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DOI | 10.1016/j.palaeo.2019.01.034 |
Mid-Holocene moisture maximum revealed by pH changes derived from branched tetraethers in loess deposits of the northeastern Tibetan Plateau | |
Duan Y.; Sun Q.; Werne J.P.; Zhao H.; Zhang D.; Zhang N.; Liu J.; Wu D.; Chen F. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 138 |
结束页码 | 149 |
卷号 | 520 |
英文摘要 | The patterns of Holocene moisture variability inferred from different proxies remain controversial in the northeastern Tibetan Plateau (NETP), which impedes our understanding of the behavior and dynamics of the East Asian Summer Monsoon (EASM). Here we present two pH records spanning the last ~12 kyr from well-dated loess-paleosol sections (YWY14 and SHD09) from the NETP. Based on the modified cyclization ratio index (CBT′) of the branched glycerol dialkyl glycerol tetraethers (brGDGTs) and regional CBT′-pH empirical relationship, the reconstructed pH values from topmost samples are consistent with the instrumental pH values of the surrounding surface soil. Our results illustrate generally similar pH trends from two loess sections characterized by alkaline conditions from 12.0 to 8.5 cal kyr BP, neutral or acidic during the mid-Holocene and alkaline conditions again during the late Holocene. The intervals of lowest CBT′-derived pH values during the mid-Holocene in our records correlate with those of highest tree pollen percentage from adjacent lake sediments and the regionally weakest aeolian activity from records of paleosol development synthesized from the Chinese Loess Plateau (CLP) in northern China, suggesting a moisture maximum during that period. Taken together, we conclude that CBT′-derived pH variability can be potentially used as an indicator of EASM evolution and the wettest climate occurred during the mid-Holocene in the NETP. The changes in summer precipitation during the Holocene on the NETP can be attributed to the interaction between the mid-latitude westerlies and the EASM circulation. © 2019 Elsevier B.V. |
英文关键词 | CBT′; East Asian summer monsoon; Westerlies; Wettest climate |
语种 | 英语 |
scopus关键词 | alkalinity; eolian process; Holocene; lacustrine deposit; loess; paleosol; pH; pollen; precipitation (climatology); summer; westerly; China; Far East; Loess Plateau; Qinghai-Xizang Plateau |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151028 |
作者单位 | College of Earth and Environmental Sciences, MOE Key Laboratory of Western China's Environmental System, Lanzhou University, Lanzhou, 730000, China; National Research Center of Geoanalysis, Beijing, 100037, China; Department of Geology and Environmental Sciences, University of Pittsburgh, Pittsburgh, PA 15260, United States; Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Reseacrh, CAS, Beijing, 100101, China |
推荐引用方式 GB/T 7714 | Duan Y.,Sun Q.,Werne J.P.,et al. Mid-Holocene moisture maximum revealed by pH changes derived from branched tetraethers in loess deposits of the northeastern Tibetan Plateau[J],2019,520. |
APA | Duan Y..,Sun Q..,Werne J.P..,Zhao H..,Zhang D..,...&Chen F..(2019).Mid-Holocene moisture maximum revealed by pH changes derived from branched tetraethers in loess deposits of the northeastern Tibetan Plateau.Palaeogeography, Palaeoclimatology, Palaeoecology,520. |
MLA | Duan Y.,et al."Mid-Holocene moisture maximum revealed by pH changes derived from branched tetraethers in loess deposits of the northeastern Tibetan Plateau".Palaeogeography, Palaeoclimatology, Palaeoecology 520(2019). |
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