Enhanced Seawater Mixing during the late Ediacaran Shuram Excursion
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摘要
The Ediacaran Shuram excursion event (SE; ca. 574-567 Ma)—the most pronounced negative inorganic carbon isotope (δ13Ccarb) anomaly in Earth's history, most likely represents a substantial oxidation of marine organic matter (OM) in the ocean. However, the physical process related to this OM oxidation remains elusive. To address this issue, we conducted integrated analyses of strontium (87Sr/86Sr) and neodymium (εNd) isotopes of marine carbonates across three SE-bearing sections from South China (Sishang and Lianghong sections) and the Tarim basin (Mochia-Khutuk section). Our results reveal an increase in 87Sr/86Sr (from 0.708 to 0.710 at Sishang section, from 0.710 to 0.713 at Lianghong section, and from 0.712 to 0.713 at Mochia-Khutuk section), and a decrease in εNd (from 7.72 to –4.27 at the Sishang section and from –0.83 to –5.57 at the Lianghong section) at the onset of SE. Notably, εNd values show large spatial variations prior to the SE (7.72 at the Sishang section, –0.83 at the Lianghong, and –4.27 at the Mochia-Khutuk section), but converge to consistently low values of about –5 during the SE. Considering the orders-of-magnitude difference in seawater residence time between Sr (>1 Myr) and Nd (<1 kyr), these coupled variations between 87Sr/86Sr and εNd are less likely to be resulted from any single process alone. In the modern ocean, seawater εNd compositions vary considerably across different regions, making εNd a potential proxy for global seawater mixing. We propose a dual-control mechanism, where intensified continental weathering of felsic rocks contributed to the rising ⁸⁷Sr/⁸⁶Sr ratios, and enhanced ocean mixing of different water masses during the SE event led to more homogeneous εNd composition of the seawater. The converged εNd values from different continents provides robust evidence for strong seawater mixing during the SE, which may have facilitated the oxidation of marine organic matter, which ultimately lead to the largest negative δ13Ccarb excursion in Earth’s history.
关键词
Shuram Excursion,Seawater Mixing
报告人
莹 王
miss 成都理工大学

稿件作者
莹 王 成都理工大学
猛 程 成都理工大学
欣阳 陈 成都理工大学
超 李 成都理工大学 沉积地质研究院
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重要日期
  • 会议日期

    06月10日

    2025

    06月13日

    2025

  • 04月15日 2025

    初稿截稿日期

主办单位
National Natural Science Foundation of China
Geobiology Society
National Committee of Stratigraphy of China
Ministry of Science and Technology
Geological Society of China
Paleontological Society of China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS)
Institute of Vertebrate Paleontology and Paleoanthropology, CAS
International Commission on Stratigraphy
International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)
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