| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350486 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2013 | 10 Pages |
Abstract
⺠Deep-sea Cenomanian-Turonian sediments are strongly bioturbated. ⺠Trace fossil diversity and abundance fluctuate in the Bonarelli Level at Rybie. ⺠The fluctuations correspond to changes of benthic foraminifers. ⺠The data point to trophic level and oxygenation of pore water changes.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Alfred Uchman, Francisco J. RodrÃguez-Tovar, Elżbieta Machaniec, Mariusz KÄdzierski,