Temporal Variation in the Chemical Index of Alteration in Early Cretaceous Black Shale as a Proxy for Paleoclimate
文献类型：期刊论文
| 作者 | Wang, Wenxia5; Gan, Zuobin5; Zhang, Xiangyu3,4,5; Li, Shoujun2,4; Xu, Yanming1 |
| 刊名 | JOURNAL OF GEOLOGY
 |
| 出版日期 | 2022-09-01 |
| 页码 | 19 |
| ISSN号 | 0022-1376 |
| DOI | 10.1086/722337 |
| 通讯作者 | Zhang, Xiangyu(xiangyu_159@126.com) |
| 英文摘要 | To better understand Early Cretaceous climate variation in inland East Asia, the temporal variation in the chemical index of alteration (CIA) was reconstructed in black shale from an outcrop of the Fajiaying Formation in the Lower Cretaceous Laiyang Group at Lingshan Island, East China. As the formation height increased, the corresponding CIA increased. The obtained index of compositional variability values and an (Al2O3)-(CaO* + Na2O)-K2O ternary diagram demonstrate that the gathered samples had not evolved into K-metasomatism during diagenesis. Moreover, low Zr concentrations parallel to the magmatic trend in the Th/Sc-versus-Zr/Sc diagram reveal that the sediment sorting and recycling did not affect the paleoweathering proxies. The lack of correlation between the CIA and Al/Si or K/Si further suggests that the paleoweathering proxies were not affected by the sediment sorting. Accordingly, as the CIA and the chemical index of weathering increased, the corresponding chemical weathering increased slightly. This is consistent with the transition from a dry-hot climate to a warm-humid one proposed by paleoclimatic proxies such as Rb/Sr, Sr/Cu, Al2O3/MgO, and clay minerals. In this study, a near-ubiquitous correlation is proposed between the variations of paleoclimate and the CIA of shale, in which a rise in humidity significantly increased the chemical weathering. Meanwhile, it was found that under the dry-hot conditions of the Early Cretaceous, chemical weathering in inland areas far from the ocean was relatively weak and dependent on atmospheric humidity. This analysis validates the CIA, as part of the stratigraphic record, to be a robust proxy for terrestrial paleoclimatic variation during the Early Cretaceous. |
| WOS关键词 | OCEANIC ANOXIC EVENT ; SEA-SURFACE TEMPERATURES ; LINGSHAN ISLAND ; SEDIMENTARY-ROCKS ; WEATHERING TRENDS ; CARBON-ISOTOPE ; VOLCANIC-ROCKS ; EVOLUTION ; STRATIGRAPHY ; PROVENANCE |
| 资助项目 | Key Laboratory of Stratigraphy and Palaeontology, Ministry of Natural Resources[KLSP1904] ; Shandong University of Science and Technology[SDKDYC190104] ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences)[123104] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000899603900001 |
| 出版者 | UNIV CHICAGO PRESS |
| 资助机构 | Key Laboratory of Stratigraphy and Palaeontology, Ministry of Natural Resources ; Shandong University of Science and Technology ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences) |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/41585]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Zhang, Xiangyu |
| 作者单位 | 1.7 Explorat Inst Geol & Mineral Resources, Linyi 276006, Shandong, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China 3.Minist Nat Resources, Key Lab Stratig & Palaeontol, Beijing 100037, Peoples R China 4.Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Shandong, Peoples R China 5.Linyi Univ, Coll Life Sci, Linyi 276000, Shandong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Wenxia,Gan, Zuobin,Zhang, Xiangyu,et al. Temporal Variation in the Chemical Index of Alteration in Early Cretaceous Black Shale as a Proxy for Paleoclimate[J]. JOURNAL OF GEOLOGY,2022:19. |
| APA | Wang, Wenxia,Gan, Zuobin,Zhang, Xiangyu,Li, Shoujun,&Xu, Yanming.(2022).Temporal Variation in the Chemical Index of Alteration in Early Cretaceous Black Shale as a Proxy for Paleoclimate.JOURNAL OF GEOLOGY,19. |
| MLA | Wang, Wenxia,et al."Temporal Variation in the Chemical Index of Alteration in Early Cretaceous Black Shale as a Proxy for Paleoclimate".JOURNAL OF GEOLOGY (2022):19. |
入库方式： OAI收割
来源：南京地质古生物研究所
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