- Abstract:
-
The Toarcian Oceanic Anoxic Event (OAE) in the Early Jurassic (∼ 183 Ma ago) was characterized by widespread near-synchronous deposition of organic-rich shales in marine settings, as well as perturbations to several isotopic systems. Characteristically, two positive carbon-isotope excursions in a range of materials are separated by an abrupt negative shift. Carbon-isotope profiles from Toarcian fossil wood collected in England and Denmark have previously been shown to exhibit this large drop ...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1016/j.epsl.2006.11.009
-
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- Journal:
- EARTH AND PLANETARY SCIENCE LETTERS
- Volume:
- 253
- Issue:
- 3-4
- Pages:
- 455-470
- Publication date:
- 2007-01-30
- DOI:
- ISSN:
-
0012-821X
- URN:
-
uuid:8fb68a4b-b8ca-48b9-bcb5-c9125eb015f0
- Source identifiers:
-
82029
- Local pid:
- pubs:82029
- Language:
- English
- Keywords:
- Copyright date:
- 2007
Journal article
Carbon-isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian Basin, Portugal)
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