Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2021.110407 |
No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang | |
Jia, Jia; Chen, Jianhui; Wang, Zhiyuan; Chen, Shengqian; Wang, Qiang; Wang, Leibin; Yang, Liwen; Xia, Dunsheng; Chen, Fahu![]() | |
通讯作者 | Chen, JH (corresponding author), Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab West Chinas Environm Syst, Lanzhou 730000, Peoples R China. |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2021 |
卷号 | 572 |
英文摘要 | Arid Central Asia (ACA) is far from oceanic moisture sources and has a prevailing arid climate; thus the environment of the region is hydroclimatically sensitive. The eastern part of ACA is dominated by the basin-mountain system. A previous study proposed that the humid mountains and the arid basins were characterized by an opposite pattern of climatic variation during the Holocene, with a long-term drying trend in the former and a wetting trend in the latter. However, robust evidence from an integrated basin-mountain system using the same geological archive is urgently needed to test this hypothesis. Here we present Holocene paleoclimatic results from two new loess sections, with reliable chronologies, from Tienshan Mountain slope. In combination with two additional loess records from the intermontane arid basin, a systematic mountain-basin comparison was carried out. The results indicate that a Holocene paleosol started to develop on the Tienshan Mountain slope (at an elevation of 1300-1600 m) during 7-5 ka, which is broadly synchronous with paleosol development in the arid basin (at an elevation of 500-800 m). Furthermore, magnetic-parameter-based precipitation reconstructions from the four loess sections all demonstrate a consistent wetting trend throughout the Holocene. Therefore, our findings do not support an anti-phased pattern of moisture/precipitation change between the humid mountains and the arid basins in eastern ACA. |
英文关键词 | Frequency-dependent magnetic susceptibility Stable carbon isotope Tienshan Mountains Westerlies |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000648525800009 |
WOS关键词 | ARID CENTRAL-ASIA ; CARBON ISOTOPIC COMPOSITION ; CHINESE CAVE RECORDS ; MAGNETIC-SUSCEPTIBILITY ; ORGANIC-MATTER ; TIEN-SHAN ; CLIMATE CHANGES ; SUMMER MONSOON ; SURFACE SOILS ; SEQUENCES |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
来源机构 | 兰州大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/368693 |
作者单位 | [Jia, Jia; Wang, Zhiyuan; Yang, Liwen] Zhejiang Normal Univ, Coll Geog & Environm Sci, Jinhua 321004, Zhejiang, Peoples R China; [Chen, Jianhui; Chen, Shengqian; Wang, Qiang; Xia, Dunsheng; Chen, Fahu] Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab West Chinas Environm Syst, Lanzhou 730000, Peoples R China; [Wang, Leibin] Guangzhou Univ, Ctr Climate & Environm Changes, Sch Geog Sci, Guangzhou, Peoples R China; [Chen, Fahu] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Jia, Jia,Chen, Jianhui,Wang, Zhiyuan,et al. No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang[J]. 兰州大学,2021,572. |
APA | Jia, Jia.,Chen, Jianhui.,Wang, Zhiyuan.,Chen, Shengqian.,Wang, Qiang.,...&Chen, Fahu.(2021).No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,572. |
MLA | Jia, Jia,et al."No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 572(2021). |
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