Gebregiorgis D, Murshed N, McHenry LJ, Muchemi F, Duong L, Bash JG, Njau JK, Stanistreet IG, Stollhofen H, Schick KD, Toth N, Ashley GM, Mertzman SA, Elliott WC (2026)
Publication Type: Journal article
Publication year: 2026
Book Volume: 699
Article Number: 114033
DOI: 10.1016/j.palaeo.2026.114033
The chemistry of illitic clays reveals an influx of fresher water in strata dated to >2 Ma from the deepest part of extinct Paleolake Olduvai in northern Tanzania, from core recovered by the Olduvai Gorge Coring Project (OGCP). Dioctahedral illite exhibits a composition approaching glauconite in these strata, suggesting a source from a greensand facies formed under lower dissolved oxygen (pO₂) conditions, or from localized, stagnant lake waters within a broader, fresher, and oxic system. This interpretation contrasts with the more saline lake conditions inferred from Mg-rich illite in the younger sediments. These findings reveal a distinct geochemical shift from earlier freshwater to later saline lake phases and confirms that Paleolake Olduvai was initially a freshwater system, providing any hominins present at that time with access to freshwater habitats.
APA:
Gebregiorgis, D., Murshed, N., McHenry, L.J., Muchemi, F., Duong, L., Bash, J.G.,... Elliott, W.C. (2026). Freshwater conditions in early Paleolake Olduvai from the Naibor Soit Formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 699. https://doi.org/10.1016/j.palaeo.2026.114033
MLA:
Gebregiorgis, Daniel, et al. "Freshwater conditions in early Paleolake Olduvai from the Naibor Soit Formation." Palaeogeography, Palaeoclimatology, Palaeoecology 699 (2026).
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