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DOI | 10.1038/s41561-021-00714-3 |
Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion | |
Bufe A.; Hovius N.; Emberson R.; Rugenstein J.K.C.; Galy A.; Hassenruck-Gudipati H.J.; Chang J.-M. | |
发表日期 | 2021 |
ISSN | 17520894 |
起始页码 | 211 |
结束页码 | 216 |
卷号 | 14期号:4 |
英文摘要 | Global climate is thought to be modulated by the supply of minerals to Earth’s surface. Whereas silicate weathering removes carbon dioxide (CO2) from the atmosphere, weathering of accessory carbonate and sulfide minerals is a geologically relevant source of CO2. Although these weathering pathways commonly operate side by side, we lack quantitative constraints on their co-variation across erosion rate gradients. Here we use stream-water chemistry across an erosion rate gradient of three orders of magnitude in shales and sandstones of southern Taiwan, and find that sulfide and carbonate weathering rates rise with increasing erosion, while silicate weathering rates remain steady. As a result, on timescales shorter than marine sulfide compensation (approximately 106–107 years), weathering in rapidly eroding terrain leads to net CO2 emission rates that are at least twice as fast as CO2 sequestration rates in slow-eroding terrain. We propose that these weathering reactions are linked and that sulfuric acid generated from sulfide oxidation boosts carbonate solubility, whereas silicate weathering kinetics remain unaffected, possibly due to efficient buffering of the pH. We expect that these patterns are broadly applicable to many Cenozoic mountain ranges that expose marine metasediments. © 2021, The Author(s). |
英文关键词 | carbon dioxide; Cenozoic; chemical reaction; chemical weathering; erosion rate; metasediment; phyllosilicate; silicate; solubility; sulfide; sulfuric acid; Taiwan |
语种 | 英语 |
来源期刊 | Nature Geoscience
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/206870 |
作者单位 | GFZ German Research Centre for Geosciences, Telegrafenberg, Potsdam, Germany; Institute of Geosciences, University of Potsdam, Potsdam, Germany; NASA Goddard Space Flight Center, Greenbelt, MD, United States; Department of Geosciences, Colorado State University, Fort Collins, CO, United States; Centre de Recherches Pétrographiques et Géochimiques, CNRS, Université de Lorraine, Nancy, France; Jackson School of Geosciences, University of Texas at Austin, Austin, TX, United States; Department of Geosciences, National Taiwan University, Taipei, Taiwan |
推荐引用方式 GB/T 7714 | Bufe A.,Hovius N.,Emberson R.,et al. Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion[J],2021,14(4). |
APA | Bufe A..,Hovius N..,Emberson R..,Rugenstein J.K.C..,Galy A..,...&Chang J.-M..(2021).Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion.Nature Geoscience,14(4). |
MLA | Bufe A.,et al."Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion".Nature Geoscience 14.4(2021). |
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