Abstract

Diversion of river waters to adjacent estuaries may occur during wetland restoration, navigation channel development, or storms. We proposed that diversions of nitrogen- and phosphorus-enriched waters from the river to estuarine waters would result in increased phytoplankton biomass and shifts to noxious or harmful algal blooms. We tested this hypothesis by conducting four seasonal microcosm experiments in which Mississippi River water was mixed at different volume ratios with ambient estuarine waters of three lakes in the upper Barataria Basin, Louisiana, USA. These lakes included two brackish lakes that were in the path of diverted Mississippi River water, and a freshwater lake that was not. The results from the 3- to 8-day experiments yielded a predictable increase in phytoplankton biomass related to nutrient additions from Mississippi River water. The subsequent decreases in the dissolved nitrate + nitrite, soluble reactive phosphorus, and silicate concentrations explained 76 to 86% of the increase in chlorophyll a concentrations in the microcosms. Our experiments showed that cyanobacteria can successfully compete with diatoms for N and P resources even under non-limiting Si conditions and that toxic cyanobacteria densities can increase to bloom levels with increased Mississippi River water inputs to ambient waters in the microcosms. Diversions of Mississippi River into adjacent estuarine waters should be considered in relation to expected and, possibly, unexpected changes in phytoplankton communities to the receiving waters and coastal ecosystems.

Highlights

  • Eutrophication is symptomatic of estuaries with relatively long water residence times and nutrient enrichment (Rabalais, 2004)

  • Our experiments showed that cyanobacteria can successfully compete with diatoms for N and P resources even under non-limiting Si conditions and that toxic cyanobacteria densities can increase to bloom levels with increased Mississippi River water

  • The higher coefficient of determination (R2) between the chlorophyll a (Chla) increase and decrease of DIN (dDIN) compared to dP and dSi indicated a stronger role for N on the phytoplankton growth compared to soluble reactive phosphorus (SRP) and Si

Read more

Summary

Introduction

Eutrophication is symptomatic of estuaries with relatively long water residence times and nutrient enrichment (Rabalais, 2004). Understanding the dynamic relationships between nutrient enrichment and phytoplankton growth is an important goal to accurately predict, manage, and, perhaps, reverse eutrophication. Assessing and predicting the consequences of eutrophication can be complicated by the various nutrient quantities and their ratios, the timing of the nutrient loadings, and the complex suite of other environmental factors and trophic interactions in receiving basins (Glibert et al, 2010). The nutrient(s) limiting phytoplankton growth in estuarine and coastal waters, for example, may include N, P, or Si limitation, as well as co-limitation (Turner et al, 1990; Sylvan et al, 2006; Ren et al, 2009; Turner & Rabalais, 2013; Paerl et al, 2016). The internal biological interactions and nutrient regeneration vary in different aquatic systems and, their responses to external nutrient inputs may differ

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call