PMID-sentid Pub_year Sent_text comp_official_name comp_offsetprotein_name organism prot_offset 18059498-7 2007 This is the first report on fungal communities from methane hydrate-bearing deep-sea marine sediments in South China Sea. Methane 52-59 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 81-84 18059498-7 2007 This is the first report on fungal communities from methane hydrate-bearing deep-sea marine sediments in South China Sea. Methane 52-59 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 117-120 18069330-3 2007 The methane content in the water column of the Chukchi sea varied from 8 nmol CH4 l(-1) in the eastern part of the sea to 31 nmol CH4 l(-1) in the northern part of the Herald Canyon. Methane 4-11 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 55-58 18069330-3 2007 The methane content in the water column of the Chukchi sea varied from 8 nmol CH4 l(-1) in the eastern part of the sea to 31 nmol CH4 l(-1) in the northern part of the Herald Canyon. Methane 4-11 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 115-118 17227418-0 2007 Diversity and abundance of sulfate-reducing microorganisms in the sulfate and methane zones of a marine sediment, Black Sea. Methane 78-85 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 120-123 15997700-8 2005 The presented findings indicate that the metabolic diversity of the Black Sea mat is wider than currently known and that probably other bacteria than those of the methane-oxidizing consortia contribute to aromatic degradation in this anoxic habitat. Methane 163-170 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 74-77 16332791-1 2005 In the northwestern Black Sea, methane oxidation rates reveal that above shallow and deep gas seeps methane is removed from the water column as efficiently as it is at sites located off seeps. Methane 31-38 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 26-29 16332791-1 2005 In the northwestern Black Sea, methane oxidation rates reveal that above shallow and deep gas seeps methane is removed from the water column as efficiently as it is at sites located off seeps. Methane 100-107 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 26-29 15198039-0 2004 [Methane content in bottom sediments and water mass of the Black Sea]. Methane 1-8 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 65-68 16119857-0 2005 [Anaerobic methane oxidation and sulfate reduction in bacterial mats of coral-like carbonate structures in the Black Sea]. Methane 11-18 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 117-120 15521181-0 2004 [The biogeochemical cycle of methane in the coastal zone and littoral of the Kandalaksha Bay of the White Sea]. Methane 29-36 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 106-109 16313004-0 2005 Preliminary studies on methane flux from the ornithogenic soils on Xi-sha atoll, South China Sea. Methane 23-30 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 93-96 16313004-1 2005 Methane flux from the ornithogenic soils was preliminarily measured by closed chamber method on Xi-sha atoll, South China Sea during March 10 to April 11, 2003 for the first time. Methane 0-7 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 122-125 15198039-1 2004 The methane content in bottom sediments and water column of the Black Sea was determined using various methods of desorption and analysis of gases and various methods of calculating their concentrations. Methane 4-11 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 70-73 15198039-6 2004 In certain deep-sea regions, peaks of methane content in the 1000-1200 m horizons of the water column were revealed, which were most probably due to local influx of abyssal waters enriched with this gas. Methane 38-45 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 16-19 15198040-0 2004 [Intensities of microbial production and oxidation of methane in bottom sediments and water mass of the Black Sea]. Methane 54-61 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 110-113 15198040-1 2004 Intensities of biogeochemical (microbial) processes of methane production and methane oxidation were determined in bottom sediments and water column of the Black Sea. Methane 55-62 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 162-165 15198040-1 2004 Intensities of biogeochemical (microbial) processes of methane production and methane oxidation were determined in bottom sediments and water column of the Black Sea. Methane 78-85 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 162-165 12169733-0 2002 Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane. Methane 66-73 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 29-32 33056993-0 2020 Plant species determine tidal wetland methane response to sea level rise. Methane 38-45 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 58-61 12244729-0 2002 [Biogeochemical cycle of methane in the northwestern shelf of the Black Sea]. Methane 25-32 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 72-75 12244729-5 2002 The delta 13C values of methane ranged from -70.7 to -81.8@1000, demonstrating its microbial origin and contradicting the concept of the migration of methane from cold seeps or from the oil fields located at the Black Sea shelf. Methane 24-31 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 218-221 33623088-0 2021 Dynamic and history of methane seepage in the SW Barents Sea: new insights from Leirdjupet Fault Complex. Methane 23-30 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 57-60 33623088-5 2021 Methane-derived authigenic carbonates precipitated due to local gas hydrate destabilization, in turn triggered by an increasing influx of warm Atlantic water and isostatic rebound linked to the retreat of the Barents Sea Ice Sheet. Methane 0-7 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 217-220 11910813-1 2002 The aragonite constructions of the Black Sea are formed in a stable anaerobic zone and are a perfect object to study the natural mechanism of anaerobic methane oxidation. Methane 152-159 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 41-44 17787481-1 1979 Methane concentrations as great as 30,000 nanoliters per liter were measured on two cruises in the northwest Caribbean Sea. Methane 0-7 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 119-122 32174499-0 2020 Multiple factors dominate the distribution of methane and its sea-to-air flux in the Bohai Sea in summer and autumn of 2014. Methane 46-53 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 91-94 32174499-1 2020 The Bohai Sea is well-known as a source of atmospheric methane (CH4). Methane 64-67 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 10-13 32342322-0 2020 First Discovery of Pogonophora (Annelida, Siboglinidae) in the Kara Sea Coincide with the Area of High Methane Concentration. Methane 103-110 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 68-71 32054937-5 2020 We quantitatively demonstrate that variations in sea level and organic carbon burial are the dominant controls on methane leakage since the Early Cretaceous. Methane 114-121 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 49-52 32054937-6 2020 Sea level controls methane seepage variations by imposing smooth trends on timescales in the order of tens of My. Methane 19-26 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 0-3 27876764-3 2016 Here we show that cyclic sedimentation pulses related to the Indian monsoon in concert with authigenic precipitation of methane-derived aragonite gave rise to a well-laminated carbonate build-up within the oxygen minimum zone off Pakistan (northern Arabian Sea). Methane 120-127 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 257-260 28698659-8 2017 Conservative estimates amount to 5 kt of methane, equivalent to 67% of the annual release from the entire North Sea. Methane 41-48 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 112-115 31467345-7 2019 Indeed, during the deglaciation and the accompanying sea-level rise, the thawing permafrost may have released important quantities of methane into the atmosphere that would have contributed to the Toarcian OAE rapid warming and its characteristic negative carbon isotope excursion. Methane 134-141 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 53-56 30709818-0 2019 Spatial-Temporal Pattern of Sulfate-Dependent Anaerobic Methane Oxidation in an Intertidal Zone of the East China Sea. Methane 56-63 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 114-117 25500510-2 2015 The products of microbial utilization of methane and other hydrocarbons fuel rich chemosynthetic communities at these sites, with much higher respiration rates compared with the surrounding deep-sea floor. Methane 41-48 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 195-198 24164560-9 2014 The abundance and distribution of anammox bacterial gene markers indicate a potentially significant contribution of anammox bacteria to the marine N cycle in the deep-sea methane seep sediments. Methane 171-178 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 167-170 23746056-3 2013 Here, we link the anaerobic oxidation of methane (AOM) to the nitrogen cycle in microbial mats of the Black Sea by using stable isotope probing. Methane 41-48 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 108-111 21392199-0 2011 Bacterial enzymes for dissimilatory sulfate reduction in a marine microbial mat (Black Sea) mediating anaerobic oxidation of methane. Methane 125-132 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 87-90 21392199-3 2011 We collected microbial mats with high AOM activity from a methane seep in the Black Sea. Methane 58-65 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 84-87 27283125-3 2016 We report intense methane emissions from the near-shore southern region of the North Sea characterized by the presence of extensive areas with gassy sediments. Methane 18-25 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 85-88 26553610-0 2015 Methane excess in Arctic surface water-triggered by sea ice formation and melting. Methane 0-7 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 52-55 26553610-2 2015 Indeed, recently observed enhanced atmospheric methane concentrations in Arctic regions with fractional sea-ice cover point to unexpected feedbacks in cycling of methane. Methane 47-54 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 104-107 26553610-2 2015 Indeed, recently observed enhanced atmospheric methane concentrations in Arctic regions with fractional sea-ice cover point to unexpected feedbacks in cycling of methane. Methane 162-169 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 104-107 26553610-3 2015 We report on methane excess in sea ice-influenced water masses in the interior Arctic Ocean and provide evidence that sea ice is a potential source. Methane 13-20 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 31-34 26553610-4 2015 We show that methane release from sea ice into the ocean occurs via brine drainage during freezing and melting i.e. in winter and spring. Methane 13-20 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 34-37 25039851-0 2014 Anaerobic oxidation of methane by sulfate in hypersaline groundwater of the Dead Sea aquifer. Methane 23-30 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 81-84 25039851-1 2014 Geochemical and microbial evidence points to anaerobic oxidation of methane (AOM) likely coupled with bacterial sulfate reduction in the hypersaline groundwater of the Dead Sea (DS) alluvial aquifer. Methane 68-75 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 173-176 24602676-0 2014 Enhanced methane emissions from oil and gas exploration areas to the atmosphere--the central Bohai Sea. Methane 9-16 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 99-102 24602676-3 2014 The central Bohai Sea was thus a source of atmospheric methane during the survey periods. Methane 55-62 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 18-21 24602676-5 2014 This study demonstrated a method to detect seafloor CH4 leakages at the sea surface, which may have applicability in many shallow sea areas with oil and gas exploration activities around the world. Methane 52-55 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 43-46 24602676-5 2014 This study demonstrated a method to detect seafloor CH4 leakages at the sea surface, which may have applicability in many shallow sea areas with oil and gas exploration activities around the world. Methane 52-55 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 72-75 24027984-0 2013 [Distribution and air-sea fluxes of methane in the Yellow Sea and the East China Sea in the spring]. Methane 36-43 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 22-25 24027984-0 2013 [Distribution and air-sea fluxes of methane in the Yellow Sea and the East China Sea in the spring]. Methane 36-43 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 58-61 24027984-0 2013 [Distribution and air-sea fluxes of methane in the Yellow Sea and the East China Sea in the spring]. Methane 36-43 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 81-84 24027984-7 2013 Sea to air CH4 fluxes were (2.85 +/- 5.11) micromol x (m2 x d)(-1) (5.18 +/- 9.99) micromol x (m2 x d)(-1) respectively, calculated using the Liss and Merlivat (LM86), the Wanninkhof (W92) relationships and in situ wind speeds, and estimated emission rates of methane from the East China Sea and the Yellow Sea range from 7.05 x 10(-2) - 12.0 x 10(-2) Tg x a(-1) and 1.17 x 10(-2) - 2.20 x 10(-2) Tg x a(-1), respectively. Methane 11-14 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 0-3 24027984-7 2013 Sea to air CH4 fluxes were (2.85 +/- 5.11) micromol x (m2 x d)(-1) (5.18 +/- 9.99) micromol x (m2 x d)(-1) respectively, calculated using the Liss and Merlivat (LM86), the Wanninkhof (W92) relationships and in situ wind speeds, and estimated emission rates of methane from the East China Sea and the Yellow Sea range from 7.05 x 10(-2) - 12.0 x 10(-2) Tg x a(-1) and 1.17 x 10(-2) - 2.20 x 10(-2) Tg x a(-1), respectively. Methane 11-14 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 288-291 24027984-7 2013 Sea to air CH4 fluxes were (2.85 +/- 5.11) micromol x (m2 x d)(-1) (5.18 +/- 9.99) micromol x (m2 x d)(-1) respectively, calculated using the Liss and Merlivat (LM86), the Wanninkhof (W92) relationships and in situ wind speeds, and estimated emission rates of methane from the East China Sea and the Yellow Sea range from 7.05 x 10(-2) - 12.0 x 10(-2) Tg x a(-1) and 1.17 x 10(-2) - 2.20 x 10(-2) Tg x a(-1), respectively. Methane 11-14 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 288-291 24027984-7 2013 Sea to air CH4 fluxes were (2.85 +/- 5.11) micromol x (m2 x d)(-1) (5.18 +/- 9.99) micromol x (m2 x d)(-1) respectively, calculated using the Liss and Merlivat (LM86), the Wanninkhof (W92) relationships and in situ wind speeds, and estimated emission rates of methane from the East China Sea and the Yellow Sea range from 7.05 x 10(-2) - 12.0 x 10(-2) Tg x a(-1) and 1.17 x 10(-2) - 2.20 x 10(-2) Tg x a(-1), respectively. Methane 260-267 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 0-3 24027984-8 2013 The Yellow Sea and East China Sea are the net sources of atmospheric methane in the spring. Methane 69-76 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 11-14 24027984-8 2013 The Yellow Sea and East China Sea are the net sources of atmospheric methane in the spring. Methane 69-76 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 30-33 22629685-0 2012 [Sulfate reduction, formation and oxidation of methane in Holocene era sediments of the Vyborg Bay, Baltic Sea]. Methane 47-54 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 107-110 22121022-0 2011 Structure of a methyl-coenzyme M reductase from Black Sea mats that oxidize methane anaerobically. Methane 76-83 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 54-57 21318266-0 2011 Effects of composition of labile organic matter on biogenic production of methane in the coastal sediments of the Arabian Sea. Methane 74-81 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 122-125 21318266-6 2011 Proteins influenced methane production in the clayey sediments of shallow depths of the Arabian Sea (r = 0.933, p < 0.001) and mangrove estuary (r = 0.981, p < 0.001) but in the sandy beach sediments, carbohydrates (r = 0.924, p < 0.001) governed the net methane production. Methane 20-27 S13 erythroblastosis (avian) oncogene homolog Homo sapiens 96-99