Probing the Saccharomyces cerevisiae centromeric DNA (CEN DNA)–binding factor 3 (CBF3) kinetochore complex by using atomic force microscopy

Yeast centromeric DNA (CEN DNA) binding factor 3 (CBF3) is a multisubunit protein complex that binds to the essential CDEIII element in CEN DNA. The four CBF3 proteins are required for accurate chromosome segregation and are considered to be core components of the yeast kinetochore. We have examined the structure of the CBF3–CEN DNA complex by atomic force microscopy. Assembly of CBF3–CEN DNA complexes was performed by combining purified CBF3 proteins with a DNA fragment that includes the CEN region from yeast chromosome III. Atomic force microscopy images showed DNA molecules with attached globular bodies. The contour length of the DNA containing the complex is ≈9% shorter than the DNA alone, suggesting some winding of DNA within the complex. The measured location of the single binding site indicates that the complex is located asymmetrically to the right of CDEIII extending away from CDEI and CDEII, which is consistent with previous data. The CEN DNA is bent ≈55° at the site of complex formation. A significant fraction of the complexes are linked in pairs, showing three to four DNA arms, with molecular volumes approximately three times the mean volumes of two-armed complexes. These multi-armed complexes indicate that CBF3 can bind two DNA molecules together in vitro and, thus, may be involved in holding together chromatid pairs during mitosis.

The first step of aminoacylation at the atomic level in histidyl-tRNA synthetase

The crystal structure of an enzyme–substrate complex with histidyl-tRNA synthetase from Escherichia coli, ATP, and the amino acid analog histidinol is described and compared with the previously obtained enzyme–product complex with histidyl-adenylate. An active site arginine, Arg-259, unique to all histidyl-tRNA synthetases, plays the role of the catalytic magnesium ion seen in seryl-tRNA synthetase. When Arg-259 is substituted with histidine, the apparent second order rate constant (kcat/Km) for the pyrophosphate exchange reaction and the aminoacylation reaction decreases 1,000-fold and 500-fold, respectively. Crystals soaked with MnCl2 reveal the existence of two metal binding sites between β- and γ-phosphates; these sites appear to stabilize the conformation of the pyrophosphate. The use of both conserved metal ions and arginine in phosphoryl transfer provides evidence of significant early functional divergence of class II aminoacyl-tRNA synthetases.

Visualization of unwinding activity of duplex RNA by DbpA, a DEAD box helicase, at single-molecule resolution by atomic force microscopy

The Escherichia coli protein DbpA is unique in its subclass of DEAD box RNA helicases, because it possesses ATPase-specific activity toward the peptidyl transferase center in 23S rRNA. Although its remarkable ATPase activity had been well defined toward various substrates, its RNA helicase activity remained to be characterized. Herein, we show by using biochemical assays and atomic force microscopy that DbpA exhibits ATP-stimulated unwinding activity of RNA duplex regardless of its primary sequence. This work presents an attempt to investigate the action of DEAD box proteins by a single-molecule visualization methodology. Our atomic force microscopy images enabled us to observe directly the unwinding reaction of a DEAD box helicase on long stretches of double-stranded RNA. Specifically, we could differentiate between the binding of DbpA to RNA in the absence of ATP and the formation of a Y-shaped intermediate after its progression through double-stranded RNA in the presence of ATP. Recent studies have questioned the designation of DbpA, in particular, and DEAD box proteins in general as RNA helicases. However, accumulated evidence and the results reported herein suggest that these proteins are indeed helicases that resemble in many aspects the DNA helicases.

Manganese oxide minerals: Crystal structures and economic and environmental significance

Manganese oxide minerals have been used for thousands of years—by the ancients for pigments and to clarify glass, and today as ores of Mn metal, catalysts, and battery material. More than 30 Mn oxide minerals occur in a wide variety of geological settings. They are major components of Mn nodules that pave huge areas of the ocean floor and bottoms of many fresh-water lakes. Mn oxide minerals are ubiquitous in soils and sediments and participate in a variety of chemical reactions that affect groundwater and bulk soil composition. Their typical occurrence as fine-grained mixtures makes it difficult to study their atomic structures and crystal chemistries. In recent years, however, investigations using transmission electron microscopy and powder x-ray and neutron diffraction methods have provided important new insights into the structures and properties of these materials. The crystal structures for todorokite and birnessite, two of the more common Mn oxide minerals in terrestrial deposits and ocean nodules, were determined by using powder x-ray diffraction data and the Rietveld refinement method. Because of the large tunnels in todorokite and related structures there is considerable interest in the use of these materials and synthetic analogues as catalysts and cation exchange agents. Birnessite-group minerals have layer structures and readily undergo oxidation reduction and cation-exchange reactions and play a major role in controlling groundwater chemistry.

Imaging ROMK1 inwardly rectifying ATP-sensitive K+ channel protein using atomic force microscopy.

The inwardly rectifying K+ channel ROMK1 has been implicated as being significant in K+ secretion in the distal nephron. ROMK1 has been shown by immunocytochemistry to be expressed in relevant nephron segments. The development of the atomic force microscope has made possible the production of high resolution images of small particles, including a variety of biological macromolecules. Recently, a fusion protein of glutathione S-transferase (GST) and ROMK1 (ROMK1-GST) has been used to produce a polyclonal antibody for immunolocalization of ROMK1. We have used atomic force microscopy to examine ROMK1-GST and the native ROMK1 polypeptide cleaved from GST. Imaging was conducted with the proteins in physiological solutions attached to mica. ROMK1-GST appears in images as a particle composed of two units of similar size. Analyses of images indicate that the two units have volumes of approximately 118 nm3, which is close to the theoretical volume of a globular protein of approximately 65 kDa (the molecular mass of ROMK1-GST). Native GST exists as a dimer, and the images obtained here are consistent with the ROMK1-GST fusion protein's existence as a heterodimer. In experiments on ROMK1 in aqueous solution, single molecules appear to aggregate, but contact to the mica was maintained. Addition of ATP to the solution produced a change in height of the aggregates. This change (which was reversible) suggests that ATP induces a structural change in the ROMK1 protein. The data show that atomic force microscopy is a useful tool for examination of purified protein molecules under near-physiological conditions, and furthermore, that structural alterations in the proteins may be continuously investigated.