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Climate-Driven Ecosystem Succession in the Sahara

The Past 6000 Years

Bibliographic Data

ID23339201
AuthorsS Kröpelin (University of Cologne, corresponding author), Dirk Verschuren (0000-0002-9116-5446, Meise Botanic Garden), Anne‐marie Lézine (0000-0002-3555-5124, Meise Botanic Garden), A-M Lézine (University of Cologne), Hilde Eggermont (Meise Botanic Garden), Christine Cocquyt (0000-0002-0047-4180, Meise Botanic Garden), Pierre Francus (0000-0001-5465-1966, Meise Botanic Garden), Jean-Pierre Cazet (Meise Botanic Garden), M Fagot (University of Cologne), B Rumes (0000-0001-8549-6743, University of Cologne), James M Russell (0000-0002-4835-7696, Meise Botanic Garden), Frank Darius (Meise Botanic Garden), Daniel J Conley (0000-0001-9668-9284, Meise Botanic Garden), M Schuster (0000-0002-4412-8685, University of Cologne), Hans Von Suchodoletz (0000-0002-4366-9383, Meise Botanic Garden), D R Engstrom (University of Cologne)
Year2008
Volume320
Issue5877
Pages765-768
Publication date2008-05-09
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueScience (JOURNAL)
Journal identifiersISSN: 0036-8075 • E-ISSN: 0193-4511
PublisherAmerican Association for the Advancement of Science (AAAS) (PUBLISHER)
DOI10.1126/science.1154913
PMID18467583
OpenAlexW2014574812
LanguageEN
Citations received96
References cited39

Desiccation of the Sahara since the middle Holocene has eradicated all but a few natural archives recording its transition from a “green Sahara” to the present hyperarid desert. Our continuous 6000-year paleoenvironmental reconstruction from northern Chad shows progressive drying of the regional terrestrial ecosystem in response to weakening insolation forcing of the African monsoon and abrupt hydrological change in the local aquatic ecosystem controlled by site-specific thresholds. Strong reductions in tropical trees and then Sahelian grassland cover allowed large-scale dust mobilization from 4300 calendar years before the present (cal yr B.P.). Today's desert ecosystem and regional wind regime were established around 2700 cal yr B.P. This gradual rather than abrupt termination of the African Humid Period in the eastern Sahara suggests a relatively weak biogeophysical feedback on climate.

Archaeology · Arid · Climate change · Climatology · Ecological succession · Ecosystem · Geography · Holocene · Monsoon · Natural (archaeology) · Physical geography · Aeolian processes and effects · Ecology · Environmental Science · Geological and Geophysical Studies Worldwide · Geology · Geology and Paleoclimatology Research · Oceanography

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Unique citing works96
Citations per year5,33
Citation span2008 - 2026 (19)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 78

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