GEOCHEMISTRY AND STABLE ISOTOPES OF A EUTROPHIC LAKE IN WESTERN MONTANA, USA
By mid-winter, two sampling sites had established a robust vertical profile with the following characteristics: a) a rapid lowering of DO concentration to values near zero about 2 to 3 m above the bottom, with a 3 to 7 ‰ increase in δ18O-DO; b) an increase in alkalinity, CO2 partial pressure, and dissolved inorganic carbon (DIC) with depth, with a 2 ‰ decrease in δ13C-DIC; and c) an increase in ammonium, H2S, silica, phosphate, Ca2+, Mn2+ and Fe2+ towards the lake bottom. These trends are explained by a combination of aerobic and anaerobic respiration, coupled with dissolution of calcite in lake sediment. The shallower of the two sampling sites had higher DO concentrations and a less steep slope of δ18O-DO vs. DO concentration, suggesting that below-ice photosynthesis was partly offsetting consumption of DO by respiration. Photosynthetic, purple, H2S-oxidizing bacteria were observed at the shallow site (6 m), but not at the deeper site (10 m). Interestingly, the δ13C-DIC of the deeper samples at the shallow site shifted several ‰ to more positive values late in the winter, with continued increase in DIC concentration. This observation is tentatively attributed to fermentative breakdown of organic matter to isotopically-heavy DIC and isotopically-light dissolved organic carbon (DOC). The water column of the entire lake became completely mixed shortly after ice-off in late May of 2011, and is normally mixed and well-oxygenated throughout the unfrozen months due to high winds.
The ability of photosynthesis to continue in certain portions of the lake during the 6+ months of ice cover could well be a critical reason why fish survive the winter season in Georgetown Lake. However, the lake is near an ecological tipping-point, and is vulnerable to increased residential development and associated nutrient loads.