Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling
文献类型：期刊论文
| 作者 | Zhang, Junpeng2 ; Li, Wenjie2; Fang, Xiang2; Wu, Xuejin1,2; Li, Chao2; Zhang, Yuandong1,2
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| 刊名 | JOURNAL OF THE GEOLOGICAL SOCIETY
 |
| 出版日期 | 2024-03-04 |
| 卷号 | 181期号:2页码:8 |
| ISSN号 | 0016-7649 |
| DOI | 10.1144/jgs2023-078 |
| 通讯作者 | Zhang, Junpeng(jpzhang@nigpas.ac.cn) |
| 英文摘要 | Previous work has proposed climatic cooling and atmosphere-ocean oxygenation as potential triggers for the Great Ordovician Biodiversification Event, with the suggestion of better oxygenated oceans during the Middle to Late Ordovician. However, recent studies have argued for spatial and temporal heterogeneity in marine redox state on several continents. Here we investigate a black-shale succession accumulated within the Tarim Platform via a combination of geochemical proxies to address these debates. Negative shifts in bulk nitrogen isotopes and synchronous increases in excess phosphorus suggest moderate-high marine primary production coinciding with the development of bottom-water anoxia, as indicated by enrichments in highly reactive iron and modest concentrations of redox-sensitive trace metals (Mo, U). Moreover, the occurrence of black shale correlates well with equivalent successions formed in deep-water marginal basins along several continents, including South China, North China, Laurentia and Baltica. This may suggest an expansion of marine anoxia in low-latitude zones of the late Darriwilian to early Sandbian oceans, probably as a result of enhanced upwelling in sync with climatic cooling. The extent and ultimate cause of marine anoxia requires further quantifying constraints at a global scale, which will enable potential links between global oceanic redox conditions and concurrent biotic changes to be evaluated in more detail. |
| WOS关键词 | REDOX CONDITIONS ; BIODIVERSIFICATION ; SULFUR ; CARBON ; OCEAN ; PHOSPHORUS ; IRON ; MOLYBDENUM ; SEDIMENTS ; EASTERN |
| 资助项目 | National Natural Science Foundation of China[735] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:001177399900001 |
| 出版者 | GEOLOGICAL SOC PUBL HOUSE |
| 资助机构 | National Natural Science Foundation of China |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/43505]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Zhang, Junpeng |
| 作者单位 | 1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 2.Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Junpeng,Li, Wenjie,Fang, Xiang,et al. Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling[J]. JOURNAL OF THE GEOLOGICAL SOCIETY,2024,181(2):8. |
| APA | Zhang, Junpeng,Li, Wenjie,Fang, Xiang,Wu, Xuejin,Li, Chao,&Zhang, Yuandong.(2024).Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling.JOURNAL OF THE GEOLOGICAL SOCIETY,181(2),8. |
| MLA | Zhang, Junpeng,et al."Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling".JOURNAL OF THE GEOLOGICAL SOCIETY 181.2(2024):8. |
入库方式： OAI收割
来源：南京地质古生物研究所
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