INVESTIGATION OF IMPACTS OF SEA-LEVEL RISE, STORM SURGE AND CLIMATE CHANGE ON MARITIME FORESTS ADJACENT TO CHINCOTEAGUE BAY, VIRGINIA USING DENDROECOLOGY TREE RING ANALYSIS
This research focuses on a site on the mainland shore of Chincoteague Bay, Virginia near Powell’s Creek. Three parallel transects beginning at the shoreline and extending backward away from the coast were sampled using an increment borer. Each transect thus fronted directly on the shoreline of Chincoteague Bay and were susceptible to intense storm surge and saltwater intrusion. At this location, multiple Loblolly Pine, and Eastern Red Cedar trees growing ~1.0m above sea-level have been analyzed, and soil samples taken to assess soil pH patterns. Tree-cores were scanned and uploaded to Image J software to make measurements of tree ring widths and perform statistical analysis.
Although analyses are ongoing, all trees demonstrate similar trends in tree ring growth patterns. Narrower annular growth in tree rings are assumed to have been formed in drier or more stressed years, and years with thicker annular growth are assumed to have been wetter. Soil pH shows a definite trend with more acidic freshwater signatures inland, and higher soil pH values were measured by the shoreline suggesting the influence of marine water is more pronounced. Another observation made in preliminary evaluation is that the tree cores obtained closest to the beach show evidence of thinner tree rings overall (relatively more stressed), most likely due to salt water intrusion or decreased vitality of the freshwater lens. In addition, trees closest to the shoreline also appear to be impacted by higher densities of Pine Bark Beetle burrow damage. It is likely that the trees, which are already stressed, are much more susceptible to beetle infestation and are unable to recover adequately.