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...

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Main Authors: Livio Ruffine, Jean-Pierre Donval, Claire Croguennec, Laurent Bignon, Dominique Birot, Anne Battani, Germain Bayon, Jean-Claude Caprais, Nadine Lantéri, Denis Levaché, Stéphanie Dupré
Format: Article
Language:English
Published: Hindawi-Wiley 2017-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2017/4240818
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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
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