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Science 29 September 2000: Vol. 289. no. 5488, pp. 2332 - 2335 DOI: 10.1126/science.289.5488.2332
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Reports
Dating of Pore Waters with 129I: Relevance for the Origin of Marine Gas Hydrates
Udo Fehn,1*
Glen Snyder,1
Per K. Egeberg2
Pore waters associated with gas hydrates at Blake Ridge in the
Atlantic Ocean were dated by measuring their iodine-129/iodine ratios.
Samples collected from sediments with ages between 1.8 and 6 million
years ago consistently yield ages around 55 million years ago. These
ages, together with the strong iodine enrichment observed in the pore
waters, suggest that the origin of iodine is related to organic
material of early Tertiary age, which probably is also the source of
the methane in the gas hydrates at this location.
1 Department of Earth and Environmental
Sciences, University of Rochester, Rochester, NY 14627, USA.
2 Department of Chemistry, Agder College,
Tordenskjoldgate 65, 4604 Kristiansand, Norway.
*
To whom correspondence should be addressed. E-mail:
fehn{at}earth.rochester.edu
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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Age variation of pore water iodine in the eastern Nankai Trough, Japan: Evidence for different methane sources in a large gas hydrate field.
- H. Tomaru, Z. Lu, U. Fehn, Y. Muramatsu, and R. Matsumoto (2007)
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35, 1015-1018
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- Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan.
- U. Fehn, G. T. Snyder, R. Matsumoto, Y. Muramatsu, and H. Tomaru (2003)
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- Microbial Communities from Methane Hydrate-Bearing Deep Marine Sediments in a Forearc Basin.
- D. W. Reed, Y. Fujita, M. E. Delwiche, D. B. Blackwelder, P. P. Sheridan, T. Uchida, and F. S. Colwell (2002)
Appl. Envir. Microbiol.
68, 3759-3770
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- Iodine-129 constraints on residence times of deep marine brines in the Canadian Shield.
- D. J. Bottomley, R. Renaud, T. Kotzer, and I. D. Clark (2002)
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30, 587-590
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