Climate Change Data Portal
| DOI | 10.1038/s41561-021-00870-6 |
| Earth's missing argon paradox resolved by recycling of oceanic crust | |
| Tucker, Jonathan M.; van Keken, Peter E.; Ballentine, Chris J. | |
| 发表日期 | 2022 |
| ISSN | 1752-0894 |
| EISSN | 1752-0908 |
| 起始页码 | 85 |
| 结束页码 | + |
| 卷号 | 15期号:1页码:10 |
| 英文摘要 | Oceanic crust subduction sequesters substantial amounts of argon in the Earth's mantle, while atmosphere-derived argon affects only the isotopic composition and not the overall budget, according to geodynamic-geochemical models of mantle convection. The extent to which primordial mantle domains have survived billions of years of convective mixing is a fundamental question in mantle dynamics and geochemistry. The observation that around half of Earth's Ar-40 is missing from the atmosphere has been used to argue for a largely primordial, convectively isolated lower mantle. This hypothesis is apparently supported by lower Ar-40/Ar-36 ratios in the mantle source of ocean-island basalts compared with mid-ocean-ridge basalts. However, strongly layered convection is contradicted by seismic tomographic observations and geodynamic constraints. Using joint geodynamic-geochemical modelling of mantle convection, we show that high Ar-40 concentrations associated with K-rich subducted oceanic crust plus unmelted material dispersed throughout the mantle can fully account for Earth's Ar-40 budget. This solution to the missing Ar paradox requires neither a substantial reduction in Earth's assumed K concentration nor large isolated domains in the mantle. We additionally show that subducted atmosphere-derived Ar has little effect on the mantle Ar-40 budget but can substantially reduce mantle Ar-40/Ar-36 ratios. Unlike He and Ne isotope systems, whose variations reflect primarily incorporation of primordial material, mantle Ar-40/Ar-36 ratios may instead result from subduction of atmosphere-derived Ar into the deep mantle. |
| 学科领域 | Geosciences, Multidisciplinary |
| 语种 | 英语 |
| WOS研究方向 | Geology |
| WOS记录号 | WOS:000742312300001 |
| 来源期刊 | NATURE GEOSCIENCE
![]() |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/272492 |
| 作者单位 | Carnegie Institution for Science; Smithsonian Institution; Smithsonian National Museum of Natural History; University of Oxford |
| 推荐引用方式 GB/T 7714 | Tucker, Jonathan M.,van Keken, Peter E.,Ballentine, Chris J.. Earth's missing argon paradox resolved by recycling of oceanic crust[J],2022,15(1):10. |
| APA | Tucker, Jonathan M.,van Keken, Peter E.,&Ballentine, Chris J..(2022).Earth's missing argon paradox resolved by recycling of oceanic crust.NATURE GEOSCIENCE,15(1),10. |
| MLA | Tucker, Jonathan M.,et al."Earth's missing argon paradox resolved by recycling of oceanic crust".NATURE GEOSCIENCE 15.1(2022):10. |
| 条目包含的文件 | 条目无相关文件。 | |||||
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。