Zinc isotope evidence for intensive magmatism immediately before the end-Permian mass extinction
文献类型：期刊论文
| 作者 | Sheng-Ao Liu; Huaichun Wu; Shu-zhong Shen (沈树忠) ; Ganqing Jiang; Shihong Zhang; Yiwen Lv; Hua Zhang (张华); Shuguang Li
|
| 刊名 | Geology
 |
| 出版日期 | 2017 |
| 卷号 | 45期号:4页码:343-346 |
| ISSN号 | 0091-7613 |
| DOI | 10.1130/G38644.1 |
| 英文摘要 | 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. |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000396125700016 |
| 出版者 | GEOLOGICAL SOC AMER, INC |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/13128]  |
| 专题 | 中国科学院南京地质古生物研究所 南京地质古生物研究所_其他 |
| 通讯作者 | Sheng-Ao Liu |
| 推荐引用方式 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. |
入库方式： OAI收割
来源：南京地质古生物研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。