scholarly journals Lake-level changes and hominin occupations in the arid Turkana basin during volcanic closure of the Omo River outflows to the Indian Ocean – comment on the published paper by Boës et al. Quaternary Research (2018), Vol. 91.2, 892–909

2019 ◽  
Vol 92 (2) ◽  
pp. 598-600
Author(s):  
Mathieu Schuster ◽  
Alexis Nutz
Keyword(s):  
Indian Ocean ◽  
Lake Level ◽  
Turkana Basin ◽  
Lake Level Changes ◽  
The Indian Ocean ◽  
Omo River ◽  
Published Paper

scholarly journals Lake-level changes and hominin occupations in the arid Turkana basin during volcanic closure of the Omo River outflows to the Indian Ocean

2018 ◽  
Vol 91 (2) ◽  
pp. 892-909 ◽  
Author(s):  
Xavier Boës ◽  
Sandrine Prat ◽  
Vincent Arrighi ◽  
Craig Feibel ◽  
Bereket Haileab ◽  
...  
Keyword(s):  
Indian Ocean ◽  
Lake Sediments ◽  
Inductively Coupled Plasma ◽  
Optical Emission ◽  
Sedimentary Facies ◽  
Emission Spectrometry ◽  
Lake Turkana ◽  
Inductively Coupled ◽  
The Indian Ocean ◽  
Omo River

AbstractIn the East African Rift, the western margin of Lake Turkana (northern Kenya) exposes Mio-Plio-Pleistocene lake sediments with dated volcanic horizons constraining basin dynamics at the astronomical time scale. Since the late Pliocene, coastal archaeological sites have formed within the lacustrine dynamics. Here, lake levels are reconstructed from 2.4 to 1.7 Ma using sedimentary facies and water/depth-controlled sediment association. The lacustrine stratigraphy is measured with a total station, and cyclostratigraphy is derived from tephrochronology. The water depths are evaluated from paleochemical properties of lake sediments analyzed by inductively coupled plasma optical emission spectrometry and inductively coupled plasma mass spectrometry. Our reconstruction highlights that Lake Turkana rose during 100 ka insolation/eccentricity maxima periods in response to higher monsoonal inputs of the Omo River. However, Lake Turkana also expanded through an insolation minimum at 2.17–1.95 Ma. This asynchronous lake phase coincides with volcanic closure of the Omo River and Lake Turkana outflow sill to the east and the Indian Ocean. An archaeological hiatus occurs during this endorheic lake phase, and alkalinity increases at the beginning of the hiatus. The lake rose again during insolation/eccentricity maxima at 1.9–1.7 Ma, and a new outflow sill opened to the west and the Nile basin. Hominin coastal occupations return during this exorheic/freshwater lake phase.

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