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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Munksgaard International Publishers
    Journal of pineal research 37 (2004), S. 0 
    ISSN: 1600-079X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Abstract  An investigation of the antioxidative UV protective effect of melatonin was performed in an in vitro irradiation model with leukocytes. Leukocytes were isolated from EDTA-treated whole blood and taken up in phosphate-buffered saline (PBS). Five of 10 aliquots were incubated with 2 mmol/L melatonin and 5 with PBS as a control. The samples were irradiated by UV light (280–360 nm, max: 310 nm) at doses between 75 and 300 mJ/cm2 or left unirradiated. Radical formation was measured using the chemiluminescence technique. Staining with trypan blue was performed to assess cell viability. Melatonin significantly suppressed radical formation in cell solutions irradiated from 75 to 300 mJ/cm2 (P ≤ 0.001). Controls showed an increase of reactive oxygen species (ROS) formation as a sign of oxidative stress when irradiated with increasing UV doses and a maximum ROS formation under 300 mJ/cm2 UV light. The cytotoxicity of UV light was reduced by melatonin up to a UV dose of 1.5 J/cm2. Leukocytes were suitable cells for the evaluation of the efficacy of melatonin as a radical scavenger under UV light. The results confirm that the clinically observed UV protective effects of melatonin may be at least partially based on its radical scavenging properties.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Copenhagen : Munksgaard International Publishers
    Journal of pineal research 31 (2001), S. 0 
    ISSN: 1600-079X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Reactive oxygen species (ROS) are presumed to be involved in inflammatory UV reactions of the skin. This in vitro study was performed to investigate the suppressive effect of melatonin in interleukin-3 (IL-3) stimulated leukocytes. Neutrophilic granulocytes were isolated from EDTA-treated whole blood and placed in a phosphate-buffered saline (PBS) containing IL-3. Cell suspensions were either treated with PBS (control) or with increasing doses of melatonin (0.1, 0.5, 1, 2, 3, 5, 7.5, 10 mmol). One PBS solution was left unirradiated and the other nine solutions (PBS and melatonin) were irradiated with 750 mJ/cm2 UVB light (280–360 nm, max: 310 nm). Radical formation was measured by the chemiluminescence technique. UV-irradiated leukocytes showed a 5-fold higher radical formation than unirradiated leukocytes. Melatonin, in increasing doses in powers of ten, led to a maximum suppression of free radicals at 10 nmol (P=0.01) and 1 mmol melatonin (P=0.001), showing a biphasic, non-linear, dose–response relationship. Melatonin, given in amounts of 0.1–10 mmol, led to a direct dose-dependent suppression of ROS. Radical formation was suppressed significantly in a range from 0.5 to 10 mmol (P=0.001). Melatonin is known to function as a radical scavenger and antioxidant; some of these melatonin effects may be receptor independent, while others may be receptor dependent.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-0819
    Keywords: Cumbal Volcano Hydrothermal system Gases Fumaroles Springs Geochemistry Isotopes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract. We present chemical and isotopic data for fumarolic vapor and thermal spring discharges from Cumbal Volcano, SW Colombia. In 1988 Cumbal showed signs of apparent reactivation. Gases and steam condensates were sampled from summit fumaroles (83–375°C) of Cumbal in 1988–1996 and discharges from thermal springs (15–37°C) on its flanks in 1995–1996. Based on relative CO2, total S (H2S+SO2), and HCl contents, fumarolic discharges are principally magmatic in composition. Fumarolic steam condensates (1993–1996) have δ18O values of –11.4 to +2.5‰ and δD values of –91 to –43‰. δ18O and δD compositions indicate mixing between local meteoric and magmatic waters. 3He/4He ratios in 1993–1996 samples (5.3–7.9 Rcor) are consistent with addition of mantle-derived helium. δ13CCO2 values for 1996 samples (–6.7 to –5.0‰) likely indicate contribution of marine-carbonate, organic sediment, and mantle-derived CO2. δ34SStotal compositions (–4.6 to +5.6‰) of 1988–1996 fumarolic discharges have magmatic signatures and may reflect cycles of deposition and remobilization of native sulfur. Thermal waters are acid-sulfate or bicarbonate in composition. Relative concentrations of chemical constituents of thermal waters imply that the composition of waters is controlled by absorption of magmatic volatiles into shallow ground- and surface waters, dilution with meteoric waters along flow paths, and dissolution of host rocks. δ18O and δD compositions are consistent with a meteoric origin of waters. δ34SStotal values for thermal spring gas discharges (9.6–10.5‰) suggest deposition of δ34S-depleted sulfur minerals along flow paths. Chemical and isotopic compositions of 1988–1995 fumarolic discharges provide evidence for input of magmatic volatiles into the Cumbal hydrothermal system. From 1995 to 1996, geochemical data show increasing hydrothermal signatures, suggesting a decline in magmatic volatile input.
    Type of Medium: Electronic Resource
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