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Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years

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TLDR
This gradual rather than abrupt termination of the African Humid Period in the eastern Sahara suggests a relatively weak biogeophysical feedback on climate.
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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Citations
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The HYDE 3.1 spatially explicit database of human‐induced global land‐use change over the past 12,000 years

TL;DR: The authors presented a tool for long-term global change studies; it is an update of the History Database of the Global Environment (HYDE) with estimates of some of the underlying demographic and agricultural driving factors.
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Anthropogenic land use estimates for the Holocene – HYDE 3.2

TL;DR: In this paper, the authors present an update and extension of HYDE, the History Database of the Global Environment (HYDE version 3.2), which is an internally consistent combination of historical population estimates and allocation algorithms with time-dependent weighting maps for land use.
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Long-term dynamic modeling of global population and built-up area in a spatially explicit way: HYDE 3.1

TL;DR: This paper describes a tool for long-term global change studies; it is an update of the History Database of the Global Environment (HYDE) with estimates of some of the underlying demographic driving factors of global change with estimated total and urban/rural population numbers, densities and fractions for the Holocene.
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The West African Sahel: A Review of Recent Studies on the Rainfall Regime and Its Interannual Variability

TL;DR: New paradigms for the monsoon and associated ITCZ and for interannual variability have emerged, and features in the upper atmosphere, as well as the Saharan Heat Low are emphasized.
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History of domestication and spread of Aedes aegypti--a review.

TL;DR: This work integrates the available information including genetics, behaviour, morphology, ecology and biogeography of the mosquito, with human history to reach a realistic and comprehensive understanding of this important vector of yellow fever, dengue and Chikungunya.
References
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Journal ArticleDOI

Catastrophic shifts in ecosystems.

TL;DR: Recent studies show that a loss of resilience usually paves the way for a switch to an alternative state, which suggests that strategies for sustainable management of such ecosystems should focus on maintaining resilience.
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Insolation values for the climate of the last 10 million years

TL;DR: In this article, new values for the astronomical parameters of the Earth's orbit and rotation (eccentricity, obliquity and precession) are proposed for paleoclimatic research related to the Late Miocene, the Pliocene and the Quaternary.
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Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate

TL;DR: The iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production, is reviewed.
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The holocene Asian monsoon : links to solar changes and North Atlantic climate

TL;DR: A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years, and shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.
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Southward Migration of the Intertropical Convergence Zone Through the Holocene

TL;DR: The Cariaco Basin record exhibits strong correlations with climate records from distant regions, including the high-latitude Northern Hemisphere, providing evidence for global teleconnections among regional climates.
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