Methane hydrates constitute a large global carbonsubduction zones

A plate tectonic mechanism for m Negative carbon isotope excursions from a new record of terrestrial organic carbon (d13Corg=2.3x) and from marine reservoir that is vulnerable to destabilization via ocean-floor disruption. Such destabilization has im-portant implications for the global cycles of bot...

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Bibliographic Details
Main Authors: A. Hope Jahren A, Clinton P. Conrad A, Nan Crystal Arens C, German Mora D, Carolina Lithgow-bertelloni B
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
methane hydrate
Aptian
seismic coupling
carbon isotope excursion
terrestrial organic matter
Methane hydrate
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.595.1762
http://www.soest.hawaii.edu/GG/FACULTY/conrad/papers/Jahren_etal_EPSL2005.pdf
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Summary:A plate tectonic mechanism for m Negative carbon isotope excursions from a new record of terrestrial organic carbon (d13Corg=2.3x) and from marine reservoir that is vulnerable to destabilization via ocean-floor disruption. Such destabilization has im-portant implications for the global cycles of both

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