The cell cycle plays fundamental roles in many cellular events, such as proliferation, survival and amplification. Deregulation of the cell cycle might lead to abnormal cell growth, which causes cancer or induces cell death through apoptosis. The eukaryotic cell cycle comprises four stages, G1, S, G2 and mitosis. One of the major tasks throughout the cell cycle is to accurately transfer genetic information from parental cells to the next generation. Thus, the two most important stages of the cell cycle are S phase, in which DNA replication occurs, and mitosis, in which the replicated chromosomes are equally segregated into two daughter cells [
1].
It is well accepted that DNA replication is initiated bi-directionally at specific loci on chromatin, namely the origins of replication. However, how these origins are selected is still not quite clear. The simplest and best understanding of origins of replication is from study of the budding yeast,
Saccharomyces cerevisiae. In this organism, replication origins are specified by the autonomous replication sequences (ARS), which are around 100 base pairs and contain a shared 11-base-pair autonomous consensus sequence (ACS). Origin Recognition Complex (ORC) binds directly to ACS to initiate DNA replication. However, even in a simple system such as this, the ACS is not sufficient in itself to predict the origin; the exact location of ACS on the chromosome is also a critical element. Active origins are usually located at intergenic regions, which explains why only 400 out of 12,000 ACS sites are functional in
S. cerevisiae [
2,
3]. On the other hand, the origins of replication of the fission yeast
Schizosaccharomyces pombe differ from those of
S. cerevisiae. First, the origins are larger in
S. Pombe, usually from 500 to 1000 base pairs; second, the origins of fission yeast do not have an ARS-like consensus sequence. However, evidence does show that the origins of replication of
S. Pombe are located mostly at intergenic regions of high A-T content. ORCs with the AT-hook domain preferentially bind to AT-rich islands of DNA to initiate DNA replication [
4-
7]. The situation is much more complicated in multicellular organisms, as DNA replication can be initiated at any location during early development of
Xenopus laevis and
Drosophila melanogaster. But during later development origins of replication are chosen from asymmetric AT-rich regions under the specific influence of epigenetic factors such as gene transcription, nucleosome position, etc. [
8-
10]. A global search for origins of replication in mouse and Chinese hamster cells revealed that CpG islands with a high GC content but a low methylation level are usually not only the sites for transcription but also for initiation of DNA replication [
11,
12]. Origins are not all fired at the same time, but instead are activated in early, mid or late stages of S phase. Furthermore, not all origins are activated during S phase. Instead, only a subset is activated during undisturbed replication whereas others, the so-called "dormant origins", are activated in the case of DNA replication stress such as DNA damage [
13-
15].
DNA replication starts with a series of sequential steps from the formation of pre-replicative complex (pre-RC) by ORC, which recognizes the origin of DNA replication during G1 phase. ORC is a heterohexamer complex contains six members, Orc1 to Orc6. They were originally identified as ARS-binding proteins in
S. cerevisiae [
3], and named sequentially from Orc1 to Orc6 according to their descending molecular weight. ORC homologue proteins (mainly Orc1 to Orc5) were later identified in almost all organisms including
Homo sapiens [
16-
18]. All ORCs can bind preferentially to asymmetric AT-rich regions of DNA and function as the loading base for the formation of the pre-RC complex. These proteins are considered to be the only proteins that directly recognize the origins of replication, however in budding yeast Noc3 protein may also be involved [
19]. Then cell division cycle 6 (Cdc6) and helicase-loading protein Cdt1 are recruited to the complex, followed by subsequent loading of the minichromosome maintenance protein (MCM) complex. The MCM complex is a heterohexamer that contains six members (Mcm2-7), and has DNA helicase activity, which will later unwind the DNA and allow bi-directional movement of the replication fork. This activation process also involves many other DNA replication factors such as CDC45, GINS complex, SLK2, Treslin, GEMC1, MCM10, DBF4 and RPA. All these proteins ensure proper loading of DNA polymerase and subsequent unwinding of DNA [
20]. The formation of pre-RC and activation of the origin of replication have to be tightly regulated to ensure that DNA replicates only once per cell cycle. Once an origin has been activated at a specific locus, it will be inactivated so that re-activation at the same locus will be inhibited within the same cell cycle. During S phase, most Cdc6 proteins are phosphorylated by cyclinA-Cdk2 and exported to the cytoplasm for degradation, whereas a subset of Cdc6 proteins remains bound to chromatin [
21]. Cdt1, a critical replication licensing factor, is also regulated by several mechanisms during S phase. Geminin, an inhibitor of Cdt1, binds to and inhibits Cdt1 on chromatin [
22,
23]. In addition, Cdt1 is ubiquitinated and degraded by SCF
skp2 and DDB1
Cul4 [
24,
25]. The MCM complex is phosphorylated by Cdc7-Dbf4 and released from the template when DNA replication is completed [
26,
27]. From G2 to M phase, Cdc6 and the MCM complex are dephosphorylated. Geminin is ubiquitinated by APC
cdc20 so that Cdt1 is released from inhibition [
28] and pre-RC can be reformed to prepare for the next round of DNA replication.