Browsing by Author "Tryon, Christian A."
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- Ancient DNA and deep population structure in sub-Saharan African foragersPublication . Lipson, Mark; Sawchuk, Elizabeth A.; Thompson, Jessica C.; Oppenheimer, Jonas; Tryon, Christian A.; Ranhorn, Kathryn L.; de Luna, Kathryn M.; Sirak, Kendra A.; Olalde, Iñigo; Ambrose, Stanley H.; Arthur, John W.; Arthur, Kathryn J. W.; Ayodo, George; Bertacchi, Alex; Cerezo-Román, Jessica I.; Culleton, Brendan J.; Curtis, Matthew C.; Davis, Jacob; Gidna, Agness O.; Hanson, Annalys; Kaliba, Potiphar; Katongo, Maggie; Kwekason, Amandus; Laird, Myra F.; Lewis, Jason; Mabulla, Audax Z. P.; Mapemba, Fredrick; Morris, Alan; Mudenda, George; Mwafulirwa, Raphael; Mwangomba, Daudi; Ndiema, Emmanuel; Ogola, Christine; Schilt, Flora; Willoughby, Pamela R.; Wright, David K.; Zipkin, Andrew; Pinhasi, Ron; Kennett, Douglas J.; Manthi, Fredrick Kyalo; Rohland, Nadin; Patterson, Nick; Reich, David; Prendergast, Mary E.Multiple lines of genetic and archaeological evidence suggest that there were major demographic changes in the terminal Late Pleistocene epoch and early Holocene epoch of sub-Saharan Africa(1-4). Inferences about this period are challenging to make because demographic shifts in the past 5,000 years have obscured the structures of more ancient populations(3,5). Here we present genome-wide ancient DNA data for six individuals from eastern and south-central Africa spanning the past approximately 18,000 years (doubling the time depth of sub-Saharan African ancient DNA), increase the data quality for 15 previously published ancient individuals and analyse these alongside data from 13 other published ancient individuals. The ancestry of the individuals in our study area can be modelled as a geographically structured mixture of three highly divergent source populations, probably reflecting Pleistocene interactions around 80-20 thousand years ago, including deeply diverged eastern and southern African lineages, plus a previously unappreciated ubiquitous distribution of ancestry that occurs in highest proportion today in central African rainforest hunter-gatherers. Once established, this structure remained highly stable, with limited long-range gene flow. These results provide a new line of genetic evidence in support of hypotheses that have emerged from archaeological analyses but remain contested, suggesting increasing regionalization at the end of the Pleistocene epoch. DNA analysis of 6 individuals from eastern and south-central Africa spanning the past approximately 18,000 years, and of 28 previously published ancient individuals, provides genetic evidence supporting hypotheses of increasing regionalization at the end of the Pleistocene.
- Geoarchaeology and heritage management: identifying and quantifying multi-scalar erosional processes at kisese II rockshelter, TanzaniaPublication . Patania, Ilaria; Porter, Samantha T.; Keegan, William F.; Dihogo, Rukia; Frank, Sara; Lewis, Jason; Mashaka, Husna; Ogutu, Julius; Skosey-LaLonde, Elena; Tryon, Christian A.; Niespolo, Elizabeth M.; Colarossi, Debra; Ranhorn, Kathryn L.Natural and anthropogenically induced soil erosion can cause serious loss of the archaeological record. Our work shows the value of multi-scalar geoarchaeological study when excavating and re-excavating rockshelters in a highly dynamic sedimentary environment where erosion is prominent. Here we present our work on Kisese II rockshelter, Tanzania, originally excavated in the 1950s and largely unpublished, that preserves an important Pleistocene-Holocene archaeological record integral to understanding the deep history of the Kondoa Rock-Art World Heritage Center. Unlike rockshelters in quiescent tectonic settings, like much of central Europe or South Africa, Kisese II exists in highly dynamic sedimentary environments associated with the active tectonics of the Great Rift Valley system exacerbated by human-induced environmental and climate change. We report on our 2017 and 2019 exploratory research that includes integrated regional-, landscape-, and site-scale geoarchaeological analyses of past and present sedimentary regimes and micromorphological analyses of the archaeological sediments. Historical records and aerial photographs document extensive changes in vegetation cover and erosional regimes since the 1920s, with drastic changes quantified between 1960 and 2019. Field survey points to an increased erosion rate between 2017 and 2019. To serve future archaeologists, heritage specialists, and local populations we combine our data in a geoarchaeological catena that includes soil, vegetation, fauna, and anthropogenic features on the landscape. At the site, micromorphological coupled with chronological analyses demonstrate the preservation of in situ Pleistocene deposits. Comparison of photographs from the 1956 and 2019 excavations show a maximum sediment loss of 68 cm in 63 years or >10% of >6-m-thick sedimentary deposit. In the studied area of the rockshelter we estimate ~1 cm/yr of erosion, suggesting the ongoing removal of much of the higher archaeological sediments which, based on the coarse stratigraphic controls and chronology of the original Inskeep excavations, would suggest the loss of much of the archaeological record of the last ~4000 years. These multi-scalar data are essential for the construction of appropriate mitigation strategies and further study of the remaining stratigraphy.