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DOI | 10.1016/j.earscirev.2020.103147 |
A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers | |
Wittmann H.; Oelze M.; Gaillardet J.; Garzanti E.; von Blanckenburg F. | |
发表日期 | 2020 |
ISSN | 0012-8719 |
卷号 | 204 |
英文摘要 | Cosmogenic nuclide analysis in sediment from the Earth's largest rivers yields mean denudation rates of the sediment-producing areas that average out the local variations commonly found in small rivers. Using this approach, we measured in situ cosmogenic 26Al and 10Be in sand of >50 large rivers over a range of climatic and tectonic regimes covering 32% of the Earth's terrestrial surface. In 35% of the analyzed rivers, we find 26Al/10Be ratios significantly lower than these nuclides´ surface-production-rate ratio of 6.75 in quartz, indicating radioactive decay over periods exceeding 0.5 Myr. We invoke a combination of slow erosion, shielding in the source area, and sediment storage and burial during long-distance transport to explain these low ratios. In the other 65% of studied rivers we find 26Al/10Be ratios within uncertainty of their surface production-rate ratio, indicating cosmogenic steady state. For these rivers, we obtain a global source area denudation rate of 141 t/km2×yr (54 mm/kyr of rock-equivalent) that translates to a flux of 3.07 ± 0.56 Gt/yr. By assuming that this sub-dataset is representative of the global land surface, we upscale this value to the total surface area for exorheic basins, thereby obtaining a global denudation flux of 15.2 ± 2.8 Gt/yr that integrates over the past 11 kyr. This value is slightly lower than published values from cosmogenic nuclides from small river basins (23 (+53/−16)) Gt/yr) upscaled using a global slope model, and also lower than modern sediment and dissolved loads exported to the oceans (24.0 Gt/yr). Our new approach confirms an estimate of global dissolved and solid matter transfer that converges to an encouragingly narrow range of within 35%; whereas the use of paired nuclides in large rivers provides estimates of the buffering timescales of sediment transport. © 2020 Elsevier B.V. |
语种 | 英语 |
scopus关键词 | cosmogenic radionuclide; denudation; fluvial deposit; quartz; sediment transport |
来源期刊 | EARTH-SCIENCE REVIEWS |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/209648 |
作者单位 | GFZ German Research Centre for Geosciences, Potsdam, Germany; Institut de Physique du Globe, Paris, France; Department of Earth and Environmental Sciences, Università di Milano-Bicocca, Milano, Italy; Institute of Geological Sciences, Freie Universität Berlin, Germany |
推荐引用方式 GB/T 7714 | Wittmann H.,Oelze M.,Gaillardet J.,et al. A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers[J],2020,204. |
APA | Wittmann H.,Oelze M.,Gaillardet J.,Garzanti E.,&von Blanckenburg F..(2020).A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers.EARTH-SCIENCE REVIEWS,204. |
MLA | Wittmann H.,et al."A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers".EARTH-SCIENCE REVIEWS 204(2020). |
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