Am. Lezine, THE WEST-AFRICAN MANGROVE - AN INDICATOR OF SEA-LEVEL FLUCTUATIONS AND REGIONAL CLIMATE CHANGES DURING THE LAST DEGLACIATION, Bulletin de la Societe geologique de France, 167(6), 1996, pp. 743-752
The review of modern and late Quaternary pollen data recording the man
grove evolution in West Africa shows that littoral and deep-sea sedime
nts have registered different signals. The first one gives evidence fo
r past sea-level variations from ca. 12,000 B.P. to ca 5,000 B.P. The
second one records the first widespread response of tropical forest ec
osystems to the last deglaciation step and enhanced monsoonal rains at
ca. 9,500 B.P.