Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes
During the scientific expedition GAZCOGNE2 at the Bay of Biscay nine gas seeps were sampled for the first time and their flux was measured using an in situ pressure-preservation sampler (PEGAZ, ©IFREMER). Overall, three sites were investigated to determine the nature and the origin of the gases bubb...
Main Authors: | , , , , , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Hindawi-Wiley
2017-01-01
|
Series: | Geofluids |
Online Access: | http://dx.doi.org/10.1155/2017/4240818 |
id |
doaj-ac0f1674890944d289ec12b0f6e1e12e |
---|---|
record_format |
Article |
spelling |
doaj-ac0f1674890944d289ec12b0f6e1e12e2020-11-25T02:28:06ZengHindawi-WileyGeofluids1468-81151468-81232017-01-01201710.1155/2017/42408184240818Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local FluxesLivio Ruffine0Jean-Pierre Donval1Claire Croguennec2Laurent Bignon3Dominique Birot4Anne Battani5Germain Bayon6Jean-Claude Caprais7Nadine Lantéri8Denis Levaché9Stéphanie Dupré10IFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceIFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceIFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceIFREMER, Unité des Recherches et Développements Technologiques, 29280 Plouzané, FranceIFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceIFREMER, Unité des Ecosystèmes Profonds, 29280 Plouzané, FranceIFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceIFPEN, 1-4 avenue de Bois-Préau, 92852 Rueil-Malmaison Cedex, FranceIFREMER, Unité des Recherches et Développements Technologiques, 29280 Plouzané, FranceTOTAL, avenue Larribau, 64000 Pau, FranceIFREMER, Unité des Géosciences Marines, 29280 Plouzané, FranceDuring the scientific expedition GAZCOGNE2 at the Bay of Biscay nine gas seeps were sampled for the first time and their flux was measured using an in situ pressure-preservation sampler (PEGAZ, ©IFREMER). Overall, three sites were investigated to determine the nature and the origin of the gases bubbling at the seafloor and forming acoustic plumes into the water column, as this was the question raised from the first geologic study of the area. This has guided our study and accordingly corresponds to the main purpose of the present article. Thus, the molecular and isotopic (δD and δ13C) analyses revealed that the gas seeps were primarily composed of methane. Both methane and ethane are of microbial origin, and the former has been generated by microbial reduction of carbon dioxide. Heavier hydrocarbons accounted for less than 0.06% mol of the total amount. Despite the microbial origin of methane, the samples exhibit subtle differences with respect to the δ13CCH4 values, which varied between −72.7 and −66.1‰. It has been suggested that such a discrepancy was predominantly governed by the occurrence of anaerobic methane oxidation. The PEGAZ sampler also enabled us to estimate the local gas fluxes from the sampled streams. The resulting values are extremely heterogeneous between seeps, ranging from 35 to 368 mLn·min−1. Assuming a steady discharge, the mean calculated methane emission for the nine seeps is of 38 kmol·yr−1. Considering the extent of the seep area, this very local estimate suggests that the Aquitaine Shelf is a very appropriate place to study methane discharge and its fate on continental shelves.http://dx.doi.org/10.1155/2017/4240818 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Livio Ruffine Jean-Pierre Donval Claire Croguennec Laurent Bignon Dominique Birot Anne Battani Germain Bayon Jean-Claude Caprais Nadine Lantéri Denis Levaché Stéphanie Dupré |
spellingShingle |
Livio Ruffine Jean-Pierre Donval Claire Croguennec Laurent Bignon Dominique Birot Anne Battani Germain Bayon Jean-Claude Caprais Nadine Lantéri Denis Levaché Stéphanie Dupré Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes Geofluids |
author_facet |
Livio Ruffine Jean-Pierre Donval Claire Croguennec Laurent Bignon Dominique Birot Anne Battani Germain Bayon Jean-Claude Caprais Nadine Lantéri Denis Levaché Stéphanie Dupré |
author_sort |
Livio Ruffine |
title |
Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes |
title_short |
Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes |
title_full |
Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes |
title_fullStr |
Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes |
title_full_unstemmed |
Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes |
title_sort |
gas seepage along the edge of the aquitaine shelf (france): origin and local fluxes |
publisher |
Hindawi-Wiley |
series |
Geofluids |
issn |
1468-8115 1468-8123 |
publishDate |
2017-01-01 |
description |
During the scientific expedition GAZCOGNE2 at the Bay of Biscay nine gas seeps were sampled for the first time and their flux was measured using an in situ pressure-preservation sampler (PEGAZ, ©IFREMER). Overall, three sites were investigated to determine the nature and the origin of the gases bubbling at the seafloor and forming acoustic plumes into the water column, as this was the question raised from the first geologic study of the area. This has guided our study and accordingly corresponds to the main purpose of the present article. Thus, the molecular and isotopic (δD and δ13C) analyses revealed that the gas seeps were primarily composed of methane. Both methane and ethane are of microbial origin, and the former has been generated by microbial reduction of carbon dioxide. Heavier hydrocarbons accounted for less than 0.06% mol of the total amount. Despite the microbial origin of methane, the samples exhibit subtle differences with respect to the δ13CCH4 values, which varied between −72.7 and −66.1‰. It has been suggested that such a discrepancy was predominantly governed by the occurrence of anaerobic methane oxidation. The PEGAZ sampler also enabled us to estimate the local gas fluxes from the sampled streams. The resulting values are extremely heterogeneous between seeps, ranging from 35 to 368 mLn·min−1. Assuming a steady discharge, the mean calculated methane emission for the nine seeps is of 38 kmol·yr−1. Considering the extent of the seep area, this very local estimate suggests that the Aquitaine Shelf is a very appropriate place to study methane discharge and its fate on continental shelves. |
url |
http://dx.doi.org/10.1155/2017/4240818 |
work_keys_str_mv |
AT livioruffine gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT jeanpierredonval gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT clairecroguennec gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT laurentbignon gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT dominiquebirot gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT annebattani gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT germainbayon gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT jeanclaudecaprais gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT nadinelanteri gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT denislevache gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes AT stephaniedupre gasseepagealongtheedgeoftheaquitaineshelffranceoriginandlocalfluxes |
_version_ |
1724840285729456128 |