating environments that may serve as high-priority targets for astrobiological exploration.
ContributorsZaloumis, Jonathan (Author) / Farmer, Jack D (Thesis advisor) / Garcia-Pichel, Ferran (Committee member) / Trembath-Reichert, Elizabeth (Committee member) / Ruff, Steven W (Committee member) / Shock, Everett L (Committee member) / Arizona State University (Publisher)
Created2021
Description
Predatory bacteria are a guild of heterotrophs that feed directly on other living bacteria. They belong to several bacterial lineages that evolved this mode of life independently and occur in many microbiomes and environments. Current knowledge of predatory bacteria is based on culture studies and simple detection in natural systems. The ecological consequences of their activity, unlike those of other populational loss factors like viral infection or grazing by protists, are yet to be assessed. During large-scale cultivation of biological soil crusts intended for arid soil rehabilitation, episodes of catastrophic failure were observed in cyanobacterial growth that could be ascribed to the action of an unknown predatory bacterium using bioassays. This predatory bacterium was also present in natural biocrust communities, where it formed clearings (plaques) up to 9 cm in diameter that were visible to the naked eye. Enrichment cultivation and purification by cell-sorting were used to obtain co-cultures of the predator with its cyanobacterial prey, as well as to identify and characterize it genomically, physiologically and ultrastructurally. A Bacteroidetes bacterium, unrelated to any known isolate at the family level, it is endobiotic, non-motile, obligately predatory, displays a complex life cycle and very unusual ultrastructure. Extracellular propagules are small (0.8-1.0 µm) Gram-negative cocci with internal two-membrane-bound compartmentalization. These gain entry to the prey likely using a suite of hydrolytic enzymes, localizing to the cyanobacterial cytoplasm, where growth begins into non-compartmentalized pseudofilaments that undergo secretion of vesicles and simultaneous multiple division to yield new propagules. I formally describe it as Candidatus Cyanoraptor togatus, hereafter Cyanoraptor. Its prey range is restricted to biocrust-forming, filamentous, non-heterocystous, gliding, bundle-making cyanobacteria. Molecular meta-analyses showed its worldwide distribution in biocrusts. Biogeochemical analyses of Cyanoraptor plaques revealed that it causes a complete loss of primary productivity, and significant decreases in other biocrusts properties such as water-retention and dust-trapping capacity. Extensive field surveys in the US Southwest revealed its ubiquity and its dispersal-limited, aggregated spatial distribution and incidence. Overall, its activity reduces biocrust productivity by 10% at the ecosystem scale. My research points to predatory bacteria as a significant, but overlooked, ecological force in shaping soil microbiomes.
ContributorsBethany Rakes, Julie Ann (Author) / Garcia-Pichel, Ferran (Thesis advisor) / Gile, Gillian (Committee member) / Cao, Huansheng (Committee member) / Jacobs, Bertram (Committee member) / Arizona State University (Publisher)
Created2022
Description
Biocrusts are microbial communities that inhabit arid soil surfaces, providing essential services to dryland ecosystems. A paradoxical filamentous cyanobacterium, Microcoleus vaginatus, resides within the biocrust. While is often pioneers the colonization of bare, nutrient-poor desert soils worldwide, it cannot fix dinitrogen. In nature, M. vaginatus coexists with a unique microbial community, a “cyanosphere”, that is characterized by a high abundance of diazotrophic heterotrophs. This suggests mutualistic relationships wherein nutrients are traded between phototrophs and heterotrophs. To explore these relationships, I performed targeted, pedigreed isolation of cyanosphere members and used co-cultivation to recreate the mutualism in culture. Results showed that, in the absence of fixed nitrogen, M. vaginatus grew well when co-cultured with cyanosphere diazotrophs, but only poorly or not at all when alone or with non-cyanosphere diazotrophs. In agreement with this, the experimental provision of nitrogen to natural populations resulted in a loss of diazotrophs from the cyanosphere compared to controls, but the addition of phosphorus did not. Additionally, the convergence of M. vaginatus trichomes into large bundles held by a common sheath was elicited in culture by the addition of cyanosphere diazotrophs, pointing to a role of cyanobacterial motility responses in the development of mutualistic interactions. I then demonstrated that the tendency of M. vaginatus to stay within bundles and close to the sheath-dwelling cyanosphere was dependent on the cyanosphere population size. This effect was likely mediated by glutamate that acted as a signaling molecule rather than as a N source and impacted the gliding speed and negative chemophobic responses on the cyanobacterium. Glutamate seems to be used as a cue to spatially optimize cyanobacterium-cyanosphere mutualistic exchanges. My findings have potential practical applications in restoration ecology, which I further pursued experimentally. Co-inoculation of soil with cyanosphere diazotrophs resulted in swifter development of biocrusts over inoculation with the cyanobacterium only. Further, their addition to disturbed native soils containing traces of cyanobacteria sufficed for the formation of cohesive biocrusts without cyanobacterial inoculation. The inclusion of such “biocrust probiotics” in biocrust restoration is recommended. Overall, this body of work elucidates the hitherto unknown role of beneficial heterotrophic bacteria in the initial formation and development of biocrusts.
ContributorsNelson, Corey (Author) / Garcia-Pichel, Ferran (Thesis advisor) / Penton, C. Ryan (Committee member) / Gile, Gillian (Committee member) / Bean, Heather (Committee member) / Arizona State University (Publisher)
Created2021