| Literature DB >> 19305635 |
Breeana L Mitchell1, Yutaka Yasui, Christopher I Li, Annette L Fitzpatrick, Paul D Lampe.
Abstract
Mass spectrometry approaches to biomarker discovery in human fluids have received a great deal of attention in recent years. While mass spectrometry instrumentation and analysis approaches have been widely investigated, little attention has been paid to how sample handling can impact the plasma proteome and therefore influence biomarker discovery. We have investigated the effects of two main aspects of sample handling on MALDI-TOF data: repeated freeze-thaw cycles and the effects of long-term storage of plasma at -70° C. Repeated freeze-thaw cycles resulted in a trend towards increasing changes in peak intensity, particularly after two thaws. However, a 4-year difference in long-term storage appears to have minimal effect on protein in plasma as no differences in peak number, mass distribution, or coefficient of variation were found between samples. Therefore, limiting freeze/thaw cycles seems more important to maintaining the integrity of the plasma proteome than degradation caused by long-term storage at -70° C.Entities:
Keywords: biomarker; long-term storage; mass spectrometry; plasma; proteomics
Year: 2005 PMID: 19305635 PMCID: PMC2657648
Source DB: PubMed Journal: Cancer Inform ISSN: 1176-9351
Characteristics of the study population
| Characteristic | N | % |
|---|---|---|
| Age (years) | Mean=74.4 | SD=3.4 |
| Gender | ||
| Male | 17 | 34.0 |
| Female | 33 | 66.0 |
| Race | ||
| White | 41 | 82.0 |
| Black | 9 | 18.0 |
| Clinical Site | ||
| Wake Forest University | 18 | 36.0 |
| University CA, Davis | 10 | 20.0 |
| Johns Hopkins | 10 | 20.0 |
| University of Pittsburgh | 12 | 24.0 |
Abbreviation: SD = Standard Deviation.
Changes in peak intensity following freeze-thaw cycle
| Changes in peak intensity | |||||
|---|---|---|---|---|---|
| Number of freeze/thaw cycles | 25th percentile | Median | 75th percentile | 95th percentile | 99th percentile |
| 2 | 0.7% | 1.7% | 3.0% | 8.3% | 19.1% |
| 3 | 1.0% | 2.4% | 4.6% | 13.8% | 43.0% |
| 4 | 1.3% | 3.5% | 7.5% | 27.4% | 67.6% |
| 5 | 1.2% | 3.1% | 7.0% | 25.8% | 51.7% |
Changes in peak intensity following freeze-thaw cycles by mass/charge
| Number of freeze/thaw cycles | Median changes in peak intensity | |||
|---|---|---|---|---|
| 35,000 | <5,000–10,000 | 10,000–20,000 | ≥20,000 | |
| 2 | 0.242% | 0.687% | 0.197% | −0.306% |
| 3 | −0.344% | 3.419% | −0.621% | −0.508% |
| 4 | −0.330% | 3.218% | −0.099% | −0.295% |
| 5 | −1.201% | 2.018% | −0.918% | −0.587% |
Peak number, variation and correlation of plasma samples from 1992/93 compared to 1996/97
| 1992/93 (25th, 75th percentile) | 1996/97 (25th, 75th percentile) | |
|---|---|---|
| Number of peaks | 636 (611, 666) | 630 (596, 673) |
| Coefficient of Variation | 14.6% (11.6%, 26.3%) | 13.7% (11.3%, 26.5%) |
| Coefficient of Variation using 5 replicates | 11.1% (8.0%, 18.8%) | 10.2% (7.9%, 19.6%) |
| Correlation | 0.40 (0.32, 0.47) | |
Comparison of the number of peaks at different mass/charge ranges in the 1992/93 and 1996/97 samples
| Mass/charge range | Median number of peaks (25th, 75th percentile) | |
|---|---|---|
| 1992/93 | 1996/97 | |
| < 5,000 | 174 (163,191) | 177 (163,194) |
| 5,000 – 10,000 | 58 (53,65) | 57 (53,63) |
| >10,000 | 401 (386,426) | 395 (376,421) |