J
John M. Hayes
Researcher at Woods Hole Oceanographic Institution
Publications - 223
Citations - 26566
John M. Hayes is an academic researcher from Woods Hole Oceanographic Institution. The author has contributed to research in topics: Mass spectrometry & Isotopes of carbon. The author has an hindex of 80, co-authored 212 publications receiving 25053 citations. Previous affiliations of John M. Hayes include University of Chicago & University of California.
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Journal ArticleDOI
Methane-consuming archaebacteria in marine sediments
TL;DR: Studies of sediments related to a decomposing methane hydrate provide strong evidence that methane is being consumed by archaebacteria that are phylogenetically distinct from known methanogens.
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A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
Deborah S. Kelley,Jeffrey A. Karson,Gretchen L. Früh-Green,Dana R. Yoerger,Timothy M. Shank,David A. Butterfield,John M. Hayes,Matthew O. Schrenk,Eric J. Olson,Giora Proskurowski,Michael V. Jakuba,A. M. Bradley,Ben Larson,Kristin A. Ludwig,Deborah Glickson,Kate Buckman,Alexander S. Bradley,William J. Brazelton,Kevin K. Roe,Mitch J. Elend,Adélie Delacour,Stefano M. Bernasconi,Marvin D. Lilley,John A. Baross,Roger E. Summons,Sean P. Sylva +25 more
TL;DR: The serpentinite-hosted Lost City hydrothermal field is a remarkable submarine ecosystem in which geological, chemical, and biological processes are intimately interlinked.
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Evidence for gammacerane as an indicator of water column stratification
J.S. Sinninghe Damsté,Fabien Kenig,Martin P. Koopmans,Jürgen Köster,Stefan Schouten,John M. Hayes,J.W. de Leeuw +6 more
TL;DR: The conclusion that gammacerane is an indicator for water column stratification, which solves two current enigmas in gammalerane geochemistry, is concluded.
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Compound-specific isotopic analyses: a novel tool for reconstruction of ancient biogeochemical processes.
TL;DR: It is shown that isotopic differences between geolipids and porphyrins related to a common source are equal to those observed in modern biosynthetic products, consistent with preservation of biologically controlled isotopic compositions during diagenesis.
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The abundance of 13c in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 ma
TL;DR: For the later Neoproterozoic, from 800 to 543 Ma (346 analyses), from the Cambrian through the Jurassic (1616 analyses), and from the Cretaceous and Cenozoic (2493 analyses) the abundance of 13 C in marine organic matter has been compiled as discussed by the authors.