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Grain-size-specific Sr–Nd isotopic evidence for the dominant role of fluvial sediments in Danube loess formation 多瑙河黄土地层中河流沉积物主导作用的粒度特征Sr-Nd同位素证据
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-14 DOI: 10.1016/j.gca.2026.03.019
Xuechao Wu, Qingzhen Hao, Slobodan B. Marković, Xinbo Gao, Long Han, Yu Fu, Yang Song, Zhipeng Wu, Shouye Yang, Zhengtang Guo
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引用次数: 0
Chronology of ungrouped achondrites Northwest Africa 11119 and 7325/8486: implications for early evolution of a heterogeneous crust on a differentiated planetesimal 西北非洲11119和7325/8486的未分组无球粒陨石年代学:对分异星子上非均质地壳早期演化的启示
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-14 DOI: 10.1016/j.gca.2026.03.014
Daniel R. Dunlap, Julia A. Cartwright, Piers Koefoed, Evgenii Krestianinov, Stephen J. Romaniello, Carl Agee, Yuri Amelin, Meenakshi Wadhwa
The chronology of ungrouped achondrites provides key insights into the timeline of igneous activity in the early Solar System. Two ungrouped achondrites – Northwest Africa (NWA) 11119 (andesite-dacite) and NWA 8486 and its pair NWA 7325 (olivine gabbro) – are the focus of this study, where their chronologies are investigated using multiple high-resolution techniques. Here we report the lead-lead (207Pb-206Pb) and manganese-chromium (53Mn-53Cr) systematics of NWA 11119, as well as the 207Pb-206Pb systematics of NWA 8486 alongside aluminum-magnesium (26Al-26Mg) systematics for NWA 7325. The U-corrected 207Pb-206Pb ages of NWA 11119 and the combined ages of NWA 7325/8486 are 4566.4 ± 0.8 Ma and 4563.8 ± 1.9 Ma, respectively. Additionally, we report the 53Mn-53Cr age of NWA 11119 to be 4564.4 ± 2.5 Ma and the 26Al-26Mg age of NWA 7325/8486 to be 4563.1 ± 0.3 Ma.
未分类无球粒陨石的年表为了解早期太阳系火成岩活动的年表提供了关键的见解。两个未分类的无球粒陨石-西北非洲(NWA) 11119(安山岩-英安岩)和NWA 8486及其对NWA 7325(橄榄辉长岩)-是本研究的重点,使用多种高分辨率技术研究了它们的年代学。在这里,我们报道了NWA 11119的铅-铅(207Pb-206Pb)和锰-铬(53Mn-53Cr)系统,NWA 8486的207Pb-206Pb系统以及NWA 7325的铝-镁(26Al-26Mg)系统。NWA 11119的铀校正207Pb-206Pb年龄和NWA 7325/8486的总年龄分别为4566.4 ± 0.8 Ma和4563.8 ± 1.9 Ma。此外,我们报道了NWA 11119的53Mn-53Cr年龄为4564.4 ± 2.5 Ma, NWA 7325/8486的26Al-26Mg年龄为4563.1 ± 0.3 Ma。
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引用次数: 0
Basin-scale sulfur cycling driven by volcanism in Southern high latitudes during the Oceanic Anoxic Event 2 海洋缺氧事件2期间南部高纬度地区火山作用驱动的盆地尺度硫循环
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-14 DOI: 10.1016/j.gca.2026.03.023
Zhiyu Zeng, Yilun Xu, Weiqi Yao
The Oceanic Anoxic Event 2 (OAE2) represents the episode of large-scale ocean oxygen loss under extreme warmth in the late Cretaceous. The initiation of the OAE2 has been attributed to massive volcanic carbon emissions related to the emplacement of Large Igneous Provinces (LIPs), accompanied by significant perturbations in biogeochemical cycles of carbon, oxygen, and sulfur. Given the lower sulfate concentration in the Cretaceous ocean than it is today, its residence time was shorter under comparable fluxes, increasing the likelihood of spatial heterogeneity in the marine sulfur cycle. Since most existing data of seawater sulfate S-isotope ratio (δ34S) for the OAE2 are reported from localities distant from LIPs, our understanding of the effects of volcanism on regional sulfur cycling and climate warming remains poorly constrained. In this study, we present marine barite δ34S and TEX86-derived sea-surface temperature (SST) records across the OAE2 from the Mentelle Basin, which was proximal to the active Kerguelen LIP (KLIP) in Southern high latitudes. Our result shows a basin-scale ∼5‰ decrease in seawater sulfate δ34S during the OAE2, followed by a recovery to the higher-than-pre-excursion value in the post-OAE2. The simple box model attributes the δ34S decline to a volcanic pulse of 6.96 × 1012 mol isotopically light sulfur released into the ocean within 50 thousand years, which is approximately threefold of the background flux. The subsequent δ34S overshoot requires a coeval increase in pyrite burial flux by 10%, indicating a modest expansion of anoxia in the Mentelle Basin. Meanwhile, the TEX86-derived SST documents prolonged warmth persisting into the post-OAE2, providing an independent constraint on thermal forcing during the recovery phase. Sustained elevated SST in the high-latitude Southern Hemisphere would not only have promoted basin-scale deoxygenation and pyrite burial beyond the initial volcanic perturbation, but also reduced the meridional SST gradient and efficiency of poleward heat redistribution, thereby acting as positive feedback that helped sustain global warming. These findings reveal the response of basin-scale sulfur cycling and persistent warmth to volcanic activities in the high-latitude ocean across the OAE2.
海洋缺氧事件2 (OAE2)代表了晚白垩世极端温暖条件下的大规模海洋氧气损失事件。OAE2的起源归因于与大火成岩省(lip)就位有关的大量火山碳排放,伴随着碳、氧和硫的生物地球化学循环的显著扰动。考虑到白垩纪海洋中硫酸盐浓度低于今天,在可比通量下,其停留时间较短,增加了海洋硫循环空间异质性的可能性。由于现有的OAE2海水硫酸盐s同位素比值(δ34S)数据大多来自远离LIPs的地区,因此我们对火山作用对区域硫循环和气候变暖的影响的认识仍然很有限。在本研究中,我们获得了来自Mentelle盆地的海相重晶石δ34S和tex86海表温度(SST)记录,该盆地位于南部高纬度地区活跃的Kerguelen LIP (KLIP)附近。我们的结果表明,在OAE2期间,海水硫酸盐δ34S在盆地尺度上下降了~ 5‰,随后在OAE2之后恢复到高于偏移前的值。简单盒模型将δ34S下降归因于5万年内释放到海洋中的6.96 × 1012 mol同位素轻硫的火山脉冲,约为背景通量的三倍。随后的δ34S超调需要黄铁矿埋藏通量同期增加10%,表明Mentelle盆地缺氧程度适度扩大。同时,由tex86导出的海温记录了持续到oae2后的持续变暖,为恢复阶段的热强迫提供了一个独立的约束。南半球高纬度海温的持续升高不仅促进了盆地尺度的缺氧和黄铁矿埋藏,而且降低了经向海温梯度和向极地热量再分配的效率,从而起到了持续全球变暖的正反馈作用。这些发现揭示了盆地尺度硫循环和持续变暖对横跨OAE2的高纬度海洋火山活动的响应。
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引用次数: 0
Lithium isotopes as a new indicator for change in hydrology 锂同位素作为水文变化的新指标
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-13 DOI: 10.1016/j.gca.2026.03.018
Yadan Hu, Fei Zhang, Chen Chen, Ying Xie, Li Deng, Xiangying Li, Xiaolong Zhang, Guang Bao, Jinzhao Liu, Zhangdong Jin
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引用次数: 0
Late Triassic hyperwarming and its link to nitrogen-cycle climate feedbacks 晚三叠纪的超暖化及其与氮循环气候反馈的联系
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-13 DOI: 10.1016/j.gca.2026.03.016
Caineng Zou, Yanjie Gong, Thomas J. Algeo, Jiubin Chen, Qingong Zhuo, Ruoyu Sun, Zhengfu Zhao, Weiyan Chen
{"title":"Late Triassic hyperwarming and its link to nitrogen-cycle climate feedbacks","authors":"Caineng Zou, Yanjie Gong, Thomas J. Algeo, Jiubin Chen, Qingong Zhuo, Ruoyu Sun, Zhengfu Zhao, Weiyan Chen","doi":"10.1016/j.gca.2026.03.016","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.016","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"51 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447934","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Permeability as the first-order control on the rate of aqueous alteration in carbonaceous chondrites 渗透率是碳质球粒陨石含水蚀变速率的一级控制因素
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-13 DOI: 10.1016/j.gca.2026.03.020
Bianka Babrián, Queenie H.S. Chan, Jens Najorka, James Malley, Lee F. White, Martin D. Suttle
{"title":"Permeability as the first-order control on the rate of aqueous alteration in carbonaceous chondrites","authors":"Bianka Babrián, Queenie H.S. Chan, Jens Najorka, James Malley, Lee F. White, Martin D. Suttle","doi":"10.1016/j.gca.2026.03.020","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.020","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"16 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447935","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The neodymium and samarium isotope compositions and cosmic ray exposure history of B-type asteroid (101955) Bennu b型小行星Bennu(101955)的钕、钐同位素组成和宇宙射线暴露史
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-12 DOI: 10.1016/j.gca.2026.03.015
Zachary A. Torrano, Michelle K. Jordan, Lori N. Willhite, Richard W. Carlson
{"title":"The neodymium and samarium isotope compositions and cosmic ray exposure history of B-type asteroid (101955) Bennu","authors":"Zachary A. Torrano, Michelle K. Jordan, Lori N. Willhite, Richard W. Carlson","doi":"10.1016/j.gca.2026.03.015","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.015","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"23 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447940","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Tracking high-field-strength-element enrichment pathways in alkaline granites: Insights from potassium and barium isotopes 碱性花岗岩中高场强元素富集路径的追踪:来自钾和钡同位素的见解
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-12 DOI: 10.1016/j.gca.2026.03.017
Hao-Cheng Yu, Zheng-Yu Long, A.E. Williams-Jones, Ralf Halama, Frédéric Moynier, Shan-Shan Li, Ming-Qian Wu, Hao-Ran Duan, Jia-Dong Ma, Nan Ju, Ze-Zhou Wang, Kun-Feng Qiu
{"title":"Tracking high-field-strength-element enrichment pathways in alkaline granites: Insights from potassium and barium isotopes","authors":"Hao-Cheng Yu, Zheng-Yu Long, A.E. Williams-Jones, Ralf Halama, Frédéric Moynier, Shan-Shan Li, Ming-Qian Wu, Hao-Ran Duan, Jia-Dong Ma, Nan Ju, Ze-Zhou Wang, Kun-Feng Qiu","doi":"10.1016/j.gca.2026.03.017","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.017","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"62 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447939","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Interaction between ilmenite-bearing cumulates and lunar mantle: implications for the origin of intermediate and high-titanium lunar basalts 含钛铁矿堆积与月幔的相互作用:对中、高钛月玄武岩成因的启示
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-11 DOI: 10.1016/j.gca.2026.03.008
Himela Moitra, Sujoy Ghosh, Tamalkanti Mukherjee, Saibal Gupta, Kuljeet Kaur Marhas
{"title":"Interaction between ilmenite-bearing cumulates and lunar mantle: implications for the origin of intermediate and high-titanium lunar basalts","authors":"Himela Moitra, Sujoy Ghosh, Tamalkanti Mukherjee, Saibal Gupta, Kuljeet Kaur Marhas","doi":"10.1016/j.gca.2026.03.008","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.008","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"93 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447941","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Assessing the fidelity of clay-size lithium isotopes as chemical-weathering tracers in detrital sedimentary successions 评估碎屑沉积层序中粘土级锂同位素作为化学风化示踪剂的保真度
IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-11 DOI: 10.1016/j.gca.2026.03.013
Xia Zhang, Chunming Lin, Robert W. Dalrymple, Cheng Cao, Daidu Fan, Guyue Tan, Xin Li
{"title":"Assessing the fidelity of clay-size lithium isotopes as chemical-weathering tracers in detrital sedimentary successions","authors":"Xia Zhang, Chunming Lin, Robert W. Dalrymple, Cheng Cao, Daidu Fan, Guyue Tan, Xin Li","doi":"10.1016/j.gca.2026.03.013","DOIUrl":"https://doi.org/10.1016/j.gca.2026.03.013","url":null,"abstract":"","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"53 1","pages":""},"PeriodicalIF":5.0,"publicationDate":"2026-03-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147447944","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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Geochimica et Cosmochimica Acta
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