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  • 1
    Electronic Resource
    Electronic Resource
    Melatonin in der Dermatologie Experimentelle und klinische Aspekte (1999)
    Springer
    Der Hautarzt 50 (1999), S. 5-11 
    Details
    ISSN: 1432-1173
    Keywords: Schlüsselwörter Melatonin (N-Acetyl-5-Methoxytryptamin) ; Zirkadianer Rhythmus ; Schlaf-Wach-Rhythmus ; Radikalfänger ; Key words Melatonin (N-acethyl-5-methoxytryptamin) ; Circadian rhythm ; Daily sleep induction ; ageing ; Free radical scavenger
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Summary Melatonin (N-acetyl-5-methoxytryptamine) is a hormone with multiple functions in humans, produced by the pineal gland and stimulated by β-adrenergic receptors. Serum melatonin levels exhibit a circadian rhythm with low levels during the day, rise in the evening and maximum levels at night between 2 and 4 a.m.. Melatonin participates in the regulation of several physiological processes such as seasonal biological rhythm, daily sleep induction, aging and modulation of immunobiological defence reactions. Furthermore, melatonin has a highly lipophilic molecular structure facilitating penetration of cell membranes and serving as an extra- and intracellular free radical scavenger. Melatonin seems to quench mainly hydroxyl radicals, the most damaging of all free radicals. Melatonin may play a role in the etiology and treatment of several dermatoses e.g. atopic eczema, psoriasis and malignant melanoma. The influence of melatonin on hair growth is another aspect. Topical application of melatonin inhibits the development of UV-erythema. Penetration through skin after topical application and oral bioavailability auxit further investigations on the pharmacokinetic and pharmacodynamic actions of melatonin.
    Notes: Zusammenfassung Melatonin (N-Acetyl-5-Methoxytryptamin) ist ein unter dem Einflußβ-adrenerger Rezeptoren von der Glandula pinealis produziertes und sezerniertes Hormon mit vielfältigem Wirkungsspektrum. Die Ausschüttung des Hormons folgt einem zirkadianen Rhythmus mit niedrigen, gleichmäßigen Spiegeln tagsüber und einem abendlichen Ansteigen und nächtlichen Peak zwischen 2.00 und 4.00 Uhr. Melatonin beeinflußt den saisonalen Biorhythmus, den Schlaf-Wach-Rhythmus, den Alterungsprozeß und moduliert immunbiologische Abwehrfunktionen. Zusätzlich besitzt Melatonin unabhängig von einem Rezeptorsystem durch seine starken lipophilen Eigenschaften die Fähigkeit, frei durch Zellmembranen zu diffundieren und im extra- wie intrazellulären Raum als Radikalfänger zu wirken. Die Affinität zu dem stark schädigenden Hydroxylradikal ist besonders groß. In der Dermatologie ergeben sich für Melatonin Perspektiven bei einigen Hauterkrankungen wie zum Beispiel dem atopischen Ekzem, der Psoriasis und dem malignen Melanom. Der Einfluß von Melatonin auf das Haarwachstum ist ein weiterer Aspekt. In topischer Anwendung hat Melatonin eine suppressive Wirkung auf die Ausbildung eines UV-Erythems. Über die Penetrationseigenschaften durch die Haut und die orale Verfügbarkeit liegen einige Erkenntnisse vor, die durch weitere Untersuchungen der Pharmakokinetik und Pharmakodynamik ergänzt werden können.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s001050050857
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  • 2
    Electronic Resource
    Electronic Resource
    Geochemical and isotopic evidence for seawater contamination of the hydrothermal system of Taal Volcano, Luzon, the Philippines (1998)
    Springer
    Bulletin of volcanology 59 (1998), S. 562-576 
    Details
    ISSN: 1432-0819
    Keywords: Key words Hydrothermal system ; Fluid geochemistry ; Stable isotopes ; Geochemical monitoring ; Taal Volcano
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The hydrologic structure of Taal Volcano has favored development of an extensive hydrothermal system whose prominent feature is the acidic Main Crater Lake (pH〈3) lying in the center of an active vent complex, which is surrounded by a slightly alkaline caldera lake (Lake Taal). This peculiar situation makes Taal prone to frequent, and sometimes catastrophic, hydrovolcanic eruptions. Fumaroles, hot springs, and lake waters were sampled in 1991, 1992, and 1995 in order to develop a geochemical model for the hydrothermal system. The low-temperature fumarole compositions indicate strong interaction of magmatic vapors with the hydrothermal system under relatively oxidizing conditions. The thermal waters consist of highly, moderately, and weakly mineralized solutions, but none of them corresponds to either water–rock equilibrium or rock dissolution. The concentrated discharges have high Na contents (〉3500 mg/kg) and low SO4/Cl ratios (〈0.3). The Br/Cl ratio of most samples suggests incorporation of seawater into the hydrothermal system. Water and dissolved sulfate isotopic compositions reveal that the Main Crater Lake and spring discharges are derived from a deep parent fluid (T≈300  °C), which is a mixture of seawater, volcanic water, and Lake Taal water. The volcanic end member is probably produced in the magmatic-hydrothermal environment during absorption of high-temperature gases into groundwater. Boiling and mixing of the parent water give rise to the range of chemical and isotopic characteristics observed in the thermal discharges. Incursion of seawater from the coastal region to the central part of the volcano is supported by the low water levels of the lakes and by the fact that Lake Taal was directly connected to the China sea until the sixteenth century. The depth to the seawater-meteoric water interface is calculated to be 80 and 160 m for the Main Crater Lake and Lake Taal, respectively. Additional data are required to infer the hydrologic structure of Taal. Geochemical surveillance of the Main Crater Lake using the SO4/Cl, Na/K, or Mg/Cl ratio cannot be applied straightforwardly due to the presence of seawater in the hydrothermal system.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s004450050210
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  • 3
    Electronic Resource
    Electronic Resource
    Non-immunologic contact urticaria from chrysanthemum con rmed by the CAST method (1999)
    Oxford, UK : Blackwell Publishing Ltd
    Contact dermatitis 41 (1999), S. 0 
    Details
    ISSN: 1600-0536
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1600-0536.1999.tb06168.x
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  • 4
    Electronic Resource
    Electronic Resource
    Effects of various grit-containing cleansers on skin barrier function (1999)
    Oxford, UK : Blackwell Publishing Ltd
    Contact dermatitis 41 (1999), S. 0 
    Details
    ISSN: 1600-0536
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Products intended for individuals in contact with strongly adhering dirt often contain grit. Various clinical test methods have been developed for evaluating the potential of personal washing products to induce skin irritation. In the present study, differences in the irritant effects of washing products containing naturally-derived grit and synthetic grit were investigated in a forearm wash test. The forearms of 16 test subjects were washed in a total of 18 treatments (4 per day for 4 days, with 2 treatments on the 5th day). Treatment consisted of continuous washing for 2 min by a technician, who gently slid his fingertips with the lather up and down the forearm. Non-invasive instrumental measurements of skin barrier function were performed. Repetitive washing for 1 week lead to increased TEWL values, skin redness and decreased stratum corneum hydration. Results indicate differences in irritancy potential due to different types of grit, their surface and concentration. It is concluded that the repeated wash test seems to be adequate for rating personal washing products that contain grit.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1600-0536.1999.tb06104.x
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  • 5
    Electronic Resource
    Electronic Resource
    Geochemistry of the volcano-hydrothermal system of El Chichón Volcano, Chiapas, Mexico (1998)
    Springer
    Bulletin of volcanology 59 (1998), S. 436-449 
    Details
    ISSN: 1432-0819
    Keywords: Key words El Chichón Volcano ; Crater Lake ; Hydrothermal system ; Volcanic gases ; Stable isotopes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The 1982 eruption of El Chichón volcano ejected more than 1 km3 of anhydrite-bearing trachyandesite pyroclastic material to form a new 1-km-wide and 300-m-deep crater and uncovered the upper 500 m of an active volcano-hydrothermal system. Instead of the weak boiling-point temperature fumaroles of the former lava dome, a vigorously boiling crater spring now discharges  / 20 kg/s of Cl-rich (∼15 000 mg/kg) and sulphur-poor ( / 200 mg/kg of SO4), almost neutral (pH up to 6.7) water with an isotopic composition close to that of subduction-type magmatic water (δD=–15‰, δ18O=+6.5‰). This spring, as well as numerous Cl-free boiling springs discharging a mixture of meteoric water with fumarolic condensates, feed the crater lake, which, compared with values in 1983, is now much more diluted (∼3000 mg/kg of Cl vs 24 030 mg/kg), less acidic (pH=2.6 vs 0.56) and contains much lower amounts of S ( / 200 mg/kg of SO4, vs 3550 mg/kg) with δ34S=0.5–4.2‰ (+17‰ in 1983). Agua Caliente thermal waters, on the southeast slope of the volcano, have an outflow rate of approximately 100 kg/s of 71  °C Na–Ca–Cl water and are five times more concentrated than before the eruption (B. R. Molina, unpublished data). Relative N2, Ar and He gas concentrations suggest extensional tectonics for the El Chichón volcanic centre. The 3He/4He and 4He/20Ne ratios in gases from the crater fumaroles (7.3Ra, 2560) and Agua Caliente hot springs (5.3Ra, 44) indicate a strong magmatic contribution. However, relative concentrations of reactive species are typical of equilibrium in a two-phase boiling aquifer. Sulphur and C isotopic data indicate highly reducing conditions within the system, probably associated with the presence of buried vegetation resulting from the 1982 eruption. All Cl-rich waters at El Chichón have a common source. This water has the appearence of a "partially matured" magmatic fluid: condensed magmatic vapour neutralized by interaction with fresh volcaniclastic deposits and depleted in S due to anhydrite precipitation. Shallow ground waters emerging around the volcano from the thick cover of fresh pumice deposits (Red waters) are Ca–SO4–rich and have a negative oxygen isotopic shift, probably due to ongoing formation of clay at low temperatures.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s004450050202
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