Pollen record and dating of sediment core GIK16776-1 off Liberia

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Autori principali: Jahns, Susanne, Hüls, Matthias, Sarnthein, Michael
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1998
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author Jahns, Susanne
Hüls, Matthias
Sarnthein, Michael
author_facet Jahns, Susanne
Hüls, Matthias
Sarnthein, Michael
collection Datos científicos de ciencias marinas y ambientales
contents Based on pollen analysis of a sediment core from the Atlantic Ocean off Liberia the West African vegetation history for the last 400 ka is reconstructed. During the cold oxygen isotope stages 12, 10, 8, 6, 4, 3 and 2 an arid climate is indicated, resulting in a southward shifting of the southern border of the savanna. Late Pleistocene glacial stages were more arid than during the Middle Pleistocene. A persistence of the rain forest in the area, even during the glacial stages, is recorded. This suggests a glacial refuge of rain forest situated in the Guinean mountains. Afromontane forests with Podocarpus occurred in the Guinean mountains from the stages 12 to 2 and disappeared after. The tree expanded from higher to lower elevations twice in the warm oxygen isotope stage 11 (pollen subzones 11d, 11b) and at least twice during the warm stage 5 (pollen subzones 5d, 5a), indicating a relative cool but humid climate for these periods.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_728710
institution PANGAEA
language en
publishDate 1998
publisher PANGAEA
record_format pangaea
spellingShingle Pollen record and dating of sediment core GIK16776-1 off Liberia
Jahns, Susanne
Hüls, Matthias
Sarnthein, Michael
GIK/IfG; GIK16776-1; Institute for Geosciences, Christian Albrechts University, Kiel; KOL; M6/5; Meteor (1986); off Liberia; Piston corer (Kiel type)
Based on pollen analysis of a sediment core from the Atlantic Ocean off Liberia the West African vegetation history for the last 400 ka is reconstructed. During the cold oxygen isotope stages 12, 10, 8, 6, 4, 3 and 2 an arid climate is indicated, resulting in a southward shifting of the southern border of the savanna. Late Pleistocene glacial stages were more arid than during the Middle Pleistocene. A persistence of the rain forest in the area, even during the glacial stages, is recorded. This suggests a glacial refuge of rain forest situated in the Guinean mountains. Afromontane forests with Podocarpus occurred in the Guinean mountains from the stages 12 to 2 and disappeared after. The tree expanded from higher to lower elevations twice in the warm oxygen isotope stage 11 (pollen subzones 11d, 11b) and at least twice during the warm stage 5 (pollen subzones 5d, 5a), indicating a relative cool but humid climate for these periods.
title Pollen record and dating of sediment core GIK16776-1 off Liberia
topic GIK/IfG; GIK16776-1; Institute for Geosciences, Christian Albrechts University, Kiel; KOL; M6/5; Meteor (1986); off Liberia; Piston corer (Kiel type)
url https://doi.org/10.1594/PANGAEA.728710