Effect of Pyomelanin Production on Oxidative Stress in an Aeromonas Zebrafish Gut Isolate

Presenter: Helena Klein

Faculty Mentor: Karen Guillemin, Cathy Robinson

Presentation Type: Poster 72

Primary Research Area: Science

Major: Biology

Bacteria have rapid growth rates, which allow us to study their adaptive evolution in the lab to selected environments. By studying the genetic changes that occur during the evolutionary process, we can learn about selective pressures experienced by bacteria when evolved in selected conditions. Through passaging of a strain of a natural zebrafish gut isolate, Aeromonas ZOR0001, we isolated one strain that has increased pigmentation compared to the wildtype. This pigmentation is a result of accumulation of pyomelanin in the extracellular environment. We confirmed through genetic sequencing a mutation in the isolate’s metabolic pathway known to be involved in pyomelanin production. Pyomelanin production has been shown in other organisms to be linked to increased resilience to oxidative stress. Therefore, we hypothesized this mutation confers a fitness advantage to this evolved isolate compared to the ancestral strain. Therefore we generated a genetic knockout of the mutated gene in the ancestral strain and used hydrogen peroxide to simulate oxidative stress in vitro. We found that the knockout strain did better than the wild type strain. This demonstrates that pyomelanin production confers resistance to oxidative stress in Aeromonas ZOR0001 which suggests an adaptive advantage for in vivo growth. Knowledge of genes that increase fitness in bacterial strains in the gut can ultimately allow for better probiotics to be developed with wide repercussions for human health.

A Lithostratigraphic Analysis of the Crooked River Mascall Formation

Presenter(s): Alexandra Thompson

Faculty Mentor(s): Samantha Hopkins

Poster 72

Session: Sciences

This project presents a comprehensive lithological and biostratigraphic record of the Miocene Mascall Formation deposits of the Crooked River Basin in Central Oregon. The Columbia River Basalt Group (CRBG) covered the Crooked River Basin and much of the Pacific Northwest in the middle Miocene, altering the landscape and ecosystem. As a result of this event, an analysis of the depositional history of this region is worthwhile because it explores the impact of large scale basalt flows on subsequent basin evolution. University of Oregon geology students have measured stratigraphic sections in four different locations across the Crooked River basin in order to quantify the differences in depositional history across the basin. The sites are stratigraphically situated between the lower boundary CRBG and upper capping Rattlesnake Ash Flow Tuff (RAFT). For each region, we have created a representative stratigraphic column, and correlated rock units between the regions. The Mascall Formation in the Crooked River Basin is consistent with published descriptions of the Lower Mascall Formation: mostly fine siltstone and sandstone with diatomite, ash, and chert deposits and some tuff strata (Bestland, 1998). Each of the four sites share characteristics of the Lower Mascall which suggests similar depositional environments across the sites; however, the sections vary in the thickness and representation of individual identifiable strata, suggesting variation in where deposition was greatest through the half-million years of the section. This is the first comprehensive assessment of the stratigraphy of the Crooked River Basin, which has significant implications for understanding landscape reorganization following volcanism.