Changes of major wind belts and vegetation zones in NW Africa 20,000–5000 yr B.P., as deduced from a marine pollen record near cap blanc
- 1 June 1988
- journal article
- research article
- Published by Elsevier in Review of Palaeobotany and Palynology
- Vol. 55 (1-3) , 101-140
- https://doi.org/10.1016/0034-6667(88)90056-5
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- Coccoliths: Production, transportation and sedimentationPublished by Elsevier ,2003
- Changes in the vegetation and trade winds in equatorial northwest Africa 140,000–70,000 yr B.P. as deduced from two marine pollen recordsPalaeogeography, Palaeoclimatology, Palaeoecology, 1988
- Isopollen maps for 18,000 years B.P. of the Atlantic offshore of northwest Africa: Evidence for paleowind circulationPaleoceanography and Paleoclimatology, 1987
- Distribution of palynomorphs in marine sediments: A record for seasonal wind patterns over NW Africa and adjacent AtlanticInternational Journal of Earth Sciences, 1986
- Commentaire sur l' “essai de reconstitution de la vegetation et du climat holocenes sur la cote septentrionale du senegal” De J. Medus (Rev. Palaeobot. Palynol., 41: 31–38)Review of Palaeobotany and Palynology, 1985
- Histoire de la végétation et du climat de l’Afrique nord-tropicale au Quaternaire recent*Bothalia, 1983
- Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years AgoScience, 1981
- Palaeoclimates of Central Sahara during the early HoloceneNature, 1977
- Effects of Holocene Climatic Change on some Tropical Geomorphic ProcessesQuaternary Research, 1976
- Palynology of a thick quaternary succession in southern SpainPalaeogeography, Palaeoclimatology, Palaeoecology, 1971