Babak Shaikh Baikloo Islam, A. C. Amirkhiz, K. Niknami
{"title":"Late Holocene Climatic Events, the Main Factor of the Cultural Decline in North Central Iran During the Bronze Age","authors":"Babak Shaikh Baikloo Islam, A. C. Amirkhiz, K. Niknami","doi":"10.4312/dp.47.25","DOIUrl":null,"url":null,"abstract":"During the Bronze Age, the cultural region of North Central Iran (NCI) suffered a longterm cultural decline, probably due to severe droughts. According to paleoclimate research, during the overall period c. 5.4–3.5 ka BP, four widely observable climatic events occurred at c. 5.3–5.0, 4.9– 4.7, 4.2–3.9, and 3.8–3.5 ka BP, and these appear to have caused widespread environmental damage in the Near East. Archaeological evidence of the NCI-region reveals political events that can be associated with the observed climatic variability. Paleoclimate research and archaeological studies can attribute, in combination, the cultural decline of NCI during the Bronze Age to the Late Holocene climate change. IZVLE∞EK – V ≠asu bronaste dobe je pri∏lo na obmo≠ju severnega dela centralnega Irana do dolgoro≠nega kulturnega zatona, ki so ga verjetno povzro≠ila obdobja hude su∏e. Glede na paleoklimatske raziskave lahko prepoznamo ∏tiri zelo izrazite podnebne dogodke v obdobju med ok. 5,4 in 3,5 tiso≠ let pred sedanjostjo (le-ti so: 5,3–5,0 tiso≠ let, 4,9–4,7 tiso≠ let, 4,2–3,9 tiso≠ let ter 3,8–3,5 tiso≠ let pred sedanjostjo), ki so povzro≠ili raz∏irjeno okoljsko ∏kodo na Bli∫njem Vzhodu. Arheolo∏ki zapisi v tej regiji ka∫ejo na politi≠ne dogodke, ki jih lahko pove∫emo s podnebno spremenljivostjo. S pomo≠jo paleoklimatskih in arheolo∏kih raziskav lahko bronastodobni kulturni zaton na obmo≠ju severnega centralnega Irana ve∫emo na pozno holocenske podnebne spremembe.","PeriodicalId":38599,"journal":{"name":"Documenta Praehistorica","volume":"47 1","pages":"446-460"},"PeriodicalIF":0.0000,"publicationDate":"2020-12-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Documenta Praehistorica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4312/dp.47.25","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"Arts and Humanities","Score":null,"Total":0}
引用次数: 4
Abstract
During the Bronze Age, the cultural region of North Central Iran (NCI) suffered a longterm cultural decline, probably due to severe droughts. According to paleoclimate research, during the overall period c. 5.4–3.5 ka BP, four widely observable climatic events occurred at c. 5.3–5.0, 4.9– 4.7, 4.2–3.9, and 3.8–3.5 ka BP, and these appear to have caused widespread environmental damage in the Near East. Archaeological evidence of the NCI-region reveals political events that can be associated with the observed climatic variability. Paleoclimate research and archaeological studies can attribute, in combination, the cultural decline of NCI during the Bronze Age to the Late Holocene climate change. IZVLE∞EK – V ≠asu bronaste dobe je pri∏lo na obmo≠ju severnega dela centralnega Irana do dolgoro≠nega kulturnega zatona, ki so ga verjetno povzro≠ila obdobja hude su∏e. Glede na paleoklimatske raziskave lahko prepoznamo ∏tiri zelo izrazite podnebne dogodke v obdobju med ok. 5,4 in 3,5 tiso≠ let pred sedanjostjo (le-ti so: 5,3–5,0 tiso≠ let, 4,9–4,7 tiso≠ let, 4,2–3,9 tiso≠ let ter 3,8–3,5 tiso≠ let pred sedanjostjo), ki so povzro≠ili raz∏irjeno okoljsko ∏kodo na Bli∫njem Vzhodu. Arheolo∏ki zapisi v tej regiji ka∫ejo na politi≠ne dogodke, ki jih lahko pove∫emo s podnebno spremenljivostjo. S pomo≠jo paleoklimatskih in arheolo∏kih raziskav lahko bronastodobni kulturni zaton na obmo≠ju severnega centralnega Irana ve∫emo na pozno holocenske podnebne spremembe.
在青铜时代,伊朗中北部的文化地区(NCI)遭受了长期的文化衰退,可能是由于严重的干旱。根据古气候研究,在约5.4–3.5 ka BP的整个时期,在约5.3–5.0、4.9–4.7、4.2–3.9和3.8–3.5 ka BP发生了四次可广泛观测的气候事件,这些事件似乎在近东造成了广泛的环境破坏。NCI地区的考古证据揭示了与观测到的气候变化有关的政治事件。古气候研究和考古研究可以将青铜时代NCI的文化衰落归因于全新世晚期的气候变化。起源∞EK——在青铜时代,我去了伊朗中部的北部,直到一段可能是由严重干旱引起的长期文化衰退。根据古气候研究,可以确定四个非常明显的气候事件,这些事件发生在现在之前大约5,4和3,5千≠年之间(分别是:5,3,5,5,0千≠多年,4,9,7千≠年份,4,3,3,9,9千≠岁月和3,8,3,5000≠年份),导致或解释了布利斯东部广泛的环境代码。在这一地区记录的考古学家也对气候变化可以说明的政治事件进行了研究。通过古气候和考古研究,伊朗中北部地区青铜时代文化的衰落可以追溯到全新世晚期的气候变化。