Julie Wilson

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Organization: University of York , England
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Title: (PhD)
Co-reporter:Martin Rusilowicz;Michael Dickinson;Adrian Charlton;Simon O’Keefe
Metabolomics 2016 Volume 12( Issue 3) pp:
Publication Date(Web):2016 March
DOI:10.1007/s11306-016-0972-2
The need for reproducible and comparable results is of increasing importance in non-targeted metabolomic studies, especially when differences between experimental groups are small. Liquid chromatography–mass spectrometry spectra are often acquired batch-wise so that necessary calibrations and cleaning of the instrument can take place. However this may introduce further sources of variation, such as differences in the conditions under which the acquisition of individual batches is performed. Quality control (QC) samples are frequently employed as a means of both judging and correcting this variation. Here we show that the use of QC samples can lead to problems. The non-linearity of the response can result in substantial differences between the recorded intensities of the QCs and experimental samples, making the required adjustment difficult to predict. Furthermore, changes in the response profile between one QC interspersion and the next cannot be accounted for and QC based correction can actually exacerbate the problems by introducing artificial differences. “Background correction” methods utilise all experimental samples to estimate the variation over time rather than relying on the QC samples alone. We compare non-QC correction methods with standard QC correction and demonstrate their success in reducing differences between replicate samples and their potential to highlight differences between experimental groups previously hidden by instrumental variation.
Co-reporter:Martin Rusilowicz;Michael Dickinson;Adrian Charlton;Simon O’Keefe
Metabolomics 2016 Volume 12( Issue 11) pp:
Publication Date(Web):2016 November
DOI:10.1007/s11306-016-1110-x
Co-reporter:Jobie Kirkwood;David Hargreaves;Simon O'Keefe
Acta Crystallographica Section F 2015 Volume 71( Issue 10) pp:1228-1234
Publication Date(Web):
DOI:10.1107/S2053230X15014892

The Protein Data Bank (PDB) is the largest available repository of solved protein structures and contains a wealth of information on successful crystallization. Many centres have used their own experimental data to draw conclusions about proteins and the conditions in which they crystallize. Here, data from the PDB were used to reanalyse some of these results. The most successful crystallization reagents were identified, the link between solution pH and the isoelectric point of the protein was investigated and the possibility of predicting whether a protein will crystallize was explored.

Co-reporter:Julie Wilson, Nienke L. van Doorn, and Matthew J. Collins
Analytical Chemistry 2012 Volume 84(Issue 21) pp:9041
Publication Date(Web):October 2, 2012
DOI:10.1021/ac301333t
Collagen peptides are analyzed using a low-cost, high-throughput method for assessing deamidation using matrix-assisted laser desorption/ionization mass spectrometry (MALDI-MS). For each chosen peptide, the theoretical distribution is calculated and the measured distribution for each sample compared with this to determine the extent of glutamine deamidation. The deamidation of glutamine (Q) to glutamic acid (E) results in a mass shift of +0.984 Da. Thus, from the resolution of our data, the second peak in the isotope distribution for a peptide containing one glutamine residue coincides with the first peak of the isotope distribution for the peptide in which the residue is deamidated. A genetic algorithm is used to determine the extent of deamidation that gives the best fit to the measured distribution. The method can be extended to peptides containing more than one glutamine residue. The extent of protein degradation assessed in this way could be used, for example, to assess the damage of collagen, and screen samples for radiocarbon dating and DNA analysis.
Oxygen, isotope of mass 17, at.
Hydrogen cation
Keratins
Oxygen, isotope of mass18, at.
Ribonuclease A
Bis(maleimido)methyl Ether
Sulfur, isotope of mass 33
Sulfur, isotope of mass36
Sulfur, isotope of mass34