The end of the ice age
Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH 4 , CO 2 , and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or...
| Published in: | Canadian Journal of Earth Sciences |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Canadian Science Publishing
1990
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1139/e90-012 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-012 |
| Summary: | Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH 4 , CO 2 , and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or more Arctic gas pools, may have initiated massive release of methane from hydrate under ice and in permafrost. The consequent greenhouse warming would have provided strong positive feedback, amplifying emission. This warming, driven by CH 4 , may have induced the release of CO 2 from the oceans to the biosphere, stabilizing the interglacial carbon cycle. |
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