Assessing and addressing the re-eutrophication of Lake Erie: Central basin hypoxia
Authors/Creators
- Donald Scavia1
- J. David Allan1
- Kristin K. Arend2
- Steven Bartell3
- Dmitry Beletsky1
- Nate S. Bosch4
- Stephen B. Brandt5
- Ruth D. Briland6
- Irem Daloğlu1
- Joseph V. DePinto7
- David M. Dolan8
- Mary Anne Evans9
- Troy M. Farmer6
- Daisuke Goto10
- Haejin Han11
- Tomas O. Höök12
- Roger Knight13
- Stuart A. Ludsin6
- Doran Mason14
- Anna M. Michalak15
- R. Peter Richards16
- James J. Roberts9
- Daniel K. Rucinski17
- Edward Rutherford14
- David J. Schwab1
- Timothy M. Sesterhenn12
- Hongyan Zhang1
- Yuntao Zhou18
- 1. University of Michigan
- 2. Old Woman Creek National Estuarine Research Reserve
- 3. Cardno ENTRIX
- 4. Grace College
- 5. Oregon State University
- 6. The Ohio State University
- 7. LimnoTech
- 8. University of Wisconsin-Green Bay
- 9. U.S. Geological Survey
- 10. University of Wisconsin-Madison
- 11. Korea Environment Institute
- 12. Purdue University
- 13. Ohio Department of Natural Resources
- 14. Great Lakes Environmental Research Laboratory
- 15. Carnegie Institute for Science
- 16. National Center for Water Quality Research
- 17. LimnoTech and University of Michigan
- 18. Carnegie Institute for Science and University of Michigan
Description
ABSTRACT
Relieving phosphorus loading is a key management tool for controlling Lake Erie eutrophication. During the 1960s and 1970s, increased phosphorus inputs degraded water quality and reduced central basin hypolimnetic oxygen levels which, in turn, eliminated thermal habitat vital to cold-water organisms and contributed to the extirpation of important benthic macroinvertebrate prey species for fishes. In response to load reductions initiated in 1972, Lake Erie responded quickly with reduced water-column phosphorus concentrations, phytoplankton biomass, and bottom-water hypoxia (dissolved oxygen <2 mg/l). Since themid-1990s, cyanobacteria blooms increased and extensive hypoxia and benthic algae returned. We synthesize recent research leading to guidance for addressing this re-eutrophication, with particular emphasis on central basin hypoxia. We document recent trends in key eutrophication-related properties, assess their likely ecological impacts, and develop load response curves to guide revised hypoxia-based loading targets called for in the 2012 Great Lakes Water Quality Agreement. Reducing central basin hypoxic area to levels observed in the early 1990s (ca. 2000 km2) requires cutting total phosphorus loads by 46% from the 2003–2011 average or reducing dissolved reactive phosphorus loads by 78% from the 2005–2011 average. Reductions to these levels are also protective of fish habitat. We provide potential approaches for achieving those new loading targets, and suggest that recent load reduction recommendations focused on western basin cyanobacteria blooms may not be sufficient to reduce central basin hypoxia to 2000 km2.
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