Influence of the Late Ordovician-Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion
文献类型：期刊论文
| 作者 | Zhang, Pengyuan3,4; Wang, Yongli3,4; Wei, Zhifu1,3; Wang, Gen1,3; Zhang, Ting1,3; He, Wei1,3; Ma, Xueyun1,3; Ma, He3,4; Wei, Jingyi3,4; Zhu, Chenxi2 |
| 刊名 | PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
 |
| 出版日期 | 2023-07-01 |
| 卷号 | 38期号:7页码:22 |
| ISSN号 | 2572-4517 |
| DOI | 10.1029/2023PA004628 |
| 英文摘要 | Although previous studies have shown that the paleoenvironment and geological processes contributed to the organic matter accumulation (OMA) and carbon isotope excursions (CIEs) during the late Ordovician-early Silurian, the dominated controlling factor for the OMA and the origins of CIEs still remains unclear due to complex interaction between various paleoenvironmental factors and geological processes. Therefore, based on the elemental geochemistry of the Wufeng-Longmaxi Formation shales in the upper Yangtze Platform, we analyzed the late Ordovician-early Silurian paleoenvironment and related geological processes, and further explored the origin of the OMA and CIEs. As a result, the Wufeng-Longmaxi Formation shale was divided into four stages. During Stage 1 (late Katian, similar to 447.62-444.50 Ma), local tectonic and volcanic activities controlled the paleoproductivity and redox conditions, facilitating the OMA. By contrast, the productivity of the surface water and the anoxic bottom water were mainly controlled by the global climate after the Hirnantian glaciation, which contributed to the OMA during Stage 2 (early Rhuddanian, similar to 444.50-441.00 Ma). The decreasing sea level and rapid uplifting of Xuefeng and Qianzhong Uplifts resulted in the organic matter depletion during Stages 3 (late Rhuddanian, similar to 441.00-440.80 Ma) and 4 (Aeronian, similar to 440.80-439.21 Ma). Besides, the release of C-12-enriched carbon reservoirs triggered by volcanic activities and C-13-enrichment caused by the OMA regulated the carbon cycling: the negative CIE may be the result of light carbon emissions, such as the reactivated organic matter and mantle derived carbon, and the Hirnantian CIE event is jointly controlled by the weakened carbon emission effect and the OMA. |
| WOS关键词 | MISSISSIPPIAN BARNETT SHALE ; SEA-LEVEL CHANGE ; SOUTH CHINA ; BLACK-SHALE ; YANGTZE BLOCK ; SEDIMENTARY-ROCKS ; MASS EXTINCTION ; GEOCHEMICAL CHARACTERISTICS ; HIRNANTIAN GLACIATION ; ENVIRONMENTAL-CHANGES |
| 资助项目 | National Key Ramp;D Program of China[2022YFF0800800] ; National Natural Science Foundation of China[41902028] ; National Natural Science Foundation of China[41972030] ; National Natural Science Foundation of China[42072038] ; National Natural Science Foundation of China[42102195] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program[2019QZKK0707] ; CAS "Light of West China" Program ; Youth Innovation Promotion Association CAS[2021425] |
| WOS研究方向 | Geology ; Oceanography ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:001042088100001 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 资助机构 | National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Key Ramp;D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; Second Tibetan Plateau Scientific Expedition and Research (STEP) Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; CAS "Light of West China" Program ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/111373]  |
| 专题 | 地质与地球物理研究所_中国科学院新生代地质与环境重点实验室 地质与地球物理研究所_兰州油气中心 |
| 通讯作者 | Wang, Yongli; Wei, Zhifu |
| 作者单位 | 1.Chinese Acad Sci, Gansu Prov Northwest Inst Ecoenvironm & Resources, Key Lab Petr Resources, Lanzhou, Peoples R China 2.China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Pengyuan,Wang, Yongli,Wei, Zhifu,et al. Influence of the Late Ordovician-Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion[J]. PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,2023,38(7):22. |
| APA | Zhang, Pengyuan.,Wang, Yongli.,Wei, Zhifu.,Wang, Gen.,Zhang, Ting.,...&Zhu, Chenxi.(2023).Influence of the Late Ordovician-Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion.PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,38(7),22. |
| MLA | Zhang, Pengyuan,et al."Influence of the Late Ordovician-Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion".PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY 38.7(2023):22. |
入库方式： OAI收割
来源：地质与地球物理研究所
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