Climate-driven ecosystem succession in the Sahara: the past 6000 years
Abstract
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.
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The mirroring of HGF and some Western African crop domestication is ascribed to cultural responses to the transition from a green Sahara to desert and subsequent climate changes.
“which are ascribed to cultural responses to the transition from a “green Sahara” to the desert and subsequent climate changes (Kropelin et al. 2008).”
From Genomic Analyses Unveil Helmeted Guinea Fowl (<i>Numida meleagris</i>) Domestication in West Africa (2021) · cites this paper as Kropelin et al. 2008
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- Authors
- Kröpelin, S., Verschuren, D., Lézine, A.-M., Eggermont, H., Cocquyt, C., Francus, P., Cazet, J.-P., Fagot, M., Rumes, B., Russell, J. M., Darius, F., Conley, D. J., Schuster, M., von Suchodoletz, H., & Engstrom, D. R.
- Affiliations
- Africa Research Unit, Institute of Prehistoric Archaeology, University of Cologne, Jennerstraße 8, D-50823 Köln, Germany.
- Meise Botanic Garden (BE)
- Science Museum of Minnesota (US)
- Venue
- Science
- Published
- 2008-05-09
- Volume
- 320
- Issue
- 5877
- Pages
- 765-768
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2014574812
- Cited by
- 679
- References
- 42
- Citations by year
- 2026: 17 · 2025: 25 · 2024: 24 · 2023: 25 · 2022: 34 · 2021: 40 · 2020: 28 · 2019: 51 · 2018: 63 · 2017: 36 · 2016: 36 · 2015: 46 · 2014: 31 · 2013: 63 · 2012: 43
- FWCI
- 24.43
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- HAL (submittedVersion)
- Ghent University Academic Bibliography (Ghent University) (submittedVersion)
- EspaceINRS (National Institute for Scientific Research (Canada)) (submittedVersion)
- Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
- Lund University Publications (Lund University) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Ecosystem dynamics and resilience
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Aeolian processes and effects
- Keywords
- African Humid Period, Holocene climate, paleoenvironmental reconstruction, northern Chad, tropical trees, dust mobilization, African monsoon, insolation forcing, hydrological change, biogeophysical feedbacks, desertification, wind regime
- MeSH terms
- Africa, Desert Climate, Biological Evolution, Fresh Water, Plants, Time, Weather, Ecosystem, Geologic Sediments, History, Ancient
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