2021
Middle East Climate Response to the Saharan Vegetation Collapse during the Mid-Holocene
Abstract: Understanding climate change in the Middle East (ME) is crucial because people’s living environment depends on rain-fed crop systems. It remains unclear if the ME climate would be affected by the Saharan vegetation collapse at the end of the mid-Holocene (MH). Proxy data suggest a transition from humid to more arid ME conditions during the period of 6.5-5 kyr BP. Using a set of idealized sensitivity experiments with an Earth System model (EC-Earth), we infer that the shift of Saharan vegetation plays a role in…
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2026
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Cited by 13 publications
(9 citation statements)
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“…The higher level of allele sharing between ancient samples from IRN and Levant in the Chalcolithic time period coincides with known transitions to more arid conditions in the Middle East during the period of 6.5-5 kyr BP (Sun et al 2021). It also agrees with the high genetic continuity and reduced genetic differentiation of farmers from southern Levant (Israel and Jordan) and Zagros Mountains (Iran) (Harney et al 2018, Lazaridis et al 2016.…”
Section: Discussionsupporting
confidence: 69%
“…The higher level of allele sharing between ancient samples from IRN and Levant in the Chalcolithic time period coincides with known transitions to more arid conditions in the Middle East during the period of 6.5-5 kyr BP (Sun et al 2021). It also agrees with the high genetic continuity and reduced genetic differentiation of farmers from southern Levant (Israel and Jordan) and Zagros Mountains (Iran) (Harney et al 2018, Lazaridis et al 2016.…”
Section: Discussionsupporting
confidence: 69%
“…Thus, we propose extensive gene flow from Levant lineages into SWA populations after domestication time, dating between ˜7,000 and 5,000 YBP, which suggested a North-Eastern path of gene flow from Levant into eastern parts of the Fertile Crescent. Given that the timing of this gene flow concurrences with a wet-to-dry transition in western parts of IRN regions such as Lakes Zeribar and Mirabad (Sun et al 2021), we hypothesize that changing precipitation patterns and temperature have favored the introgression of adaptive introgression genes from the Levant genetic resource into the SWA region. The same climate transition is proposed to have driven the migration of heat-resistant indicine cattle to SWA after 4,200 BP (Verdugo et al 2019).…”
Section: Discussionmentioning
confidence: 92%
“…The high level of allele sharing between ancient samples from IRN and Levant in the Chalcolithic period coincides with known transitions to more arid conditions in the Middle East (6.5–5 kyr BP) ( Sun et al, 2021 ). These results are also consistent with the high genetic continuity and reduced genetic differentiation among farmers from southern Levant (Israel and Jordan) and the Zagros Mountains (Iran) ( Harney et al, 2018 ; Lazaridis et al, 2016 ).…”
Section: Discussionsupporting
confidence: 62%
“…Thus, we propose extensive gene flow from Levant lineages into SWA populations after domestication, dating between ~7 000 and 5 000 YBP, suggesting a northeastern path of gene flow from Levant into eastern parts of the Fertile Crescent. Given that the timing of this gene flow coincides with a wet-to-dry transition in western IRN regions, such as Lake Zeribar and Lake Mirabad ( Sun et al, 2021 ), we hypothesize that changing precipitation and temperature patterns may have favored introgression of adaptive genes from the Levant populations to the SWA region. The same climate transition is proposed to have driven the migration of heat-resistant indicine cattle to SWA after 4 200 BP ( Verdugo et al, 2019 ).…”
Section: Discussionmentioning
confidence: 98%
“…growth conditions, and growing season duration (Goodwin et al, 2021;H. Liu et al, 2018;Lu et al, 2019;Sun et al, 2021;Shen, Liu, Henderson, et al, 2022;Yang et al, 2021;Zarei et al, 2021). These changes in vegetation lead to variations in vegetation NPP, and, thereafter, affect the global carbon cycle (Euskirchen et al, 2006;Piao et al, 2013).…”
mentioning
confidence: 99%
