Vibracores through living oyster reefs allow us to measure the age of the reef and examine the environmental history of it's growth. Once opened, the core can be sampled for shell content, grainsize, organic content, and material for radiocarbon dating. Many reefs in NC estuaries have existed in the same location for hundreds of years, building vertically upon old shell to keep up with sea-level rise and prevent sediment burial.
Researchers prepare to sink a core tube into a natural oyster reef located in Ward Creek, NC.
A core tube opened to expose the shell and sediment for sampling and radiocarbon dating.
Measuring elevations and sampling living oysters around a reef in the Rachel Carson Preserve, NC. Living oyster density and growth are not constant across the reef, resulting in differing rates of accretion over the area of the reef, and possibly leading to the elongated shapes these reefs often take.
Researchers collect representative samples of living oysters from different locations around an elongated reef.
Eisemann, E.R., Rodriguez A.B., F. Joel Fodrie (August 2025) Investigating oyster-reef morphodynamics to optimize nature-based infrastructure. US Coastal Research Program In Progress Review. Oral Presentation.
Eisemann, E.R., Rodriguez, A.B. (December 2024) Transition of oyster reefs from subtidal to intertidal under conditions of sea-level rise and land use change. Poster presentation at the 2024 AGU Annual Meeting. Washington D.C.
Eisemann, E.R., Rodriguez, A.B. (December 2023) Natural intertidal oyster reef loss due to marsh encroachment. Oral presentation at the 2023 AGU Annual Meeting. San Francisco, CA. https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1302664