Structure and conformational changes of DNA topoisomerase II visualized by electron microscopy.

Type II DNA topoisomerases, which create a transient gate in duplex DNA and transfer a second duplex DNA through this gate, are essential for topological transformations of DNA in prokaryotic and eukaryotic cells and are of interest not only from a mechanistic perspective but also because they are targets of agents for anticancer and antimicrobial chemotherapy. Here we describe the structure of the molecule of human topoisomerase II [DNA topoisomerase (ATP-hydrolyzing), EC 5.99.1.3] as seen by scanning transmission electron microscopy. A globular approximately 90-angstrom diameter core is connected by linkers to two approximately 50-angstrom domains, which were shown by comparison with genetically truncated Saccharomyces cerevisiae topoisomerase II to contain the N-terminal region of the approximately 170-kDa subunits and that are seen in different orientations. When the ATP-binding site is occupied by a nonhydrolyzable ATP analog, a quite different structure is seen that results from a major conformational change and consists of two domains approximately 90 angstrom and approximately 60 angstrom in diameter connected by a linker, and in which the N-terminal domains have interacted. About two-thirds of the molecules show an approximately 25 A tunnel in the apical part of the large domain, and the remainder contain an internal cavity approximately 30 A wide in the large domain close to the linker region. We propose that structural rearrangements lead to this displacement of an internal tunnel. The tunnel is likely to represent the channel through which one DNA duplex, after capture in the clamp formed by the N-terminal domains, is transferred across the interface between the enzyme's subunits. These images are consistent with biochemical observations and provide a structural basis for understanding the reaction of topoisomerase II.

Purification of a ligand for the EPH-like receptor HEK using a biosensor-based affinity detection approach.

Advances in screening technologies allowing the identification of growth factor receptors solely by virtue of DNA or protein sequence comparison call for novel methods to isolate corresponding ligand growth factors. The EPH-like receptor tyrosine kinase (RTK) HEK (human EPH-like kinase) was identified previously as a membrane antigen on the LK63 human pre-B-cell line and overexpression in leukemic specimens and cell lines suggested a role in oncogenesis. We developed a biosensor-based approach using the immobilized HEK receptor exodomain to detect and monitor purification of the HEK ligand. A protein purification protocol, which included HEK affinity chromatography, achieved a 1.8 X 10(6)-fold purification of an approximately 23-kDa protein from human placental conditioned medium. Analysis of specific sHEK (soluble extracellular domain of HEK) ligand interactions in the first and final purification steps suggested a ligand concentration of 40 pM in the source material and a Kd of 2-3 nM. Since the purified ligand was N-terminally blocked, we generated tryptic peptides and N-terminal amino acid sequence analysis of 7 tryptic fragments of the S-pyridylethylated protein unequivocally matched the sequence for AL-1, a recently reported ligand for the related EPH-like RTK REK7 (Winslow, J.W., Moran, P., Valverde, J., Shih, A., Yuan, J.Q., Wong, S.C., Tsai, S.P., Goddard, A., Henzel, W.J., Hefti, F., Beck, K.D., & Caras, I.W. (1995) Neuron 14, 973-981). Our findings demonstrate the application of biosensor technology in ligand purification and show that AL-1, as has been found for other ligands of the EPH-like RTK family, binds more than one receptor.

Isolation of an oxygen-sensitive FNR protein of Escherichia coli: interaction at activator and repressor sites of FNR-controlled genes.

The Escherichia coli fnr gene product, FNR, is a DNA binding protein that regulates a large family of genes involved in cellular respiration and carbon metabolism during conditions of anaerobic cell growth. FNR is believed to contain a redox/O2-sensitive element for detecting the anaerobic state. To investigate this process, a fnr mutant that encodes an altered FNR protein with three amino acid substitutions in the N-terminal domain was constructed by site-directed mutagenesis. In vivo, the mutant behaved like a wild-type strain under anaerobic conditions but had a 14-fold elevated level of transcriptional activation of a reporter gene during aerobic cell growth. The altered fur gene was overexpressed in E. coli and the resultant FNR protein was purified to near homogeneity by using anaerobic chromatography procedures. An in vitro Rsa I restriction site protection assay was developed that allowed for the assessment of oxygen-dependent DNA binding of the mutant FNR protein. The FNR protein was purified as a monomer of M(r) 28,000 that contained nonheme iron at 2.05 +/- 0.34 mol of Fe per FNR monomer. In vitro DNase I protection studies were performed to establish the locations of the FNR-binding sites at the narG, narK, dmsA, and hemA promoters that are regulated by either activation or repression of their transcription. The sizes of the DNA footprints are consistent with the binding of two monomers of FNR that protect the symmetrical FNR-recognition sequence TTGAT-nnnnATCAA. Exposure of the FNR protein or protein-DNA complex to air for even short periods of time (approximately 5 min) led to the complete loss of DNA protection at a consensus FNR recognition site. A model whereby the FNR protein exists in the cell as a monomer that assembles on the DNA under anaerobic conditions to form a dimer is discussed.

UME6 is a central component of a developmental regulatory switch controlling meiosis-specific gene expression.

The UME6 gene of Saccharomyces cerevisiae was identified as a mitotic repressor of early meiosis-specific gene expression. It encodes a Zn2Cys6 DNA-binding protein which binds to URS1, a promoter element needed for both mitotic repression and meiotic induction of early meiotic genes. This paper demonstrates that a complete deletion of UME6 causes not only vegetative derepression of early meiotic genes during vegetative growth but also a significant reduction in induction of meiosis-specific genes, accompanied by a severe defect in meiotic progression. After initiating premeiotic DNA synthesis the vast majority of cells (approximately 85%) become arrested in prophase and fail to execute recombination; a minority of cells (approximately 15%) complete recombination and meiosis I, and half of these form asci. Quantitative analysis of the same early meiotic transcripts that are vegetatively derepressed in the ume6 mutant, SPO11, SPO13, IME2, and SPO1, indicates a low level of induction in meiosis above their vegetative derepressed levels. In addition, the expression of later meiotic transcripts, SPS2 and DIT1, is significantly delayed and reduced. The expression pattern of early meiotic genes in ume6-deleted cells is strikingly similar to that of early meiotic genes with promoter mutations in URS1. These results support the view that UME6 and URS1 are part of a developmental switch that controls both vegetative repression and meiotic induction of meiosis-specific genes.

Subparsec-scale structure and evolution of Centaurus A (NGC5128).

We present a series of 8.4-GHz very-long-baseline radio interferometry images of the nucleus of Centaurus A (NGC5128) made with a Southern Hemisphere array, representing a 3.3-year monitoring effort. The nuclear radio jet is approximately 50 milliarcseconds in extent, or at the 3.5-megaparsec distance of NGC5128, approximately 1 parsec in length. Subluminal motion is seen and structural changes are observed on time scales shorter than 4 months. High-resolution observations at 4.8 and 8.4 GHz made in November 1992 reveal a complex morphology and allow us to unambiguously identify the self-absorbed core located at the southwestern end of the jet.

Reversible phosphorylation controls the activity of cyclosome-associated cyclin-ubiquitin ligase.

Cyclin B/cdc2 is responsible both for driving cells into mitosis and for activating the ubiquitin-dependent degradation of mitotic cyclins near the end of mitosis, an event required for the completion of mitosis and entry into interphase of the next cell cycle. Previous work with cell-free extracts of rapidly dividing clam embryos has identified two specific components required for the ubiquitination of mitotic cyclins: E2-C, a cyclin-selective ubiquitin carrier protein that is constitutively active during the cell cycle, and E3-C, a cyclin-selective ubiquitin ligase that purifies as part of a approximately 1500-kDa complex, termed the cyclosome, and which is active only near the end of mitosis. Here, we have separated the cyclosome from its ultimate upstream activator, cdc2. The mitotic, active form of the cyclosome can be inactivated by incubation with a partially purified, endogenous okadaic acid-sensitive phosphatase; addition of cdc2 restores activity to the cyclosome after a lag that reproduces that seen previously in intact cells and in crude extracts. These results demonstrate that activity of cyclin-ubiquitin ligase is controlled by reversible phosphorylation of the cyclosome complex.

Identification of endothelin 1 and big endothelin 1 in secretory vesicles isolated from bovine aortic endothelial cells.

Vesicles containing endothelin 1 (ET-1) were isolated from bovine aortic endothelial cells (BAECs) by fractionation of homogenates on sucrose density gradients by ultracentrifugation. The vesicles were localized at the 1.0/1.2 M sucrose interface using a specific anti-ET-1-(16-21) RIA. Identification of ET-1 and big ET-1 in this fraction was confirmed by HPLC analysis combined with RIA. Morphological examination of the ET-1-enriched fraction by electron microscopy identified clusters of vesicles approximately 100 nm in diameter. Immunostaining of ultrathin cryosections prepared from the vesicle fraction for ET-1 or big ET-1 showed clusters of 15-nm gold particles attached to or within vesicles. Immunofluorescence staining of whole BAECs using a specific ET-1-(16-21) IgG purified by affinity chromatography revealed punctate granulation of the cell cytoplasm viewed under light microscopy. This distinct pattern of staining was shown by confocal light microscopy to be intracellular. Immunofluorescence staining of whole cells with a polyclonal antiserum for big ET-1-(22-39) showed a defined perinuclear localization of precursor molecule. Hence, several different approaches have demonstrated that ET-1 and big ET-1 are localized within intracellular vesicles in BAECs, suggesting that these subcellular compartments are an important site for processing of big ET-1 by endothelin-converting enzyme.

Chloroplast gene sequence data suggest a single origin of the predisposition for symbiotic nitrogen fixation in angiosperms.

Of the approximately 380 families of angiosperms, representatives of only 10 are known to form symbiotic associations with nitrogen-fixing bacteria in root nodules. The morphologically based classification schemes proposed by taxonomists suggest that many of these 10 families of plants are only distantly related, engendering the hypothesis that the capacity to fix nitrogen evolved independently several, if not many, times. This has in turn influenced attitudes toward the likelihood of transferring genes responsible for symbiotic nitrogen fixation to crop species lacking this ability. Phylogenetic analysis of DNA sequences for the chloroplast gene rbcL indicates, however, that representatives of all 10 families with nitrogen-fixing symbioses occur together, with several families lacking this association, in a single clade. This study therefore indicates that only one lineage of closely related taxa achieved the underlying genetic architecture necessary for symbiotic nitrogen fixation in root nodules.

Sundrypeices of the Plate given to the College, 1736 September 18

One-page inventory of the silver, including the weight of each object, donor, and dates; one passage is crossed out, and written diagonal to the inventory are the words "Fort London Farmer London." Docketed on the verso with an address to the Right Honorable Samuel Bishop of York.

(Appendix) Oxygen isotope record and carbonate mineralogy of the top part of ODP Hole 101-633A

Hole 633A was drilled in the southern part of Exuma Sound on the toe-of-slope of the southeastern part of Great Bahama Bank during ODP Leg 101. The top 55 m, collected as a suite of six approximately 9.5-m-long hydraulic piston cores, represents a Pliocene-Pleistocene sequence of periplatform carbonate ooze, a mixture of pelagic calcite (foraminifer and coccolith tests), some pelagic aragonite (pteropod tests), and bank-derived fine aragonite and magnesian calcite. A 1.6-m.y.-long hiatus was identified at 43.75 mbsf using calcareous nannofossil biostratigraphy and magnetostratigraphy. The 43.75-m-thick periplatform sequence above the hiatus is a complete late Pliocene-Quaternary record of the past 2.15 m.y. The d18O curve, primarily based on Globigerinoides sacculifera, clearly displays high-frequency/low-amplitude cycles during the early Pleistocene and low-frequency/high-amplitude cycles during the middle and late Pleistocene. Variations in aragonite content in the fine fraction of the periplatform ooze show a cyclic pattern throughout the Pleistocene, as previously observed in piston cores of the upper Pleistocene. These variations correlate well with the d18O record: high aragonite corresponds to light interglacial d18O values, and vice versa. Comparison of the d18O record and the aragonite curve helps to identify 23 interglacial and glacial oxygen-isotope stages, corresponding to 10.5 aragonite cycles (labeled A to K) commonly established during the middle and late Pleistocene (0.9 Ma-present). Strictly based on the aragonite curve, another 11 aragonite cycles, labeled L to V, were identified for the early Pleistocene (0.9 to 1.6 Ma). Mismatches between the d18O record and the aragonite curve occur mainly at some of the glacial-to-interglacial transitions, where aragonite increases usually lag behind d18O depletion. When one visually connects the minima on the Pleistocene aragonite curve, low-frequency (0.4 to 0.5 m.y.) supercycles seem to be superimposed on the high-frequency cycles. The timing of this supercycle roughly matches the timing of the Pleistocene carbonate preservation supercycles described in the Pacific, Indian, and Atlantic oceans. Mismatches between aragonite and d18O cycles are even more obvious for the late Pliocene (1.6 to 2.15 Ma). Irregular aragonite variations are observed for the late Pliocene, although after the onset of late Pleistocene-like glaciations in the North Atlantic Ocean 2.4 m.y. ago the d18O record has shown a mode of high-frequency/low-amplitude cycles. Initiation of climatically induced aragonite cycles occurs only at the Pliocene-Pleistocene transition, 1.6 m.y. ago. After that time, aragonite cycles are fully developed throughout the Quaternary. The 11-m-thick periplatform sequence below the hiatus represents a lower Pliocene interval between 3.75 and 4.45 Ma. The bottom half (4.25-4.45 Ma) has a fairly constant, high aragonite content (averaging 60%) and high sedimentation rates (28 m/m.y.) and corresponds to the end of the prolonged early Pliocene interglacial interval (4.1-5.0 Ma), established as a worldwide high sea-level stand. The second half (3.75-4.25 Ma), in which aragonite content decreases by successive steps, paralleled by a gradual 5180 enrichment in Globigerinoides sacculifera and low sedimentation rates (10 m/m.y), corresponds to the climatic deterioration established worldwide between 4.1 and 3.8 Ma, to a decrease of carbonate preservation observed in the equatorial Pacific Ocean, and to a global sea-level decline. Dolomite, a ubiquitous secondary component in the lower Pliocene, is interpreted as being authigenic and possibly related to diagenetic transformation of primary bank-derived fine magnesian calcite. Transformation of the primary mineralogical composition of the periplatform ooze was evidently minor, as the sediments have retained a detailed record of the Pliocene-Pleistocene climatic evolution. Clear evidence of diagenetic transformations in the periplatform ooze includes (1) the disappearance of magnesian calcite in the upper 20 m of Hole 633A, (2) the occurrence of calcite overgrowths on foraminiferal tests and microclasts at intermittent chalky core levels, and (3) the ubiquitous presence of authigenic dolomite in the lower Pliocene.

Report of Her Majesty's Commissioners appointed to inquire into the state, discipline, studies, and revenues of the University of Dublin, and of Trinity College : together with appendices, containing evidence, suggestions, and correspondence. /

Title is preceded on title page by: Dublin University Commission.

The confessions of St. Augustine; books I-IX (selections)

"A selected bibliography": p. 55-61.

Answer to skeptics; a translation of St. Augustine's Contra academicos,

222.8 A9AK

The confessions of St. Augustine.

Mode of access: Internet.

The Old English version of the enlarged rule of Chrodegang together with the Latin original. An Old English version of the Capitula of Theodulf together with the Latin original. An interlinear Old English rendering of the Epitome of Benedict of Aniane.

"A fuller introduction, together with notes and a glossary, is in preparation."--Temporary pref.