Paerl Hans W, Xu Hai, Hall Nathan S, Zhu Guangwei, Qin Boqiang, Wu Yali, Rossignol Karen L, Dong Linghan, McCarthy Mark J, Joyner Alan R
Institute of Marine Sciences, The University of North Carolina at Chapel Hill, Morehead City, North Carolina, United States of America.
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing, PR China.
PLoS One. 2014 Nov 18;9(11):e113123. doi: 10.1371/journal.pone.0113123. eCollection 2014.
Excessive anthropogenic nitrogen (N) and phosphorus (P) inputs have caused an alarming increase in harmful cyanobacterial blooms, threatening sustainability of lakes and reservoirs worldwide. Hypertrophic Lake Taihu, China's third largest freshwater lake, typifies this predicament, with toxic blooms of the non-N2 fixing cyanobacteria Microcystis spp. dominating from spring through fall. Previous studies indicate N and P reductions are needed to reduce bloom magnitude and duration. However, N reductions may encourage replacement of non-N2 fixing with N2 fixing cyanobacteria. This potentially counterproductive scenario was evaluated using replicate, large (1000 L), in-lake mesocosms during summer bloom periods. N+P additions led to maximum phytoplankton production. Phosphorus enrichment, which promoted N limitation, resulted in increases in N2 fixing taxa (Anabaena spp.), but it did not lead to significant replacement of non-N2 fixing with N2 fixing cyanobacteria, and N2 fixation rates remained ecologically insignificant. Furthermore, P enrichment failed to increase phytoplankton production relative to controls, indicating that N was the most limiting nutrient throughout this period. We propose that Microcystis spp. and other non-N2 fixing genera can maintain dominance in this shallow, highly turbid, nutrient-enriched lake by outcompeting N2 fixing taxa for existing sources of N and P stored and cycled in the lake. To bring Taihu and other hypertrophic systems below the bloom threshold, both N and P reductions will be needed until the legacy of high N and P loading and sediment nutrient storage in these systems is depleted. At that point, a more exclusive focus on P reductions may be feasible.
过多的人为氮(N)和磷(P)输入导致有害蓝藻水华惊人地增加,威胁着全球湖泊和水库的可持续性。中国第三大淡水湖太湖富营养化,就是这种困境的典型代表,从春季到秋季,非固氮蓝藻微囊藻属的有毒水华占据主导。先前的研究表明,需要减少氮和磷以降低水华的规模和持续时间。然而,减少氮可能会促使固氮蓝藻取代非固氮蓝藻。在夏季水华期间,使用重复的大型(1000升)湖泊中宇宙对此潜在的适得其反的情况进行了评估。添加氮和磷导致浮游植物产量最高。促进氮限制的磷富集导致固氮类群(鱼腥藻属)增加,但并未导致非固氮蓝藻被固氮蓝藻显著取代,固氮率在生态上仍然微不足道。此外,相对于对照,磷富集未能增加浮游植物产量,表明在此期间氮是最具限制作用的养分。我们认为,微囊藻属和其他非固氮属可以通过在湖泊中储存和循环的现有氮和磷来源方面胜过固氮类群,从而在这个浅水、高浊度、富营养化的湖泊中保持优势。为了使太湖和其他富营养化系统低于水华阈值,需要同时减少氮和磷,直到这些系统中高氮和磷负荷以及沉积物养分储存的遗留问题耗尽。到那时,更专注于减少磷可能是可行的。