A Forward Genetic Screen for Genes Required in C. elegans Embryonic Morphogenesis

Presenter(s): Alexander Miller − Biology

Faculty Mentor(s): Bruce Bowerman, Molly Jud

Oral Session 3M

Research Area: Natural/Physical Sciences

Funding: NIH funding, Oregon Undergraduate Researchers in SPUR (OURS) summer scholarship

Our research in the Bowerman laboratory focuses on embryonic morphogenesis in the soil nematode, Caenorhabditis elegans. Morphogenesis is the coordinated movement and shape changes of cells that occur during development in all animals. Defects in this process can cause a variety of human disorders, including neural tube closure, vascular, and
limb developmental defects. My research involves a forward genetic screen for genes required in C. elegans embryonic morphogenesis, utilizing a collection of roughly 1,000 temperature-sensitive embryonic lethal (TS-EL) mutants previously created in the Bowerman laboratory. TS-EL mutants are first terminally phenotyped to identify mutants with penetrant morphogenetic defects, which are then genetically characterized to isolate recessive, loss-of-function, single-mutant alleles. We identify the mutant genes through a combination of SNP-mapping and whole-genome sequencing to find candidate genes, followed by complementation testing with null alleles when available. Mutant strains are sent to our collaborators, the Zhirong Bao laboratory at the Sloan Kettering Cancer Center, for single cell-fate lineaging. This allows us to more accurately distinguish between morphogenesis and cell fate patterning defective mutants. I have terminally-phenotyped nineteen mutants, fourteen of which have penetrant phenotypes (where 70% of embryos display a single phenotype), and genetically characterized six recessive, single mutants. Alleles or388ts and or1113ts have been genetically identified to be mutations in the gene let-19, which is a transcriptional coactivation subunit containing Mediator domains. Allele or542ts is a mutation in the gene chaf-1, a chromatin assembly factor likely regulating gene transcription. Allele or614ts is a mutation in the zwl-1, which codes for a kinetochore protein. While let-19 and chaf-1 fall within the scope of this project, our allele of zwl-1 is probably a weak cell division-defective instead of a morphogenesis-defective mutant, and thus is no longer being studied. Most of the genes we have identified are involved in gene expression regulation, suggesting there is a preexisting gene regulatory program for morphogenesis. Future work is to be done to expand our and the Bao laboratory’s roster of genes known to be required for morphogenesis. This research will help to create a deeper understanding of the basic genetic pathways and cell biological changes required for embryonic morphogenesis in C. elegans, thus improving our comprehension of human development.

Quantifying Ocean Dynamics through Iceberg Tracking in Ilulissat Fjord

Presenter(s): Richelle Ann Cabatic − Physics

Faculty Mentor(s): David Sutherland, Kristin Schild

Poster 2

Research Area: Natural/Physical Sciences

Funding: NSF Iceberg Grant – Sutherland Lab

When Greenland’s tidewater glaciers reach the ocean, they break off numerous icebergs into fjords. These icebergs travel through the fjord and out into the ocean. All the while different types of water circulate through the fjord, meeting with the glacier’s terminus and affecting it’s stability. The tidewater glacier, Jakobshavn Isbrae, and it’s accompanying fjord, Ilulissat Fjord, is of particular interest due to its very active export of icebergs. Many studies have addressed Jakobshavn’s glacial front, but little is known about Ilulissat’s ocean circulation due to the difficulty of collecting field measurements in the ice-choked region. Through our study, we deploy transmitting GPS units on icebergs in Ilulissat Fjord, thereby tracking iceberg movement and, in part, the region’s ocean circulation. Using icebergs as proxies for surface circulation thus provides an alternative to deploying marine instruments that have minimal likelihood for survival in the treacherous fjord environment. Preliminary results of our study show that: at a distance of 35km away from the glacier terminus, iceberg movement is no longer dominated by glacial calving events; there are eddy circulation patterns at fjord widening locations; and, that the studied icebergs move at an average speed of 0.8 km/hr. This study has the potential to help oceanographers and engineers learn more about the Ilulissat system’s circulation dynamics, and inform glaciologists about how Jakobshavn Glacier melt rates and acceleration is affected by the circulation.