Vertebrate genomes are mosaics of isochores - namely, of long (>300 kb), compositionally homogeneous DNA segments that can be subdivided into a small number of families characterized by different GC levels. In the human genome (which is representative of a number of mammalian genomes, and, more broadly, of the genomes of warm-blooded vertebrates), the compositional range of isochores is 30%-60% GC, and five families of isochores have been identified: two GC-poor families, L1 and L2, together representing 62% of the genome, and three GC-rich families, H1, H2, and H3, representing 22%, 9%, and 3%, respectively (the remaining 4% of the genome is formed by satellite and ribosomal DNA). Gene concentration is strikingly nonuniform, being highest in the H3 isochore family, lowest in the L1+L2 families, and intermediate in the H1+H2 families. The H3 family corresponds to T(elomeric) bands of metaphase chromosomes, and the L1+L2 families correspond to G(iemsa) bands, whereas R(everse) bands comprise both GC-poor and GC-rich isochores. The compositional distributions of large genome fragments, of exons (and their codon positions), and of introns are correlated with each other. They represent compositional patterns and are very different between the genomes of cold- and warm-blooded vertebrates, mainly in that the former are much less heterogeneous in base composition and never reach the highest GC levels attained by the latter. Only relatively small compositional differences are found among the genomes of either cold- or warm-blooded vertebrates. Compositional patterns allow one to define two modes in genome evolution: a conservative mode, with no compositional change, and a transitional (or shifting) mode, with compositional changes. The conservative mode can be observed among either cold- or warm-blooded vertebrates. The transitional mode comprises both major and minor compositional changes. In vertebrate genomes, the major changes are associated with the appearance of GC-rich and very GC-rich isochores in mammalian and avian genomes. Mutational biases play a role in both modes of compositional evolution. According to one viewpoint, the fixation of compositionally biased mutations is responsible for the transitional mode of evolution of bacterial genomes; in the conservative mode of evolution of vertebrates, they accomplish their role in conjunction with differences either in chromatin structures that modulate replication errors or in chromatin transcriptional activities that may lead to various extents of repair-DNA synthesis. According to another viewpoint, defended here, selection controls, at the isochore level, the fixation of compositionally biased mutations, both in the conservative and in the transitional mode of evolution.
CITATION STYLE
Bernardi, G. (1993). The vertebrate genome: Isochores and evolution. Molecular Biology and Evolution, 10(1), 186–204. https://doi.org/10.1093/oxfordjournals.molbev.a039994
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