| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350557 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2012 | 12 Pages |
Abstract
âºWe present geochemical reconstruction of the L. Cretaceous Oil Shale (OSM), Israel. âºWe observed coupling between surface water productivity and sea floor conditions. âºAnoxic-dysoxic bottom water conditions are indicated by the various proxies. âºA transition in time from anoxia to dysoxia is indicated within the Oil Shale (OSM). âºThe Benthic foraminifera of the OSM were adapted to minimum oxygen conditions.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Aya Schneider-Mor, Heiko Alsenz, Sarit Ashckenazi-Polivoda, Peter Illner, Sigal Abramovich, Shimon Feinstein, Ahuva Almogi-Labin, Zsolt Berner, Wilhelm Püttmann,