<HashMap><database>biostudies-literature</database><scores/><additional><submitter>von der Meden J</submitter><funding>National Geographic Society</funding><funding>DST-NRF Centre of Excellence in Palaeosciences</funding><funding>Australian Research Council Discovery Early Career Research Award</funding><funding>DST-NRF Centre Of Excellence in Palaeosciences</funding><funding>University of Cape Town</funding><funding>National Research Foundation</funding><pagination>e0270104</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9299332</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>17(7)</volume><pubmed_abstract>Detailed, well-dated palaeoclimate and archaeological records are critical for understanding the impact of environmental change on human evolution. Ga-Mohana Hill, in the southern Kalahari, South Africa, preserves a Pleistocene archaeological sequence. Relict tufas at the site are evidence of past flowing streams, waterfalls, and shallow pools. Here, we use laser ablation screening to target material suitable for uranium-thorium dating. We obtained 33 ages covering the last 110 thousand years (ka) and identify five tufa formation episodes at 114-100 ka, 73-48 ka, 44-32 ka, 15-6 ka, and ~3 ka. Three tufa episodes are coincident with the archaeological units at Ga-Mohana Hill dating to ~105 ka, ~31 ka, and ~15 ka. Based on our data and the coincidence of dated layers from other local records</pubmed_abstract><journal>PloS one</journal><pubmed_title>Tufas indicate prolonged periods of water availability linked to human occupation in the southern Kalahari.</pubmed_title><pmcid>PMC9299332</pmcid><funding_grant_id>VC2030</funding_grant_id><funding_grant_id>Competitive Programme for Rated Researchers 120806</funding_grant_id><funding_grant_id>DE 190100160</funding_grant_id><funding_grant_id>student bursary</funding_grant_id><funding_grant_id>Operations grants - CoE2017-065; COE2018-05OP; COE2019-OP17</funding_grant_id><funding_grant_id>AOP150924142990</funding_grant_id><funding_grant_id>Waitt Grant</funding_grant_id><funding_grant_id>Operations grant - COE2018-10OP</funding_grant_id><funding_grant_id>Research Development Grant for Y-rated Researchers</funding_grant_id><pubmed_authors>von der Meden J</pubmed_authors><pubmed_authors>Pickering R</pubmed_authors><pubmed_authors>Weij R</pubmed_authors><pubmed_authors>Wilkins J</pubmed_authors><pubmed_authors>Green H</pubmed_authors><pubmed_authors>Greig A</pubmed_authors><pubmed_authors>Schoville BJ</pubmed_authors><pubmed_authors>Hellstrom J</pubmed_authors><pubmed_authors>Woodhead J</pubmed_authors><pubmed_authors>Khumalo W</pubmed_authors></additional><is_claimable>false</is_claimable><name>Tufas indicate prolonged periods of water availability linked to human occupation in the southern Kalahari.</name><description>Detailed, well-dated palaeoclimate and archaeological records are critical for understanding the impact of environmental change on human evolution. Ga-Mohana Hill, in the southern Kalahari, South Africa, preserves a Pleistocene archaeological sequence. Relict tufas at the site are evidence of past flowing streams, waterfalls, and shallow pools. Here, we use laser ablation screening to target material suitable for uranium-thorium dating. We obtained 33 ages covering the last 110 thousand years (ka) and identify five tufa formation episodes at 114-100 ka, 73-48 ka, 44-32 ka, 15-6 ka, and ~3 ka. Three tufa episodes are coincident with the archaeological units at Ga-Mohana Hill dating to ~105 ka, ~31 ka, and ~15 ka. Based on our data and the coincidence of dated layers from other local records</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022</publication><modification>2025-04-05T14:07:15.35Z</modification><creation>2022-08-08T10:59:41.598Z</creation></dates><accession>S-EPMC9299332</accession><cross_references><pubmed>35857764</pubmed><doi>10.1371/journal.pone.0270104</doi></cross_references></HashMap>