International
Tables for Crystallography Volume F Crystallography of biological macromolecules Edited by M. G. Rossmann and E. Arnold © International Union of Crystallography 2006 |
International Tables for Crystallography (2006). Vol. F. ch. 23.3, p. 588
Section 23.3.1. Introduction
a
Molecular Biology Institute, University of California, Los Angeles, Los Angeles, CA 90095–1570, USA |
In 1953, James Watson and Francis Crick solved the structure of double-helical DNA (Watson & Crick, 1953; Crick & Watson, 1954
). So what has a dedicated cadre of X-ray crystallographers been doing for the subsequent 45 years? That is the subject of this chapter: the advance of our knowledge of nucleic acid duplexes, primarily from single-crystal X-ray diffraction, and the biological implications of this new knowledge. The focus will be primarily on DNA because much more is known about it, but DNA/RNA hybrids and duplex RNA will also be considered. Because the emphasis is on the geometry of the nucleic acid double helix, exotic structures, such as quadruplexes, hammerhead ribozymes and aptamers, will be omitted, as will larger-scale structures such as tRNA.
Fibre diffraction showed that there were two basic forms of DNA duplex: the common B form and a more highly crystalline A form (Fig. 23.3.1.1) that, in some but not all sequences, could be produced by dehydrating the fibre (Franklin & Gosling, 1953
; Langridge et al., 1960
; Arnott, 1970
; Leslie et al., 1980
). A- and B-DNA are contrasted in Figs. 23.3.1.2
and 23.3.1.3
. The high-humidity B form has base pairs sitting squarely on the helix axis and roughly perpendicular to that axis. In contrast, in the low-humidity A form, the base pairs are displaced off the helix axis by ca 4 Å and are inclined 10–20° away from perpendicularity to that axis. The two grooves in B-DNA are of comparable depth because base pairs sit on the helix axis, but the major groove is wider than the minor because of asymmetry of attachment of base pairs to the backbone chains. In A-DNA, the minor groove is broad and shallow, whereas the major groove is cavernously deep (all the way from the surface of the helix, to the helix axis, and beyond) but can be quite narrow.
Pohl and co-workers had shown in the 1970s that alternating poly(dC-dG) is special in that it undergoes a reversible salt- or alcohol-induced conformation change (Pohl & Jovin, 1972; Pohl, 1976
). Hence, it was not surprising that when DNA synthesis methods advanced to the stage where oligonucleotide crystallization became feasible, two separate research groups – those of Alexander Rich at MIT and Richard Dickerson at Caltech – elected to synthesize, crystallize and solve a short, alternating C-G oligomer. The result was a third family of DNA duplexes, Z-DNA (Fig. 23.3.1.4)
, first as the hexamer C-G-C-G-C-G (Z1) and then the tetramer C-G-C-G (Z3). (References to A-, B- and Z-DNA structures are listed at the end of Tables A23.3.1.1
, A23.3.1.2
and A23.3.1.3
in the Appendix
, respectively. They are cited by numbers beginning with A, B or Z.) Single-crystal analyses of the traditional helix types soon followed: B-DNA as C-G-C-G-A-A-T-T-C-G-C-G (B1), and A-DNA as both C-C-G-G (A1) and G-G-T-A-T-A-C-C (A2).
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