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• W2028262882 endingPage "379" @default.
• W2028262882 startingPage "359" @default.
• W2028262882 abstract "Biogeochemical dynamics under seasonal ice cover were investigated in the shallow (<10 m) water column of highly productive Georgetown Lake, western Montana, USA. This high altitude (1,800 m) reservoir is well-mixed in summer, but becomes strongly stratified under ice cover (mid-November–mid-May). A rapid drop in dissolved oxygen (DO) concentration and rise in dissolved inorganic carbon (DIC) concentration was observed after the onset of ice, with a corresponding increase in δ18O-DO and decrease in δ13C-DIC, likely caused by respiration (R) of organic carbon. Photosynthesis/respiration ratios (P/R) estimated from simultaneous measurement of DO and δ18O-DO were near unity prior to ice formation but then systematically decreased with time and depth in the lake under ice cover. P/R in the water column was higher at a shallower monitoring site compared to a deeper site near the dam outlet, which may have been important for over-winter survival of salmonids. By March, the bottom 3 m of the water column at both sites was anoxic, with the bottom 1 m being euxinic. Elevated concentrations of dissolved sulfide, ammonium, phosphate, Fe2+, and Mn2+ in deep water suggest coupling of organic carbon degradation with reduction of a number of electron acceptors (e.g., Fe3+, $${text{NO}}_{3}^{ - } ,;{text{SO}}_{4}^{2 - }$$ ). The concentrations and δ34S values of H2S in the deep water and $${text{SO}}_{4}^{2 - }$$ in the shallow water were similar, indicating near-complete reduction of sulfate in the euxinic zone. Late in the winter, an influx of isotopically heavy DIC was noted in the deep water coincident with a buildup of dissolved CH4 to concentrations >1 mM. These trends are attributed to acetoclastic methanogenesis in the benthic sediments. This pool of dissolved CH4 was likely released from the lake to the atmosphere during spring ice-off and lake turnover." @default.
• W2028262882 created "2016-06-24" @default.
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• W2028262882 date "2014-06-28" @default.
• W2028262882 modified "2023-10-10" @default.
• W2028262882 title "Stable isotopes track biogeochemical processes under seasonal ice cover in a shallow, productive lake" @default.
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• W2028262882 cites W1964373009 @default.
• W2028262882 cites W1965414173 @default.
• W2028262882 cites W1966396852 @default.
• W2028262882 cites W1966680325 @default.
• W2028262882 cites W1966929556 @default.
• W2028262882 cites W1967968324 @default.
• W2028262882 cites W1973441434 @default.
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• W2028262882 cites W1986674931 @default.
• W2028262882 cites W1988288219 @default.
• W2028262882 cites W1988731088 @default.
• W2028262882 cites W1989662389 @default.
• W2028262882 cites W1993554541 @default.
• W2028262882 cites W1994360423 @default.
• W2028262882 cites W1995772381 @default.
• W2028262882 cites W1997685178 @default.
• W2028262882 cites W1997774861 @default.
• W2028262882 cites W1998980067 @default.
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• W2028262882 cites W2022136159 @default.
• W2028262882 cites W2022233734 @default.
• W2028262882 cites W2022354197 @default.
• W2028262882 cites W2030699273 @default.
• W2028262882 cites W2032854853 @default.
• W2028262882 cites W2035985368 @default.
• W2028262882 cites W2039248536 @default.
• W2028262882 cites W2044127701 @default.
• W2028262882 cites W2044725720 @default.
• W2028262882 cites W2045047668 @default.
• W2028262882 cites W2045458102 @default.
• W2028262882 cites W2050839188 @default.
• W2028262882 cites W2054436302 @default.
• W2028262882 cites W2058653258 @default.
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• W2028262882 cites W2072191315 @default.
• W2028262882 cites W2082786725 @default.
• W2028262882 cites W2082916169 @default.
• W2028262882 cites W2084026036 @default.
• W2028262882 cites W2088901620 @default.
• W2028262882 cites W2093579001 @default.
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• W2028262882 cites W2112478326 @default.
• W2028262882 cites W2120052366 @default.
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• W2028262882 cites W2132641762 @default.
• W2028262882 cites W2138812961 @default.
• W2028262882 cites W2139074555 @default.
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• W2028262882 doi "https://doi.org/10.1007/s10533-014-0005-z" @default.
• W2028262882 hasPublicationYear "2014" @default.
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