Were climatic forcings the main driver for mid-holocene changes in settlement dynamics on the Varamin Plain (Central Iranian Plateau)?

PLoS One. 2023 Oct 31;18(10):e0290181. doi: 10.1371/journal.pone.0290181. eCollection 2023.

Abstract

Settlement crises in ancient cultures of Western Asia are commonly thought to be caused by climatic events such as severe droughts. However, the insufficient climate proxy situation in this region challenges the inference of clear relationships between climate and settlement dynamics. We investigate the Holocene climatic changes on the Varamin Plain in the context of the climatic history of Western Central Asia by using a transient comprehensive Earth System Model simulation (8 ka BP to pre-industrial), a high-resolution regional snapshot simulation and a synthesis of pollen-based climate reconstructions. In line with the reconstructions, the models reveal only slightly varying mean climatic conditions on the Varamin Plain but indicate substantial changes in seasonality during the Holocene. Increased precipitation during spring, combined with lower temperature and potentially stronger snow accumulation on the upstream Alborz mountains may have led to an increased water supply on the alluvial fan during the vegetation period and thus to more favourable conditions for agricultural production during the Mid-Holocene compared to modern times. According to the model, dry periods on the Central Iranian Plateau are related to particularly weak Westerly winds, fostering the subsidence in the mid-troposphere and hampering precipitation over the region. The model reveals that dry periods have spatially heterogenous manifestations, thus explaining why they do not appear in all proxy records in the wider study region. In fact, the climatic signal may depend on local environmental conditions. The interaction of the topography with the atmospheric circulation leads to additional spatial heterogeneity. Although our results provide several indications for a connection between climate and settlement dynamics, the small overall changes in moisture call into question whether climate is the main driver for settlement discontinuities on the Central Iranian Plateau. To shed further light on this issue, more high-resolution long-term proxy records are needed.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Climate*
  • Iran
  • Seasons
  • Temperature
  • Wind*

Grants and funding

This study contributes to the project “Mobile villages and dynamic landscapes: the Varamin Plain from the late 5th to the early 3rd mill. BCE” (Project number 424609853) within the priority programme 2176 “The Iranian Highlands: Resilience and Integration of Premodern Societies” funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation, www.dfg.de). (FK, RBe, SP, RBu, BS) This work contributes to the project PalMod, funded by the German Federal Ministry of Education and Research (BMBF, www.bmbf.de), Research for Sustainability initiative (FONA, www.fona.de) and the Cluster of Excellence EXC 2037 “CLICCS - Climate, Climatic Change, and Society” (Project Number: 390683824), funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation, www.dfg.de) under Germany‘s Excellence Strategy. AD was financed by PalMod (Grant number: 01LP1920A) and partly by CLICCS. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.