| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350389 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2013 | 12 Pages |
Abstract
⺠A negative carbon isotope excursion is noted in the Late Sinemurian. ⺠This CIE occurs in both the marine and terrestrial realms. ⺠The event coincides with the acmes of two thermophilic palynomorphs. ⺠These geochemical and palynological data indicate a warming event. ⺠It represents a release of isotopically light carbon.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
James B. Riding, Melanie J. Leng, Sev Kender, Stephen P. Hesselbo, Susanne Feist-Burkhardt,