<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Briatico G</submitter><funding>Deutscher Akademischer Austauschdienst</funding><funding>Sapienza Università di Roma</funding><funding>Ministero degli Affari Esteri e della Cooperazione Internazionale</funding><funding>Eberhard Karls Universität Tübingen</funding><pagination>6619</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC10950861</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>14(1)</volume><pubmed_abstract>Pleistocene environments are among the most studied issues in paleoecology and human evolution research in eastern Africa. Many data have been recorded from archaeological sites located at low and medium elevations (≤ 1500 m), whereas few contexts are known at 2000 m and above. Here, we present a substantial isotopic study from Melka Kunture, a complex of prehistoric sites located at 2000-2200 m above sea level in the central Ethiopian highlands. We analyzed the stable carbon and oxygen isotopic composition of 308 faunal tooth enamel samples from sites dated between 2.02 and 0.6 Ma to investigate the animal diets and habitats. The carbon isotopic results indicate that the analyzed taxa had C&lt;sub>4&lt;/sub>-dominated and mixed C&lt;sub>3&lt;/sub>-C&lt;sub>4&lt;/sub> diets with no significant diachronic ch</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>The Pleistocene high-elevation environments between 2.02 and 0.6 Ma at Melka Kunture (Upper Awash Valley, Ethiopia) based upon stable isotope analysis.</pubmed_title><pmcid>PMC10950861</pmcid><funding_grant_id>“Grandi Scavi di Ateneo” - SA11715C7C936C01</funding_grant_id><funding_grant_id>Forschungsstipendien – Kurzstipendien 57552336</funding_grant_id><funding_grant_id>Borse di mobilità all’estero” - Decreto N.16052020, Prot. N.0044296</funding_grant_id><funding_grant_id>"Grandi Scavi di Ateneo" - SA11715C7C936C01</funding_grant_id><funding_grant_id>Borse di mobilità all'estero" - Decreto N.16052020, Prot. N.0044296</funding_grant_id><funding_grant_id>Forschungsstipendien - Kurzstipendien 57552336</funding_grant_id><funding_grant_id>ARC-001666</funding_grant_id><pubmed_authors>Bocherens H</pubmed_authors><pubmed_authors>Geraads D</pubmed_authors><pubmed_authors>Melis RT</pubmed_authors><pubmed_authors>Briatico G</pubmed_authors><pubmed_authors>Mussi M</pubmed_authors></additional><is_claimable>false</is_claimable><name>The Pleistocene high-elevation environments between 2.02 and 0.6 Ma at Melka Kunture (Upper Awash Valley, Ethiopia) based upon stable isotope analysis.</name><description>Pleistocene environments are among the most studied issues in paleoecology and human evolution research in eastern Africa. Many data have been recorded from archaeological sites located at low and medium elevations (≤ 1500 m), whereas few contexts are known at 2000 m and above. Here, we present a substantial isotopic study from Melka Kunture, a complex of prehistoric sites located at 2000-2200 m above sea level in the central Ethiopian highlands. We analyzed the stable carbon and oxygen isotopic composition of 308 faunal tooth enamel samples from sites dated between 2.02 and 0.6 Ma to investigate the animal diets and habitats. The carbon isotopic results indicate that the analyzed taxa had C&lt;sub>4&lt;/sub>-dominated and mixed C&lt;sub>3&lt;/sub>-C&lt;sub>4&lt;/sub> diets with no significant diachronic ch</description><dates><release>2024-01-01T00:00:00Z</release><publication>2024 Mar</publication><modification>2025-04-05T14:46:21.497Z</modification><creation>2025-04-05T14:46:21.497Z</creation></dates><accession>S-EPMC10950861</accession><cross_references><pubmed>38503829</pubmed><doi>10.1038/s41598-024-56768-x</doi></cross_references></HashMap>