CD-ROM version contents: Supplementary materials to Geology and geomorphology of Barbados.

"Chapter 1 shows that the windward slope of Barbados and its terraced morphology evolved principally by wave erosion during uplift and eustatic oscillation, rather than by biohermal growth. Chapter 2 describes the interplay of erosion and limestone deposition during eustatic oscillation over a span of 700,000 years. It represents the first comprehensive field and chronologic study to integrate marine erosion and deposition with tectonic uplift rates to determine emergence values and rates of the stratigraphic and evolutionary model. Chapter 3 describes the distributions, lithology, depositional environments, and ages of the limestone stratigraphic subunits for seven study areas in southeastern Barbados"--

This book on geology and hydrogeology of carbonate islands is volume 54 in the Developments in Sedimentology series.

Deep-water (below wave base) processes, although generallyhidden from view, shape the sedimentary record of more than 65% ofthe Earth’s surface, including large parts of ancientmountain belts. This book aims to inform advanced-levelundergraduate and postgraduate students, and professional Earthscientists with interests in physical oceanography and hydrocarbonexploration and production, about many of the important physicalaspects of deep-water (mainly deep-marine) systems. The authorsconsider transport and deposition in the deep sea, trace-fossilassemblages, and facies stacking patterns as an archive of theunderlying controls on deposit architecture (e.g., seismicity,climate change, autocyclicity). Topics include modern and ancientdeep-water sedimentary environments, tectonic settings, and howbasinal and extra-basinal processes generate the typicalcharacteristics of basin slopes, submarine canyons, contouritemounds and drifts, submarine fans, basin floors and abyssalplains.