| Literature DB >> 25477864 |
Wen-Chao Li1, Zhe-Jin Zhong1, Pan-Pan Zhu1, En-Ze Deng1, Hui Ding1, Wei Chen2, Hao Lin1.
Abstract
DNA replication is a highly precise process that is initiated from origins of replication (ORIs) and is regulated by a set of regulatory proteins. The mining of DNA sequence information will be not only beneficial for understanding the regulatory mechanism of replication initiation but also for accurately identifying ORIs. In this study, the GC profile and GC skew were calculated to analyze the compositional bias in the Saccharomyces cerevisiae genome. We found that the GC profile in the region of ORIs is significantly lower than that in the flanking regions. By calculating the information redundancy, an estimation of the correlation of nucleotides, we found that the intensity of adjoining correlation in ORIs is dramatically higher than that in flanking regions. Furthermore, the relationships between ORIs and nucleosomes as well as transcription start sites were investigated. Results showed that ORIs are usually not occupied by nucleosomes. Finally, we calculated the distribution of ORIs in yeast chromosomes and found that most ORIs are in transcription terminal regions. We hope that these results will contribute to the identification of ORIs and the study of DNA replication mechanisms.Entities:
Keywords: GC profile; GC skew; Saccharomyces cerevisiae; distribution of ORIs; information redundancy; origin of replication
Year: 2014 PMID: 25477864 PMCID: PMC4235382 DOI: 10.3389/fmicb.2014.00574
Source DB: PubMed Journal: Front Microbiol ISSN: 1664-302X Impact factor: 5.640
Predicted results of different parameters using a support vector machine.
| Method | Performance evaluationb | ||
|---|---|---|---|
| GC profile | 0.7605 | 0.7728 | 0.7667 |
| GC skew | 0.6247 | 0.5778 | 0.6012 |
| 0.5309 | 0.5704 | 0.5506 | |
| Nucleosome ( | 0.7448 | 0.7575 | 0.7511 |
| Nucleosome (ethanol) | 0.7071 | 0.7840 | 0.7456 |
| Nucleosome (YPD) | 0.7567 | 0.7811 | 0.7689 |
| Nucleosome (galactose) | 0.7485 | 0.7910 | 0.7697 |