Expression of the Early Toarcian negative carbon-isotope excursion in separated carbonate microfractions (Jurassic, Paris Basin)
The causes of the pronounced negative excursion in carbon-isotope values that was recorded during the Early Toarcian Oceanic Anoxic Event (T-OAE) are still under debate, particularly with regard to the local versus global pattern of the excursion, and the extent to which recorded signals are under a...
| المؤلفون الرئيسيون: | , , , , |
|---|---|
| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
2009
|