نمایش مختصر رکورد

dc.contributor.authorShaikh Baikloo Islam, Babaken_US
dc.contributor.authorChaychi Amirkhiz, Ahmaden_US
dc.date.accessioned1401-01-30T19:44:50Zfa_IR
dc.date.accessioned2022-04-19T19:44:51Z
dc.date.available1401-01-30T19:44:50Zfa_IR
dc.date.available2022-04-19T19:44:51Z
dc.date.issued2020-12-01en_US
dc.date.issued1399-09-11fa_IR
dc.date.submitted2022-03-13en_US
dc.date.submitted1400-12-22fa_IR
dc.identifier.citationShaikh Baikloo Islam, Babak, Chaychi Amirkhiz, Ahmad. (2020). Human-Climate Connection in North Central Iran Between 6000 and 2700 BCE. Iranian Journal of Archaeological Studies, 10(1), 75-93. doi: 10.22111/ijas.2020.6792en_US
dc.identifier.issn2251-743X
dc.identifier.urihttps://dx.doi.org/10.22111/ijas.2020.6792
dc.identifier.urihttps://ijas.usb.ac.ir/article_6792.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/900189
dc.description.abstractDuring the Holocene, man's challenges with climate entered a new phase. Holocene climatic cycles, by creatingdry events, have imposed many subsistence tensions on water-dependent communities. The semi-arid and aridregion of North Central Iran, which has been very vulnerable to any climate change, experienced unfavorableenvironmental conditions during these climatic events. So far, only a handful of Early Holocene rural settlementshave been found in the region, possibly because of the mostly arid climate of the period. In general, the firstevidence of Neolithic villages in North Central Iran dates back to the beginning of the Middle Holocene, afterthe 8.2 ka BP event. The first cultural flourishing of this region can be seen from the last quarter of the sixthmillennium BCE. Each cultural flourishing period seems to have declined for some time with the occurrence ofa dry event. The effects of climatic tensions on human societies in North Central Iran have been found around6500-6000, 5700-5400, 5000-4700, 4300-4000, and 3300-2700 BCE. According to data analysis, the frequency ofsettlements and the trend of cultural progress gradually peaked from the early sixth millennium to the mid-fourthmillennium BC, but in the second half of the latter millennium, a gradual decline began which led to the BronzeAge collapse in ca. 2700 BCE. This event probably occurred due to the drop in temperature and the increase in thefrequency and severity of aridity in the transition phase to the Late Holocene.en_US
dc.languageEnglish
dc.language.isoen_US
dc.publisherUniversity of Sistan and Baluchestanen_US
dc.relation.ispartofIranian Journal of Archaeological Studiesen_US
dc.relation.isversionofhttps://dx.doi.org/10.22111/ijas.2020.6792
dc.subjectPaleoclimateen_US
dc.subjectMiddle Holoceneen_US
dc.subjectDry eventen_US
dc.subjectNorth Central Iranen_US
dc.subjectCultural evolutionen_US
dc.titleHuman-Climate Connection in North Central Iran Between 6000 and 2700 BCEen_US
dc.typeTexten_US
dc.typeResearch Articleen_US
dc.contributor.departmentDepartment of History and Archaeology, Science and Research Branch, Islamic Azad University, Tehran, Iran.en_US
dc.contributor.departmentIranian Center of Archaeological Research Department of Cultural and Historical Material Dtudiesen_US
dc.citation.volume10
dc.citation.issue1
dc.citation.spage75
dc.citation.epage93
nlai.contributor.orcid0000-0003-4826-2360


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