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| Zagros Paleolithic | |
|---|---|
| Name | Zagros Paleolithic |
| Region | Zagros Mountains |
| Period | Paleolithic |
| Dates | Lower to Upper Paleolithic |
| Notable sites | Shanidar, Yafteh, Warwasi, Kaldar, Bawa Yawan |
| Major cultures | Mousterian, Zagros Aurignacian |
Zagros Paleolithic The Zagros Paleolithic denotes the prehistoric sequence of hominin occupation in the Zagros Mountains of western Iran, eastern Iraq, and southeastern Turkey during the Paleolithic. It encompasses lithic industries, faunal assemblages, and human fossils that inform debates about Neanderthal and early modern Homo sapiens dispersals, interbreeding, and adaptive strategies in Southwest Asia. Research on the sequence connects fieldwork by institutions such as the Smithsonian Institution, British Museum, University of Cambridge, and University of Tehran with theoretical frameworks developed at the Max Planck Institute for Evolutionary Anthropology and the Institute of Archaeology, University College London.
The Zagros Paleolithic spans occupations associated with the Lower Paleolithic, Middle Paleolithic, and Upper Paleolithic, including industries linked to Acheulean, Mousterian, and early Upper Paleolithic technocomplexes. Key questions involve the role of the Zagros as a corridor between the Levantine corridor, the Euphrates River basin, and the Central Asian steppe, as well as its contribution to models of Out of Africa dispersal and regional continuity versus replacement. Prominent field programs by the Iranian Cultural Heritage, Handicrafts and Tourism Organization, the Royal Geographical Society, and collaborations with the Max Planck Society have advanced stratigraphic, chronometric, and paleoenvironmental syntheses.
The Zagros range extends from southeastern Turkey through western Iran into northern Iraq, straddling the Kurdistan Region and bordering the Persian Gulf and Mesopotamia. Tectonic uplift from the collision of the Arabian Plate and the Eurasian Plate created folded limestones, fluvial terraces, and karstic caves that preserve Paleolithic deposits at sites like Shanidar Cave and Yafteh Cave. Geological mapping by teams from the Geological Society of London and the Iranian National Institute for Oceanography and Atmospheric Science informs understanding of terrace formation, loess sequences correlated with the Marine Isotope Stages, and palaeoseismic influences recorded by the International Union of Geological Sciences frameworks.
Radiometric work using radiocarbon dating, optically stimulated luminescence, and uranium–thorium dating has been conducted at layers attributed to MIS 6, MIS 5, MIS 4, and MIS 3, refining Middle-to-Upper Paleolithic transitions. Chronologies from assemblages at Warwasi Rock-Shelter, Kaldar Cave, and Bawa Yawan contribute to debates about the timing of the arrival of anatomically modern humans versus persistence of Neanderthals. Comparative frameworks reference chronostratigraphic syntheses from the Levantine Sequence and the Central Asian Paleolithic sequence produced by teams at the University of Oxford and the Max Planck Institute.
Notable localities include Shanidar Cave (famous for Neanderthal remains and possible mortuary behavior), Yafteh Cave (Upper Paleolithic assemblages), Warwasi Rock-Shelter (stratified Middle-to-Upper Paleolithic sequence), Kaldar Cave (Mousterian and blade industries), and Bawa Yawan (recently reported human fossils). Excavations led by researchers associated with the Smithsonian Institution, University of Tehran, Zagros Archaeological Project, and the French Archaeological Delegation in Iran have recovered stone tool assemblages, micromammal faunas, and human skeletal material. Comparative reference is made to finds from the Levantine Corridor such as Skhul and Qafzeh and to Central Asian sites like Denisova Cave.
Industries include Acheulean-like large cutting tools, Levallois and discoidal Mousterian reduction strategies, and blade-based Upper Paleolithic technologies akin to Zagros or local variants of the Aurignacian. Raw material procurement shows transport of chert, radiolarite, and obsidian across catchments, studied through sourcing by the British Geological Survey and trace-element work at the Max Planck Institute for the Science of Human History. Use-wear and residue analyses by teams from the University of Cambridge and the University of Paris document hafting and hunting-tool use, while ansa and backed bladelets recall parallels with contemporaneous industries in the Levant and Anatolia.
Zooarchaeological assemblages include caprines such as goat and sheep progenitors, wild bovids, and small mammals and birds indicating seasonal hunting strategies documented by analysts at the Natural History Museum, London and the Smithsonian Institution. Stable isotope studies and pollen records from cave sequences tie habitat shifts to stadial–interstadial oscillations captured in Greenland ice core records and Mediterranean speleothem chronologies developed by the European Geosciences Union community. These datasets inform models of foraging mobility, resource scheduling, and refuge areas proposed by scholars affiliated with the University of Cambridge and the Max Planck Institute.
Fossils attributed to Neanderthal populations at Shanidar and contested remains from sites like Bawa Yawan document morphology, trauma, and potential ritual behaviors analyzed using CT scanning and ancient DNA protocols at the Max Planck Institute for Evolutionary Anthropology and the Wellcome Sanger Institute. Paleopathology studies link skeletal evidence to care and social networks, while ancient DNA and protein sequencing inform discussions of admixture between Neanderthals and anatomically modern humans as part of broader narratives including findings from Denisova Cave and Skhul and Qafzeh.
Archaeological work in the Zagros has involved field programs by the Iranian Cultural Heritage, Handicrafts and Tourism Organization, multinational teams from the University of Pennsylvania, University of Cambridge, University of Tehran, French National Centre for Scientific Research, and support from the National Geographic Society. Methodological advances include stratigraphic excavation, microstratigraphy, Bayesian chronological modeling, lithic refitting, microwear, zooarchaeology, palaeobotany, and biomolecular approaches (ancient DNA, proteomics) developed at the Max Planck Institute for Evolutionary Anthropology, the Wellcome Sanger Institute, and the University of Copenhagen. Interdisciplinary collaborations with geochronologists at the Swiss Federal Institute of Technology and climate modelers at the Potsdam Institute for Climate Impact Research continue to refine interpretations.
Category:Paleolithic sites Category:Archaeology of Iran Category:Prehistory of Iraq