| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350611 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2011 | 17 Pages |
Abstract
⺠Synchronous but inverse response of carbonate systems to increase in nutrient input. ⺠Increased weathering controls nutrient influx and nannoplankton production. ⺠More humid climates are most probably the cause for weathering intensification. ⺠Pelagic production matches Valanginian carbon isotopic fluctuations. ⺠Combination of cooling and nutrient increase led of carbonate platform demise.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Benjamin Gréselle, Bernard Pittet, Emanuela Mattioli, Michael Joachimski, Nicolas Barbarin, Laurent Riquier, Stéphane Reboulet, Emmanuelle Pucéat,