Barrett

Barrett, The Honors College at Arizona State University proudly showcases the work of undergraduate honors students by sharing this collection exclusively with the ASU community.

Barrett accepts high performing, academically engaged undergraduate students and works with them in collaboration with all of the other academic units at Arizona State University. All Barrett students complete a thesis or creative project which is an opportunity to explore an intellectual interest and produce an original piece of scholarly research. The thesis or creative project is supervised and defended in front of a faculty committee. Students are able to engage with professors who are nationally recognized in their fields and committed to working with honors students. Completing a Barrett thesis or creative project is an opportunity for undergraduate honors students to contribute to the ASU academic community in a meaningful way.

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Evaluating Drivers of Chemodenitrification in Tropical Peat Soil

Description
Nitrous oxide (N2O) is a major contributor to the greenhouse effect and to stratospheric ozone depletion. In soils, nitrogen reduction is performed by biotic and abiotic processes, including microbial denitrification and chemical denitrification. Chemical denitrification, or chemodenitrification, is the abiotic step-wise reduction of nitrate (NO3-), nitrite (NO2-), or nitric oxide…

Nitrous oxide (N2O) is a major contributor to the greenhouse effect and to stratospheric ozone depletion. In soils, nitrogen reduction is performed by biotic and abiotic processes, including microbial denitrification and chemical denitrification. Chemical denitrification, or chemodenitrification, is the abiotic step-wise reduction of nitrate (NO3-), nitrite (NO2-), or nitric oxide (NO) to N2O in anoxic environments, with high turnover rates particularly in acidic soils. Chemodenitrification was identified in various environments, but the mechanism is still not understood. In this study, the factors influencing abiotic reduction of NO2- to N2O in acidic tropical peat soil are examined. These factors include pH, organic matter content, and dissolved ferrous iron. Anoxic peat soil from sites located in the Peruvian Amazon was used for incubations. The results show that peat soil (pH ~4.5) appears to reduce NO2- more quickly in the presence of lower pH and higher Fe(II) concentrations. NO2- is completely reduced in excess Fe(II), and Fe(II) is completely oxidized in excess NO2-, providing evidence for the proposed mechanism of chemodenitrification. In addition, first order reaction rate constants kFe(II) and kNO2- were calculated using concentration measurements over 4 hours, to test for the hypothesized reaction rate relationships kFe(II): kFe(II) kFe(II)~NO2- > kFe(II)>NO2- and kNO2-: kFe(II)NO2-. The NO2- k values followed the anticipated pattern, although the Fe(II) k value data was inconclusive. Organic material may also play a role in NO2- reduction through chemodenitrification, and future experimentation will test this possibility. How and to what extent the pH and the concentrations of organic matter and Fe(II) affect the kinetic rate of chemodenitrification will lend insight into the N2O production potential of natural tropical peatlands.
ContributorsTylor, Kaitlyn Marie (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Day, Thomas (Committee member) / School of Life Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2016-05
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Assessment of the Vertical Stratification of Microbial Community Structure in Permafrost Peatlands

Description
Peatlands are a type of wetlands where the rate of accumulation of organic matter exceed the rate of decomposition and have accumulated more than 30 cm of peat (Joosten and Clark, 2002). Peatlands store approximately 30% of all terrestrial carbon as recalcitrant peat, partially decomposed plant and microbial biomass, while…

Peatlands are a type of wetlands where the rate of accumulation of organic matter exceed the rate of decomposition and have accumulated more than 30 cm of peat (Joosten and Clark, 2002). Peatlands store approximately 30% of all terrestrial carbon as recalcitrant peat, partially decomposed plant and microbial biomass, while simultaneously producing almost 40% of the globally emitted methane (Schmidt et al., 2016), making peatlands an important component of the carbon budgets. Published research indicates that the efficiency of carbon usage among microbial communities can determine the soil-carbon response to rising temperatures (Allison et al. 2010). By determining carbon consumption in peatland soils, total community respiration response, and community structure change with additions, models of carbon use efficiency in permafrost peatlands will be well-informed and have a better understanding of how the peatlands will respond to, and utilize, increased availability of carbon compounds due to the melting permafrost. To do this, we will sequence Lutose deep core samples to observe baseline microbial community structure at different depths and different age-gradients, construct substrate incubations of glucose and propionate and observe community respiration response via a gas chromatography flame ionization detector, track the glucose and propionate additions with high-performance liquid chromatography (HPLC), and sequence the samples once more to determine if there was a deviation from the initial community structure obtained prior to the incubations. We found that our initial sequencing data was supported by previous work (Lin et al., 2014), however we were unable to sequence samples post-incubation due to time constraints. In this sequencing analysis we found that the strongest variable that made samples biologically similar was the age-gradient site in which they were extracted. We found that the group with glucose additions produced the most carbon dioxide compared with the other treatments, but was not the treatment that dominated the production of methane. Finally, in the HPLC samples that were analyzed, we found that glucose is likely forming the most by-product accumulation from mass balance calculations, while propionate is likely forming the least. Future experimentation should focus on the shortcomings of this experiment. Further analysis of 16S rRNA sequencing data from after the incubations should be analyzed to determine the change in microbial community structure throughout the experiment. Furthermore, HPLC analysis for the several samples need to be done and followed up with mass balance to determine where the added glucose and propionate are being allocated within the soil. Once these pieces of the puzzle are put into place, our original question of how the microbial community structure changes at different depths and age-gradients within permafrost peatlands will be conclusively answered.
ContributorsFrese, Alexander Nicholas (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / van Paassen, Leon (Committee member) / Sarno, Analissa (Committee member) / School of Life Sciences (Contributor) / School of Mathematical and Statistical Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2018-05
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Preliminary Metabolic Reconstruction of Two Methane Producing Microbes: Methanoregula boonei 6A8 and Methanosphaerula palustris E1-9c

Description
Methane (CH4) is very important in the environment as it is a greenhouse gas and important for the degradation of organic matter. During the last 200 years the atmospheric concentration of CH4 has tripled. Methanogens are methane-producing microbes from the Archaea domain that complete the final step in breaking down…

Methane (CH4) is very important in the environment as it is a greenhouse gas and important for the degradation of organic matter. During the last 200 years the atmospheric concentration of CH4 has tripled. Methanogens are methane-producing microbes from the Archaea domain that complete the final step in breaking down organic matter to generate methane through a process called methanogenesis. They contribute to about 74% of the CH4 present on the Earth's atmosphere, producing 1 billion tons of methane annually. The purpose of this work is to generate a preliminary metabolic reconstruction model of two methanogens: Methanoregula boonei 6A8 and Methanosphaerula palustris E1-9c. M. boonei and M. palustris are part of the Methanomicrobiales order and perform hydrogenotrophic methanogenesis, which means that they reduce CO2 to CH4 by using H2 as their major electron donor. Metabolic models are frameworks for understanding a cell as a system and they provide the means to assess the changes in gene regulation in response in various environmental and physiological constraints. The Pathway-Tools software v16 was used to generate these draft models. The models were manually curated using literature searches, the KEGG database and homology methods with the Methanosarcina acetivorans strain, the closest methanogen strain with a nearly complete metabolic reconstruction. These preliminary models attempt to complete the pathways required for amino acid biosynthesis, methanogenesis, and major cofactors related to methanogenesis. The M. boonei reconstruction currently includes 99 pathways and has 82% of its reactions completed, while the M. palustris reconstruction includes 102 pathways and has 89% of its reactions completed.
ContributorsMahendra, Divya (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Wang, Xuan (Committee member) / Stout, Valerie (Committee member) / Barrett, The Honors College (Contributor) / Computing and Informatics Program (Contributor) / School of Life Sciences (Contributor) / Biomedical Informatics Program (Contributor)
Created2014-05
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Early Assessment of Phage Communities in Amazon Peatland Soils

Description
Little is known about the diversity and role of bacteriophages in carbon (C) rich ecosystems such as peatlands in tropical and temperate regions. In fact, there is no currently published assessment of phage abundance on diversity in a key tropical ecosystem such as Amazon peatlands. To better understand phage assemblages…

Little is known about the diversity and role of bacteriophages in carbon (C) rich ecosystems such as peatlands in tropical and temperate regions. In fact, there is no currently published assessment of phage abundance on diversity in a key tropical ecosystem such as Amazon peatlands. To better understand phage assemblages in terrestrial ecosystems and how bacteriophages influence organic C cycling to final products like CO2 and CH4, phage communities and phage-like particles were recovered, quantified, and viable phage particles were enriched from pore water from contrasting Amazon peatlands. Here we present the first results on assessing Amazon bacteriophages on native heterotrophic bacteria. Several steps to test for methodological suitability were taken. First, the efficiency of iron flocculation method was determined using fluorescent microscopy counts of phage TLS, a TolC-specific and LPS-specific bacteriophage, and Escherichia coli host pre- and post-extraction method. One-hundred percent efficiency and 0.15% infectivity was evidenced. Infectivity effects were determined by calculating plaque forming units pre and post extraction method. After testing these methods, fieldwork in the Amazon peatlands ensued, where phages were enriched from pore water samples. Phages were extracted and concentrated by in tandem filtering rounds to remove organic matter and bacteria, and then iron flocculation to bind the phages and allow for precipitation onto a filter. Phage concentrates were then used for overall counts, with fluorescent microscopy, as well as phage isolation attempts. Phage isolations were performed by first testing for lysis of host cells in liquid media using OD600 absorbance of cultures with and without phage concentrate as well as attempts with the cross-streaking methods. Forty-five heterotrophic bacterial isolates obtained from the same Amazon peatland were challenged with phage concentrates. Once a putative host was found, steps were taken to further propagate and isolate the phage. Several putative phages were enriched from Amazon peatland pore water and require further characterization. TEM imaging was taken of two phages isolated from two plaques. Genomes of selected phages will be sequenced for identification. These results provide the groundwork for further characterizing the role bacteriophage play in C cycling and greenhouse gas production from Amazon peatland soils.
ContributorsSpring, Jessica Lynette (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Haydel, Shelley (Committee member) / Misra, Rajeev (Committee member) / School of Life Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2016-05

Expanding Membrane Based Isolation of Terrestrial Bacteria: Effects of Microaerophilic and Vitamin Proficient Conditions on Amazonian Peat

Description

Due to complex requirements and relationships found in terrestrial soil environments, less than 2% of bacteria has been cultured using traditional cultivation methods. The soil substrate membrane system (SSMS) is a method designed to overcome these limitations by incorporating the environmental soil as substrate. This work examines the improvements achievable…

Due to complex requirements and relationships found in terrestrial soil environments, less than 2% of bacteria has been cultured using traditional cultivation methods. The soil substrate membrane system (SSMS) is a method designed to overcome these limitations by incorporating the environmental soil as substrate. This work examines the improvements achievable through SSMS in combination with two variables known to affect microbial growth: microaerophilic conditions and vitamin availability, on Peruvian peatland soils of varying nutrient levels; poor (San Jorge), intermediate (Quistococha), and rich (Buena Vista). First, a preliminary study was performed to enhance the knowledge of SSMS applications. Following, soil samples were pre-incubated according to their treatments and inoculated onto membranes for 3 weeks. New membranes were inoculated from the first membrane's enrichment and incubated for 2 weeks. Verified microcolonies were transferred onto dilute media (dR2G 1:5 or RAVAN) through direct streaking and spreading of dilutions (10-3, 10-5, 10-7). Colony appearance was monitored with colonies being isolated and purified. Buena Vista produced the largest, most diverse microcolonies as well as the most isolates. Quistococha produced the fewest microcolonies and isolates and was the only Peatland with increased success rates in the control group. Nearly a 4:1 recovery of isolates was observed for Buena Vista's and San Jorge's treatment groups compared to their control groups. With nearly 300 isolates in isolation and sequencing, it can be concluded that SSMS improves the recovery of terrestrial bacteria, and ongoing work aims to identify the recovered isolates. 
ContributorsSoto, Noemi (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Vael, Lilly (Committee member) / Barrett, The Honors College (Contributor) / School of Life Sciences (Contributor)
Created2023-05

Determining the effect of immune checkpoint blockade on macrophages against Lewis Lung Carcinoma

Description
Immunotherapy uses the body’s immune system to find and terminate cancerous cells, and has revolutionized cancer treatment. However, in certain cancers, such as lung cancer, less than 50% of patients respond to treatment. This is in part due to the immunosuppressive tumor microenvironment, which is composed of factors that promote…

Immunotherapy uses the body’s immune system to find and terminate cancerous cells, and has revolutionized cancer treatment. However, in certain cancers, such as lung cancer, less than 50% of patients respond to treatment. This is in part due to the immunosuppressive tumor microenvironment, which is composed of factors that promote tumor growth and proliferation. Tumor cells create a highly immunosuppressive microenvironment by triggering the anti-inflammatory phenotype of myeloid immune cells, which largely consist of tumor-associated macrophages (TAMs). Anti-PD-1 and anti-PD-L1 immune checkpoint blockade therapy helps promote the T cell anti-tumor response by releasing the brakes on cytotoxic T-cells. However, it is unclear how TAMs respond to these immune checkpoint antibodies. Our lab hypothesizes that blockade of the PD-1/PD-L1 signaling pathway drives a pro-inflammatory macrophage phenotype. This hypothesis is supported by data generated in the B16F10 murine melanoma model, but it is unknown whether macrophage response to PD-L1 blockade is generalizable to other tumor contexts. Thus, the goal of the project is to determine the impact of immune checkpoint blockade on murine macrophages in the Lewis Lung Carcinoma (LLC) model. Using Flow Cytometry, macrophage phenotypes will be analyzed to confirm whether a pro- inflammatory or anti-tumor response is generated.
ContributorsKorpe, Sara (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Lancaster, Jessica (Committee member) / Barrett, The Honors College (Contributor) / Economics Program in CLAS (Contributor) / School of Life Sciences (Contributor)
Created2024-05
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Evaluating the Consumption Rates of Primary Versus Secondary Fermentation Substrates and Methane Production of Northern Peatlands

Description
Northern peatland carbon cycling is under close observation and is critical to include in models projecting the future effects of climate change as these ecosystems represent a significant source of atmospheric methane (CH4). Changes in the in situ conditions, brought upon by the warming climate, could alter the rates of…

Northern peatland carbon cycling is under close observation and is critical to include in models projecting the future effects of climate change as these ecosystems represent a significant source of atmospheric methane (CH4). Changes in the in situ conditions, brought upon by the warming climate, could alter the rates of organic matter decomposition and accelerate the emissions of greenhouse, changing northern peatland’s status as a carbon sink. In order to develop a better understanding of the climate’s effect on the microbial community composition, carbon decomposition cascade, and flux of CH4 and CO2, anoxic soil microcosms were supplemented with either glucose or propionate to test the distinct intermediary metabolism of four northern peatland sites with statistically similar geochemistry that exist across a climate gradient. Lutose (LT) and Bog Lake (BL) consumed the supplemented glucose at the highest rates, 42.6 mg/L per day and 39.5 mg/L per day respectively. Chicago Bog (CB) and Daring Lake (DL) consumed the supplemented propionate at the highest rates, 5.26 mg/L per day and 4.34 mg/L per day respectively. BL microcosms showed low levels of methanogenesis as CH4 concentrations reached a maximum of 2.61 µmol/g dry soil in the treatments. In DL, the site with the highest production of CH4, the low abundance of hydrogenotrophic methanogens (Methanocellaceae and Methanoregulaceae) and relatively steady concentrations of acetate and formate could indicate that these are the more desired methanogenic substrates. These findings are indicative of the differences in metabolic potential found across these geochemically similar peatlands, lending to climate variables being a major driver in microbial community potential. To further characterize the intermediary metabolism and the effect of the climate gradient in these sites, future experimentations should incorporate 13C DNA-stable isotope probing data, establish a mass balance of the system, and incubate the microcosms at their respective in situ temperatures.
ContributorsBourquin, Brandon Phillip (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Marcus, Andrew (Committee member) / Sarno, Analissa F. (Committee member) / School of Life Sciences (Contributor) / Barrett, The Honors College (Contributor)
Created2020-05
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Ecological Diversity of Methanotrophs in Amazon Peatlands

Description

Tropical peatlands play a critical role in global carbon storage and greenhouse gas flux, yet the role of microbial communities in these ecosystems remains poorly understood. Methane-oxidizing bacteria (MOB) are considered an efficient biological filter for methane and can mitigate its release into the atmosphere, facilitating an ecosystem’s capacity to…

Tropical peatlands play a critical role in global carbon storage and greenhouse gas flux, yet the role of microbial communities in these ecosystems remains poorly understood. Methane-oxidizing bacteria (MOB) are considered an efficient biological filter for methane and can mitigate its release into the atmosphere, facilitating an ecosystem’s capacity to become a net sink. Prokaryotic gene amplicon surveys targeting a unique biomarker instead of a universal one (i.e., 16S rRNA) can reveal a more comprehensive analysis of microbial communities with ecological functions (i.e., methanotrophy). The alpha subunit of particulate methane monooxygenase (pmoA) is commonly targeted as a phylogenetic biomarker for both aerobic and anaerobic MOB. Here, we tested three different primer sets and investigated their ability to assess methanotrophic diversity across three biogeochemically distinct tropical peatland sites in the Pastaza-Marañón foreland basin (PMFB) in western Amazonia. The results showed that sequencing using 16S rRNA and pmoA genes revealed differences in MOB taxonomic identification in 21 tropical peat soils. Beta diversity analysis of pmoA genes suggests that site location is not the main driver of differences in MOB community makeup. This work offers insight into the strengths and weaknesses of targeted gene amplicon surveys using 16S and pmoA from tropical peat soils as a case study.
ContributorsBrzezinski, Hannah (Author) / Cadillo-Quiroz, Hinsby (Thesis director) / Wojciechowski, Martin (Committee member) / Barrett, The Honors College (Contributor) / School of Life Sciences (Contributor)
Created2022-05