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Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin

Nature volume 295, pages 198–202 (1982)Cite this article

Abstract

Petroleum has been dredged from an active hydrothermal mound area in the southern rift of Guaymas Basin, Gulf of California. This organic matter is composed of gasoline-range aliphatic and aromatic hydrocarbons and predominantly residual polar asphaltic material. The aliphatic hydrocarbons of two bitumen samples have very different boiling range and composition. Both samples contain polynuclear aromatic hydrocarbons and olefins, which indicate formation at pyrolytic temperatures. The overall compositional data indicate an origin from biological detritus by thermal alteration and rapid quenching by hydrothermal removal, followed by condensation at the seabed.

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Author information

Author notes

  1. Bernd R. T. Simoneit

    Present address: School of Oceanography, Oregon State University, Corvallis, Oregon, 97331, USA

Authors and Affiliations

  1. Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California, 90024, USA

    Bernd R. T. Simoneit

  2. Marine Physical Laboratory, Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California, 92093, USA

    Peter F. Lonsdale

Authors
  1. Bernd R. T. Simoneit
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  2. Peter F. Lonsdale
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Simoneit, B., Lonsdale, P. Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin. Nature 295, 198–202 (1982). https://doi.org/10.1038/295198a0

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