Abstract
The interface between maritime forests and inter‐tidal salt marshes along the southeastern coast of the United States is a major ecological boundary characterized by a sequence of botanical zones that typically consist of pine/ oak forest>Iva>Juncus>Salicornia>Spartina. In addition to questions regarding the physical and chemical factors that govern this ecotone, this interface is of interest because of the potential for groundwater flow to transfer nutrients and pollutants from developed uplands to the adjacent marshes. The interface is also of interest because it is presumably migrating upslope as a result of ongoing sea level rise and concomitant aquifer salinization.A new Web site, http://links.baruch.sc.edu/data/GRNDWATER/data/data.htm, contains long‐term and spatially dense measurements of groundwater heads and salinity from a network of nested piezometers that has been installed along three forest‐marsh transects across the Crab Haul Creek finger marsh basin at the North Inlet‐Winyah Bay National Estuarine Research Reserve in Georgetown County South Carolina (Figure 1).
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