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
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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

始新世古气候波动的化学风化和高原盐湖沉积物记录
造山、风化和气候之间的相互作用引起了地球科学界的极大关注。本文以柴达木盆地始新统下干柴沟组(LGCG)混合岩为研究对象,从岩石学、矿物学和地球化学等方面对其风化强度进行了评价。岩性特征显示LGCG混合岩的高频沉积旋回(<10 m),由下向上划分为块状砂岩、层状粉质页岩、层状粉质灰岩和层状白云岩4种岩相。物源分析表明,这些混合沉积物主要来源于大陆岛弧背景下的长英质火山物源。化学风化强度指数(CIA、风化化学指数、蚀变斜长石指数)与沉积旋回具有较强的一致性,在单个旋回中先上升后逐渐下降。蚀变化学指数为51.1% ~ 67.2%,表明风化强度弱至中等。相关分析表明,化学风化强度的周期性变化与规律的古气候演化和陆源输入变化密切相关,而这些变化受西风带移动的控制。在西风增强期,强降水形成温暖湿润的古气候条件,导致以细粒粘土矿物为主的陆源输入增多,化学风化强度中等。在西风带减弱期,降水减少导致古气候条件寒冷干燥,陆源输入减少,碎屑沉积物较粗,风化强度较弱。本研究从高分辨率化学风化记录的角度为始新世西风转移和古气候演化提供了新的证据和见解。
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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.
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