TY - JOUR
T1 - Biome reconstruction from pollen and plant macrofossil data for Africa and the Arabian peninsula at 0 and 6000 years
AU - Jolly, Dominique
AU - Prentice, I. Colin
AU - Bonnefille, Raymonde
AU - Ballouche, Aziz
AU - Bengo, Martin
AU - Brenac, Patrice
AU - Buchet, Guillaume
AU - Burney, David
AU - Cazet, Jean Pierre
AU - Cheddadi, Rachid
AU - Edorh, Therese
AU - Elenga, Hilaire
AU - Elmoutaki, Saida
AU - Guiot, Joel
AU - Laarif, Fouzia
AU - Lamb, Henry
AU - Lezine, Anne Marie
AU - Maley, Jean
AU - Mbenza, Muaka
AU - Peyron, Odile
AU - Reille, Maurice
AU - Reynaud-Farrera, Isabelle
AU - Riollet, Guy
AU - Ritchie, Jim C.
AU - Roche, Emile
AU - Scott, Louis
AU - Ssemmanda, Immaculate
AU - Straka, Herbert
AU - Umer, Mohammed
AU - Van Campo, Elise
AU - Vilimumbalo, Sikiminywa
AU - Vincens, Annie
AU - Waller, Martyn
PY - 1998
Y1 - 1998
N2 - Biome reconstruction from pollen and plant macrofossil data provides an objective method to reconstruct past vegetation. Biomes for Africa and the Arabian peninsula have been mapped for 6000 years BP and provide a new standard for the evaluation of simulated palaeovegetation distributions. A test using modern pollen data shows the robustness of the biomization method, which is able to predict the major vegetation types with a high confidence level. The application of the procedure to the 6000 years data set (pollen and plant macrofossil analyses) shows systematic differences from the present that are consistent with the numerous previous regional and continental interpretations, while providing a more extensive and more objective basis for such interpretations. Madagascar, eastern, southern and central Africa show only minor changes in terms of biomes, compared to present. Major changes in biome distributions occur north of 15°N, with steppe in many low-elevation sites that are now desert, and temperate xerophytic woods/scrub and warm mixed forest in the Saharan mountains. These shifts in biome distributions imply significant changes in climate, especially precipitation, between 6000 years and present, reflecting a change in monsoon extent combined with a southward expansion of Mediterranean influence.
AB - Biome reconstruction from pollen and plant macrofossil data provides an objective method to reconstruct past vegetation. Biomes for Africa and the Arabian peninsula have been mapped for 6000 years BP and provide a new standard for the evaluation of simulated palaeovegetation distributions. A test using modern pollen data shows the robustness of the biomization method, which is able to predict the major vegetation types with a high confidence level. The application of the procedure to the 6000 years data set (pollen and plant macrofossil analyses) shows systematic differences from the present that are consistent with the numerous previous regional and continental interpretations, while providing a more extensive and more objective basis for such interpretations. Madagascar, eastern, southern and central Africa show only minor changes in terms of biomes, compared to present. Major changes in biome distributions occur north of 15°N, with steppe in many low-elevation sites that are now desert, and temperate xerophytic woods/scrub and warm mixed forest in the Saharan mountains. These shifts in biome distributions imply significant changes in climate, especially precipitation, between 6000 years and present, reflecting a change in monsoon extent combined with a southward expansion of Mediterranean influence.
KW - 6000 years BP
KW - Africa
KW - Arabian peninsula
KW - Biome
KW - Madagascar
KW - Plant functional type
KW - Plant macrofossil
KW - Pollen
UR - http://www.scopus.com/inward/record.url?scp=0032464885&partnerID=8YFLogxK
U2 - 10.1046/j.1365-2699.1998.00238.x
DO - 10.1046/j.1365-2699.1998.00238.x
M3 - Article
AN - SCOPUS:0032464885
SN - 0305-0270
VL - 25
SP - 1007
EP - 1027
JO - Journal of Biogeography
JF - Journal of Biogeography
IS - 6
ER -