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Detailed Reference Information |
Van Dover, C.L., Reynolds, G.T., Chave, A.D. and Tyson, J.A. (1996). Light at deep-sea hydrothermal vents. Geophysical Research Letters 23: doi: 10.1029/96GL02151. issn: 0094-8276. |
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Ambient light spectral data were acquired at two deep-sea hydrothermal vents with a temperature of ~350 ¿C; the Hole-to-Hell site on the East Pacific Rise at 9 ¿N and the Snake-Pit site on the Mid-Atlantic Ridge. Measurements were made with a simple, multi-channel photometer which simultaneously detected light in four 100 nm-wide bands over the wavelength range of 650--1050 nm. Most of the light detected is near-infrared (750--1050 nm), but there is a 19¿ greater photon flux than expected from thermal radiation alone at shorter wavelengths (650--750 nm) at the Hole-to-Hell vent. At Snake Pit, more light in the 750--850 nm band was observed 10 cm above the orifice where the temperature was 50--100 ¿C than at the 350 ¿C vent opening. These data suggest the presence of non-thermal light sources in the vent environment. Some possible non-thermal mechanisms are identified, but further data will be required to resolve them. ¿ American Geophysical Union 1996 |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Tectonophysics, Hydrothermal systems, Volcanology, Hydrothermal systems, Marine Geology and Geophysics, Heat flow (benthic) and hydrothermal processes, Oceanography, Biological and Chemical, Microbiology |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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