2009
DOI: 10.1016/j.gca.2008.12.030
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Differential aerobic and anaerobic oxidation of hydrocarbon gases discharged at mud volcanoes in the Nile deep-sea fan

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Cited by 52 publications
(52 citation statements)
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“…The occurrence of hydrocarbons (ϾC 4 ) other than natural gas is known for the Paclele Mici mud volcano (28), but for the Amon mud volcano and Nyegga methane seeps, there have been no assessments for the presence of hydrocarbons higher than C 4 to date (32,33,52). While the detection of putative assA homologues is expected for natural gas seepages due to the degradation of short-chain alkanes via fumarate addition (5,53), the discovery of only bssA genes related to Desulfobacula toluolica in Amon mud volcano sediments was unexpected.…”
Section: Discussionmentioning
confidence: 99%
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“…The occurrence of hydrocarbons (ϾC 4 ) other than natural gas is known for the Paclele Mici mud volcano (28), but for the Amon mud volcano and Nyegga methane seeps, there have been no assessments for the presence of hydrocarbons higher than C 4 to date (32,33,52). While the detection of putative assA homologues is expected for natural gas seepages due to the degradation of short-chain alkanes via fumarate addition (5,53), the discovery of only bssA genes related to Desulfobacula toluolica in Amon mud volcano sediments was unexpected.…”
Section: Discussionmentioning
confidence: 99%
“…The DNA was extracted with a Power soil RNA extraction kit and DNA elution accessory kit (MO BIO Laboratories, Carlsbad, CA). Sediment samples from the Amon mud volcano in the eastern Nile deep-sea fan (station 929, dive 240 [33]) and Guaymas Basin hydrocarbon seeps in the Gulf of California (dive 5473 [34]) were collected from below a microbial mat. The DNA was extracted as described by Kleindienst PCR amplification.…”
Section: Methodsmentioning
confidence: 99%
“…Geochemical studies of anoxic deep-sea sediments provided the first indications that propane and butane are also degraded under anoxic conditions, suggesting a significant influence on the carbon and sulfur cycles in hydrocarbon-impacted environments. These data include the 13 C-enrichment of propane and butane in sediment interstitial waters atop gas hydrates (Sassen et al, 2004) or at deep sea mud volcanoes (Mastalerz et al, 2009), sulfate-reduction rates much higher than could be accounted for by anaerobic oxidation of methane in hydrothermal sediments or at cold seeps Kallmeyer and Boetius, 2004;Orcutt et al 2004Orcutt et al , 2010Kleindienst et al, 2012), or the apparent consumption of shortchain alkanes at mud volcanoes (Niemann et al, 2006). In addition, oxidation of propane under anoxic conditions has been determined in sediments collected from marine gas seeps (Quistad and Valentine, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…Each of these three fluxes would be substantially larger if not for microbial oxidation in the sediments and water column (68). Methane, ethane, and propane are subject to anaerobic oxidation in anoxic sediments and water columns (44,53,68) or to aerobic oxidation in oxic and suboxic water columns and oxygenated surface sediment (10,47,53,80). We focus here on aerobic oxidation.…”
mentioning
confidence: 99%