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USF scientists announce initial findings from Piney Point research effort

University of South Florida College of Marine Science researchers today shared their initial findings of how the Tampa Bay ecosystem has responded to the controlled discharges of nutrient-rich wastewater released from the retired Piney Point fertilizer processing plant. The scientists launched their first research cruise on April 7 and have returned to the water several times since.

Key takeaways from the USF research team:

  • Early results indicate that the effects of the wastewater discharge were localized in nature, not widespread.
  • Concentrations of nutrients have declined over time and are now more typical of those in the historical record for this part of Tampa Bay. Model results show that the concentrations of nutrients within the discharged water have been diluted at least 1000-fold since the initial release.
  • A diatom bloom of about 25 square kilometers in size around Port Manatee that formed in response to the discharge has dissipated over time. Diatoms are single-celled microalgae called phytoplankton. Chlorophyll concentrations (a proxy for phytoplankton biomass) are within the range generally observed in Tampa Bay during April and May.

Remaining unanswered questions for researchers:

  • Are longer-term impacts of the discharged water on the Tampa Bay ecosystem likely to be manifested? If so, how?
  • The nutrient chemistry of Tampa Bay is complex. Questions remain about nutrient cycling in response to a rapid influx of wastewater. For example:
  • Were nutrients and heavy metals (e.g., lead, copper, zinc) from the discharge sequestered in the sediments? If so, will storms stimulate phytoplankton blooms?
  • Will there be an impact to seagrasses and other marine life that live on the bottom?
  • What may have been the impact to fish health?

“The area in the immediate vicinity of Port Manatee was subject to a spike in nutrient concentrations and a corresponding increase in phytoplankton abundance,” College of Marine Science Dean Tom Frazer said. “Our initial field sampling efforts and data acquired from remote sensing platforms confirmed high concentrations of chlorophyll, which is a proxy for phytoplankton abundance. Recent data indicate, however, that the response was short lived. Phytoplankton abundance continues to decline and water chemistry values are typical of those reported in the historical record.”

The field team, led by USF chemical oceanographer Kristen Buck collected water and sediment samples from a suite of stations in the vicinity of Port Manatee and locations beyond the affected area. The sampling and subsequent data analyses confirmed that the phytoplankton responded quickly to the nutrient pulse, but the assemblage was dominated by diatoms and not toxic phytoplankton responsible for red tides. The algal bloom has since dissipated. The end of the algae bloom was confirmed in satellite imagery analyzed by physical oceanographer Chuanmin Hu.

The team’s sampling efforts were guided by a model provided by physical oceanographer Bob Weisberg. The model forecasts the movement of discharged water and its constituents based on tides, winds and river input.