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DOI | 10.1016/j.epsl.2021.116826 |
Variations of the East Asian monsoon over the past 800 kyr constrained by the boron isotope composition of paleo-rainwater inferred from loess-paleosol deposits in NE China | |
Lei F.; Wei H.-Z.; Yi S.-W.; Zeng L.; Lu H.-Y. | |
发表日期 | 2021 |
ISSN | 0012821X |
卷号 | 561 |
英文摘要 | Based on a study of the boron (B) isotope geochemistry of the loess-paleosol sequence of the Niuyangzigou section (NYZG) in Northeast (NE) China, the boron isotopic composition of paleo-rainwater (δ11Bpr) is used for the first time as a potential proxy for tracing changes in the East Asian summer monsoon (EASM) since the mid-Pleistocene. The acid-soluble phase of loess in NE China, which is characteristically a sandy loess, has lower boron concentrations (0.26 to 0.89 μg/g) and more positive δ11B values, from −12.1‰ to +9.4‰, compared to the loess of the Chinese Loess Plateau (CLP). According to the mass balance of boron accumulation from three distinct sources, a mathematical inversion calculation is used to quantify the proportion of boron from each source and to capture the original δ11Bpr signature. The resulting δ11Bpr values range from +6.8 ± 0.95‰ in loess layers to +17.3 ± 3.32‰ in paleosol layers, and the boron accumulated in loess-paleosol layers is shown to be mainly from atmospheric precipitation and silicate weathering. Synchronous variations of reconstructed δ11Bpr and other loess-based proxies, both in NE China and in the CLP, are observed over a large spatial range and on several temporal scales. The linkage of δ11Bpr to the intensity of the EASM is attributed to the kinetic boron isotope fractionation associated with vapor-precipitate phase separation along the transport path of moisture-bearing air masses. A Rayleigh fractionation model is proposed to interpret δ11Bpr in terms of the proportion of water vapor loss after multi-step fractionation processes, which is independent of temperature. The monsoon record based on δ11Bpr shows a significant shift at ∼430 ka, implying an abrupt weakening of the EASM after the Mid-Brunhes Event (MBE), which provides evidence for regional disparities in monsoon evolution in response to the MBE. The ice volume in Northern Hemisphere is a possible factor controlling changes in the EASM in NE China over the past 800 kyr. © 2021 Elsevier B.V. |
关键词 | B isotopic compositionEast Asian summer monsoonloess-paleosol sequencepaleo-rainwaterRayleigh isotope fractionation |
英文关键词 | Atmospheric thermodynamics; Boron; Exploratory geochemistry; Fractionation; Isotopes; Phase separation; Sediments; Silicates; Weathering; Atmospheric precipitation; Boron isotope fractionation; Chinese Loess Plateau; East Asian summer monsoon; Fractionation process; Inversion calculations; Rayleigh fractionation; Synchronous variation; Boron deposits; boron isotope; isotopic composition; isotopic fractionation; loess; monsoon; paleoclimate; paleosol; Pleistocene; rainwater; temporal variation; China; Loess Plateau |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203180 |
作者单位 | School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, China; State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China; School of Resources and Environmental Engineering, Ludong University, Yantai, 264025, China |
推荐引用方式 GB/T 7714 | Lei F.,Wei H.-Z.,Yi S.-W.,et al. Variations of the East Asian monsoon over the past 800 kyr constrained by the boron isotope composition of paleo-rainwater inferred from loess-paleosol deposits in NE China[J],2021,561. |
APA | Lei F.,Wei H.-Z.,Yi S.-W.,Zeng L.,&Lu H.-Y..(2021).Variations of the East Asian monsoon over the past 800 kyr constrained by the boron isotope composition of paleo-rainwater inferred from loess-paleosol deposits in NE China.Earth and Planetary Science Letters,561. |
MLA | Lei F.,et al."Variations of the East Asian monsoon over the past 800 kyr constrained by the boron isotope composition of paleo-rainwater inferred from loess-paleosol deposits in NE China".Earth and Planetary Science Letters 561(2021). |
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