Articles | Volume 12, issue 10
https://doi.org/10.5194/se-12-2439-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-2439-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 Oct 2021
Research article |
| 28 Oct 2021
| 28 Oct 2021
What makes seep carbonates ignore self-sealing and grow vertically: the role of burrowing decapod crustaceans
Jean-Philippe Blouet
CORRESPONDING AUTHOR
Department of Geosciences, University of Fribourg, 1700 Fribourg, Switzerland
Department of Geosciences, Environment and Society, Université Libre de Bruxelles, 1050 Brussels, Belgium
Fluid Venting System Research Group, 54000 Nancy, France
Patrice Imbert
Fluid Venting System Research Group, 54000 Nancy, France
Laboratoire des fluides complexes et leurs réservoirs, LFCR, E2S-UPPA, CNRS, TotalEnergies, Université de Pau et Pays de l'Adour, 64000 Pau, France
Sutieng Ho
CORRESPONDING AUTHOR
Fluid Venting System Research Group, 54000 Nancy, France
Ocean Center, National Taiwan University, 10671 Taipei, Taiwan
Andreas Wetzel
Department of Environmental Sciences – Geology, University of Basel, 4056 Basel, Switzerland
Anneleen Foubert
Department of Geosciences, University of Fribourg, 1700 Fribourg, Switzerland
Related authors
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
Short summary
Short summary
A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Maxim Rubin-Blum, Eyal Rahav, Guy Sisma-Ventura, Yana Yudkovski, Zoya Harbozov, Or Bialik, Oded Ezra, Anneleen Foubert, Barak Herut, and Yizhaq Makovsky
EGUsphere, https://doi.org/10.5194/egusphere-2024-1285, https://doi.org/10.5194/egusphere-2024-1285, 2024
Short summary
Short summary
Geochemical cycles and biodiversity are altered at transition zones of chemosynthetic ecosystems, chemotones. We asked if burrowing alters the functionality of these habitats. We surveyed the seafloor, analyzed sediment properties, and explored microbial communities in ghost shrimp burrows. We made an exciting discovery of chemosynthetic biofilms, linking them to macromolecule turnover and nutrient cycling, using metagenomics. This phenomenon may play an important role in biogeochemical cycles.
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, and Anneleen Foubert
Clim. Past, 18, 1915–1945, https://doi.org/10.5194/cp-18-1915-2022, https://doi.org/10.5194/cp-18-1915-2022, 2022
Short summary
Short summary
The investigation of a 9 m long sediment core recovered at ca. 300 m water depth demonstrates that cold-water coral mound build-up within the East Melilla Coral Province (southeastern Alboran Sea) took place during both interglacial and glacial periods. Based on the combination of different analytical methods (e.g. radiometric dating, micropaleontology), we propose that corals never thrived but rather developed under stressful environmental conditions.
Robin Fentimen, Eline Feenstra, Andres Rüggeberg, Efraim Hall, Valentin Rime, Torsten Vennemann, Irka Hajdas, Antonietta Rosso, David Van Rooij, Thierry Adatte, Hendrik Vogel, Norbert Frank, Thomas Krengel, and Anneleen Foubert
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-82, https://doi.org/10.5194/cp-2020-82, 2020
Manuscript not accepted for further review
Short summary
Short summary
This study describes the development of a cold-water Coral mound in the southeast alboran sea over the last 300 ky. Mound development follows interglacial-glacial cycles.
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
Short summary
Short summary
A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Related subject area
Subject area: The evolving Earth surface | Editorial team: Stratigraphy, sedimentology, geomorphology, morphotectonics, and palaeontology | Discipline: Sedimentology
Impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, The Dolomites, Northern Italy)
The influence of extraction of various solvents on chemical properties on Chang 7 shale, Ordos Basin, China
Application of the creeping flow restoration method to an analogue model
Deep vs. shallow – two contrasting theories? A tectonically activated Late Cretaceous deltaic system in the axial part of the Mid-Polish Trough: a case study from southeast Poland
Miocene high elevation in the Central Alps
Dawn and dusk of Late Cretaceous basin inversion in central Europe
Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam scanning electron microscopy imaging
Birth and closure of the Kallipetra Basin: Late Cretaceous reworking of the Jurassic Pelagonian–Axios/Vardar contact (northern Greece)
Sediment history mirrors Pleistocene aridification in the Gobi Desert (Ejina Basin, NW China)
Tectonic processes, variations in sediment flux, and eustatic sea level recorded by the 20 Myr old Burdigalian transgression in the Swiss Molasse basin
Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits
Can anaerobic oxidation of methane prevent seafloor gas escape in a warming climate?
Precipitation of dolomite from seawater on a Carnian coastal plain (Dolomites, northern Italy): evidence from carbonate petrography and Sr isotopes
The Ogooue Fan (offshore Gabon): a modern example of deep-sea fan on a complex slope profile
Formation of linear planform chimneys controlled by preferential hydrocarbon leakage and anisotropic stresses in faulted fine-grained sediments, offshore Angola
From oil field to geothermal reservoir: assessment for geothermal utilization of two regionally extensive Devonian carbonate aquifers in Alberta, Canada
Sedimentary mechanisms of a modern banded iron formation on Milos Island, Greece
Onyedika Anthony Igbokwe, Jithender J. Timothy, Ashwani Kumar, Xiao Yan, Mathias Mueller, Alessandro Verdecchia, Günther Meschke, and Adrian Immenhauser
EGUsphere, https://doi.org/10.31223/X53D27, https://doi.org/10.31223/X53D27, 2023
Short summary
Short summary
We present a workflow that models the impact of stress regime change on the Latemar carbonate buildup using displacement-based linear elastic FEM and outcrop analysis. Stress-dependent heterogeneous apertures and effective permeability were calculated from boundary conditions constrained by the study area's stress directions. Our results show that simulated far-field stresses at NW-SE subsidence deformation and N-S Alpine deformation increased the overall fracture aperture and permeability.
Yan Cao, Zhijun Jin, Rukai Zhu, and Kouqi Liu
Solid Earth, 14, 1169–1179, https://doi.org/10.5194/se-14-1169-2023, https://doi.org/10.5194/se-14-1169-2023, 2023
Short summary
Short summary
Fourier transform infrared (FTIR) was performed on shale before and after solvent extraction. The extraction yield from shale with THF is higher than other solvents. The organic-C-normalized yield of a mature sample is higher than other samples. The aromaticity of organic matter increases, and the length of organic matter aliphatic chains does not vary monotonically with increasing maturity. The results will help in the selection of organic solvents for oil-washing experiments of shale.
Melchior Schuh-Senlis, Guillaume Caumon, and Paul Cupillard
EGUsphere, https://doi.org/10.5194/egusphere-2023-2039, https://doi.org/10.5194/egusphere-2023-2039, 2023
Short summary
Short summary
This paper presents the application of a numerical method for restoring models of the subsurface to a previous state in their deformation history, acting as a numerical time machine for geological structures. The method is applied to a model based on a laboratory experiment. The results show that using more natural conditions in the computation of the deformation allows us to assess the value of some previously unknown physical parameters of the different materials inside the model.
Zbyszek Remin, Michał Cyglicki, and Mariusz Niechwedowicz
Solid Earth, 13, 681–703, https://doi.org/10.5194/se-13-681-2022, https://doi.org/10.5194/se-13-681-2022, 2022
Short summary
Short summary
Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted as the deepest and most subsiding part of the basin during the Cretaceous times. We interpret this area conversely, as representing a landmass – the Łysogóry–Dobrogea Land. Inversion-related tectonics, uplift on the one hand and enhanced subsidence on the other, drove the development of the Szozdy Delta within the axial part of the basin. New heavy mineral data suggest different burial histories.
Emilija Krsnik, Katharina Methner, Marion Campani, Svetlana Botsyun, Sebastian G. Mutz, Todd A. Ehlers, Oliver Kempf, Jens Fiebig, Fritz Schlunegger, and Andreas Mulch
Solid Earth, 12, 2615–2631, https://doi.org/10.5194/se-12-2615-2021, https://doi.org/10.5194/se-12-2615-2021, 2021
Short summary
Short summary
Here we present new surface elevation constraints for the middle Miocene Central Alps based on stable and clumped isotope geochemical analyses. Our reconstructed paleoelevation estimate is supported by isotope-enabled paleoclimate simulations and indicates that the Miocene Central Alps were characterized by a heterogeneous and spatially transient topography with high elevations locally exceeding 4000 m.
Thomas Voigt, Jonas Kley, and Silke Voigt
Solid Earth, 12, 1443–1471, https://doi.org/10.5194/se-12-1443-2021, https://doi.org/10.5194/se-12-1443-2021, 2021
Short summary
Short summary
Basin inversion in central Europe is believed to have started during Late Cretaceous (middle Turonian) and probably proceeded until the Paleogene. Data from different marginal troughs in central Europe point to an earlier start of basin inversion (in the Cenomanian). The end of inversion is overprinted by general uplift but had probably already occurred in the late Campanian to Maastrichtian. Both the start and end of inversion occurred with low rates of uplift and subsidence.
Arne Jacob, Markus Peltz, Sina Hale, Frieder Enzmann, Olga Moravcova, Laurence N. Warr, Georg Grathoff, Philipp Blum, and Michael Kersten
Solid Earth, 12, 1–14, https://doi.org/10.5194/se-12-1-2021, https://doi.org/10.5194/se-12-1-2021, 2021
Short summary
Short summary
In this work, we combined different imaging and experimental measuring methods for analysis of cross-scale effects which reduce permeability of tight reservoir rocks. Simulated permeability of digital images of rocks is often overestimated, which is caused by non-resolvable clay content within the pores of a rock. By combining FIB-SEM with micro-XCT imaging, we were able to simulate the true clay mineral abundance to match experimentally measured permeability with simulated permeability.
Lydia R. Bailey, Filippo L. Schenker, Maria Giuditta Fellin, Miriam Cobianchi, Thierry Adatte, and Vincenzo Picotti
Solid Earth, 11, 2463–2485, https://doi.org/10.5194/se-11-2463-2020, https://doi.org/10.5194/se-11-2463-2020, 2020
Short summary
Short summary
The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
Georg Schwamborn, Kai Hartmann, Bernd Wünnemann, Wolfgang Rösler, Annette Wefer-Roehl, Jörg Pross, Marlen Schlöffel, Franziska Kobe, Pavel E. Tarasov, Melissa A. Berke, and Bernhard Diekmann
Solid Earth, 11, 1375–1398, https://doi.org/10.5194/se-11-1375-2020, https://doi.org/10.5194/se-11-1375-2020, 2020
Short summary
Short summary
We use a sediment core from the Gobi Desert (Ejina Basin, NW China) to illustrate the landscape history of the area. During 2.5 million years a sediment package of 223 m thickness has been accumulated. Various sediment types document that the area turned from a playa environment (shallow water environment with multiple flooding events) to an alluvial–fluvial environment after the arrival of the Heihe in the area. The river has been diverted due to tectonics.
Philippos Garefalakis and Fritz Schlunegger
Solid Earth, 10, 2045–2072, https://doi.org/10.5194/se-10-2045-2019, https://doi.org/10.5194/se-10-2045-2019, 2019
Short summary
Short summary
The controls on the 20 Myr old Burdigalian transgression in the Swiss Molasse basin have been related to a reduction in sediment flux, a rise in global sea level, or tectonic processes in the adjacent Alps. Here, we readdress this problem and extract stratigraphic signals from the Upper Marine Molasse deposits in Switzerland. In conclusion, we consider rollback tectonics to be the main driving force controlling the transgression, which is related to a deepening and widening of the basin.
Laura Stutenbecker, Peter M. E. Tollan, Andrea Madella, and Pierre Lanari
Solid Earth, 10, 1581–1595, https://doi.org/10.5194/se-10-1581-2019, https://doi.org/10.5194/se-10-1581-2019, 2019
Short summary
Short summary
The Aar and Mont Blanc regions in the Alps are large granitoid massifs characterized by high topography. We analyse when these granitoids were first exhumed to the surface. We test this by tracking specific garnet grains, which are exclusively found in the granitoid massifs, in the sediments contained in the alpine foreland basin. This research ties in with ongoing debates on the timing and mechanisms of mountain building.
Christian Stranne, Matt O'Regan, Martin Jakobsson, Volker Brüchert, and Marcelo Ketzer
Solid Earth, 10, 1541–1554, https://doi.org/10.5194/se-10-1541-2019, https://doi.org/10.5194/se-10-1541-2019, 2019
Maximilian Rieder, Wencke Wegner, Monika Horschinegg, Stefanie Klackl, Nereo Preto, Anna Breda, Susanne Gier, Urs Klötzli, Stefano M. Bernasconi, Gernot Arp, and Patrick Meister
Solid Earth, 10, 1243–1267, https://doi.org/10.5194/se-10-1243-2019, https://doi.org/10.5194/se-10-1243-2019, 2019
Short summary
Short summary
The formation of dolomite (CaMg(CO3)2), an abundant mineral in Earth's geological record, is still incompletely understood. We studied dolomites embedded in a 100 m thick succession of coastal alluvial clays of Triassic age in the southern Alps. Observation by light microscopy and Sr isotopes suggests that dolomites may spontaneously from concentrated evaporating seawater, in coastal ephemeral lakes or tidal flats along the western margin of the Triassic Tethys sea.
Salomé Mignard, Thierry Mulder, Philippe Martinez, and Thierry Garlan
Solid Earth, 10, 851–869, https://doi.org/10.5194/se-10-851-2019, https://doi.org/10.5194/se-10-851-2019, 2019
Short summary
Short summary
A large quantity a continental material is transported to the oceans by the world rivers. Once in the ocean, these particles can be transported down the continental shelf thanks to underwater avalanches. The repetition of such massive events can form very important sedimentary deposits at the continent–ocean transition. Data obtained during an oceanic cruise in 2010 allowed us to study such a system located offshore of Gabon and to evaluate the importance sediment transport in this area.
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
Short summary
Short summary
A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Leandra M. Weydt, Claus-Dieter J. Heldmann, Hans G. Machel, and Ingo Sass
Solid Earth, 9, 953–983, https://doi.org/10.5194/se-9-953-2018, https://doi.org/10.5194/se-9-953-2018, 2018
Short summary
Short summary
This study focuses on the assessment of the geothermal potential of two extensive upper Devonian aquifer systems within the Alberta Basin (Canada). Our work provides a first database on geothermal rock properties combined with detailed facies analysis (outcrop and core samples), enabling the identification of preferred zones in the reservoir and thus allowing for a more reliable reservoir prediction. This approach forms the basis for upcoming reservoir studies with a focus on 3-D modelling.
Ernest Chi Fru, Stephanos Kilias, Magnus Ivarsson, Jayne E. Rattray, Katerina Gkika, Iain McDonald, Qian He, and Curt Broman
Solid Earth, 9, 573–598, https://doi.org/10.5194/se-9-573-2018, https://doi.org/10.5194/se-9-573-2018, 2018
Short summary
Short summary
Banded iron formations (BIFs) are chemical sediments last seen in the marine sedimentary record ca. 600 million years ago. Here, we report on the formation mechanisms of a modern BIF analog in the Cape Vani sedimentary basin (CVSB) on Milos Island, Greece, demonstrating that rare environmental redox conditions, coupled to submarine hydrothermal activity and microbial processes, are required for these types of rocks to form in the modern marine biosphere.
Cited articles
Agirrezabala, L. M., Kiel, S., Blumenberg, M., Schäfer, N., and Reitner, J.: Outcrop analogues of pockmarks and associated methane-seep carbonates: A case study from the Lower Cretaceous (Albian) of the Basque-Cantabrian Basin, western Pyrenees; Palaeogeogr. Palaeocl., 390, 94–115, https://doi.org/10.1016/j.palaeo.2012.11.020, 2013. a, b
Allen, J. R. L.: Principles of physical sedimentology, reprinted (with corrections), Springer US, 272 pp., https://doi.org/10.1007/978-1-4613-2545-1, 1992. a
Artru, P. and Gauthier, J.: Etude géochimique d'une séquence des “terres noires”; application au problème de l'écologie de spongiaires constructeurs, B. Soc. Géol. Fr., S7-VIII, 405–412, 10.2113/gssgfbull.S7-VIII.3.405, 1966. a
Baudrimont, A. and Dubois, P.: Un bassin mésogéen du domaine péri-alpin: le Sud-Est de la France, Bulletin Centres de Recherche Exploration-Production Elf Aquitaine, 1, 261–308, 1977. a
Bayon, G., Henderson, G. M., and Bohn, M.: U–Th stratigraphy of a cold seep carbonate crust, Chem. Geol., 260, 47–56, 2009. a
Berndt, C.: Focused fluid flow in passive continental margins, Philos. T. R. Soc. A, 363, 2855–2871, 2005. a
Blouet, J. P., Arndt, S., Imbert, P., and Regnier, P.: Are seep carbonates quantitative proxies of CH4 leakage? Modeling the influence of sulfate reduction and anaerobic oxidation of methane on pH and carbonate precipitation, Chem. Geol., 577, 120254, https://doi.org/10.1016/j.chemgeo.2021.120254, 2021a. a
Blouet, J. P., Imbert, P., Foubert, A., Ho, S., and Dupont, G.: From seep carbonates down to petroleum systems: An outcrop study from the southeastern France Basin, AAPG Bull., 105, 1033–1064, 2021b. a
Blouet, J. P., Wetzel, A., and Ho, S.: Fluid conduits formed along burrows of giant bivalves at a methane seep site, southern Taiwan, Mar. Petrol. Geol., 105123, https://doi.org/10.1016/j.marpetgeo.2021.105123, 2021c. a
Boetius, A., Ravenschlag, K., Schubert, C. J., Rickert, D., Widdel, F., Gieseke, A., Amann, R., Jørgensen, B. B., Witte, U., and Pfannkuche, O.: A marine microbial consortium apparently mediating anaerobic oxidation of methane, Nature, 407, 623–626, https://doi.org/10.1038/35036572, 2000. a
Botz, R., Pokojski, H. D., Schmitt, M., and Thomm, M.: Carbon isotope fractionation during bacterial methanogenesis by CO2 reduction, Org. Geochem., 25, 255–262, 1996. a
Bromley, R. G.: Trace fossils; biology, taphonomy and applications, Chapman and Hall, London, UK, 1996. a
Bunz, S., Mienert, J., and Berndt, C.: Geological controls on the Storegga gas-hydrate system of the mid-Norwegian continental margin, Earth Planet. Sc. Lett., 209, 291–307, 2003. a
Casenave, V., Gay, A., and Imbert, P.: Spider structures: records of fluid venting from methane hydrates on the Congo continental slope. Les structures en araignée: enregistrement d'échappements de fluide provenant des hydrates de méthane sur la pente continentale du Congo, B. Soc. Géol. Fr., 188, 27, https://doi.org/10.1051/bsgf/2017189, 2017. a
Cathles, L. M., Su, Z., and Chen, D.: The physics of gas chimney and pockmark formation, with implications for assessment of seafloor hazards and gas sequestration, Mar. Petrol. Geol., 27, 82–91, 2010. a
D'Andrea, A. F. and DeWitt, T. H.: Geochemical ecosystem engineering by the mud shrimp Upogebia pugettensis (Crustacea: Thalassinidae) in Yaquina Bay, Oregon: Density-dependent effects on organic matter remineralization and nutrient cycling, Limnol. Oceanogr., 54, 1911–1932, 2009. a
De Boever, E., Huysmans, M., Muchez, P., Dimitrov, L., and Swennen, R.: Controlling factors on the morphology and spatial distribution of methane-related tubular concretions–Case study of an Early Eocene seep system, Mar. Petrol. Geol., 26, 1580–1591, 2009. a
Dupré, S., Loubrieu, B., Pierre, C., Scalabrin, C., Guérin, C., Ehrhold, A., Ogor, A.,
Gautier, E., Ruffine, L., Biville, R., Saout, J., Breton, C., Floodpage, J., and Lescanne, M.: The Aquitaine Shelf edge (Bay of Biscay): A primary outlet for microbial methane release, Geophys. Res. Lett., 47, e2019GL084561, https://doi.org/10.1029/2019GL084561, 2020. a
Dworschak, P. C. and de Rodrigues, S. A.: A modern analogue for the trace fossil Gyrolithes: burrows of the thalassinidean shrimp Axianassa australis, Lethaia, 30, 41–52, 1997. a
Forster, S. and Graf, G.: Continuously measured changes in redox potential influenced by oxygen penetrating from burrows of Callianassa subterranena, Hydrobiologia, 235, 527–532, 1992. a
Gaillard, C., Bourseau, J.-P., Boudeulle, M., Pailleret, P., Rio, M., and Roux, M.: Les pseudo-biohermes de Beauvoisin (Drôme): un site hydrothermal sur la marge téthysienne à l'Oxfordien?, B. Soc. Géol. Fr., 1, 69–78, 1985. a
Gaillard, C., Rio, M., Rolin, Y., and Roux, M.: Fossil chemosynthetic communities related to vents or seeps in sedimentary basins: the pseudobioherms of southeastern France compared to other world examples, Palaios, 7, 451–465, https://doi.org/10.2307/3514829, 1992. a
Gay, A., Lopez, M., Cochonat, P., Sultan, N., Cauquil, E., and Brigaud, F.: Sinuous pockmark belt as indicator of a shallow buried turbiditic channel on the lower slope of the Congo Basin, West African Margin, Geol. Soc. Lond. Spec. Publ., 216, 173–189, https://doi.org/10.1144/GSL.SP.2003.216.01.12, 2003. a
Gay, A., Favier, A., Potdevin, J. L., Lopez, M., Bosch, D., Tribovillard, N., Ventalon, S., Cavailhes, T., Neumaier, M., Revillon, S., Travé, A., Bruguier, O., Delmas, D., Delmas, D., and Nevado, C.: Poly-phased fluid flow in the giant fossil pockmark of Beauvoisin, SE basin of France, BSGF-Earth Sciences Bulletin, 191, 35, https://doi.org/10.1051/bsgf/2020036, 2020. a, b, c, d, e, f
Gingras, M. K. and Zonneveld, J.-P.: Tubular tidalites: A biogenic sedimentary structure indicative of tidally influenced sedimentation, J. Sediment. Res., 85, 845–854, 2015. a
Gingras, M. K., Baniak, G., Gordon, J., Hosikovski, J., Konhauser, K. O., La Croix, A., Lemiski, R., Mendoza, C., Pemberton, S. G., Polo, C., and Zonneveld, J.-P.: Porosity and permeability in bioturbated sediments, in: Developments in Sedimentology, edited by: Knaust, D. and Bromley, R. G., Elsevier, Vol. 64, 837–868, https://doi.org/10.1016/B978-0-444-53813-0.00027-7, 2012. a
Greinert, J., Bohrmann, G., and Elvert, M.: Stromatolitic fabric of authigenic carbonate crusts: result of anaerobic methane oxidation at cold seeps in 4,850 m water depth, Int. J. Earth Sci., 91, 698–711, 2002. a
Griffis, R. B. and Suchanek, T. H.: A model of burrow architecture and trophic modes in thalassinidean shrimp (Decapoda: Thalassinidea), Mar. Ecol.-Prog. Ser., 79, 171–183, 1991. a
Haas, A., Peckmann, J., Elvert, M., Sahling, H., and Bohrmann, G.: Patterns of carbonate authigenesis at the Kouilou pockmarks on the Congo deep-sea fan, Mar. Geol., 268, 129–136, 2010. a
Heggland, R.: Gas seepage as an indicator of deeper prospective reservoirs. A study based on exploration 3D seismic data, Mar. Petrol. Geol., 15, 1–9, 1998. a
Ho, S., Cartwright, J. A., and Imbert, P.: Vertical evolution of fluid venting structures in relation to gas flux, in the Neogene-Quaternary of the Lower Congo Basin, Offshore Angola, Mar. Geol., 332, 40–55, 2012. a
Ho, S., Carruthers, D., and Imbert, P.: Insights into the permeability of polygonal faults from their intersection geometries with Linear Chimneys: a case study from the Lower Congo Basin, Carnets Geol., 16, 17–26, https://doi.org/10.4267/2042/58718, 2016. a, b
Ho, S., Hovland, M., Blouet, J.-P., Wetzel, A., Imbert, P., and Carruthers, D.: Formation of linear planform chimneys controlled by preferential hydrocarbon leakage and anisotropic stresses in faulted fine-grained sediments, offshore Angola, Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, 2018a. a
Ho, S., Imbert, P., Hovland, M., Wetzel, A., Blouet, J.-P., and Carruthers, D.: Downslope-shifting pockmarks: interplay between hydrocarbon leakage, sedimentations, currents and slope's topography, Int. J. Earth Sci., 107, 2907–2929, https://doi.org/10.1007/s00531-018-1635-5, 2018b. a
Hovland, M.: Pockmarks and the recent geology of the central section of the Norwegian Trench, Mar. Geol., 47, 283–301, 1982. a
Hovland, M.: On the self-sealing nature of marine seeps, Cont. Shelf Res., 22, 2387–2394, https://doi.org/10.1016/S0278-4343(02)00063-8, 2002. a
Hovland, M., Talbot, M., Olaussen, S., and Aasberg, L.: Recently formed methane-derived carbonates from the North Sea floor, Petroleum Geochemistry, in: Exploration of the Norwegian Shelf, Springer, 263–266, https://doi.org/10.1007/978-94-009-4199-1_22, 1985. a
Hovland, M., Croker, P. F., and Martin, M.: Fault-associated seabed mounds (carbonate knolls?) off western Ireland and north-west Australia, Mar. Petrol. Geol., 11, 232–246, https://doi.org/10.1016/0264-8172(94)90099-X, 1994. a
Hustoft, S., Bunz, S., and Mienert, J.: Three‐dimensional seismic analysis of the morphology and spatial distribution of chimneys beneath the Nyegga pockmark field, offshore mid-Norway, Basin Res., 22, 465–480, 2010. a
IFP: Le bassin du Sud-Est, son exploration et ses perspectives pétrolières, v. fascicule 2, Réf 29 881-2, 213 pp., 1982a. a
IFP: Le bassin du Sud-Est, son exploration et ses perspectives pétrolières, v. fascicule 1, Réf 29 881-1, 73 pp., IFP, Rueil-Malmaison, 1982b. a
IFP: Le bassin du Sud-Est, son exploration et ses perspectives pétrolières, v. fascicule 3, Réf 29 881-3, 6 pp., IFP, Rueil-Malmaison, 1982c. a
Jensen, P., Aagaard, I., Burke Jr., R. A., Dando, P. R., Jørgensen, N. O., Kuijpers, A., Laier, T., O'Hara, S. C. M., and Schmaljohann, R.: “Bubbling reefs” in the Kattegat: submarine landscapes of carbonate-cemented rocks support a diverse ecosystem at methane seeps, Mar. Ecol.-Prog. Ser., 83, 103–112, 1992. a
Jourabchi, P., Van Cappellen, P., and Regnier, P.: Quantitative interpretation of pH distributions in aquatic sediments: A reaction-transport modeling approach, Am. J. Sci., 305, 919–956, 2005. a
Judd, A. and Hovland, M.: Seabed fluid flow: the impact on geology, biology and the marine environment, Cambridge University Press, Cambridge, UK, 2007. a
Katsman, R., Ostrovsky, I., and Makovsky, Y.: Methane bubble growth in fine-grained muddy aquatic sediment: insight from modeling, Earth Planet. Sc. Lett., 377, 336–346, 2013. a
Keller, M. A. and Isaacs, C. M.: An evaluation of temperature scales for silica diagenesis in diatomaceous sequences including a new approach based on the Miocene Monterey Formation, California, Geo-Mar. Lett., 5, 31–35, 1985. a
Kiel, S., Campbell, K. A., and Gaillard, C.: New and little known mollusks from ancient chemosynthetic environments, Zootaxa, 2390, 26–48, 2010. a
Knaust, D.: Atlas of trace fossils in well core: appearance, taxonomy and interpretation, Springer, Cham, Switzerland, https://doi.org/10.1007/978-3-319-49837-9, 2017. a
Krause, F. F., Clark, J., Sayegh, S. G., and Perez, R. J.: Tube worm fossils or relic methane expulsing conduits?, Palaios, 24, 41–50, 2009. a
Lemoine, M., Bas, T., Arnaud-Vanneau, A., Arnaud, H., Dumont, T., Gidon, M., Bourbon, M., de Graciansky, P.-C., Rudkiewicz, J.-L., and Mégard-Galli, J.: The continental margin of the Mesozoic Tethys in the Western Alps, Mar. Petrol. Geol., 3, 179–199, https://doi.org/10.1016/0264-8172(86)90044-9, 1986. a
Lemoine, M., de Graciansky, P. C., and Tricart, P.: De l'océan à la chaîne de montagnes: tectonique des plaques dans les Alpes, Gordon and Breach Science Publishers, London, UK, 207 pp., 2000. a
Liebetrau, V., Augustin, N., Kutterolf, S., Schmidt, M., Eisenhauer, A., Garbe-Schönberg, D., and Weinrebe, W.: Cold-seep-driven carbonate deposits at the Central American forearc: contrasting evolution and timing in escarpment and mound settings, Int. Jo. Earth Sci., 103, 1845–1872, 2014. a
Loseth, H., Gading, M., and Wensaas, L.: Hydrocarbon leakage interpreted on seismic data, Mar. Petrol. Geol., 26, 1304–1319, 2009. a
Ligtenberg, J.: Unravelling the petroleum system by enhancing fluid migration paths in seismic data using a neural network-based pattern recognition technique, Geofluids, 3, 255–261, 2003. a
Mascle, A. and Vially, R.: The petroleum systems of the Southeast Basin and Gulf of Lion (France), Geol. Soc. Lond. Spec. Publ., 156, 121–140, https://doi.org/10.1144/GSL.SP.1999.156.01.08, 1999. a
Masini, E., Manatschal, G., and Mohn, G.: The Alpine Tethys rifted margins: Reconciling old and new ideas to understand the stratigraphic architecture of magma‐poor rifted margins, Sedimentology, 60, 174–196, https://doi.org/10.1111/sed.12017, 2013. a
Mazzini, A., Duranti, D., Jonk, R., Parnell, J., Cronin, B., Hurst, A., and Quine, M.: Palaeo-carbonate seep structures above an oil reservoir, Gryphon Field, Tertiary, North Sea, Geo-Mar. Lett., 23, 323–339, https://doi.org/10.1007/s00367-003-0145-y, 2003. a
Meesook, A., Sha, J., Yamee, C., and Saengsrichan, W.: Faunal associations, paleoecology and paleoenvironment of marine Jurassic rocks in the Mae Sot, PhopPhra, and Umphang areas, western Thailand, Sci. China Ser. D, 52, 2001–2023, 2009. a
Milkov, A. V. and Etiope, G.: Revised genetic diagrams for natural gases based on a global dataset of > 20,000 samples, Org. Geochem., 125, 109–120, 2018. a
Montenat, C. and Patillet, J.: Septarias à hydrocarbures dans les “Terres noires” d'Orpierre (?Hautes-Alpes), C.R. Acad. Sci., 266, 1–3, 1968. a
Mourgues, R., Bureau, D., Bodet, L., Gay, A., and Gressier, J. B.: Formation of conical fractures in sedimentary basins: Experiments involving pore fluids and implications for sandstone intrusion mechanisms, Earth Planet. Sc. Lett., 313, 67–78, 2012. a
Naudts, L., Greinert, J., Artemov, Y., Beaubien, S. E., Borowski, C., and De Batist, M.: Anomalous sea-floor backscatter patterns in methane venting areas, Dnepr paleo-delta, NW Black Sea, Mar. Geol., 251, 253–267, 2008. a
Negra, M. H., Zagrarni, M. F., Hanini, A., and Strasser, A.: The filament event near the Cenomanian-Turonian boundary in Tunisia: filament origin and environmental signification, B. Soc. Géol. Fr., 182, 507–519, 2011. a
Oddou, R.: Les nodules baritiques, géodes de Provence, Les Éditions du Piat, Le Puy, France, 100 pp., 2004. a
Orgeval, M. and Zimmermann, M.: Perspectives pétrolières de la zone subalpine, Bassin Méridional, Bureau de Recherches du Pétrole, Mission du Couloir Rhodanien, Bureau de Recherches Geologiques et Minieres, Orléans, France, 145 pp., 1957. a
Orcutt, B. N., Joye, S. B., Kleindienst, S., Knittel, K., Ramette, A., Reitz, A., Samarkin, V., Treude, T., and Boetius, A.: Impact of natural oil and higher hydrocarbons on microbial diversity, distribution, and activity in Gulf of Mexico cold-seep sediments, Deep-Sea Res. Pt. II, 57, 2008–2021, https://doi.org/10.1016/j.dsr2.2010.05.014, 2010. a
Peckmann, J., Goedert, J. L., Thiel, V., Michaelis, W., and Reitner, J.: A comprehensive approach to the study of methane‐seep deposits from the Lincoln Creek Formation, western Washington State, USA, Sedimentology, 49, 855–873, 2002. a
Peckmann, J., Goedert, J. L., Heinrichs, T., Hoefs, J., and Reitner, J.: The Late Eocene “Whiskey Creek” methane-seep deposit (western Washington State), Facies, 48, 241–253, 2003. a
Pellenard, P., Tramoy, R., Pucéat, E., Huret, E., Martinez, M., Bruneau, L., and Thierry, J.: Carbon cycle and sea-water palaeotemperature evolution at the Middle–Late Jurassic transition, eastern Paris Basin (France), Mar. Petrol. Geol., 53, 30–43, 2014.
Pemberton, G. S. and Buckley, D. E.: Supershrimp: Deep bioturbation in the Strait of Canso, Nova Scotia, Science, 192, 790–791, 1976. a
Petersen, C. J., Bunz, S., Hustoft, S., Mienert, J., and Klaeschen, D.: High-resolution P-Cable 3D seismic imaging of gas chimney structures in gas hydrated sediments of an Arctic sediment drift, Mar. Petrol. Geol., 27, 1981–1994, 2010. a
Plaza-Faverola, A., Bunz, S., and Mienert, J.: Repeated fluid expulsion through sub-seabed chimneys offshore Norway in response to glacial cycles, Earth Planet. Sci. Lett., 305, 297–308, https://doi.org/10.1016/j.epsl.2011.03.001, 2011. a, b
Regnier, P., Dale, A. W., Arndt, S., LaRowe, D. E., Mogollón, J., and Van Cappellen, P.: Quantitative analysis of anaerobic oxidation of methane (AOM) in marine sediments: a modeling perspective, Earth-Sci. Rev., 106, 105–130, 2011. a
Rodriguez-Tovar, F. J., Mayoral, E., Santos, A., Dorador, X., and Wetzel, A.: Crowded tubular tidalites in Miocene shelf sandstones of southern Iberia, Palaeogeogr. Palaeocl., 521, 1–9, 2019. a
Rolin, Y., Gaillard, C., and Roux, M.: Ecologie des pseudobiohermes des Terres Noires jurassiques liés à paléo-sources sous-marines. Le site oxfordien de Beauvoisin (Drôme, Bassin du Sud-Est, France), Palaeogeogr. Palaeocl., 80, 79–105, https://doi.org/10.1016/0031-0182(90)90123-O, 1990. a
Roure, F., Brun, J.-P., Colletta, B., and Van Den Driessche, J.: Geometry and kinematics of extensional structures in the Alpine foreland basin of southeastern France, J. Struct. Geol., 14, 503–519, https://doi.org/10.1016/0191-8141(92)90153-N, 1992. a, b
Sander, M. V. and Black, J. E.: Crystallization and recrystallization of growth-zoned vein quartz crystals from epithermal systems; implications for fluid inclusion studies, Econ. Geol., 83, 1052–1060, 1988. a
Sarnthein, M.: Stratigraphic contamination by vertical bioturbation in Holocene shelf sediments, in: 24th International Geological Congress, Section 6, 432–436, 24th International geological Congress, Montréal, Canada, 1972. a
Savrda, C. E.: Trace fossils and marine benthic oxygenation, in: Trace Fossils: Concepts, Problems, Prospects, edited by: Miller III, W., Elsevier, Amsterdam, 149–158, 2007. a
Schäfer, W.: Wirkungen der Benthos Organismen auf den jungen Schichtverband, Senkenbergiana Lethaia, 37, 183–263, 1956. a
Stamhuis, E. J., Schreurs, C. E., and Videler, J. J.: Burrow architecture and turbative activity of the thalassinid shrimp Callianassa subterranea from the central North Sea, Mar. Ecol.-Prog. Ser., 151, 155–163, 1997. a
Suess, E., Carson, B., Ritger, S. D., Moore, J. C., Jones, M. L., Kulm, L. D., and Cochrane, G. R.: Biological communities at vent sites along the subduction zone off Oregon, Bulletin of the Biological Society of Washington, 6, 475–484, https://doi.org/10.1016/0198-0149(88)90079-9, 1985. a
Wetzel, A.: Ökologische und stratigraphische Bedeutung biogener Gefüge in quartären Sedimenten am NW-afrikanischen Kontinentalrand, “Meteor” Forschungs-Ergebnisse, Reihe C, 34, 1–47, 1981. a
Wetzel, A.: Ecologic interpretation of deep-sea trace fossil communities, Palaeogeogr. Palaeocl., 85, 47–69, 1991. a
Wetzel, A.: The preservation potential of ash layers in the deep-sea: the example of the 1991-Pinatubo ash in the South China Sea, Sedimentology, 56, 1992–2009, 2009. a
Wetzel, A., Carmona, N., and Ponce, J.: Tidal signature recorded in burrow fill, Sedimentology, 61, 1198–1210, 2014. a
Wheatcroft, R. A.: Preservation potential of sedimentary event layers, Geology, 18, 843–845, 1990. a
Whiticar, M. J.: Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane, Chem. Geol., 161, 291–314, 1999. a
Wiese, F., Kiel, S., Pack, A., Walliser, E. O., and Agirrezabala, L. M.: The beast burrowed, the fluid followed–Crustacean burrows as methane conduits, Mar. Petrol. Geol., 66, 631–640, 2015. a
Zwicker, J., Smrzka, D., Himmler, T., Monien, P., Gier, S., Goedert, J., and Peckmann, J.: Rare earth elements as tracers for microbial activity and early diagenesis: A new perspective from carbonate cements of ancient methane-seep deposits, Chem. Geol., 501, 77–85, https://doi.org/10.1016/j.chemgeo.2018.10.010, 2018. a
Short summary
Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine sediments. Seep carbonates may act as seals and force lateral deviations of rising hydrocarbons. However, crustacean burrows may act as efficient vertical fluid channels allowing hydrocarbons to pass through upward, thereby allowing the vertical growth of carbonate stacks over time. This mechanism may explain the origin of carbonate columns in marine sediments throughout hydrocarbon provinces worldwide.
Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine...
