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      Mercury loading within the Selenga River basin and Lake Baikal, Siberia

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          Legacy impacts of all-time anthropogenic emissions on the global mercury cycle

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            Is Open Access

            Sixty years of environmental change in the world's largest freshwater lake – Lake Baikal, Siberia

            High-resolution data collected over the past 60 years by a single family of Siberian scientists on Lake Baikal reveal significant warming of surface waters and long-term changes in the basal food web of the world's largest, most ancient lake. Attaining depths over 1.6 km, Lake Baikal is the deepest and most voluminous of the world's great lakes. Increases in average water temperature (1.21 °C since 1946), chlorophyll a (300% since 1979), and an influential group of zooplankton grazers (335% increase in cladocerans since 1946) may have important implications for nutrient cycling and food web dynamics. Results from multivariate autoregressive (MAR) modeling suggest that cladocerans increased strongly in response to temperature but not to algal biomass, and cladocerans depressed some algal resources without observable fertilization effects. Changes in Lake Baikal are particularly significant as an integrated signal of long-term regional warming, because this lake is expected to be among those most resistant to climate change due to its tremendous volume. These findings highlight the importance of accessible, long-term monitoring data for understanding ecosystem response to large-scale stressors such as climate change.
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              Increasing Rates of Atmospheric Mercury Deposition in Midcontinental North America

              Mercury contamination of remote lakes has been attributed to increasing deposition of atmospheric mercury, yet historic deposition rates and inputs from terrestrial sources are essentially unknown. Sediments of seven headwater lakes in Minnesota and Wisconsin were used to reconstruct regional modern and preindustrial deposition rates of mercury. Whole-basin mercury fluxes, determined from lake-wide arrays of dated cores, indicate that the annual deposition of atmospheric mercury has increased from 3.7 to 12.5 micrograms per square meter since 1850 and that 25 percent of atmospheric mercury deposition to the terrestrial catchment is exported to the lake. The deposition increase is similar among sites, implying regional or global sources for the mercury entering these lakes.
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                Author and article information

                Journal
                Environmental Pollution
                Environmental Pollution
                Elsevier BV
                02697491
                April 2020
                April 2020
                : 259
                : 113814
                Article
                10.1016/j.envpol.2019.113814
                205cd191-d952-4597-9315-02e5f1aa2c31
                © 2020

                https://www.elsevier.com/tdm/userlicense/1.0/

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