(Q57411344)

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Methane hydrate-bearing seeps as a source of aged dissolved organic carbon to the oceans

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Methane hydrate-bearing seeps as a source of aged dissolved organic carbon to the oceans (English)

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radiocarbon dating

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Christopher L Osburn

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Christopher L. Osburn

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John W. Pohlman

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James E. Bauer

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William F. Waite

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N. Ross Chapman

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publication date

28 November 2010

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Nature Geoscience

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4

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1

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37-41

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https://scigraph.springernature.com/pub.10.1038/ngeo1016

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Discussion Reporting of 14C Data

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21 January 2018

Global estimates of hydrate-bound gas in marine sediments: how much is really out there?

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Global inventory of methane clathrate: sensitivity to changes in the deep ocean

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Global biogeochemical cycles: progress and problems

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Oceanic methane biogeochemistry

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Ocean margins as a significant source of organic matter to the deep open ocean

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The stable carbon isotope biogeochemistry of acetate and other dissolved carbon species in deep subseafloor sediments at the northern Cascadia Margin

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Estimates of methane output from mud extrusions at the erosive convergent margin off Costa Rica

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Methane discharge from a deep-sea submarine mud volcano into the upper water column by gas hydrate-coated methane bubbles

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Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum

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Assessing sulfate reduction and methane cycling in a high salinity pore water system in the northern Gulf of Mexico

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Linear Regressions in Fishery Research

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10.1038/NGEO1016

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