Evidence for methanogenesis on slope sites during the late Paleocene and early Eocene: Carbonate concretions from the Dukla Nappe, outer Carpathians, Poland
The late Paleocene to early Eocene was a prolonged period of global warming punctuated by abrupt intervals of rapid temperature rise. These hyperthermal events, especially including the Paleocene-Eocene thermal maximum, are characterized by negative carbon isotope excursions (CIEs), which signify ma...
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| Format: | Others |
| Language: | English |
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2011
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| Online Access: | http://hdl.handle.net/1911/61775 |