中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean

文献类型:期刊论文

作者Tan, Zhaozhao3,4,5; Wu, Jinxiang3,4,5; Jia, Wanglu4,5; J., Li; B., Kendall; J., Song; P., Peng
刊名CHEMICAL GEOLOGY
出版日期2023
卷号623页码:121410
关键词BLACK SHALES INTEGRATIVE STRATIGRAPHY EUXINIC SEDIMENTS TRACE-METALS MO IRON FRACTIONATION MANGANESE PROXIES DEEP
ISSN号0009-2541
DOI10.1016/j.chemgeo.2023.121410
英文摘要The Mo isotope composition of late Ediacaran global seawater and the global extent of ocean oxygenation are still debated due to the complex controls on sedimentary Mo isotope compositions and the rarity with which sediments directly capture global seawater Mo isotope compositions. Deep-water sulfidic sediments from modern severely restricted basins like the Black Sea have the best chance of capturing global seawater Mo isotope compositions. However, few studies have focused on sedimentary Mo isotope variations and their causes in late Ediacaran restricted basins. In this study, we present Mo isotope data for a new section from the Chengkou sub-basin of South China. The sedimentary rocks, mostly organic-rich mudstones, in this restricted basin have authigenic δ98Mo values from ?0.01‰ to 1.27‰. Comparison of δ98Mo values with redox-sensitive elemental abundances reveals variation in the extent of Mn-oxide shuttling, related to enhanced hydrothermal activity and the inflow of open-ocean seawater, as the main cause of sedimentary Mo isotope variation in the Chengkou sub-basin. An unambiguous negative correlation between δ98Mo and Mn content points to a greater importance of Mn-oxide shuttling than Fe-oxide shuttling on the sedimentary Mo isotope signatures. Variations in the intensity of Mn-oxide shuttling were likely linked to changes in Mn inputs and the extent of basin restriction. A compilation of late Ediacaran sedimentary Mo isotope data suggests overall limited Mo isotope variation in (semi) restricted late Ediacaran basins, but local factors causing the variation are different and may result in the heaviest Mo isotopic signal in these settings being slightly lighter than that of open seawater. Using the observed negative linear relationships between δ98Mo values and the shuttling-sensitive proxies (V/TOC and Mn), the Mo isotope compositions recorded in the Chengkou sub-basin yield a reliable estimate of 1.3–1.6‰ for the δ98Mo of late Ediacaran global seawater. This value is slightly higher than the δ98Mo estimated for global seawater in the Cryogenian and early-middle Ediacaran, suggesting the extent of ocean oxygenation during the late Ediacaran Period was more similar to the oceans during Mesozoic Oceanic Anoxic Events than to the modern ocean. ? 2023 Elsevier B.V.
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000954980900001
源URL[http://ir.gig.ac.cn/handle/344008/80334]  
专题有机地球化学国家重点实验室
同位素地球化学国家重点实验室
作者单位1.Department of Earth and Environmental Sciences, 200 University Avenue West, University of Waterloo, Waterloo; ON; N2L 3G1, Canada
2.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou; 510640, China
3.University of Chinese Academy of Sciences, Beijing; 100049, China
4.CAS Center for Excellence in Deep Earth Science, Guangzhou; 510640, China
5.State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou; 510640, China
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GB/T 7714
Tan, Zhaozhao,Wu, Jinxiang,Jia, Wanglu,et al. Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean[J]. CHEMICAL GEOLOGY,2023,623:121410.
APA Tan, Zhaozhao.,Wu, Jinxiang.,Jia, Wanglu.,J., Li.,B., Kendall.,...&P., Peng.(2023).Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean.CHEMICAL GEOLOGY,623,121410.
MLA Tan, Zhaozhao,et al."Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean".CHEMICAL GEOLOGY 623(2023):121410.

入库方式: OAI收割

来源:广州地球化学研究所

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