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  • 1
    Publication Date: 2003-02-22
    Description: Accumulating evidence suggests that methane has been released episodically from hydrates trapped in sea floor sediments during many intervals of rapid climate warming. Here we show that sediments from the Santa Barbara Basin deposited during warm intervals in the last glacial period contain molecular fossils that are diagnostic of aerobic and anaerobic methanotrophs. Sediment intervals with high abundances of these compounds indicate episodes of vigorous methanotrophic activity in methane-laden water masses. Signals for anaerobic methanotrophy in 44,100-year-old sediment are evidence for particularly intense methane emissions and suggest that the basin's methane cycle can profoundly affect oxygen budgets in the water column.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hinrichs, Kai-Uwe -- Hmelo, Laura R -- Sylva, Sean P -- New York, N.Y. -- Science. 2003 Feb 21;299(5610):1214-7.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geology and Geophysics, Woods Hole Oceanographic Institution (WHOI), Woods Hole, MA 02543, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12595688" target="_blank"〉PubMed〈/a〉
    Keywords: Aerobiosis ; Anaerobiosis ; Animals ; Archaea/*metabolism ; Bacteria/*metabolism ; Bacteria, Aerobic/metabolism ; Bacteria, Anaerobic/metabolism ; Biomass ; Carbon Isotopes ; Climate ; Eukaryota/physiology ; Fossils ; Geologic Sediments/chemistry/*microbiology ; Methane/*analysis/*metabolism ; Methylococcaceae/metabolism ; Oxygen/analysis ; Plankton/physiology ; Seawater/*chemistry/microbiology ; Triterpenes/*analysis ; Water Microbiology
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2001-07-21
    Description: Microorganisms living in anoxic marine sediments consume more than 80% of the methane produced in the world's oceans. In addition to single-species aggregates, consortia of metabolically interdependent bacteria and archaea are found in methane-rich sediments. A combination of fluorescence in situ hybridization and secondary ion mass spectrometry shows that cells belonging to one specific archaeal group associated with the Methanosarcinales were all highly depleted in 13C (to values of -96 per thousand). This depletion indicates assimilation of isotopically light methane into specific archaeal cells. Additional microbial species apparently use other carbon sources, as indicated by significantly higher 13C/12C ratios in their cell carbon. Our results demonstrate the feasibility of simultaneous determination of the identity and the metabolic activity of naturally occurring microorganisms.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Orphan, V J -- House, C H -- Hinrichs, K U -- McKeegan, K D -- DeLong, E F -- New York, N.Y. -- Science. 2001 Jul 20;293(5529):484-7.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Monterey Bay Aquarium Research Institute, Moss Landing, CA 95039, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11463914" target="_blank"〉PubMed〈/a〉
    Keywords: Anaerobiosis ; Carbon Isotopes/analysis ; Deltaproteobacteria/chemistry/classification/*metabolism ; Geologic Sediments/*microbiology ; In Situ Hybridization, Fluorescence ; Lipids/analysis ; Methane/*metabolism ; Methanosarcinales/chemistry/classification/*metabolism ; Oceans and Seas ; Oligonucleotide Probes ; Oxidation-Reduction ; Phylogeny ; RNA, Archaeal/genetics ; RNA, Bacterial/genetics ; RNA, Ribosomal/genetics ; Spectrometry, Mass, Secondary Ion ; Sulfates/metabolism
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2008-07-22
    Description: Deep drilling into the marine sea floor has uncovered a vast sedimentary ecosystem of microbial cells. Extrapolation of direct counts of stained microbial cells to the total volume of habitable marine subsurface sediments suggests that between 56 Pg (ref. 1) and 303 Pg (ref. 3) of cellular carbon could be stored in this largely unexplored habitat. From recent studies using various culture-independent techniques, no clear picture has yet emerged as to whether Archaea or Bacteria are more abundant in this extensive ecosystem. Here we show that in subsurface sediments buried deeper than 1 m in a wide range of oceanographic settings at least 87% of intact polar membrane lipids, biomarkers for the presence of live cells, are attributable to archaeal membranes, suggesting that Archaea constitute a major fraction of the biomass. Results obtained from modified quantitative polymerase chain reaction and slot-blot hybridization protocols support the lipid-based evidence and indicate that these techniques have previously underestimated archaeal biomass. The lipid concentrations are proportional to those of total organic carbon. On the basis of this relationship, we derived an independent estimate of amounts of cellular carbon in the global marine subsurface biosphere. Our estimate of 90 Pg of cellular carbon is consistent, within an order of magnitude, with previous estimates, and underscores the importance of marine subsurface habitats for global biomass budgets.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lipp, Julius S -- Morono, Yuki -- Inagaki, Fumio -- Hinrichs, Kai-Uwe -- England -- Nature. 2008 Aug 21;454(7207):991-4. doi: 10.1038/nature07174. Epub 2008 Jul 20.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Organic Geochemistry Group, Department of Geosciences and MARUM Center for Marine Environmental Sciences, University of Bremen, PO Box 330 440, 28334 Bremen, Germany.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18641632" target="_blank"〉PubMed〈/a〉
    Keywords: Archaea/chemistry/genetics/*physiology ; Bacteria/genetics/isolation & purification ; Bacterial Physiological Phenomena ; *Biomass ; Carbon/metabolism ; Colony Count, Microbial ; Genes, Archaeal/genetics ; Genes, Bacterial/genetics ; Geologic Sediments/*microbiology ; Membrane Lipids/metabolism ; Oceans and Seas ; RNA, Ribosomal, 16S/genetics
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2009-10-03
    Description: The course of the biotic recovery after the impact-related disruption of photosynthesis and mass extinction event at the Cretaceous-Paleogene boundary has been intensely debated. The resurgence of marine primary production in the aftermath remains poorly constrained because of the paucity of fossil records tracing primary producers that lack skeletons. Here we present a high-resolution record of geochemical variation in the remarkably thick Fiskeler (also known as the Fish Clay) boundary layer at Kulstirenden, Denmark. Converging evidence from the stable isotopes of carbon and nitrogen and abundances of algal steranes and bacterial hopanes indicates that algal primary productivity was strongly reduced for only a brief period of possibly less than a century after the impact, followed by a rapid resurgence of carbon fixation and ecological reorganization.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sepulveda, Julio -- Wendler, Jens E -- Summons, Roger E -- Hinrichs, Kai-Uwe -- New York, N.Y. -- Science. 2009 Oct 2;326(5949):129-32. doi: 10.1126/science.1176233.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Organic Geochemistry Group, Department of Geosciences, and Center for Marine Environmental Sciences (MARUM), University of Bremen, 28334 Bremen, Germany. juliosep@mit.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19797658" target="_blank"〉PubMed〈/a〉
    Keywords: Biomarkers/analysis ; Carbon Isotopes ; Cyanobacteria/physiology ; Denmark ; *Ecosystem ; Eukaryota/*physiology ; *Extinction, Biological ; Geologic Sediments ; Nitrogen Isotopes ; Photosynthesis ; Phytoplankton/physiology ; Polycyclic Compounds/analysis ; Seawater/chemistry/*microbiology ; Time ; Triterpenes/analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2012-10-16
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hinrichs, Kai-Uwe -- Inagaki, Fumio -- New York, N.Y. -- Science. 2012 Oct 12;338(6104):204-5. doi: 10.1126/science.1229296.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, 28359 Bremen, Germany. khinrichs@uni-bremen.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23066067" target="_blank"〉PubMed〈/a〉
    Keywords: *Biomass ; Carbon/metabolism ; Colony Count, Microbial ; Geologic Sediments/*microbiology ; Oceans and Seas ; Organic Chemicals/chemistry/metabolism
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2004-12-25
    Description: Diverse microbial communities and numerous energy-yielding activities occur in deeply buried sediments of the eastern Pacific Ocean. Distributions of metabolic activities often deviate from the standard model. Rates of activities, cell concentrations, and populations of cultured bacteria vary consistently from one subseafloor environment to another. Net rates of major activities principally rely on electron acceptors and electron donors from the photosynthetic surface world. At open-ocean sites, nitrate and oxygen are supplied to the deepest sedimentary communities through the underlying basaltic aquifer. In turn, these sedimentary communities may supply dissolved electron donors and nutrients to the underlying crustal biosphere.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉D'Hondt, Steven -- Jorgensen, Bo Barker -- Miller, D Jay -- Batzke, Anja -- Blake, Ruth -- Cragg, Barry A -- Cypionka, Heribert -- Dickens, Gerald R -- Ferdelman, Timothy -- Hinrichs, Kai-Uwe -- Holm, Nils G -- Mitterer, Richard -- Spivack, Arthur -- Wang, Guizhi -- Bekins, Barbara -- Engelen, Bert -- Ford, Kathryn -- Gettemy, Glen -- Rutherford, Scott D -- Sass, Henrik -- Skilbeck, C Gregory -- Aiello, Ivano W -- Guerin, Gilles -- House, Christopher H -- Inagaki, Fumio -- Meister, Patrick -- Naehr, Thomas -- Niitsuma, Sachiko -- Parkes, R John -- Schippers, Axel -- Smith, David C -- Teske, Andreas -- Wiegel, Juergen -- Padilla, Christian Naranjo -- Acosta, Juana Luz Solis -- New York, N.Y. -- Science. 2004 Dec 24;306(5705):2216-21.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Ocean Drilling Program Leg 201 Shipboard Scientific Party, NASA Astrobiology Institute, University of Rhode Island Graduate School of Oceanography, South Ferry Road, Narragansett, RI 02882, USA. dhondt@gso.uri.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/15618510" target="_blank"〉PubMed〈/a〉
    Keywords: Bacteria/growth & development/isolation & purification/*metabolism ; Carbon/metabolism ; Colony Count, Microbial ; *Ecosystem ; Electron Transport ; Geologic Sediments/*microbiology ; Iron/metabolism ; Manganese/metabolism ; Methane/metabolism ; Nitrates/metabolism ; Oxidants/metabolism ; Oxidation-Reduction ; Pacific Ocean ; Peru ; Photosynthesis ; Seawater/chemistry ; Sulfates/metabolism ; Thermodynamics
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 2015-07-02
    Description: Article Freshwater wetlands are among the largest natural sources of methane to the atmosphere. Here, the authors report rates of anaerobic methane oxidation which rival those in marine environments, highlighting the importance of a long-overlooked anaerobic methane sink. Nature Communications doi: 10.1038/ncomms8477 Authors: K. E. A. Segarra, F. Schubotz, V. Samarkin, M. Y. Yoshinaga, K-U Hinrichs, S. B. Joye
    Electronic ISSN: 2041-1723
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 8
    Publication Date: 2013-03-16
    Description: Sediment-covered basalt on the flanks of mid-ocean ridges constitutes most of Earth's oceanic crust, but the composition and metabolic function of its microbial ecosystem are largely unknown. By drilling into 3.5-million-year-old subseafloor basalt, we demonstrated the presence of methane- and sulfur-cycling microbes on the eastern flank of the Juan de Fuca Ridge. Depth horizons with functional genes indicative of methane-cycling and sulfate-reducing microorganisms are enriched in solid-phase sulfur and total organic carbon, host delta(13)C- and delta(34)S-isotopic values with a biological imprint, and show clear signs of microbial activity when incubated in the laboratory. Downcore changes in carbon and sulfur cycling show discrete geochemical intervals with chemoautotrophic delta(13)C signatures locally attenuated by heterotrophic metabolism.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lever, Mark A -- Rouxel, Olivier -- Alt, Jeffrey C -- Shimizu, Nobumichi -- Ono, Shuhei -- Coggon, Rosalind M -- Shanks, Wayne C 3rd -- Lapham, Laura -- Elvert, Marcus -- Prieto-Mollar, Xavier -- Hinrichs, Kai-Uwe -- Inagaki, Fumio -- Teske, Andreas -- New York, N.Y. -- Science. 2013 Mar 15;339(6125):1305-8. doi: 10.1126/science.1229240.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC 27599, USA. mark.lever@biology.au.dk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23493710" target="_blank"〉PubMed〈/a〉
    Keywords: Base Sequence ; Carbon/*metabolism ; Methane/*metabolism ; Methanomicrobiales/classification/genetics/*metabolism ; Methanosarcinales/classification/genetics/*metabolism ; Molecular Sequence Data ; Multigene Family ; Phylogeny ; Sequence Analysis, DNA ; *Silicates ; Sulfur/*metabolism
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 9
    Publication Date: 2014-05-09
    Description: Sulfate reduction is a globally important redox process in marine sediments, yet global rates are poorly quantified. We developed an artificial neural network trained with 199 sulfate profiles, constrained with geomorphological and geochemical maps to estimate global sulfate-reduction rate distributions. Globally, 11.3 teramoles of sulfate are reduced yearly (~15% of previous estimates), accounting for the oxidation of 12 to 29% of the organic carbon flux to the sea floor. Combined with global cell distributions in marine sediments, these results indicate a strong contrast in sub-sea-floor prokaryote habitats: In continental margins, global cell numbers in sulfate-depleted sediment exceed those in the overlying sulfate-bearing sediment by one order of magnitude, whereas in the abyss, most life occurs in oxic and/or sulfate-reducing sediments.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bowles, Marshall W -- Mogollon, Jose M -- Kasten, Sabine -- Zabel, Matthias -- Hinrichs, Kai-Uwe -- New York, N.Y. -- Science. 2014 May 23;344(6186):889-91. doi: 10.1126/science.1249213. Epub 2014 May 8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany. bowlesmw@uni-bremen.de. ; MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany. Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany. Department of Earth Sciences-Geochemistry, Faculty of Geosciences, Utrecht University, Netherlands. ; MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany. Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany. ; MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24812207" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon/*metabolism ; Ecosystem ; Geologic Sediments/*microbiology ; Neural Networks (Computer) ; Oxidation-Reduction ; Seawater/*microbiology ; Sulfates/*metabolism
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 2015-07-25
    Description: Microbial life inhabits deeply buried marine sediments, but the extent of this vast ecosystem remains poorly constrained. Here we provide evidence for the existence of microbial communities in ~40 degrees to 60 degrees C sediment associated with lignite coal beds at ~1.5 to 2.5 km below the seafloor in the Pacific Ocean off Japan. Microbial methanogenesis was indicated by the isotopic compositions of methane and carbon dioxide, biomarkers, cultivation data, and gas compositions. Concentrations of indigenous microbial cells below 1.5 km ranged from 〈10 to ~10(4) cells cm(-3). Peak concentrations occurred in lignite layers, where communities differed markedly from shallower subseafloor communities and instead resembled organotrophic communities in forest soils. This suggests that terrigenous sediments retain indigenous community members tens of millions of years after burial in the seabed.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Inagaki, F -- Hinrichs, K-U -- Kubo, Y -- Bowles, M W -- Heuer, V B -- Hong, W-L -- Hoshino, T -- Ijiri, A -- Imachi, H -- Ito, M -- Kaneko, M -- Lever, M A -- Lin, Y-S -- Methe, B A -- Morita, S -- Morono, Y -- Tanikawa, W -- Bihan, M -- Bowden, S A -- Elvert, M -- Glombitza, C -- Gross, D -- Harrington, G J -- Hori, T -- Li, K -- Limmer, D -- Liu, C-H -- Murayama, M -- Ohkouchi, N -- Ono, S -- Park, Y-S -- Phillips, S C -- Prieto-Mollar, X -- Purkey, M -- Riedinger, N -- Sanada, Y -- Sauvage, J -- Snyder, G -- Susilawati, R -- Takano, Y -- Tasumi, E -- Terada, T -- Tomaru, H -- Trembath-Reichert, E -- Wang, D T -- Yamada, Y -- New York, N.Y. -- Science. 2015 Jul 24;349(6246):420-4. doi: 10.1126/science.aaa6882. Epub 2015 Jul 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Nankoku, Kochi 783-8502, Japan. Research and Development Center for Marine Resources, JAMSTEC, Yokosuka 237-0061, Japan. ; MARUM Center for Marine Environmental Sciences, University of Bremen, D-28359 Bremen, Germany. ; Center for Deep-Earth Exploration, JAMSTEC, Yokohama 236-0061, Japan. Research and Development Center for Ocean Drilling Science, JAMSTEC, Yokohama 236-0001, Japan. ; College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA. ; Research and Development Center for Marine Resources, JAMSTEC, Yokosuka 237-0061, Japan. Department of Subsurface Geobiological Analysis and Research, JAMSTEC, Yokosuka 237-0061, Japan. ; Research and Development Center for Marine Resources, JAMSTEC, Yokosuka 237-0061, Japan. Department of Biogeochemistry, JAMSTEC, Yokosuka 237-0061, Japan. ; Center for Geomicrobiology, Department of Bioscience, Aarhus University, DK-8000 Aarhus C, Denmark. ; Department of Environmental Genomics, J. Craig Venter Institute, Rockville, MD 20850, USA. ; Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki 305-8567, Japan. ; Department of Geology and Petroleum Geology, School of Geosciences, University of Aberdeen, Aberdeen AB2A 3UE, UK. ; Department of Applied Geosciences and Geophysics, Montanuniversitat, 8700 Leoben, Austria. ; School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK. ; Environmental Management Research Institute, AIST, Tsukuba, Ibaraki 305-8569, Japan. ; The State Key Laboratory of Pharmaceutical Biotechnology, School of Life Science, Nanjing University, Nanjing, Jiangsu 210093, China. ; Center for Advanced Marine Core Research, Kochi University, Nankoku, Kochi 783-8502, Japan. ; Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. ; Petroleum and Marine Resources Research Division, Korea Institute of Geoscience and Mineral Resources, Yuseong-gu, Daejeon 305-350, Korea. ; Department of Earth Sciences, University of New Hampshire, Durham, NH 03824, USA. ; Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE 68588, USA. ; Department of Earth Sciences, University of California Riverside, Riverside, CA 92521, USA. ; Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA. ; Department of Earth Science, Rice University, Houston, TX 77005, USA. ; School of Earth Science, University of Queensland, Brisbane Queensland 4072, Australia. ; Department of Subsurface Geobiological Analysis and Research, JAMSTEC, Yokosuka 237-0061, Japan. ; Marine Works Japan, Yokosuka 237-0063, Japan. ; Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba 263-8522, Japan. ; Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. ; Research and Development Center for Ocean Drilling Science, JAMSTEC, Yokohama 236-0001, Japan. Department of Urban Management, Graduate School of Engineering, Kyoto University, Kyoto 615-8540, Japan.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26206933" target="_blank"〉PubMed〈/a〉
    Keywords: Aquatic Organisms/*classification/genetics/metabolism ; Archaea/*classification/genetics/metabolism ; Bacteria/*classification/genetics/metabolism ; Biomarkers/metabolism ; Carbon Dioxide/metabolism ; Coal/*microbiology ; Geologic Sediments/*microbiology ; Japan ; Methane/metabolism ; Methanococcus/classification/genetics/metabolism ; Methanosarcina barkeri/classification/genetics/metabolism ; *Microbial Consortia ; Pacific Ocean ; Seawater/*microbiology
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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