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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.
Afiliación
  • Lin M; Department of Chemistry and Biochemistry, University of California, San Diego, La Jolla, CA 92093; manglin.ucsd@gmail.com mthiemens@ucsd.edu.
  • Kang S; Research Center for Environmental Changes, Academia Sinica, Taipei 115, Taiwan.
  • Shaheen R; State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000 Lanzhou, China.
  • Li C; Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, 100101 Beijing, China.
  • Hsu SC; University of Chinese Academy of Sciences, 100049 Beijing, China.
  • Thiemens MH; Department of Chemistry and Biochemistry, University of California, San Diego, La Jolla, CA 92093.
Proc Natl Acad Sci U S A ; 115(27): 6964-6969, 2018 07 03.
Article en En | MEDLINE | ID: mdl-29915076
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 nineteenth-century 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 Δ33S-δ34S 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.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Isótopos de Azufre / Aire Idioma: En Revista: Proc Natl Acad Sci U S A Año: 2018 Tipo del documento: Article Pais de publicación: Estados Unidos

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Isótopos de Azufre / Aire Idioma: En Revista: Proc Natl Acad Sci U S A Año: 2018 Tipo del documento: Article Pais de publicación: Estados Unidos