2017
Rapid termination of the African Humid Period triggered by northern high-latitude cooling
Abstract: The rapidity and synchrony of the African Humid Period (AHP) termination at around 5.5 ka are debated, and it is unclear what caused a rapid hydroclimate response. Here we analysed the hydrogen isotopic composition of sedimentary leaf-waxes (δDwax) from the Gulf of Guinea, a proxy for regional precipitation in Cameroon and the central Sahel-Sahara. Our record indicates high precipitation during the AHP followed by a rapid decrease at 5.8–4.8 ka. The similarity with a δDwax record from northern East Africa sugg…
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Cited by 100 publications
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“…2), an increase that probably started some centuries before, according to superregional dust reconstructions (12,16) and climate simulations (28,29), and that continues today, as indicated by present-day data from the studied cave. Such a net increase is consistent with the long-term desertification process experienced by northern Africa, including the Sahara and the Sahel, starting around 5.5 ka BP with the rapid demise of the AHP (~11.7 to 5 ka BP) (33)(34)(35), and continuing more gradually over the remainder of the Holocene (13). During these later millennia, the progressive aridification in northern Africa is reflected by lake levels (8,36), vegetation changes (37), human settlements (38), and dust fluxes over the northwest African margin (12,14,15,33) (Fig.…”
Section: Long-term Saharan Dust Increasesupporting
confidence: 75%
“…2), an increase that probably started some centuries before, according to superregional dust reconstructions (12,16) and climate simulations (28,29), and that continues today, as indicated by present-day data from the studied cave. Such a net increase is consistent with the long-term desertification process experienced by northern Africa, including the Sahara and the Sahel, starting around 5.5 ka BP with the rapid demise of the AHP (~11.7 to 5 ka BP) (33)(34)(35), and continuing more gradually over the remainder of the Holocene (13). During these later millennia, the progressive aridification in northern Africa is reflected by lake levels (8,36), vegetation changes (37), human settlements (38), and dust fluxes over the northwest African margin (12,14,15,33) (Fig.…”
Section: Long-term Saharan Dust Increasesupporting
confidence: 75%
“…Based on this regional reference SST record, we are unable to detect any evidence for an abrupt SST change in the Gulf of Guinea associated with the LHRC, ruling out an oceanic control. Furthermore, marine records from the region do not show change in the hydrology at the time of the LHRC (41,46). Further indications for limited hydrological change (including change in precipitation seasonality) during the LHRC are presented in SI Appendix.…”
Section: Discussionmentioning
confidence: 90%
“…The abrupt or progressive nature, and the exact age of the beginning and end of the "African Humid Period" are, however, still debated (deMenocal et al, 2000;Hoelzmann et al, 2004;Gasse et al, 2008;Tierney and deMenocal, 2013;Foerster et al, 2012;Shanahan et al, 2015;Gatto and Zerboni, 2015;Collins et al, 2017). Unfortunately, our dates are too sparse to allow us to specify this point.…”
Section: Comparison With Other Areas and Discussionmentioning
confidence: 95%
