Presence of Hummock and Hollow Microtopography Reflects Shifting Balances of Shallow Subsidence and Root Zone Expansion Along Forested Wetland River Gradients
Author:
Funder
U.S. Geological Survey
Publisher
Springer Science and Business Media LLC
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics
Link
https://link.springer.com/content/pdf/10.1007/s12237-023-01227-5.pdf
Reference53 articles.
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2. Brinson, M.M., H.D. Bradshaw, and M.N. Jones. 1985. Transitions in forested wetlands along gradients of salinity and hydroperiod. Journal of the Elisha Mitchell Scientific Society 101: 76–94.
3. Cahoon, D.R., D.J. Reed, and J.W. Day Jr. 1995. Estimating shallow subsidence in microtidal salt marshes of the southeastern United States: Kay and Barghoorn revisited. Marine Geology 128: 1–9. https://doi.org/10.1016/0025-3227(95)00087-F.
4. Cahoon, D.R., J.C. Lynch, B.C. Perez, B. Segura, R.D. Holland, C. Stelly, G. Stephenson, and P. Hensel. 2002. High precision measurements of wetland sediment elevation: II. The rod surface elevation table. Journal of Sedimentary Research 72: 734–739. https://doi.org/10.1306/020702720734.
5. Callaway, J.C., D.R. Cahoon, and J.C. Lynch. 2013. The surface elevation table-marker horizon method for measuring wetland accretion and elevation dynamics. In Methods in biogeochemistry of wetlands, ed. R.D. DeLaune, et al., 901–917. Madison, Wisconsin: Soil Science Society of America. https://doi.org/10.2136/sssabookser10.c46.
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