(Q59082062)

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Is the CH4, H2 and CO venting from submarine hydrothermal systems produced by thermophilic bacteria?

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Is the CH4, H2 and CO venting from submarine hydrothermal systems produced by thermophilic bacteria? (English)

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John A. Baross

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Marvin D. Lilley

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2

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Louis I. Gordon

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3

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English

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publication date

July 1982

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Nature

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volume

298

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issue

5872

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page(s)

366-368

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exact match

https://scigraph.springernature.com/pub.10.1038/298366a0

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Generic Assignments, Strain Histories and Properties of Pure Cultures of Cyanobacteria

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21 January 2018

A Major Helium-3 Source at 15{degrees}S on the East Pacific Rise

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7 January 2021

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Submarine thermal sprirngs on the galapagos rift

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7 January 2021

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East pacific rise: hot springs and geophysical experiments

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Sulfide Deposits from the East Pacific Rise Near 21 N

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7 January 2021

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Geothermal System at 21{degrees}N

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Dietary carbon sources of mussels and tubeworms from Galápagos hydrothermal vents determined from tissue 14C activity

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7 January 2021

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Calvin-Benson cycle and sulphide oxidation enzymes in animals from sulphide-rich habitats

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The environmental crisis: quantifying geosphere interactions

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Determination of the C1 to C4 Hydrocarbons in Sea Water by Gas Chromatography

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7 January 2021

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10.1038/298366A0

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1019805903

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(Q59082062)

Is the CH4, H2 and CO venting from submarine hydrothermal systems produced by thermophilic bacteria?

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