KMS Nanjing Institute of Geology and Palaeonotology,CAS
| Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction | |
| Sheng-Ao Liu; Huaichun Wu; Shu-zhong Shen (沈树忠); Ganqing Jiang; Shihong Zhang; Yiwen Lv; Hua Zhang (张华); Shuguang Li | |
| 2017 | |
| Source Publication | Geology
 |
| ISSN | 0091-7613 |
| Volume | 45Issue:4Pages:343-346 |
| Abstract | The end-Permian extinction is typically ascribed to massive volcanic eruptions, but direct geochemical evidence linking the two independent events is generally lacking. Zinc is an important micronutrient of marine phytoplanktons, and Zn isotope (delta Zn-66) ratios of seawater are markedly higher than those of volcanic rocks and riverine waters. We conducted high-resolution Zn concentration and Zn isotope analyses on carbonate rocks across the Permian-Triassic boundary (PTB) in the Meishan section of south China. An abrupt increase of Zn concentration and a concomitant 0.5 parts per thousand decrease in delta Zn-66 occur similar to 35 k.y. before the mass extinction and carbon isotope (delta C-13) minima. Mass balance calculation demonstrates that a 0.5 parts per thousand negative shift in delta Zn-66 within thousands of years requires rapid and massive input of isotopically light Zn from volcanic ashes, hydrothermal inputs, and/or extremely fast weathering of large igneous provinces. A positive delta Zn-66 shift of as much as 1.0 parts per thousand following the mass extinction demonstrates that primary productivity recovered and reached a maximum in fewer than 360 k.y. Our finding provides insights into the marine Zn cycling across the PTB and clarifies the temporal relationship and duration of events, including intensive volcanism, carbon isotope excursion, mass extinction, and widespread ocean anoxia. |
| DOI | 10.1130/G38644.1 |
| Indexed By | SCI |
| Language | 英语 |
| WOS Research Area | Geology |
| WOS Subject | Geology |
| WOS ID | WOS:000396125700016 |
| Publisher | GEOLOGICAL SOC AMER, INC |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.nigpas.ac.cn/handle/332004/13128 |
| Collection | 中国科学院南京地质古生物研究所 |
| Corresponding Author | Sheng-Ao Liu |
| Recommended Citation GB/T 7714 | Sheng-Ao Liu,Huaichun Wu,Shu-zhong Shen ,et al. Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction[J]. Geology,2017,45(4):343-346. |
| APA | Sheng-Ao Liu.,Huaichun Wu.,Shu-zhong Shen .,Ganqing Jiang.,Shihong Zhang.,...&Shuguang Li.(2017).Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction.Geology,45(4),343-346. |
| MLA | Sheng-Ao Liu,et al."Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction".Geology 45.4(2017):343-346. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| Zinc isotope evidenc（284KB） | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | Application Full Text | |
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