GEOCHRONOLOGY OF THE VIRGINIA COASTAL PLAIN: A REVIEW OF AGES, TECHNIQUES, AND CORE SAMPLING FOR LUMINESCENCE DATING
We provide a review of geochronological techniques that are best suited for inland Coastal Plain, barrier island, and shallow-water shelf materials (i.e., clastic sediments, carbonates, and fossils). The dating techniques covered will include: trapped charge (luminescence and electron spin resonance), radiocarbon, cosmogenic radionuclide, amino acid racemization, Uranium-series, and paleomagnetism.
Much of the Coastal Plain is low-relief and subsurface investigations rely on drilling and coring for sample collection. When targeting core samples for luminescence dating, two important factors relate to the integrity of the natural luminescence signal and the representation of the dose rate environment. The equivalent dose sample should remain light-safe such that the burial dose is not reset (zeroed) by light exposure, and the sediment sampled for dose rate must accurately represent all units within at least 15 cm above and below the equivalent dose sample. Examples and discussion of guidelines for sampling sediment core for luminescence dating are discussed, and preferred protocols are dependent on the extraction method, sedimentology, core integrity, and storage conditions.