Authigenic carbonate formation revealed by lipid biomarker inventory at hydrocarbon seeps: A case study from the Okinawa Trough
暂无分享,去创建一个
N. Wu | H. Guan | Zhilei Sun | H. Cao | Wei Geng | Shengyi Mao | Lanfang Xu | Xianrong Zhang | Cuiling Xu
[1] Libo Wang,et al. Methane seepage inferred from pore water geochemistry in shallow sediments in the western slope of the Mid-Okinawa Trough , 2018, Marine and Petroleum Geology.
[2] J. Peckmann,et al. Lipid biomarker patterns of authigenic carbonates reveal fluid composition and seepage intensity at Haima cold seeps, South China Sea , 2018, Journal of Asian Earth Sciences.
[3] Xiaotong Peng,et al. Biogeochemical processes controlling authigenic carbonate formation within the sediment column from the Okinawa Trough , 2018 .
[4] Xiaotong Peng,et al. Formation of carbonate pipes in the northern Okinawa Trough linked to strong sulfate exhaustion and iron supply , 2017 .
[5] J. Peckmann,et al. A carbonate-based proxy for sulfate-driven anaerobic oxidation of methane , 2016 .
[6] G. Escarguel,et al. The alkyl glycerol ether lipid composition of heterotrophic sulfate reducing bacteria strongly depends on growth substrate , 2016 .
[7] M. Könneke,et al. From ether to acid: A plausible degradation pathway of glycerol dialkyl glycerol tetraethers , 2016 .
[8] D. Feng,et al. Methane seepage intensities traced by biomarker patterns in authigenic carbonates from the South China Sea , 2015 .
[9] T. Pape,et al. Formation of seep carbonates along the Makran convergent margin, northern Arabian Sea and a molecular and isotopic approach to constrain the carbon isotopic composition of parent methane , 2015 .
[10] R. Seifert,et al. Authigenic carbonate formation and its impact on the biomarker inventory at hydrocarbon seeps – A case study from the Holocene Black Sea and the Plio-Pleistocene Northern Apennines (Italy) , 2015 .
[11] Helong Wei,et al. A unique Fe-rich carbonate chimney associated with cold seeps in the Northern Okinawa Trough, East China Sea , 2015 .
[12] J. Peckmann,et al. Time integrated variation of sources of fluids and seepage dynamics archived in authigenic carbonates from Gulf of Mexico Gas Hydrate Seafloor Observatory , 2014 .
[13] M. Natalicchio,et al. Seep deposits from northern Istria, Croatia: a first glimpse into the Eocene seep fauna of the Tethys region , 2014, Geological Magazine.
[14] E. Suess. Marine cold seeps and their manifestations: geological control, biogeochemical criteria and environmental conditions , 2014, International Journal of Earth Sciences.
[15] Ziyin Wu,et al. Distribution, features, and influence factors of the submarine topographic boundaries of the Okinawa Trough , 2014, Science China Earth Sciences.
[16] D. Feng,et al. Factors controlling the types of microbial consortia in cold-seep environments: A molecular and isotopic investigation of authigenic carbonates from the South China Sea , 2013 .
[17] A. Boetius,et al. Seafloor oxygen consumption fuelled by methane from cold seeps , 2013 .
[18] P. López‐García,et al. Microbial methane turnover at Marmara Sea cold seeps: a combined 16S rRNA and lipid biomarker investigation , 2013, Geobiology.
[19] Xiao-Lei Liu,et al. Extending the known range of glycerol ether lipids in the environment: structural assignments based on tandem mass spectral fragmentation patterns. , 2012, Rapid communications in mass spectrometry : RCM.
[20] S. Kasten,et al. Reconstructing changes in seep activity by means of pore water and solid phase Sr/Ca and Mg/Ca ratios in pockmark sediments of the Northern Congo Fan , 2011 .
[21] J. Peckmann,et al. Changing redox conditions at cold seeps as revealed by authigenic carbonates from Alaminos Canyon, northern Gulf of Mexico , 2011 .
[22] A. Boetius,et al. Factors controlling the distribution of anaerobic methanotrophic communities in marine environments: Evidence from intact polar membrane lipids , 2011 .
[23] J. Peckmann,et al. Patterns of carbonate authigenesis at the Kouilou pockmarks on the Congo deep-sea fan , 2010 .
[24] J. Peckmann,et al. Molecular fossils reveal fluid composition and flow intensity at a Cretaceous seep , 2009 .
[25] Stefan Schouten,et al. The carbon isotopic response of algae, (cyano)bacteria, archaea and higher plants to the late Cenomanian perturbation of the global carbon cycle: Insights from biomarkers in black shales from the Cape Verde Basin (DSDP Site 367) , 2008 .
[26] H. Niemann,et al. Diagnostic lipid biomarker and stable carbon isotope signatures of microbial communities mediating the anaerobic oxidation of methane with sulphate , 2008 .
[27] A. Boetius,et al. Intact polar lipids of anaerobic methanotrophic archaea and associated bacteria , 2008 .
[28] Jeffrey P. Chanton,et al. Microbial activity in surficial sediments overlying acoustic wipeout zones at a Gulf of Mexico cold seep , 2008 .
[29] J. Damsté,et al. Carbonate formation by anaerobic oxidation of methane : Evidence from lipid biomarker and fossil 16S rDNA , 2008 .
[30] Zhao Ke-bin. Geological Factors for the Development and Newly Advances in Exploration of Gas Hydrate in East China Sea Slope and Okinawa Trough , 2008 .
[31] M. Hutnak. Seabed Fluid Flow , 2007 .
[32] R. Amann,et al. Novel microbial communities of the Haakon Mosby mud volcano and their role as a methane sink , 2006, Nature.
[33] K. Campbell. Hydrocarbon seep and hydrothermal vent paleoenvironments and paleontology: Past developments and future research directions , 2006 .
[34] R. Seifert,et al. Lipid geochemistry of methane-seep-related Black Sea carbonates , 2005 .
[35] V. Thiel,et al. Methane-derived carbonate build-ups and associated microbial communities at cold seeps on the lower Crimean shelf (Black Sea) , 2005 .
[36] T. Treude,et al. Spatial variations of methanotrophic consortia at cold methane seeps: implications from a high‐resolution molecular and isotopic approach , 2005 .
[37] Rudolf Amann,et al. Diversity and Distribution of Methanotrophic Archaea at Cold Seeps , 2005, Applied and Environmental Microbiology.
[38] K. Nauhaus,et al. Environmental regulation of the anaerobic oxidation of methane: a comparison of ANME-I and ANME-II communities. , 2005, Environmental microbiology.
[39] R. Seifert,et al. Membrane lipid patterns typify distinct anaerobic methanotrophic consortia. , 2004, Proceedings of the National Academy of Sciences of the United States of America.
[40] V. Thiel,et al. Carbon cycling at ancient methane-seeps , 2004 .
[41] J. Peckmann,et al. The Late Eocene ‘Whiskey Creek’ methane-seep deposit (western Washington State) , 2003 .
[42] Klaus Wallmann,et al. Fluid flow, methane fluxes, carbonate precipitation and biogeochemical turnover in gas hydrate-bearing sediments at Hydrate Ridge, Cascadia Margin: numerical modeling and mass balances , 2003 .
[43] Gabriel J. Bowen,et al. Spatial distribution of δ18O in meteoric precipitation , 2002 .
[44] H. Cypionka,et al. Phospholipid analysis as a tool to study complex microbial communities in marine sediments. , 2002, Journal of microbiological methods.
[45] E. Delong,et al. Methane-Consuming Archaea Revealed by Directly Coupled Isotopic and Phylogenetic Analysis , 2001, Science.
[46] E. Hopmans,et al. Archaeal lipids in Mediterranean Cold Seeps : Molecular proxies for anaerobic methane oxidation , 2001 .
[47] J. M. Hayes,et al. Comparative Analysis of Methane-Oxidizing Archaea and Sulfate-Reducing Bacteria in Anoxic Marine Sediments , 2001, Applied and Environmental Microbiology.
[48] V. Thiel,et al. Molecular signals for anaerobic methane oxidation in Black Sea seep carbonates and a microbial mat , 2001 .
[49] W. Shanks. Stable Isotopes in Seafloor Hydrothermal Systems: Vent fluids, hydrothermal deposits, hydrothermal alteration, and microbial processes , 2001 .
[50] J. Greinert,et al. Gas Hydrate‐Associated Carbonates and Methane‐Venting at Hydrate Ridge: Classification, Distribution, and Origin of Authigenic Lithologies , 2001 .
[51] G. Aloisi,et al. Methane-related authigenic carbonates of eastern Mediterranean Sea mud volcanoes and their possible relation to gas hydrate destabilisation , 2000 .
[52] Olaf Pfannkuche,et al. A marine microbial consortium apparently mediating anaerobic oxidation of methane , 2000, Nature.
[53] R. Pancost,et al. Biomarker Evidence for Widespread Anaerobic Methane Oxidation in Mediterranean Sediments by a Consortium of Methanogenic Archaea and Bacteria , 2000, Applied and Environmental Microbiology.
[54] C. Paull,et al. 29. Methane-derived authigenic carbonates associated with gas hydrate decomposition and fluid venting above the Blake Ridge Diapir , 2000 .
[55] S. Mazzullo. Organogenic Dolomitization in Peritidal to Deep-Sea Sediments , 2000 .
[56] R. Seifert,et al. Highly isotopically depleted isoprenoids: molecular markers for ancient methane venting , 1999 .
[57] E. Suess,et al. Anaerobic methane oxidation associated with marine gas hydrates: superlight C-isotopes from saturated and unsaturated C20 and C25 irregular isoprenoids , 1999, Naturwissenschaften.
[58] R. Shinjo,et al. Geochemical and Sr‐Nd isotopic characteristics of volcanic rocks from the Okinawa Trough and Ryukyu Arc: Implications for the evolution of a young, intracontinental back arc basin , 1999 .
[59] Peter G. Brewer,et al. Methane-consuming archaebacteria in marine sediments , 1999, Nature.
[60] K. Black,et al. Fatty acids in surface sediment at the Hebridean shelf edge, west of Scotland , 1998 .
[61] W. Borowski,et al. Marine pore-water sulfate profiles indicate in situ methane flux from underlying gas hydrate , 1996 .
[62] C. Paull,et al. Effects of ion exclusion and isotopic fractionation on pore water geochemistry during gas hydrate formation and decomposition , 1995 .
[63] S. Hsu,et al. Structural and Kinematic Evolutions of the Okinawa Trough Backarc Basin , 1995 .
[64] H. Takada,et al. Diagenesis of biomarkers in Biwa Lake sediments over 1 million years , 1990 .
[65] M. Kimura,et al. Back Arc Extension in the Okinawa Trough , 1987 .
[66] I. Kaplan,et al. The lipid geochemistry of Antarctic marine sediments: Bransfield Strait , 1987 .
[67] E. Suess,et al. Methane-derived authigenic carbonates formed by subduction-induced pore-water expulsion along the Oregon/Washington margin , 1987 .
[68] S. Rowland,et al. Stereochemical studies of acyclic isoprenoids—XII. Lipids of methanogenic bacteria and possible contributions to sediments☆ , 1984 .
[69] D. Davidson,et al. Oxygen-18 enrichment in the water of a clathrate hydrate☆ , 1983 .
[70] B. Simoneit. The Black Sea, a sink for terrigenous lipids , 1977 .
[71] R. Barnes,et al. Methane production and consumption in anoxic marine sediments , 1976 .
[72] W. Reeburgh,et al. METHANE CONSUMPTION IN CARIACO TRENCH WATERS AND SEDIMENTS , 1976 .
[73] D. McKirdy,et al. Relationship between Ratio of Pristane to Phytane, Crude Oil Composition and Geological Environment in Australia , 1973 .
[74] J. Smith,et al. Isoprenoid Hydrocarbons in Coal and Petroleum , 1969, Nature.
[75] G. Eglinton,et al. CHAPTER 8 – The Distribution of Alkanes , 1963 .
[76] H. Craig. Isotopic Variations in Meteoric Waters , 1961, Science.