Laboratory of Physiological Chemistry, State University Groningen, Netherlands.

To obtain more information about the arrangement of Hind III restriction fragments in the tRNA-rRNA region of the Neurospora crassa mitochondrial (mt) DNA we have cleaved the mtDNA with Hpa I and Hind II. We could construct additional cleavage maps for these enzymes. Hybridization of rRNAs to Hind II fragments confirmed the existence of an intervening region of about 2,300 basepairs in the 24S rRNA (Hahn et al., Cell, in press). About seven tRNA genes, among which the genes for tRNA1Ser and tRNAMetM, are located in a segment of about 5,000 bp separating the 24S and 17S rRNA genes. Another cluster of 14 tRNA genes is found adjacent to the other end of the 24S gene. The genes for tRNALeu1 and tRNAMetF are located in this cluster.     

The Chemistry of Ilexol. I.

Ilexol, a new triterpenoid alcohol isolated from the barks of several species of the Genus Ilex, has now been oxidized with chromium trioxide to yield a ketone, designated as ilexone of C₃₀H₄₈O, m.p. 239.5–240.5°, and – 68.74°, which gives oxirne of m. p. 256.5–257.5°, 2,4-dinitrophenylhydrazone of m.p. 260–261°, and positive Zimmermann test.

On reduction with sodium and ethanol as well as with lithium aluminum hydride, it has been shown that ilexone is regenerated to yield an alcohol proved to be identical with natural ilexol.

On reduction according to the procedure of Huang-Minion, ilexone has been shown to yield an oxygen-free compound, designated as ilexene of C₃₀H₅₀, and m.p. 241–242°.

It seems most likely that ilexol might be a triterpenoid alcohol of C₃₀H₄₉OH, an alcoholic hydroxyl group of which is secondary in nature, and moreover attached at C–3 in its molecule.     

The Chemistry of Ilexol. IV.

It has now been shown that Acetate A previously obtained by isomerizing ilexol acetate is nothing other than urs-13 (18)-en-3β-yl acetate prepared from α-amyrin, furnishing conclusive evidence for its conversion into one of the compounds of the ursane series.

Isoilexol, oxidized with chromium trioxide at room temperature, afforded a ketone named isoilexone, C₃₀H₄₈O, m.p. 194–195°, +75.90° (c, 0.527), and oxidized with the same oxidant at 70–80°, another ketone named isoilexenedione, C₃₀H₄₆O₂, m.p. 221-223°, +16.28° (c, 0.307).

Huang-Milon reduction of these ketones afforded one and the same deoxy compound named isoilexene, C₃₀H₅₀, m.p. 183–185°, +48.34° (c, 0.290), which might well be assumed to constitute a pair of optical antipodes with olean-13 (18)-ene, C₃₀H₅₀, m.p. 184-185°, ?48.50° (c, 0.545).     

Chemistry and biodiversity: Darwinism, evolution, and speciation. An opposing view

Complex structures produced by noncatalyzed multi‐step chemical processes must have highly probable origins and assembly routes. Within any frame of reference, life is easily the most‐complex self‐assembled structure known to man. It is not possible to calculate a finite time for biogenesis by statistical mechanics, but the abundance of life makes it reasonable to propose an accelerating principle of nature that naturally shortened the time for cell formation to a billion years or less. This hypothetical principle, which I have called valence‐orbital bias, is thought to be responsible for the discrepancy between statistics and observation, and carries with it, as a conditio sine qua non, multiple origins of life. The new concept resolves the differences between the predictions based on statistical mechanics and the relatively rapid appearance of life during the post‐accretion period. It suggests as well that species and variants, the units of propagation, may also have been the units of evolution. Produced in profusion by chemistry, the origins are culled by natural selection, whereby failure means extinction, not adaptation. Biodiversity, thus, becomes a direct consequence of chemistry without positive feedback from the environment and without a constructive role for mutation.     

Diacridines: bifunctional intercalators. I. Chemistry, physical chemistry and growth inhibitory properties.

The synthesis, as well as the rationale for synthesis of diacridines, double intercalators, as potential inhibitors of nucleic acid synthesis is presented. The syntheses of (9-acridyl)-putrescine and -spermine, and bis(-9-acridyl)-putrescine, -spermidine, -spermine diamines and of bis(6-chloro-2-methoxy-9-acridyl)-putrescine and -spermine diamines, all substituted on the terminal NH2 groups are described. In addition, the homologous series of diacridines connected by the amino groups of the diamines NH2(CH2)nNH2 (where n = 2,3,4,6,8,10,12,14,16,18) to the C-9 of the diacridines has been synthesized. The chemical properties of these compounds as well as their molecular relationship to DNA are presented. The effect of the double intercalators on the Tm of DNA and of (A)n - (U)n, (dA)n - (dT)n, (G)n - (C)n and on (dG)n - (dC)n have been determined. The double acridine intercalators produce a much greater increase of the Tm of these nucleic acids than do the single acridine intercalators. They also profoundly affect the Tm of DNA in physiological salt concentrations; under these latter conditions the single intercalators have no effect. The relationship between the length of the chain connecting the two acridine rings and the inhibition of the growth of P-388 cells in vitro and vivo is presented. Their growth inhibitory properties appear, in general, to parallel their intercalative abilities.     

Sediment Chemistry of Lake Bhim Tal,U. P., India

Certain chemical constituents (NO₃-N, bio-available P, Ca, Na, K, Mn, Cu, Co and organic matter) together with pH, Eh and clay content of surface sediments at various depths of the overlying water in Lake Bhim Tal were examined during 1977—1978. In addition, NH₃-N and dissolved oxygen at the mud-water interface (water immediately above the sediments) were measured. The values of Eh, pH and NO₃-N in the sediments showed a negative relationship with water depth and positive relationship with dissolved oxygen at the interface. The other variables of the sediment were positively related to water depth and negatively related to dissolved oxygen at the interface. Organic matter, K, Na and Ca showed positive relationship with the amount of clay while the cations (K, Na, Ca) and trace metals (Cu, Mn, Co) showed a positive relationship with the amount of organic matter in the sediments.     

Chemistry and biology of boron.

Boron is an essential nutrient for certain organisms, notably vascular plants and diatoms. Cyanobacteria require boron for formation of nitrogen-fixing heterocysts and boron may be beneficial to animals. Boron deficiency in plants produces manifold symptoms: many functions have been postulated. Deficiency symptoms first appear at growing points, within hours in root tips and within minutes or seconds in pollen tube tips, and are characterized by cell wall abnormalities. Boron-deficient tissues are brittle or fragile, while plants grown on high boron levels may have unusually flexible or resilient tissues. Borate forms cyclic diesters with appropriate diols or polyols. The most stable are formed with cis-diols on a furanoid ring. Two compounds have this structure physiologically: ribose in ribonucleotides and RNA, and apiose in the plant cell wall. Germanium can substitute for boron in carrot cell cultures. Both boron and germanium are localized primarily in the cell wall. We postulate that borate-apiofuranose ester cross-links are the auxin-sensitive acid-growth link in vascular plants, that the cyanobacterial heterocyst envelope depends on borate cross-linking of mannopyranose and/or galactopyranose residues in a polysaccharide-lipid environment, and that boron in diatoms forms ester cross-links in the polysaccharide cell wall matrix rather than boron-silicon interactions. Complexing of ribonucleotides is probably a factor in boron toxicity.