Records of Chemical Weathering and Plateau Saline Lake Sediments Linked to Paleoclimate Fluctuations During the Eocene

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Peng Pang, Xiucheng Tan, Kunyu Wu, Songtao Wu, Haoting Xing, Menglin Zhang, Na Zhang, Wei Deng
{"title":"Records of Chemical Weathering and Plateau Saline Lake Sediments Linked to Paleoclimate Fluctuations During the Eocene","authors":"Peng Pang,&nbsp;Xiucheng Tan,&nbsp;Kunyu Wu,&nbsp;Songtao Wu,&nbsp;Haoting Xing,&nbsp;Menglin Zhang,&nbsp;Na Zhang,&nbsp;Wei Deng","doi":"10.1029/2025GC012171","DOIUrl":null,"url":null,"abstract":"<p>Interactions between mountain building, weathering and climate draw significant attention within the geoscience community. In this study, the mixed rocks from the Eocene Lower Ganchaigou Formation (LGCG) of the Qaidam Basin are employed for weathering intensity evaluation by petrology, mineralogy, and geochemistry. Lithological characteristics indicate high-frequency sedimentary cycles (&lt;10 m) of the LGCG mixed rocks, which are identified by a single cycle with four lithofacies from bottom to top: massive sandstones, laminated silty shales, laminated silty limestones, and bedded dolomites. Provenance analysis suggests a predominant felsic volcanic source within a continental island arc background for these mixed sediments. Chemical weathering intensity indices (CIA, chemical index of weathering, and plagioclase index of alteration) show a high coherence with sedimentary cycles, initially increasing and gradually decreasing in a single cycle. Chemical index of alteration values ranged from 51.1% to 67.2%, indicating weak to moderate weathering intensity. Additionally, correlation analysis reveals that the cyclical variations of chemical weathering intensity correlate strongly with regular paleoclimate evolution and terrigenous input changes, which were controlled by the shift of the westerlies. During the westerly strengthening periods, stronger precipitation results in a warm and humid paleoclimate conditions, leading to higher terrigenous input dominated by fine-grained clay minerals with moderate chemical weathering intensity. During the westerly weakening periods, less rainfall leads to a cold and dry paleoclimate conditions, resulting in lower terrigenous input dominated by coarser clastic sediments and weak weathering intensity. Our study provides new evidence and insights into the westerly shift and paleoclimate evolution in the Eocene from the perspective of high-resolution chemical weathering records.</p>","PeriodicalId":50422,"journal":{"name":"Geochemistry Geophysics Geosystems","volume":"26 3","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2025-03-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2025GC012171","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemistry Geophysics Geosystems","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2025GC012171","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Interactions between mountain building, weathering and climate draw significant attention within the geoscience community. In this study, the mixed rocks from the Eocene Lower Ganchaigou Formation (LGCG) of the Qaidam Basin are employed for weathering intensity evaluation by petrology, mineralogy, and geochemistry. Lithological characteristics indicate high-frequency sedimentary cycles (<10 m) of the LGCG mixed rocks, which are identified by a single cycle with four lithofacies from bottom to top: massive sandstones, laminated silty shales, laminated silty limestones, and bedded dolomites. Provenance analysis suggests a predominant felsic volcanic source within a continental island arc background for these mixed sediments. Chemical weathering intensity indices (CIA, chemical index of weathering, and plagioclase index of alteration) show a high coherence with sedimentary cycles, initially increasing and gradually decreasing in a single cycle. Chemical index of alteration values ranged from 51.1% to 67.2%, indicating weak to moderate weathering intensity. Additionally, correlation analysis reveals that the cyclical variations of chemical weathering intensity correlate strongly with regular paleoclimate evolution and terrigenous input changes, which were controlled by the shift of the westerlies. During the westerly strengthening periods, stronger precipitation results in a warm and humid paleoclimate conditions, leading to higher terrigenous input dominated by fine-grained clay minerals with moderate chemical weathering intensity. During the westerly weakening periods, less rainfall leads to a cold and dry paleoclimate conditions, resulting in lower terrigenous input dominated by coarser clastic sediments and weak weathering intensity. Our study provides new evidence and insights into the westerly shift and paleoclimate evolution in the Eocene from the perspective of high-resolution chemical weathering records.

Abstract Image

求助全文
约1分钟内获得全文 求助全文
来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信