Evidence for methane and hydrogen sulfide venting imprinted on a Quaternary eolianite from southern Israel
Two different and physically separated chemosynthetic communities of bacteria are responsible for the formation of the Beeri native sulfur deposit hosted in a Late Quaternary sandstone on the southern coastal plain of Israel. The enriched concentrations are distributed over an area of about 1 km sup...
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Veröffentlicht in: | Geo-marine letters 1994-06, Vol.14 (2-3), p.170-176 |
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