Quantification of oxidized levels of specific RNA species using an aldehyde reactive probe

Emerging evidence has shown that oxidation of RNA, including messenger RNA (mRNA), is elevated in several age-related diseases, although investigation of oxidized levels of individual RNA species has been limited. Recently we reported that an aldehyde reactive probe (ARP) quantitatively reacts with oxidatively modified depurinated/depyrimidinated (abasic) RNA. Here we report a novel method to isolate oxidized RNA using ARP and streptavidin beads. An oligo RNA containing abasic sites that were derivatized with ARP was pulled down by streptavidin beads, whereas a control oligo RNA was not. In vitro oxidized RNA, as well as total cellular RNA, isolated from oxidatively stressed cells was also pulled down, dependent on oxidation level, and concentrated in the pull-down fraction. Quantitative reverse transcription polymerase chain reaction (RT-PCR) using RNA in the pull-down fraction demonstrated that several gene transcripts were uniquely increased in the fraction by oxidative stress. Thus, our method selectively concentrates oxidized RNA by pull-down and enables the assessment of oxidation levels of individual RNA species. (C) 2011 Elsevier Inc. All rights reserved.

Crosslinking Studies To Probe Substrate Binding By Soybean Lipoxygenase-1

Soybean lipoxygenase-1 (SBLO-1) catalyzes the oxygenation of polyunsaturated fatty acids into conjugated diene hydroperoxides. The three dimensional structure of SBLO-1 is known, but it is not certain how substrates bind. One hypothesis involves the transient separation of helix-2 and helix-11 located on the exterior of the molecule in front of the active site iron. A second hypothesis involves a conformational change in the side chains of residues leucine 541 and threonine 259. To test these hypotheses, site directed mutagenesis was used to create a cysteine mutation on each helix, which could allow for the formation of a disulfide linkage. Disulfide formation between the two cysteines in the T259C,S545C mutant was found to be unfavorable, but later shown to be present at higher pH values using SDS-PAGE. Treatment of the T259C,S545C with the crosslinker 2,3-dibromomaleimide (DBM) resulted in a 50% reduction in catalytic activity. No loss of activity was observed when the single mutant, S545C, or the wild type was treated with DBM. Single mutants T259C and L541C both showed approximately 20% reduction in the rate after addition of DBM. Double mutants T259C,L541C and S263C,S545C showed approximately 30% reduction in the rate after addition of DBM. Single mutants T259C and L541C showed an increase in activity after incubation with NEM. Double mutants T259C,S545C and T259C,L541C showed an increase in activity after incubation with NEM. The S263C,S545C double mutant showed a slight decrease in activity in the presence of NEM. It is unclear how the NEM and DBM are interacting with the molecule, but this can easily be determined through mass spectrometry experiments.

Monitoring Stormwater Redistribution Into Low Resistivity Soils Using Noninvasive Geophysical Techniques

Water held in the unsaturated zone is important for agriculture and construction and is replenished by infiltrating rainwater. Monitoring the soil water content of clay soils using ground-penetrating radar (GPR) has not been researched, as clay soils cause attenuation of GPR signal. In this study, GPR common-midpoint soundings (CMPs) are used in the clayey soils of the Miller Run floodplain to monitor changes in the soil water content (SWC) before and after rainfall events. GPR accomplishes this task because increases in water content will increase the dielectric constant of the subsurface material, and decrease the velocity of the GPR wave. Using an empirical relationship between dielectric constant and SWC, the Topp relation, we are able to calculate a SWC from these velocity measurements. Non-invasive electromagnetics, resistivity, and seismic were performed, and from these surveys, the layering at the field site was delineated. EM characterized the horizontal variation of the soil, allowing us to target the most clay rich area. At the CMP location, resistivity indicates the vertical structure of the subsurface consists of a 40 cm thick layer with a resistivity of 100 ohm*m. Between 40 cm and 1.5 m is a layer with a resistivity of 40 ohm*m. The thickness estimates were confirmed with invasive auger and trenching methods away from the CMP location. GPR CMPs were collected relative to a July 2013 and September 2013 storm. The velocity observations from the CMPs had a precision of +/- 0.001 m/ns as assessed by repeat analysis. In the case of both storms, the GPR data showed the expected relationship between the rainstorms and calculated SWC, with the SWC increasing sharply after the rainstorm and decreasing as time passed. We compared these data to auger core samples collected at the same time as the CMPs were taken, and the volumetric analysis of the cores confirmed the trend seen in the GPR, with SWC values between 3 and 5 percent lower than the GPR estimates. Our data shows that we can, with good precision, monitor changes in the SWC of conductive soils in response to rainfall events, despite the attenuation induced by the clay.