The climate of the Younger Dryas as a boundary for Einkorn domestication

The domestication of the Neolithic founder crops of the Near East has recently been a topic of debate particularly with respect to how rapidly the domestication of these crops occurred. One school of thought maintains that these processes lasted several thousand years (‘protracted model’ with ‘gathering’, ‘cultivation’ and ‘domestication’ as three stages of a continuum, each taking up to several thousand years), while another favors the view that domestication occurred much more quickly, over several hundred years at most (‘rapid transition’). Our study focuses on one of these crops, 1-grained domesticated Einkorn wheat, incorporating data from geology, vegetation history, and climate. In the Karacadağ region of southeastern Turkey, where 1-grained Einkorn wheat was domesticated, the climate was severe (i.e. cold and dry) during the Younger Dryas. The climate of the Younger Dryas acted as boundary during which a) conditions were not suitable for ‘cultivation’, and b) Einkorn would have retreated to refugia exhibiting more suitable moisture-bearing soils that would have made ‘gathering’ difficult. Around 11600 cal. b.p., the Younger Dryas ended and a very rapid climatic amelioration commenced at the beginning of the Early Holocene, enabling grasses to spread throughout the region. A ritual PPNA/PPNB site (G?bekli Tepe) and associated PPNB settlements such as Nevali ?ori and ?ay?nü were established at this time. In the settlements of Nevali ?ori and Cafer H?yük, the oldest domesticated Einkorn was found in the earliest archaeological layers. This confirms that the inhabitants made use of domesticated 1-grained Einkorn from the very beginning of settlement activity, although they continued to practice a mixed lifestyle as hunter-gatherers and farmers. For ?ay?nü the issue is more complex, but here domesticated Einkorn also appears around the same time. In summary, by 10400 cal. b.p. domesticated 1-grained Einkorn was present in large quantities at a variety of sites. This would give a maximum window of time lasting approximately 1,200 years and is therefore not in agreement with the ‘protracted’ model but would be consistent with a ‘rapid transition’. It is improbable that the ‘cultivation’ of wild Einkorn was practiced in the Karacadağ region, since wild Einkorn was plentiful during the favorable growing conditions following the Younger Dryas, making it more likely that ‘gathering’ would have been practiced. Because Einkorn has not been found in early settlements in the southern Levant, this crop cannot have been ‘gathered’ and ‘cultivated’ there but instead was ‘domesticated’ independently and solely in southeastern Turkey. Therefore, the YD acts as a boundary, providing a maximum time frame for 1-grained Einkorn domestication.