Proceedings of the Fourth Caldwell Conference, St. Catherines Island, Georgia, March 27-29, 2009.

391 p. : ill. (chiefly col.), maps (chiefly col.) ; 26 cm. "Issued March 23, 2011."This edited volume addresses the geoarchaeology of St. Catherines Island (Georgia). The field of geoarchaeology has typically been defined as either geology pursued within an archaeological framework or (sometimes the reverse) as archaeology framed with the help of geological methodology. Either way, the formalized objectives of geoarchaeology define a broad range of pursuits, from placing archaeological sites into relative and absolute temporal context through the application of stratigraphic principles and absolute dating techniques, to understanding the natural processes of site formation, to reconstructing the landscapes that existed around a site or group of sites at the time of occupation. The editors of this volume have generally followed the lead of G.R. Rapp and C.L. Hill (2006, Geoarchaeology : the earth-science approach to archaeological interpretation) by stressing the importance of multiple viewpoints and methodologies in applying geoscience techniques to evaluate the archaeological record. In the broadest sense, then, Geoarchaeology of St. Catherines Island applies multiple earth science concepts, techniques, or knowledge bases to the known archaeological record and the processes that created that record. This volume consists of 16 papers presenting the newest research on the stratigraphic and geomorphological evolution of the St. Catherines Island landscape. Of particular interest are presentations addressing the relative timing and nature of sedimentation, paleobiology, sea level change, stream capture, hydrology, and erosional patterning evident on St. Catherines Island (and to some degree the rest of the Georgia Bight). These papers were initially presented at the Fourth Caldwell Conference, cosponsored by the American Museum of Natural History and the St. Catherines Island Foundation, held on St. Catherines Island (Georgia), March 27-29, 2009. Table of contents: Why this archaeologist cares about geoarchaeology : some pasts and futures of St. Catherines Island / David Hurst Thomas -- Evolution of late Pleistocene-Holocene climates and environments of St. Catherines Island and the Georgia Bight / Fredrick J. Rich, Anthony Vega, and Frank J. Vento -- Geoarchaeological research at St. Catherines Island : defining the geological foundation / Gale A. Bishop, Brian K. Meyer, R. Kelly Vance, and Fredrick J. Rich -- Development of a late Pleistocene-Holocene genetic stratigraphic framework for St. Catherines Island : archaeological implications / Frank J. Vento and Patty A. Stahlman -- Ichnological diagnosis of ancient storm-washover fans, Yellow Banks Bluff, St. Catherines Island / Anthony J. Martin and Andrew K. Rindsberg -- Quaternary vegetation and depositional history of St. Catherines Island / Fredrick J. Rich and Robert K. Booth -- Recent shoreline erosion and vertical accretion patterns, St. Catherines Island / Donald B. Potter Jr. -- Role of storm events in beach ridge formation, St. Catherines Island / Harold B. Rollins, Kathi Beratan, and James E. Pottinger -- Drainage changes at Ossabaw, St. Catherines, and Sapelo sounds and their influence on island morphology and spit building on St. Catherines Island / Timothy M. Chowns -- Vibracores and vibracore transects : constraining the geological and cultural history of St. Catherines Island / Gale A. Bishop, David Hurst Thomas, Matthew C. Sanger, Brian K. Meyer, R. Kelly Vance, Robert K. Booth, Fredrick J. Rich, Donald B. Potter, and Timothy Keith-Lucas -- Application of ground penetrating radar to investigations of the stratigraphy, structure, and hydrology of St. Catherines Island / R. Kelly Vance, Gale A. Bishop, Fredrick J. Rich, Brian K. Meyer, and Eleanor J. Camann -- Postsettlement dispersal and dynamic repopulation of estuarine habitats by adult Mercenaria mercenaria, St. Catherines Island / Robert S. Prezant, Harold B. Rollins, and Ronald B. Toll -- The foundation for sea turtle geoarchaeology and zooarchaeology : morphology of recent and ancient sea turtle nests, St. Catherines Island, Georgia, and Cretaceous Fox Hills Sandstone, Elbert County, Colorado / Gale A. Bishop, Fredric L. Pirkle, Brian K. Meyer, and William A. Pirkle -- Sea turtle habitat deterioration on St. Catherines Island : defining the modern transgression / Gale A. Bishop and Brian K. Meyer -- Modeling indigenous hunting and harvesting of sea turtles and their eggs on the Georgia Coast / Gale A. Bishop, David Hurst Thomas, and Brian K. Meyer -- Geomorphology, sea level, and marine resources : St. Catherines Island / Harold B. Rollins and David Hurst Thomas -- Appendix 1. Noncultural radiocarbon record from St. Catherines Island : a compendium -- Appendix 2. Vibracore record from St. Catherines Island : a compendium.Conference sponsored by the American Museum of Natural History and the St. Catherines Island Foundation

Unravelling Phanerozoic evolution of radial to rosette trace fossils

Feeding trace fossils, produced by either deposit or detritus feeders and showing radial to rosetted morphology, are all included in the same architectural category. These radial to rosette ichnofossils are widely recorded worldwide throughout the Phanerozoic and have attracted the attention of numerous ichnologists for decades. Construction of a database summarizing occurrences of radial to rosette trace fossils through the Phanerozoic shows that representatives of this category occurred for the first time during the Fortunian, which accounts for the appearance of at least 12% of the total number of ichnogenera in this category. Overall, 32% of all known rosette ichnogenera resulted from the Cambrian Explosion. A second ichnodiversity increase took place (20%) during the Ordovician. Subsequent to the Great Ordovician Biodiversification Event, this architectural category shows minor fluctuations in ichnodiversity resulting in a long-term plateau. The apparent decline in ichnodiversity by the end of the Cenozoic could reflect a taphonomic artefact resulting from the difficulties of identifying cumulative trace fossils in highly bioturbated modern sediments. Our data set indicates that several radial to rosette ichnogenera (e.g. Arenituba, Dactylophycus, Gyrophyllites, Phoebichnus, Volkichnium) occurred first in shallow-marine settings and then migrated to either deeper-water or marginal-marine environments, while others (e.g. Asterichnus, Cladichnus, Dactyloidites) apparently first occurred in deep-sea environments and then migrated to shallower waters.Fil: Muñoz, Diego Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Mangano, Maria Gabriela. University of Saskatchewan; Canadá. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Buatois, Luis Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. University of Saskatchewan; Canad