Abstract
Diatom study of two 14C-dated cores from lake Tigalmamine shows a step-wise re-establishment of wet and warm conditions during the Late Glacial, at c9.5 and at c7.5 ka BP. Abrupt regressive events are recorded at c10.4, c8-7 and c4.5 ka BP. Their causes have to be sought at the scale of the African Continent, or even at a global scale. There is an abridged English version. -English summary
| Translated title of the contribution | Abrupt hydroclimatic changes in the Middle Atlas, Morocco, since the last glacial maximum |
|---|---|
| Original language | French |
| Pages (from-to) | 259-265 |
| Number of pages | 7 |
| Journal | Comptes Rendus - Academie des Sciences, Serie II |
| Volume | 313 |
| Issue number | 2 |
| Publication status | Published - 1991 |