2018
DOI: 10.1016/j.scitotenv.2017.12.348
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Internal phosphorus loading from sediments causes seasonal nitrogen limitation for harmful algal blooms

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Cited by 247 publications
(90 citation statements)
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“…Support for this hypothesis occurs if water or summer air temperature is an important predictor of HABs with a positive drift coefficient. Longer summer : Longer seasons of high temperature increase the opportunity for cyanobacterial growth (Anneville et al ; Deng et al ; Visser et al ). Support for this hypothesis occurs if spring air temperature is an important predictor of HABs with a positive drift coefficient. Internal phosphorus loading : Higher temperature increases the rate of internal phosphorus loading, driving HABs (Jeppesen et al ; Matisoff et al ; Orihel et al ; Ding et al ). Support for this hypothesis occurs if water or summer air temperature is an important predictor of TP with a positive drift coefficient, and TP is an important predictor of HABs with a positive drift coefficient. Load driving : Greater precipitation amounts increase nutrient loading, driving HABs (Reichwaldt and Ghadouani ; Michalak et al ).…”
Section: Methodsmentioning
confidence: 99%
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“…Support for this hypothesis occurs if water or summer air temperature is an important predictor of HABs with a positive drift coefficient. Longer summer : Longer seasons of high temperature increase the opportunity for cyanobacterial growth (Anneville et al ; Deng et al ; Visser et al ). Support for this hypothesis occurs if spring air temperature is an important predictor of HABs with a positive drift coefficient. Internal phosphorus loading : Higher temperature increases the rate of internal phosphorus loading, driving HABs (Jeppesen et al ; Matisoff et al ; Orihel et al ; Ding et al ). Support for this hypothesis occurs if water or summer air temperature is an important predictor of TP with a positive drift coefficient, and TP is an important predictor of HABs with a positive drift coefficient. Load driving : Greater precipitation amounts increase nutrient loading, driving HABs (Reichwaldt and Ghadouani ; Michalak et al ).…”
Section: Methodsmentioning
confidence: 99%
“…This occurs through increased growth rates of harmful cyanobacterial species relative to other species (Paerl and Huisman ; Carey et al ; Visser et al ), through extending of the summer growing season (Anneville et al ; Deng et al ; Visser et al ) and through increased vertical stratification resulting in greater fitness by cyanobacteria that are able to regulate their buoyancy (Wagner and Adrian ; Carey et al ; Posch et al ; Taranu et al ; Visser et al ). Higher temperature also increases internal phosphorus loading from sediments through increased rates of soil diffusivity and increased rates of soil phosphorus regeneration (Matisoff et al ), and this internal phosphorus source has been shown be a significant proportion of the overall phosphorus budget in some lakes (Jeppesen et al ; Ho and Michalak ; Orihel et al ; Ding et al ). Second, greater overall precipitation and more extreme precipitation events are hypothesized to increase HABs through the generation of greater nutrient runoff (Reichwaldt and Ghadouani ; Michalak et al ), although this could be balanced by greater precipitation flushing nutrient‐rich waters out of the ecosystem prior to bloom formation (Anderson et al ; Reichwaldt and Ghadouani ).…”
mentioning
confidence: 99%
“…However, bioavailable phosphorus could be supplemented when required by enzymatic hydrolysis of EHP. There are numerous nutrient supplementation pathways for freshwater lakes, such as nitrogen fixation from the atmosphere (Jean, Cassar, Setzer, & Bellenger, ), release of nutrients from sediments (Cao, Wang, He, Luo, & Zheng, ; Ding et al., , ), and microbial activity (Bai et al., ). Recent study indicated that Fe‐P‐S system in water–sediment interface has great impacts on phosphorus circulation in aquatic systems (Chen et al., ).…”
Section: Resultsmentioning
confidence: 99%
“…In addition, this process decreased the pore water soluble Fe(II), overlying water soluble Fe(II) and DGT-labile Fe by 16% ( Figure 6). The newly formed Fe(III) oxyhydroxides adsorbed SRP and DGTlabile P from overlying water and sediments (Einsele 1936;Søndergaard et al 2003;Ding et al 2018;Giles et al 2016), fixed the P into sediment as NaOH-P (Chen et al 2015;Lewandowski et al 2007), decreased the SRP and DGT-labile P concentrations in overlying water and sediments (Figures 2, 3), and increased the NaOH-P in the surface 0-0.5 cm sediments ( Figure 5). Moreover, the R value in the aerobic sediments was lower than that in the control sediments (Table 2), indicating that the SRP replenishment abilities of sediment particles in the aerobic group were lower than those of the control group (Harper et al 1998).…”
Section: Discussionmentioning
confidence: 99%