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Mid-Holocene hydroclimatic optimum recorded in a stalagmite from Shalaii Cave, northern Iraq

Fleitmann, D; Bosomworth, M; Al-Manmi, M; Leng, M; Sahy, D; Radner, K; Morgan, A; ... Altaweel, Mark; + view all (2025) Mid-Holocene hydroclimatic optimum recorded in a stalagmite from Shalaii Cave, northern Iraq. Quaternary Science Reviews , 365 , Article 109286. 10.1016/j.quascirev.2025.109286. Green open access

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Abstract

In Mesopotamia, climate is regarded as an important contributing factor to major socio-cultural transformations. However, the scarcity of Holocene paleoclimate reconstructions in this region impedes analysis of potential climate-human interactions. Furthermore, current hydroclimatic scenarios for Mesopotamia are predominantly based on oxygen isotope (δ18O) proxy records from the eastern Mediterranean, whereas the paleoclimatic significance of δ18O remains debated. Here, we present a Holocene stalagmite multi-proxy record from Shalaii Cave in northern Mesopotamia. Based on stable isotope, trace element and strontium isotope measurements, our new Shalaii Cave record suggests that long-term changes in δ18O were influenced by multiple factors, such as δ18O changes of the source of moisture, amount and seasonality of rainfall. The Shalaii Cave trace element and strontium isotope records indicate rather dry conditions during the early Holocene and wettest conditions during the mid-Holocene. This mid-Holocene hydroclimate optimum at Shalaii Cave is in good agreement with other non-isotopic records from SW-Asia, such as pollen evidence for concurrent rapid forest expansion and peaking lake levels. The mid-Holocene hydroclimatic optimum is most likely related to an increase in the amount of spring precipitation related to the remote influence of the Indian summer monsoon (desert-monsoon mechanism) and spring insolation-driven weakening of the Arabian anticyclone. In particular the latter northward migration of the Arabian anticyclone in spring promoted a longer spring rainfall season.

Type: Article
Title: Mid-Holocene hydroclimatic optimum recorded in a stalagmite from Shalaii Cave, northern Iraq
Open access status: An open access version is available from UCL Discovery
DOI: 10.1016/j.quascirev.2025.109286
Publisher version: https://doi.org/10.1016/j.quascirev.2025.109286
Language: English
Additional information: Crown Copyright © 2025 Published by Elsevier Ltd. Thisis an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL SLASH
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS > Institute of Archaeology
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS > Institute of Archaeology > Institute of Archaeology Gordon Square
URI: https://discovery.ucl.ac.uk/id/eprint/10206081
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