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"Contributors from twelve countries wrote the twelve chapters in this Special Paper, and they address a range of topics, including climatic and hydrologic modeling, paleogeographic reconstruction of Late Quaternary landscapes, palynology and paleoclimate reconstruction, and geoarchaeological studies, both onshore and offshore. The volume serves as a timely reference for continuing research in a region harboring a number of newly independent states that are now faced with population pressure and a variety of environmental issues."--
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Major events of human prehistory such as the post-glacial recolonization of Northern Europe and the spread of agriculture through the Mediterranean took place on landscapes that are now, at least partially, underwater. Large parts of this submerged terrain are accessible to divers and can be investigated archaeologically. Prehistoric underwater research has emerged in recent decades as a distinct sub-discipline, developing approaches and methodologies that can be applied in coastal regions worldwide. As a result there is growing awareness of the potential for underwater archaeology to transform our ideas about the course of prehistory. This volume examines existing practice and new developments in the field of submerged prehistoric landscape research. The 25 peer-reviewed contributions from leading authors cover the results of recent research on three continents and the application of methodologies and techniques for site discovery, investigation and interpretation.
This book presents a comprehensive, contemporary review of tidal environments and deposits. Individual chapters, each written by world-class experts, cover the full spectrum of coastal, shallow-marine and even deep-marine settings where tidal action influences or controls sediment movement and deposition. Both siliciclastic and carbonate deposits are covered. Various chapters examine the dynamics of sediment transport by tides, and the morphodynamics of tidal systems. Several chapters explore the occurrence of tidal deposits in the stratigraphic context of entire sedimentary basins. This book is essential reading for both coastal geologists and managers, and geologists interested in extracting hydrocarbons from complex tidal successions.
Links have recently been established between the study of death assemblages by archaeologists and paleontologists (taphonomy) and the application of physical anthropology concepts to the medicolegal investigation of death (forensic anthropology). Forensic Taphonomy explains these links in a broad-based, multidisciplinary volume. It applies taphonomic models in modern forensic contexts and uses forensic cases to extend taphonomic theories. Review articles, case reports, and chapters on methodology round out this book's unique approach to forensic science.
Papers cover the entire spectrum of eolian investigations, ranging from the microscopic level to regional synthesis as well as ancient eolian deposits and their interpretation.
Current sea level rise is due significantly to global warming, which will increase sea level over the coming century and longer periods. Increasing temperatures result in sea level rise by the thermal expansion of water and through the addition of water to the oceans from the melting of continental ice sheets. Values for predicted sea level rise over the course of this century typically range from 90 to 880 mm. This book presents research data on sea level rise, coastal engineering, shorelines and tides, including the tides and topography of the Strait of Gibraltar; tidal energy use for the future and sea level variation along the Estonian coast of the Baltic Sea. Also discussed herein is the potential impacts of sea-level rise on the Atlantic and Gulf of Mexico coasts and coastal management of shorelines in Colombia, South America.
This text describes the changes that occur in coastal landforms during a rising sea level. Evidence from subsiding coasts, theoretical models and geological changes during marine transgressions are assembled to indicate the global alterations that will take place due to the greenhouse effect.