Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2018.09.026 |
A Late Pleistocene-Holocene multi-proxy record of climate variability in the Jazmurian playa, southeastern Iran | |
Vaezi, Alireza1; Ghazban, Fereydoun1; Tavakoli, Vahid2; Routh, Joyanto3; Beni, Abdolmajid Naderi4; Bianchi, Thomas S.5; Curtis, Jason H.5; Kylin, Henrik3,6 | |
通讯作者 | Routh, Joyanto |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2019 |
卷号 | 514页码:754-767 |
英文摘要 | We present a multi-proxy record from a 5-m long sediment core from the Jazmurian playa in southeastern Iran to provide insights into globally-recognized major climatic events since the Last Glacial Maximum (LGM). In particular, we examined how variability in the Indian Ocean Summer Monsoon (IOSM) and Mid-Latitude Westerlies (MLW) contribute to distinct environmental changes in this arid to hyper-arid region in the interior of West Asia. While interior West Asia showed cold windy conditions during the LGM and post-LGM, southeast Iran experienced quiescent conditions similar to south Asia. The presence of fine-grained sediments, low magnetic susceptibility, and a decrease in aeolian inputs from ca. 21 to 14 cal kyr BP, suggests that effects of both wind and precipitation were minimal during these quiescent conditions. Increased fluvial inputs, coupled with a low abundance of evaporite minerals in Jazmurian sediments, indicated a greater influence of the IOSM between 14 and 13.2 cal kyr BP. In contrast, the Jazmurian playa was dry and dusty between 13.2 and 11.4 cal kyr BP, as reflected by an increase in aeolian sands, and the presence of evaporite minerals. This was followed by a period of strong IOSM activity during the early Holocene, coinciding with higher fluvial input ca. 11.4 cal kyr BP. The early Holocene in southeast Iran was wetter than other analogs in south Asia because of inputs from both IOSM and MWL. Several intense dry periods with sharp increases in aeolian inputs occurred after the early Holocene, due to the southward migration of the Intertropical Convergence Zone. Precipitation sources changed from a monsoon-dominated regime to one influenced mainly by the MLW during the late-Holocene. These results show that palaeoenvironmental changes in the Jazmurian playa, located at the border of IOSM and MLW zones, were primarily governed by global and regional paleoclimatic changes. |
英文关键词 | Paleoenvironment Monsoon Westerlies Sediments Chemical proxies Aeolian |
类型 | Article |
语种 | 英语 |
国家 | Iran ; Sweden ; USA ; South Africa |
收录类别 | SCI-E |
WOS记录号 | WOS:000456355800055 |
WOS关键词 | RADIOCARBON AGE CALIBRATION ; INDIAN-SUMMER MONSOON ; HIGH-RESOLUTION ; ENVIRONMENTAL SIGNIFICANCE ; LACUSTRINE SEDIMENTS ; ISOTOPE RECORDS ; THAR DESERT ; WEST ASIA ; LOESS ; BASIN |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/217859 |
作者单位 | 1.Univ Tehran, Grad Fac Environm, Enghelab Sq, Tehran 1417853111, Iran; 2.Univ Tehran, Coll Sci, Sch Geol, Enghelab Sq, Tehran 1417853111, Iran; 3.Linkoping Univ, Dept Themat Studies Environm Change, SE-58183 Linkoping, Sweden; 4.Iranian Natl Inst Oceanog & Atmospher Sci, Etemadzadeh St, Tehran 1411813389, Iran; 5.Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA; 6.North West Univ, Environm Sci & Management;, Res Unit, Potchefstroom, South Africa |
推荐引用方式 GB/T 7714 | Vaezi, Alireza,Ghazban, Fereydoun,Tavakoli, Vahid,et al. A Late Pleistocene-Holocene multi-proxy record of climate variability in the Jazmurian playa, southeastern Iran[J],2019,514:754-767. |
APA | Vaezi, Alireza.,Ghazban, Fereydoun.,Tavakoli, Vahid.,Routh, Joyanto.,Beni, Abdolmajid Naderi.,...&Kylin, Henrik.(2019).A Late Pleistocene-Holocene multi-proxy record of climate variability in the Jazmurian playa, southeastern Iran.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,514,754-767. |
MLA | Vaezi, Alireza,et al."A Late Pleistocene-Holocene multi-proxy record of climate variability in the Jazmurian playa, southeastern Iran".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 514(2019):754-767. |
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