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Formins are potent regulators of actin dynamics that can remodel the actin cytoskeleton to control cell shape, cell cytokinesis, and cell morphogenesis. The defining feature of formins is the formin homology 2 (FH2) domain (Paul and Pollard, 2008), which promotes actin filament assembly while processively moving along the polymerizing filament barbed end. INFT-1 is one of six formin family members present in Caenorhabditis elegans (Hunt-Newbury et al., 2007) and is most closely related to vertebrate INF2, an inverted formin with regulatory domains in the C- rather than N-terminus. Nematode INFT-1 contains both formin homology 1 (FH1) and formin homology 2 (FH2) domains. However, it does not share the regulatory N-terminal Diaphanous Inhibitory Domain (DID) domain and C-terminal Diaphanous Autoregulatory Domain (DAD) domain found in mammalian INF2. In contrast to mammalian INF2, the sequence of INFT-1 starts immediately at FH1 domain and C-terminal region of INFT-1 shares little homology with INF2, suggesting that elegans INFT-1 is regulated by other mechanisms. We used fluorescence spectroscopy to determine the effect of INFT-1 FH1FH2 on actin assembly and total internal reflection fluorescence microscopy to investigate how INFT-1 formin homology 1 and formin homology 2 domains (FH1FH2) mediate filament nucleation and elongation. INFT-1 FH1FH2 nucleates actin filament and promote actin assembly. However, INFT-1 FH1FH2 reduces filament barbed-end elongation rates in the absence or presence of profilin. Evidences demonstrated that INFT-1 is non-processive, indicating a unique mechanism of nucleation. INFT-1 nucleation efficiency is similar to the efficiency of Arabidopsis FORMIN1 (AFH1), another non-processive formin. High phosphate affected the assembly activity of INFT-1 FH1FH2 in the absence or presence of profilin. INFT is thus the second example of a non-processive formin member and will allow a more detailed understanding of the mechanistic difference between processive and non-processive formins. / Master of Science

Since the 1970s, a growing body of research has suggested that bacteria play an active role in precipitation. These bacteria are capable of catalyzing the formation of ice at relatively warm temperatures utilizing a specific protein family which aids in the binding of water molecules. However, the overall biodiversity, concentration, and relationship of ice nucleation active (ice+) bacteria with air mass trajectories and precipitation chemistry is not well studied. Precipitation events were collected over 15 months in Blacksburg, VA and ice+ bacteria were isolated from these samples. From these samples, 33,134 total isolates were screened for ice nucleation activity (INA) at -8 °C. A total of 593 of these isolated positively confirmed for INA at the same temperature in subsequent tests. The precipitation events had a mean concentration of 384±147 colony forming units per liter. While the majority of confirmed ice+ bacteria belonged to the gammaproteobacteria, a well-studied class of bacteria, including ice+ species of Pseudomonas, Pantoea, and Xanthomonas, two isolates were identified as Lysinibacillus, a Gram-positive member of the Firmicute phylum. These two isolates represent the first confirmed non-gammaproteobacteria with INA. After further characterization, the two isolates of Lysinibacillus did not appear to use a protein to freeze water. Instead, the Lysinibacillus isolates used a secreted, nanometer-sized molecule that is heat, lysozyme, and proteinase resistant. In an attempt to identify the mechanism responsible for this activity, species type strains were tested for INA and UV mutants were generated to knock out the ice+ phenotype. Based on these results, only members of the species L. parviboronicapiens exhibit INA and the genes responsible for the activity may lie within a type-1 polyketide synthase/non-ribosomal peptide synthase gene cluster. This gene cluster is absent from the genomes of all non-ice+ strains of Lysinibacillus, and contains mutations in five of the nine ice nucleation inactive mutants generated from the rain isolated strain. To better understand the phylogenetic relationship among ice+ Lysinibacillus, a comprehensive reference guide was compiled to provide the most up-to-date information regarding the genus and each of its species. This reference will be available to other researchers investigating Lysinibacillus species or other closely related genera. / PHD

A new paradigm for the formation of calcified skeletons suggests mineralization proceeds through amorphous calcium carbonate (ACC) precursors. The implications of this strategy in carbonate crystallization are widespread, particularly for understanding factors controlling impurity and isotopic signatures in calcium carbonates. The first chapter is a literature review of the biomineralization processes used by two important model organisms: the sea urchin larva and the foraminifera. Sea urchin larvae provide a thoroughly studied example of mineralization by an ACC pathway that is under biological control through regulation of protein chemistry and the local mineralization environment. A review of how foraminifera produce their test structures is also examined to explore the question of how organisms regulate the Mg content in proportion to the temperature their environments of formation. The second chapter demonstrates that acidic biomolecules regulate the composition of ACC for a suite of model carboxylated molecules. The physical basis for the systematic trend in Mg content is related to the ability of the affinity of the biomolecule for binding Ca versus Mg. The third chapter builds on these findings to explore the transformation of Mg-rich ACC precursors to calcites of exceptionally high Mg-contents that could not be produced by classical step-dominated growth processes. The data indicate that these materials are likely a result of a nucleation-dominated pathway. The final, fourth chapter develops Raman spectroscopy-based calibrations for determining Mg contents in ACC. The calibrations are based upon peak position or peak width of the carbonate υ₁ stretch. / Ph. D.