2018
DOI: 10.1371/journal.pone.0192029
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Middle and Later Stone Age chronology of Kisese II rockshelter (UNESCO World Heritage Kondoa Rock-Art Sites), Tanzania

Abstract: The archaeology of East Africa during the last ~65,000 years plays a central role in debates about the origins and dispersal of modern humans, Homo sapiens. Despite the historical importance of the region to these discussions, reliable chronologies for the nature, tempo, and timing of human behavioral changes seen among Middle Stone Age (MSA) and Later Stone Age (LSA) archaeological assemblages are sparse. The Kisese II rockshelter in the Kondoa region of Tanzania, originally excavated in 1956, preserves a ≥ 6… Show more

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Cited by 68 publications
(43 citation statements)
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“…East Africa is a useful region to study because of its relatively large number of archeological sequences that sample the MSA/LSA transition, including Enkapune ya Muto, Kisese II, multiple sites at Lukenya Hill, Magosi, Magubike, Mtongwe, Mumba, Nasera, Panga ya Saidi, and Shurmai; individual MSA and LSA sites in the Lake Victoria basin, Olduvai Gorge, and Kuumbi Cave provide additional constraints on the transition but lack extensive stratigraphic sequences or large sample sizes sufficient to assess change over time (Table ). East Africa as defined here encompasses ~1.77 million km 2 and can serve as a useful point of comparison for other similarly sized regions that also preserve MSA/LSA sequences, such as Ethiopia and the Horn of Africa (~1.88 million km 2 ), as well as southern Africa (~2.09 million km 2 ) …”
Section: Why East Africa?mentioning
confidence: 99%
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“…East Africa is a useful region to study because of its relatively large number of archeological sequences that sample the MSA/LSA transition, including Enkapune ya Muto, Kisese II, multiple sites at Lukenya Hill, Magosi, Magubike, Mtongwe, Mumba, Nasera, Panga ya Saidi, and Shurmai; individual MSA and LSA sites in the Lake Victoria basin, Olduvai Gorge, and Kuumbi Cave provide additional constraints on the transition but lack extensive stratigraphic sequences or large sample sizes sufficient to assess change over time (Table ). East Africa as defined here encompasses ~1.77 million km 2 and can serve as a useful point of comparison for other similarly sized regions that also preserve MSA/LSA sequences, such as Ethiopia and the Horn of Africa (~1.88 million km 2 ), as well as southern Africa (~2.09 million km 2 ) …”
Section: Why East Africa?mentioning
confidence: 99%
“…I assume but cannot yet demonstrate the use of Central Rift Valley obsidian for Shurmai (70 km source distance) and the more distant Kisese II. I assume this because of the lack of clear evidence for the use of other obsidian sources in the Rift Valley or elsewhere …”
Section: Partitioning East Africamentioning
confidence: 99%
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