Taylor Mattioli, Dr. Stacy Endriss, Dr. Devon Eulie
The invasive grass Phragmites australis subsp. australis (hereafter ‘Phragmites’) negatively affects marsh ecosystems by outcompeting native vegetation, reducing fish and waterfowl habitat, altering biogeochemical cycles, increasing fire risk, and reducing the aesthetic value. Further, widespread attempts to reduce Phragmites through physical and chemical removal techniques often fail to reduce its abundance and may harm native ecosystems more than leaving Phragmites unmanaged. Phragmites may also provide beneficial ecosystem services that increase coastal resiliency, including sediment accretion, soil stabilization. and carbon sequestration. Thus, understanding whether the benefits of managing Phragmites outweigh its risk is critical to effective management. In today’s world of increasing sea level rise (SLR) and global change, this approach requires understanding of both the relative costs-benefits of Phragmites vs. its management and of Phragmites compared to the desired management outcome—restored native plant communities. Coastal North Carolina is well suited for investigating these tradeoffs, as increasing coastal resiliency and managing Phragmites, which often outcompetes diverse native Spartina alterniflora (hereafter ‘Spartina’), are both state-wide priorities.
The objective of this research is to investigate how the performance of and ecosystem services provided by Phragmites vs. Spartina are affected by Phragmites management SLR and salinity. To this end, we ask:
Do SLR and increasing salinity differentially affect Phragmites vs. Spartina performance?
Does Phragmites provide more beneficial ecosystems services (i.e., carbon sequestration and accretion) than Spartina in the face of predicted global change (i.e., SLR and increasing salinity)?
Figure 1: A simplified diagram of the "marsh organs" installed at each site. Different levels mimic sea level rise.
Figure 2: Map of where marsh organs were installed. Our sites occur along a salinity gradient, with Site 1 representing low salinity (<0.5 ppt), Site 2 representing medium salinity (0.5-30 ppt), and Site 3 (>30 ppt) representing high salinity.
Three sites have been established along the lower Cape Fear River that span a low (<0.5 ppt), medium (0.5-30 ppt), and high (>30 ppt) salinity gradient. At each site, two marsh organs have been built, one with soil from managed stands of Phragmites and one with soil from unmanaged stands of Phragmites. Each organ will represent four elevation levels: current marsh elevation (0 in.) and three commonly predicted regional SLR scenarios (2.4 in., 5.8 in., and 6.8 in. by 2045). Each elevation level will include six 10-cm PVC pipe mesocosms, three with Phragmites propagules and three with Spartina propagules. We will measure plant height and stem density biweekly until November 2023, when we will harvest, dry, and weight aboveground and belowground biomass. We will also measure soil stabilization as the density of belowground growth, calculated by dividing belowground biomass by the mesocosm volume. Using mass spectrometry, we will measure the carbon content of 1 soil sample from each mesocosm to estimate carbon sequestration.
Lead PI: Taylor Mattioli (Student UNCW)
Co-PI: Dr. Stacy Endriss and Dr. Devon Eulie (UNCW)
This study is being conducted by researchers or receiving funding from: