Dataset for article „Winter atmospheric nutrients and pollutants deposition on West Sayan mountain lakes (Siberia)“
URI (для ссылок/цитирований):
https://elib.sfu-kras.ru/handle/2311/135098Автор:
Diaz-de-Quijano, Daniel
Ageev, Aleksander Vladimirovich
Ivanova, Elena Anatolevna
Anishchenko, Olesia Valerevna
Дата:
2020Table S1. Location and morphological characteristics of the studied lakes in Ergaki Natural Park and land use/land cover percentages of their watersheds in percentage.
Table S2. Raw lake water physicochemical data. 2011 and 2012 observations were obtained from the authors of previous studies (and coauthors of this study). 2015 and 2017 data belong to the present study and were not published before. Note differences in sample depths, including composite samples in 2011 and 2012.
Table S3. Raw physicochemical data of snow core samples. Chemical magnitudes are shown in µg·l-1 and mg·m-2. SCPs are in counts·l⁻¹ and counts·m⁻².
Аннотация:
The world map of anthropogenic atmospheric nitrogen deposition and its effects on natural ecosystems is not described with equal precision everywhere. In this paper, we report atmospheric nutrient, sulphate and spheroidal carbonaceous particles (SCPs) deposition rates, based on snowpack analyses, of a formerly unexplored Siberian mountain region. Then, we discuss their potential effects on lake phytoplankton biomass limitation. We estimate that the nutrient depositions observed in the late season snowpack (40±16 mg NO₃-N·m⁻² and 0.58±0.13 mg TP-P·m⁻²) would correspond to yearly depositions lower than 119±71 mg NO3-N·m⁻²·y⁻¹ and higher than 1.71±0.91 mg TP-P·m⁻²·y⁻¹. These yearly deposition estimates would approximately fit the predictions of global deposition models and correspond to the very low nutrient deposition range although they are still higher than world background values. In spite of the fact that such low atmospheric nitrogen deposition rate would be enough to induce nitrogen limitation in unproductive mountain lakes, phosphorus deposition was also extremely low and the lake water N:P ratio resulted to be unaffected by atmospheric nutrient deposition. In the end, the studied lakes phytoplankton appeared to be hanging on the fence between phosphorus and nitrogen limitation. We conclude that these pristine lakes are fragile sensitive systems exposed to the predicted climate warming, increased winter precipitation, enhanced forest fires and shifts in anthropogenic nitrogen emissions that could finally couple their water chemistry to that of atmospheric nutrient deposition and unlock temperature-inhibited responses of phytoplankton to nutrient shifts.