Abstract
The eukaryote centromere was initially defined cytologically as the primary constriction on vertebrate chromosomes and functionally as a chromosomal feature with a relatively low recombination frequency. Structurally, the centromere is the foundation for sister chromatid cohesion and kinetochore formation. Together these provide the basis for interaction between chromosomes and the mitotic spindle, allowing the efficient segregation of sister chromatids during cell division. Although centromeric (CEN) DNA is highly variable between species, in all cases the functional centromere forms in a chromatin domain defined by the substitution of histone H3 with the centromere specific H3 variant centromere protein A (CENPβA), also known as CENH3. Kinetochore formation and function are dependent on a variety of regional epigenetic modifications that appear to result in a loop chromatin conformation providing exterior CENH3 domains for kinetochore construction, and interior heterochromatin domains essential for sister chromatid cohesion. In addition pericentric heterochromatin provides a structural element required for spindle assembly checkpoint function. Advances in our understanding of CENH3 biology have resulted in a model where kinetochore location is specified by the epigenetic mark left after dilution of CENH3 to daughter DNA strands during S phase. This results in a selfβrenewing and selfβreinforcing epigenetic state favorable to reliably mark centromere location, as well as to provide the optimal chromatin configuration for kinetochore formation and function. J. Cell. Biochem. 104: 2027β2039, 2008. Β© 2008 WileyβLiss, Inc.