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DOI | 10.1073/pnas.1801935115 |
Atmospheric sulfur isotopic anomalies recorded at Mt. Everest across the Anthropocene | |
Lin, Mang; Kang, Shichang; Shaheen, Robina; Li, Chaoliu; Hsu, Shih-Chieh; Thiemens, Mark H. | |
发表日期 | 2018 |
ISSN | 0027-8424 |
卷号 | 115期号:27 |
英文摘要 | Increased anthropogenic-induced aerosol concentrations over the Himalayas and Tibetan Plateau have affected regional climate, accelerated snow/glacier melting, and influenced water supply and quality in Asia. Although sulfate is a predominant chemical component in aerosols and the hydrosphere, the contributions from different sources remain contentious. Here, we report multiple sulfur isotope composition of sedimentary sulfates from a remote freshwater alpine lake near Mount Everest to reconstruct a two-century record of the atmospheric sulfur cycle. The sulfur isotopic anomaly is utilized as a probe for sulfur source apportionment and chemical transformation history. The nineteenthcentury record displays a distinct sulfur isotopic signature compared with the twentieth-century record when sulfate concentrations increased. Along with other elemental measurements, the isotopic proxy suggests that the increased trend of sulfate is mainly attributed to enhancements of dust-associated sulfate aerosols and climate-induced weathering/erosion, which overprinted sulfur isotopic anomalies originating from other sources (e.g., sulfates produced in the stratosphere by photolytic oxidation processes and/or emitted from combustion) as observed in most modern tropospheric aerosols. The changes in sulfur cycling reported in this study have implications for better quantification of radiative forcing and snow/glacier melting at this climatically sensitive region and potentially other temperate glacial hydrological systems. Additionally, the unique Delta S-33-delta S-34 pattern in the nineteenth century, a period with extensive global biomass burning, is similar to the Paleoarchean (3.6-3.2 Ga) barite record, potentially providing a deeper insight into sulfur photochemical/thermal reactions and possible volcanic influences on the Earth's earliest sulfur cycle. |
关键词 | Himalayasmass-independent fractionationaerosolglacierArchean |
学科领域 | Science & Technology - Other Topics |
语种 | 英语 |
WOS研究方向 | Multidisciplinary Sciences |
来源期刊 | PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/111956 |
作者单位 | Univ Calif San Diego, Dept Chem & Biochem, La Jolla, CA 92093 USA |
推荐引用方式 GB/T 7714 | Lin, Mang,Kang, Shichang,Shaheen, Robina,et al. Atmospheric sulfur isotopic anomalies recorded at Mt. Everest across the Anthropocene[J]. 中国科学院西北生态环境资源研究院,2018,115(27). |
APA | Lin, Mang,Kang, Shichang,Shaheen, Robina,Li, Chaoliu,Hsu, Shih-Chieh,&Thiemens, Mark H..(2018).Atmospheric sulfur isotopic anomalies recorded at Mt. Everest across the Anthropocene.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,115(27). |
MLA | Lin, Mang,et al."Atmospheric sulfur isotopic anomalies recorded at Mt. Everest across the Anthropocene".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 115.27(2018). |
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