Chemical weathering evidence for East Asian Summer Monsoon rainfall variability in the upper reaches of the Yellow River since the Early Pleistocene
The East Asian Summer Monsoon (EASM) is critically important for determining the spatial variability of precipitation in the continental interior of East Asia. Hence, knowledge of past EASM variability may help predict the response of monsoon rainfall to ongoing global climate change, with important...
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| Veröffentlicht in: | Palaeogeography, palaeoclimatology, palaeoecology Jg. 618; S. 111523 |
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| Format: | Journal Article |
| Sprache: | Englisch |
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Elsevier B.V
15.05.2023
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| ISSN: | 0031-0182, 1872-616X |
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| Abstract | The East Asian Summer Monsoon (EASM) is critically important for determining the spatial variability of precipitation in the continental interior of East Asia. Hence, knowledge of past EASM variability may help predict the response of monsoon rainfall to ongoing global climate change, with important implications for the living environment of the large human population of East Asia. In this study, we obtained several geochemical records from the Hetao Basin in the upper reaches of the Yellow River (UYR), which we use to reconstruct variations in chemical weathering intensity since 1.68 Ma. Our results suggest that chemical weathering was significantly intensified during the interval of ∼0.47–0.18 Ma, evidenced by lower Rb/Sr and αAlSr values, and higher LEF Mg/Al values, within the lacustrine sediments during this period. This enhanced chemical weathering was closely linked to increased monsoon rainfall associated with a strong EASM. The long-term trends of EASM rainfall in the UYR were caused by variations in the atmospheric circulation over the Pacific Ocean, such as the ENSO cycle and the PDO phase transition, which may act as testable factors in the prediction of future EASM rainfall.
•Long-term monsoon rainfall variation was evidenced by chemical weathering index.•Interglacial East Asian Summer Monsoon was strong from ∼0.47 to ∼0.18 Ma.•Pacific SST gradients play crucial roles in monsoon rainfall patterns in East Asia. |
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| AbstractList | The East Asian Summer Monsoon (EASM) is critically important for determining the spatial variability of precipitation in the continental interior of East Asia. Hence, knowledge of past EASM variability may help predict the response of monsoon rainfall to ongoing global climate change, with important implications for the living environment of the large human population of East Asia. In this study, we obtained several geochemical records from the Hetao Basin in the upper reaches of the Yellow River (UYR), which we use to reconstruct variations in chemical weathering intensity since 1.68 Ma. Our results suggest that chemical weathering was significantly intensified during the interval of ∼0.47–0.18 Ma, evidenced by lower Rb/Sr and αᴬˡSr values, and higher LEF Mg/Al values, within the lacustrine sediments during this period. This enhanced chemical weathering was closely linked to increased monsoon rainfall associated with a strong EASM. The long-term trends of EASM rainfall in the UYR were caused by variations in the atmospheric circulation over the Pacific Ocean, such as the ENSO cycle and the PDO phase transition, which may act as testable factors in the prediction of future EASM rainfall. The East Asian Summer Monsoon (EASM) is critically important for determining the spatial variability of precipitation in the continental interior of East Asia. Hence, knowledge of past EASM variability may help predict the response of monsoon rainfall to ongoing global climate change, with important implications for the living environment of the large human population of East Asia. In this study, we obtained several geochemical records from the Hetao Basin in the upper reaches of the Yellow River (UYR), which we use to reconstruct variations in chemical weathering intensity since 1.68 Ma. Our results suggest that chemical weathering was significantly intensified during the interval of ∼0.47–0.18 Ma, evidenced by lower Rb/Sr and αAlSr values, and higher LEF Mg/Al values, within the lacustrine sediments during this period. This enhanced chemical weathering was closely linked to increased monsoon rainfall associated with a strong EASM. The long-term trends of EASM rainfall in the UYR were caused by variations in the atmospheric circulation over the Pacific Ocean, such as the ENSO cycle and the PDO phase transition, which may act as testable factors in the prediction of future EASM rainfall. •Long-term monsoon rainfall variation was evidenced by chemical weathering index.•Interglacial East Asian Summer Monsoon was strong from ∼0.47 to ∼0.18 Ma.•Pacific SST gradients play crucial roles in monsoon rainfall patterns in East Asia. |
| ArticleNumber | 111523 |
| Author | Wang, Fei Li, Zaijun Wang, Xin Feng, Qi Li, Ruolin Li, Baofeng Chen, Weiyu |
| Author_xml | – sequence: 1 givenname: Baofeng surname: Li fullname: Li, Baofeng email: libf@lzb.ac.cn organization: Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China – sequence: 2 givenname: Qi surname: Feng fullname: Feng, Qi organization: Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China – sequence: 3 givenname: Fei surname: Wang fullname: Wang, Fei organization: Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China – sequence: 4 givenname: Zaijun surname: Li fullname: Li, Zaijun organization: Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China – sequence: 5 givenname: Xin surname: Wang fullname: Wang, Xin organization: Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China – sequence: 6 givenname: Ruolin surname: Li fullname: Li, Ruolin organization: Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China – sequence: 7 givenname: Weiyu surname: Chen fullname: Chen, Weiyu organization: Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China |
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| CitedBy_id | crossref_primary_10_1016_j_gloplacha_2023_104224 crossref_primary_10_1016_j_jhydrol_2025_133717 crossref_primary_10_1016_j_catena_2024_108570 crossref_primary_10_1016_j_palaeo_2025_112837 crossref_primary_10_5194_esd_15_1509_2024 |
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| Copyright | 2023 Elsevier B.V. |
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| Keywords | Upper reaches of the Yellow River East Asian Summer Monsoon Pacific Ocean atmospheric circulation Chemical weathering |
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| Title | Chemical weathering evidence for East Asian Summer Monsoon rainfall variability in the upper reaches of the Yellow River since the Early Pleistocene |
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