First evidence for Holocene rainfall in the Tanezrouft hyperdesert and its margins
Fresh water lakelets existed between c. 10.2 and 5.5 ka B.P. along the margins of the Tanezrouft desert. Palaeosols have been observed on the plateau itself, above eolian formations nearby TL dated at 18-9 ka: they give evidence of a steppic vegetal cover of still unknown extension, even in this pre...
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| Veröffentlicht in: | Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 1990-08, Vol.79 (3), p.333-338 |
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| container_title | Palaeogeography, palaeoclimatology, palaeoecology |
| container_volume | 79 |
| creator | Petit-Maire, N. Commelin, D. Fabre, J. Fontugne, M. |
| description | Fresh water lakelets existed between c. 10.2 and 5.5 ka B.P. along the margins of the Tanezrouft desert. Palaeosols have been observed on the plateau itself, above eolian formations nearby TL dated at 18-9 ka: they give evidence of a steppic vegetal cover of still unknown extension, even in this present-day rainless desert. |
| doi_str_mv | 10.1016/0031-0182(90)90026-4 |
| format | Article |
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| identifier | ISSN: 0031-0182 |
| ispartof | Palaeogeography, palaeoclimatology, palaeoecology, 1990-08, Vol.79 (3), p.333-338 |
| issn | 0031-0182 1872-616X |
| language | eng |
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| source | Elsevier ScienceDirect Journals Complete |
| subjects | Continental interfaces, environment Earth sciences Earth, ocean, space Exact sciences and technology Freshwater Marine and continental quaternary Ocean, Atmosphere Sciences of the Universe Surficial geology |
| title | First evidence for Holocene rainfall in the Tanezrouft hyperdesert and its margins |
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