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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Negendank, Jörg F W; Büchel, Georg; Hansen, R B; Hofmann, W; Irion, G; Haverkamp, B; Lorenz, V; Scharf, B; Sonne, V; Usinger, H; Weiler, H (1985): The Meerfelder Maar lake deposits. Zeitschrift für Gletscherkunde und Glazialgeologie, 21, 67-70, hdl:10013/epic.42900.d002
    Publication Date: 2023-05-12
    Description: A core from Meerfelder Maar, with a basal age of 29,000 years, provides a continuous sedimentary sequence from Late-Glacial times to the present. It includes the stratigraphical marker of the Laach Pumice Tuff. Sedimentological, geochemical, palynological, palaeobiological, palaeomagnetic and palaeontological analyses permit reconstructions of the history of the lake and its catchment area, and hence of the climate of the region, to be made. The discovery of Middle Oligocene marine, detrital fossils in the maar sediments provides insights into the palaeogeography of the Eifel region during Tertiary times.
    Keywords: B4; DRILL; Drilling/drill rig; Meerfelder Maar, Germany
    Type: Dataset
    Format: application/pdf, 215.7 kBytes
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  • 2
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 59 (1972), S. 467-467 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 59 (1972), S. 158-164 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 65 (1978), S. 515-519 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Notes: Abstract Extensive mineral alteration in the older land surfaces of the eastern Amazonian lowland has led to complete impoverishment of the soils in respect of their inorganic nutrient contents. Large-scale use of this area for agricultural purposes seems impossible. In the western Amazonian lowland, younger land surfaces (Pliocene) have developed along with Pleistocene flood plains. The mineral alteration in the soil profiles of this area, which are partly characterized by poor drainage, has resulted in impoverishment of soils to a lesser degree. These soils can be used to a limited extent for agricultural purposes, especially at the level of a subsistence economy.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 62 (1975), S. 179-180 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Histochemistry and cell biology 99 (1993), S. 75-83 
    ISSN: 1432-119X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract Lipophilic cationic fluorescent dyes (D) specifically stain the mitochondria of living cells. A perfusion chamber for cell cultures is described, which can be used to determine the kinetics of vital staining of the mitochondria of single selected cells in situ. In these experiments styrylpyridinium dyes and cultures of HeLa cells were used. The dyes differ strongly in their lipophilic properties; R m values and the partition coefficients P o/w between n-octanol (o) and water (w) were determined in order to characterize their lipophilicity. In the thermostat-regulated chamber the concentration of the dye C D can be increased from C D=0 to C D〉0 within a few seconds (concentration jump). Thus, the time t=0 for the beginning of the vital staining and the dye concentration in the cell medium during the staining experiment, C D=const., are unambiguously defined. The concentration of the dye, C b, which is bound to the mitochondria (b), is proportional to the intensity of the fluorescence I b. On the other hand, the free dye molecules (f) in the aqueous medium exhibit practically no fluorescence, I f≪I b. The intensity of the fluorescence I=I b was measured as a function of time t; the measured values were corrected for photobleaching. The fluorescence intensity I(t) at first increases linearly with t and reaches a saturation value for t → ∞. In the linear range of I(t) the flow J o=(dI/dt)o of the dye into the cell depends strongly on the dye concentration and increases linearly with C D. The concentration range C D=10−9−10−5 M at 37° C was investigated. From the linear correlation between J o and C D it follows that the kinetics of the vital staining of mitochondria is controlled by diffusion. At t=0 the flow of the xenobiotic agent through the cell membrane determines the rate of staining. The slope dJ o/dC D of the plot J o vs C D describes the efficiency of dye accumulation at the mitochondria and strongly increases with increasing lipophilicity of the dye molecules. Thus lipophilic dyes pass through the cell membrane more easily than less lipophilic molecules.
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  • 9
    ISSN: 1432-119X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Summary The fluorochrome AMHA (3-amino-6-methoxy-9-(2-hydroxyethylamino)acridine) stains the nuclear chromatin and the chromosomes of living HeLa cells. At relatively low dye concentrations C F≤10−4 M and short incubation periods t I≤2 h cell growth is not affected by the drug. But at higher C F and longer t I the population doubling time of the cell cultures rapidly increases, and finally the cells die. In vital staining experiments the dye AMHA preferentially binds to the DNA of the nuclei and to the chromosomes of the cells, respectively. The dye binding to DNA has been proved by the absorption and emission microspectra of the stained cells, and by the comparison with authentic spectra of AMHA bound to DNA in aqueous solutions. Within the limits of experimental errors both types of spectra are identical. The spectra of DNA-bound AMHA show a characteristic gap of ca. 3500 cm−1 between the 0-0-transitions of the long wave length 1 L a absorption and the fluorescence. AMHA molecules dissolved in the polar solvent water have a gap of even 4100 cm−1. This energy gap shows that the electron distribution of AMHA is strongly changed by light absorption and emission. Finally, using absorption spectroscopy, we investigated the binding of AMHA to DNA in aqueous solutions over a wide range of concentrations of the dye, of nuceleic acid (calf thymus), and of the competitor NaCl respectively. The Scatchard binding isotherms were determined. With the method of competitive salt effect three different bonds of AMHA to DNA can be distinguished even at low dye concentrations: The intercalation 1 of the fluorochrome F, binding constant K F1=1,1·105 M −1, binding parameter n 1=0,15; the pre-intercalative or external binding 2, K F2=6,9·105 M −1, n 2=0,21; the external binding 3, K F3=2,8·105 M −1, n 3=0,55. Externally bound dye molecules 2 and 3 occupy two phosphodiester residues of the DNA. A detailed discussion of the data and the competitive salt effect shows that in living cells only intercalated and small amounts of pre-intercalatively bound molecules 1 and 2 exist. The binding constant K F1=1,1·105 M −1 of AMHA is unusual high in comparison with the constants of intercalation of other dyes, K F1=(1–4)·104 M −1. Therefore, the amount of intercalated AMHA is also relatively high, and it is possible to visualize the DNA-bound fluorochrome in the nuclei and chromosomes of the living cells under the fluorescence microscope.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The 1000 km long Ok Tedi/Fly River system receives about 66 Mt/year of mining waste from the Ok Tedi copper-gold porphyry mine. Mine input has increased the suspended sediment load of the Middle Fly River about 5–10 times over the natural background. A significant yet unknown amount of copper-rich material deposits unevenly in the extensive tropical lowland floodplain. Recent alluvial sediments of the Fly River floodplain have copper contents of 620 mg/kg (±1σ: 430–900), whereas the regional background is 40 mg/kg (±σ: 25–60). This pattern is mirrored and enhanced by the gold dispersal pattern with a 7 ppb Au background versus a 140–275 ppb population in mine-derived material. Very high deposition rates (around 4 cm/y) of mine-derived sediment were determined in locations close to the creeks and channels which link the Fly River with the outer floodplain. A thin layer of 1–5 cm of copper-rich material (400–900 mg/kg Cu) was usually found on the bottom of drowned (tributary) valley lakes. Average dissolved copper content in waters of the inner floodplain is around 9 μg/l (±1σ: 5–14) as compared to unpolluted water from the outer floodplain with 〈 2 μg/l Cu. The present Fly River water, about 600 km downstream of the mine site, has concentrations of 17 ± 3 μg/l dissolved Cu.
    Type of Medium: Electronic Resource
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