Palynology of marine sediment cores from the West African coast

• Main Authors: Agwu, Chiori O C, Beug, Hans-Jürgen
• Format: Dataset
• Language: English
• Published: PANGAEA 1982
• Subjects: ARKTIS 1993; East Atlantic; GIK12309-3; GIK12310-4; GIK12329-6; GIK12392-1; KAL; Kasten corer; M12392-1; M25; M30; M30_184; M8_017-2; M8017B; Meteor (1964); North Atlantic Ocean; PC; Piston corer; SPC; Sphincter corer; VA132; VA132-18-1; Valdivia (1961); Westafrika 1973; Arktis; Arktis*; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.548485; https://doi.org/10.1594/PANGAEA.548485

Seven sediment cores from the cruises of the "Meteor" and "Valdivia" were examined palynologically. The cores were retrieved from the lower continental slope in the area of between 33.5° N and 8° N, off the West African coast. Most of the cores contain sediments from the last Glacial and Interglacial period. In some cases, the Holocene sediments are missing. Some individual cores contain sediments also from earlier Glacial and Interglacial periods. The main reason for making this palynological study was to find out the differences between the vegetation of Glacial and Interglacial periods in those parts of West Africa which at present belong to the Mediterranean zone, the Sahara and the zones of the savannas and tropical forests. In today's Mediterranean vegetation zone at core 33.5° N, forests and deciduous forests in particular, are missing during Glacial conditions. Semi-deserts are found instead of these. In the early isotope stage 1, there is a very significant development of forests which contain evergreen oaks; this is the Mediterranean type of vegestation development. The Sahara type of vegetation development is shown in four cores from between 27° N and 19° N. The differences between Glacial and Interglacial periods are very small. It must be assumed therefore that in this latitudes, both Glacial and Interglacial conditions gave rise to desert generally. The results are in favour of a slightly more arid climate during Glacial and more humid one during Interglacial periods. The southern boundary of the Sahara and the adjacent savannas with grassland and tropical woods were situated more to the south during the Glacial periods than they were during the Interglacial ones. In front of today's savanna belt, it can be seen from the palynological results that there are considerable differences between the vegetation of Glacial and Interglacial periods. The woods are more important in Interglacial periods. During the Glacial periods these are replaced from north to south decreasingly by grassland (savanna and ...