The effects of nitrogen deposition reduction on nutrient
loading
in freshwaters have been widely studied, especially in remote regions.
However, understanding of the ecological effects is still rather limited.
Herein, we re-estimated nitrogen deposition, both of wet and dry deposition,
in Lake Taihu with monthly monitoring data from 2010 to 2021. Our
results showed that the atmospheric deposition of reactive nitrogen
(namely NH4
+ and NO3
–) in Lake Taihu was 4.94–11.49 kton/yr, which equaled 13.9%–27.3%
of the riverine loading. Dry deposition of NH4
+ and NO3
– contributed 53.1% of the bulk
deposition in Lake Taihu. Ammonium was the main component of both
wet and dry deposition, which may have been due to the strong agriculture-related
activities around Lake Taihu. Nitrogen deposition explained 24.9%
of the variation in phytoplankton community succession from 2010 to
2021 and was the highest among all the environmental factors. Atmospheric
deposition offset the effects of external nitrogen reduction during
the early years and delayed the emergence of nitrogen-fixing cyanobacterial
dominance in Lake Taihu. Our results implied that a decrease in nitrogen
deposition due to a reduction in fertilizer use, especially a decrease
in NH4
+ deposition, could limit diatoms and
promote non-nitrogen-fixing cyanobacterial dominance, followed by
nitrogen-fixing taxa. This result was also applied to other shallow
eutrophic lakes around the middle and lower reaches of the Yangtze
River, where significant reduction of fertilizer use recorded during
the last decades.