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...
Main Authors: | , , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
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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 |
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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