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Updated: Apr 19, 2026

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Design and Use of a Full Flow Sampling System FFS for the Quantification of Methane Emissions
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Palaeoceanografía: liberación de metano en el período Jurásico Temprano
Paul B Wignall1, John M McArthur, Crispin T S Little
1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. wignall@earth.leeds.ac.uk
Nature
|June 2, 2006
Resumen
El calentamiento del Jurásico temprano puede no ser por la liberación de metano. Una nueva investigación sugiere que los rápidos cambios de isótopos de carbono podrían deberse a las condiciones locales del océano, no a la liberación global de metano de los clatratos.
Área de la Ciencia:
- Paleoclimatología Paleoclimatología
- La geoquímica es la geoquímica.
Sus antecedentes:
- El período Jurásico Temprano experimentó un calentamiento global significativo, potencialmente relacionado con la liberación de metano de los clatratos.
- Kemp y otros. identificó tres agudas excursiones delta13C(org), atribuyéndolas a eventos de liberación de metano.
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