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1. Electron micrographs of ultra-thin sections of Staphylococcus aureus and Micrococcus lysodeikticus in Vestopal as embedding medium disclose a multiplicity of DNA containing threads with varying interparticular distances.
2. The diameter of these threads is about one tenth of the average optimal section thickness.
3. This section thickness inevitably is implicated in the visualization of the internal distances between the threads as well as in some common trends in the DNA pool, a fact that has to be accounted for in the analysis of the macromolecules.
4. By spreading lysozyme protoplasts of M. lysodeikticus on a water-air interface in a Langmuir trough and by transferring this surface layer to carbon supported Formvar films, two-dimensional systems can be demonstrated which as a thread of constant width comprise the total DNA content of one microorganism each.
5. Such a macromolecular system shows equally shaped, coiled loops in a peripheral zone and many crossings towards the center. Branching of threads never has been observed so far.
From this evidence we conlude:
a) Intracellular DNA in these bacteria seems to exist in one pool as a “woolen ball” which is centered in the cytoplasm as a more or less dense object.
b) This “woolen ball“ embodies the total amount of DNA most probably as one single threadlike unit.
6. Partial destruction of the thread system of protoplasts will result upon changing optimal spreading conditions.
7. The same kind of destruction is shown upon isolation of the DNA from protoplasts, the length of the threads being an inverse function of the number of precipitation steps showing purification.
Über das Absorptionsverhalten verschiedener Quarzglassorten im Spektralbereich von 150 μ bis 275 μ
(1961)
The Tanzawa mountainland consists of a pyroclastic complex chiefly of basic composition which is intruded by a large mass of quartz-diorite at the center. This complex, well-known as the Misaka series, is the products of largescale geosynclinal volcanisms which took place during the period from the latest Oligocene to the middle Miocene in age. As compared with other geologic units, the present complex is characterized by its unusually thick accumulation of pyroclastic rocks, and by the intense hydrothermal alteration of the rocks, furnishing us an excellent section of the so-called green tuff series in the southeastern region of the Fossa Magna. Also the development of the products of interesting metamorphism of the quartz-diorite to the surrounding pyroclastic rocks is a feature uncommon in the other green tuff series of the above region. The crustal movement occurring during the volcanisms, however, make the structure of this complex highly complicate. In addition, the topographically unfavourable condition of this mountainland causes great hindrance to the geological investigation of this complex. Accordingly, the true natures of the complex remain unknown both stratigraphically and petrographically. Since 1948, the writer has been studying on the complex distributed in the eastern region of the Tanzawa massif from the volcano-stratigraphical point of view, some of the results of which have been published as miscellaneous reports. The main scope of this paper is to describe the stratigraphy, petrography, and the tectonic history of this complex. In this paper are also discussed the characteristics of the volcanic activities and the alterations represented by the same complex.
Es wird versucht, Beweise für die indirekte Strahlenwirkung zu erbringen und die einzelnen Reaktionsschritte, die bei Röntgenstrahlen-Wirkung auf wäßrige Lysinlösungen ablaufen, zu erkennen. Zur Untersuchung der durch HO2 oder OH-Radikale ausgelösten Wirkungen wurden 2 Versuchsreihen durchgeführt:
1. Bestrahlung bei Anwesenheit von Sauerstoff,
2. Bestrahlung bei Sauerstoffmangel.
Außerdem wurde der Einfluß der Dosis, Dosisleistung, Temperatur und verschiedener Substrat-Konzentrationen untersucht.
Schließlich wurde versucht, die experimentell gewonnenen Ergebnisse mit Hilfe von Radikalwirkungen, die sich auf
a) Decarboxylierungen,
b) Desaminierungen,
c) und Veränderungen des Kohlenstoff-Gerüstes erstrecken, zu deuten.