Kunshan Bao , Weidan Shen , Zhongle Zhou , Yang Gao
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引用次数: 0
Abstract
Quantitatively distinguishing the historical record of potentially harmful trace element (PHTE) pollution in alpine wetland sediments enables an understanding of the nature and scale of Anthropocene human impact. In this study, we present PHTE and stable isotope (Pb and Hg) records for a sediment core from Jiulongchi wetland, Fanjing Mountain, southwest China. We calculate the chemical index of alteration and enrichment factors, and conduct multivariate statistics to reveal that the PHTEs in these wetland sediments were mainly regulated by weathering and erosion processes, as well as organic matter content. The pollution history for the last 1300 years is reconstructed from stable Pb and Hg isotopes, PHTE enrichment factors and accumulation rates. Coal combustion is shown to be a major anthropogenic source for PHTE input into the wetland, commencing in the 1940s and amplified during the 1950s. The research findings reflect the pattern of anthropogenic environmental changes in a remote tourist-hotspot area, which can aid in formulating policies to achieve a sustainable and environmentally healthy future for a vulnerable but important ecosystem.
AnthropoceneEarth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
6.30
自引率
0.00%
发文量
27
审稿时长
102 days
期刊介绍:
Anthropocene is an interdisciplinary journal that publishes peer-reviewed works addressing the nature, scale, and extent of interactions that people have with Earth processes and systems. The scope of the journal includes the significance of human activities in altering Earth’s landscapes, oceans, the atmosphere, cryosphere, and ecosystems over a range of time and space scales - from global phenomena over geologic eras to single isolated events - including the linkages, couplings, and feedbacks among physical, chemical, and biological components of Earth systems. The journal also addresses how such alterations can have profound effects on, and implications for, human society. As the scale and pace of human interactions with Earth systems have intensified in recent decades, understanding human-induced alterations in the past and present is critical to our ability to anticipate, mitigate, and adapt to changes in the future. The journal aims to provide a venue to focus research findings, discussions, and debates toward advancing predictive understanding of human interactions with Earth systems - one of the grand challenges of our time.