A persistent oxygen anomaly reveals the fate of spilled methane in the deep Gulf of Mexico
Kessler, J.D.; Valentine, D.L.; Redmond, M.C.; Du, M.; Chan, E.W.; Mendes, S.D.; Quiroz, E.W.; Villanueva, C.J.; Shusta, S.S.; Werra, L.M.; Yvon-Lewis, S.; Weber, T.C. (2011). A persistent oxygen anomaly reveals the fate of spilled methane in the deep Gulf of Mexico. Science (Wash.) 331(6015): 312-315. https://dx.doi.org/10.1126/science.1199697
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075; e-ISSN 1095-9203, meer
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| Auteurs | | Top |
- Kessler, J.D.
- Valentine, D.L.
- Redmond, M.C.
- Du, M.
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- Chan, E.W.
- Mendes, S.D.
- Quiroz, E.W.
- Villanueva, C.J.
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- Shusta, S.S.
- Werra, L.M.
- Yvon-Lewis, S.
- Weber, T.C.
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| Abstract |
Methane was the most abundant hydrocarbon released during the 2010 Deepwater Horizon oil spill in the Gulf of Mexico. Beyond relevancy to this anthropogenic event, this methane release simulates a rapid and relatively short-term natural release from hydrates into deep water. Based on methane and oxygen distributions measured at 207 stations throughout the affected region, we find that within similar to 120 days from the onset of release similar to 3.0 x 10(10) to 3.9 x 10(10) moles of oxygen were respired, primarily by methanotrophs, and left behind a residual microbial community containing methanotrophic bacteria. We suggest that a vigorous deepwater bacterial bloom respired nearly all the released methane within this time, and that by analogy, large-scale releases of methane from hydrate in the deep ocean are likely to be met by a similarly rapid methanotrophic response. |
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