Cite
Foraminiferal and Sedimentary Record of Late Holocene Barrier Island Evolution, Pea Island, North Carolina: The Role of Storm Overwash, Inlet Processes, and Anthropogenic Modification.
MLA
Culver, Stephen J., et al. “Foraminiferal and Sedimentary Record of Late Holocene Barrier Island Evolution, Pea Island, North Carolina: The Role of Storm Overwash, Inlet Processes, and Anthropogenic Modification.” Journal of Coastal Research, vol. 22, no. 4, July 2006, pp. 836–46. EBSCOhost, https://doi.org/10.2112/03-0103.1.
APA
Culver, S. J., Ames, D. V., Corbett, D. R., Mallinson, D. J., Riggs, S. R., Smith, C. G., & Vance, D. J. (2006). Foraminiferal and Sedimentary Record of Late Holocene Barrier Island Evolution, Pea Island, North Carolina: The Role of Storm Overwash, Inlet Processes, and Anthropogenic Modification. Journal of Coastal Research, 22(4), 836–846. https://doi.org/10.2112/03-0103.1
Chicago
Culver, Stephen J., Dorothea V. Ames, D. Reide Corbett, David J. Mallinson, Stanley R. Riggs, Christopher G. Smith, and David J. Vance. 2006. “Foraminiferal and Sedimentary Record of Late Holocene Barrier Island Evolution, Pea Island, North Carolina: The Role of Storm Overwash, Inlet Processes, and Anthropogenic Modification.” Journal of Coastal Research 22 (4): 836–46. doi:10.2112/03-0103.1.