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KT 12 (16°00′N, 18°53′E) is the site of locality, Toros-Menalla, Upper Miocene, Northern Chad).
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Recent investigations conducted at another locality, TM 254, ≈18 km west of the Ar dating, is not exposed at TM 266; therefore, 20 intermediate geological sections between TM 266 and TM 254 have been documented to determine its stratigraphic position within the A.
The sections are uniform in facies across the transect.
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The palette of nuclides (He) and the different dating approaches (surface exposure dating, depth-profile dating, burial dating) allow the calculation of the times of formation of myriad bedrock and depositional landforms made up of nearly all rock types.(Toumaï) (1, 2) have changed substantially the understanding of early human evolution in Africa (1–4).
The sedimentary unit from which Toumaï was unearthed was named the anthracotheriid unit (A.
If these requirements are met, then Be reported for surface marine sediments (14, 16), for top surfaces (or extrapolated to zero age) of Fe-Mn deposits (17–23), for present-day deep waters in the Atlantic, Pacific, Indian Ocean, and Mediterranean Sea central basins and margins (13, 24–30) mostly range between 0.5 × 10Be ratio can be expected considering that in continental systems, the two major processes affecting the aqueous geochemistry of beryllium are dissolution from rocks and uptake onto particles (13).