ALBERT

Note: Contents: Preface. - List of abbreviations. - 1. Sea-level changes: the emergence of a Quaternary perspective. - 1.1 Introduction. - 1.2 The Quaternary Period. - 1.3 Sea-Jevel changes: historical development of ideas. - 1.4 Observations from classical antiquity until the nineteenth century. - 1.4.1 Early Mediterranean studies. - 1.4.2 Eighteenth-century writings on universal changes to the Earth. - 1.4.3 Diluvial Theory - the universal flood. - 1.4.4 The Temple of Serapis: a compelling case for relative sea-level change. - 1.4.5 Lavoisier and the concepts of transgression and regression. - 1.5 Glacial action and recognition of the Ice Ages. - 1.5.1 Louis Agassiz and the Glacial Theory. - 1.5.2 The Croll-Milankovitch Hypothesis. - 1.6 Vertical changes in land and sea Ievel related to Quaternary climate. - 1.6.1 Charles Darwin and James Dana. - 1.6.2 Insights from around the world. - 1. 7 Evolution of ideas in the twentieth century. - 1. 7.1 Developments in Europe. - 1.7.2 Advances in geochemistry and geochronology. - 1.7.3 Oxygen-isotope records from marine sediments and ice cores. - 1.7.4 Geophysical models of sea-level changes. - 1.7.5 Sequence stratigraphy. - 1.7.6 International concern and a focus on current and future sea-level trends. - 1.8 Theoretical concepts relevant to the study of Quaternary sea-level changes. - 1.9 Synthesis and way forward. - 1.9.1 Revisiting old ideas. - 1.9.2 Quaternary sea-level changes: the status quo. - 2. The causes of Quaternary sea-level changes. - 2.1 Introduction. - 2.2 Sea Ievel and sea-level changes: some definitions. - 2.2.1 Sea Ievel and base Ievel. - 2.2.2 Relative sea-level changes. - 2.3 Processes responsible for relative sea-level changes in the Quaternary. - 2.3.1 Glacio-eustasy. - 2.3.2 lsostasy. - 2.3.3 Glacial isostasy and relative sea-Ievel changes. - 2.3.4 Hydro-isostasy and relative sea-level changes. - 2.3.5 The geoid and changes to its configuration. - 2.3.6 Global variation in geophysical response and equatorial ocean siphoning. - 2.4 Tectonism, volcanism, and other processes resulting in relative sea-level changes. - 2.4.1 Teetonic movements. - 2.4.2 Volcanism and its link to sea-level changes. - 2.4.3 Lithospheric flexure. - 2.4.4 Changes in tidal range. - 2.4.5 Steric changes, meteorological changes, and the role of ENSO events. - 2.5 Geophysical models and the sea-!evel equation. - 2.6 Synthesis and conclusions. - 3. Palaeo-sea-level indicators. - 3.1 Introduction. - 3.1.1 Fixed and relational sea-level indicators. - 3.1.2 Relative sea-level changes, sea-level index points, and indicative meaning. - 3.1.3 Sources of uncertainty in palaeo-sea-Ievel estimation. - 3.1.4 Palaeo-sea-level curve or envelope?. - 3.1.5 Facies architecture, allostratigraphy, and sea-level changes. - 3.2 Pleistocene and Holocene palaeo-sea-level indicators compared. - 3.3 Corals and coral reefs. - 3.3.1 Reefs and Pleistocene sea Ievels. - 3.3.2 Reefs and Holocene sea Ievels. - 3.3.3 Conglomerates and recognition of in-situ corals. - 3.3.4 Microatolls. - 3.4 Other biological sea-level indicators. - 3.4.1 Fixed biological indicators. - 3.4.2 Mangroves. - 3.4.3 Salt-marsh sediments and microfossil analysis. - 3.4.4 Seagrass. - 3.4.5 Marine molluscs. - 3.4.6 Submerged forests. - 3.5 Geomorphological and geological sea-level indicators. - 3.5.1 Marine terraces and shore platforms. - 3.5.2 Shoreline notches and visors. - 3.5.3 Isolation basins. - 3.5.4 Beach ridges. - 3.5.5 Cheniers. - 3.5.6 Aeolianites. - 3.5.7 Calcretes. - 3.5.8 Beachrock. - 3.6 Geoarchaeology and sea-level changes. - 3.7 Synthesis and conclusions. - 4. Methods of dating Quaternary sea-level changes. - 4.1 Introduction. - 4.1.1 Terminology. - 4.1.2 Historical approaches used for evaluating geological age of coastal deposits. - 4.2 Radiocarbon dating. - 4.2.1 Underlying principles of the radiocarbon method. - 4.2.2 Age range. - 4.2.3 Measurement techniques. - 4.2.4 Isotopic fractionation. - 4.2.5 Marine reservoir and hard-water effects. - 4.2.6 Secular 14C/ 12C variation and the calibration of radiocarbon ages to sidereal years. - 4.2.7 Cantamination and sample pre-treatment strategies. - 4.2.8 Statistical considerations: comparisons of radiocarbon age and pooling of results. - 4.3 Uranium-series disequilibrium dating. - 4.3.1 Underlying principles of U-series disequilibrium dating. - 4.3.2 U-series dating of marine carbonates. - 4.3.3 U-series dating of other materials. - 4.4 Oxygen-isotope stratigraphy. - 4.5 Luminescence dating methods. - 4.5.1 Quantifying the cumulative effects of environmental radiation dose. - 4.5.2 Age range of luminescence methods. - 4.5.3 Anomalaus fading and partial bleaching. - 4.6 Electron spin resonance dating. - 4.7 Amino acid racemisation dating. - 4.7.1 The amino acid racemisation reaction. - 4.7.2 Environmental factors that influence racemisation. - 4.7.3 Sources of uncertainty in AAR dating. - 4.7.4 Application of AAR to dating coastal successions. - 4.8 Cosmogenic dating. - 4.9 Other dating techniques. - 4.9.1 Event markers. - 4.9.2 Palaeomagnetism. - 4.10 Synthesis and conclusions. - 5 Vertical displacement of shorelines. - 5.5.1 Introduction. - 5.2 Plate tectonics and implications for coastlines globally. - 5.2.1 Lithospheric plate domains. - 5.2.2 Plate margins. - 5.2.3 Plate tectonics and coastal classification. - 5.2.4 Ocean plate dynamics and island types. - 5.3 Styles of tectonic deformation and rates of uplift or subsidence. - 5.3.1 Coseismic uplift. - 5.3.2 Epeirogenic uplift. - 5.3.3 Folding and warping. - 5.3.4 Isostasy. - 5.3.5 Lithospheric flexure. - 5.3.6 Mantle plumes. - 5.3.7 Subsidence and submerged shorelines. - 5.4 The last interglacial shoreline: a reference for quantifying vertical displacement. - 5.4.1 Terrace age and elevation. - 5.4.2 Constraints on using the last interglacial shoreline as a benchmark. - 5.5 Coastlines in tectonically 'stable' cratonic regions. - 5.5.1 Australia. - 5.5.2 Southern Africa. - 5.6 Coastlines of emergence. - 5.6.1 Huon Peninsula. - 5.6.2 Barbados. - 5.6.3 Convergent continental margins: Chile. - 5.7 Vertical crustal movements associated with glacio-isostasy: Scandinavia. - 5.8 The Mediterranean Basin . - 5.8.1 Italy. - 5.8.2 Greece. - 5.9 The Caribbean region. - 5.9.1 Southern Florida and the Bahamas. - 5.9.2 Other Caribbean sites and more tectonically active islands. - 5.10 Divergent spreading-related coastlines: Red Sea. - 5.11 Pacific Plate. - 5.11.1 Pacific islands. - 5.11.2 Hawaii. - 5.11.3 Japan. - 5.11.4 New Zealand. - 5.12 Synthesis and conclusions. - 6. Pleistocene sea-level changes. - 6.1 Introduction. - 6.2 Prelude to the Pleistocene. - 6.3 Pleistocene icesheets. - 6.4 Early Pleistocene sea Ievels. - 6.4.1 Roe Calcarenite, Roe Plains, southern Australia. - 6.4.2 The Crag Group, southeastern England. - 6.S The middle Pleistocene Transition. - 6.6 Middle Pleistocene sea-level changes. - 6.7 Sea-level highstands of the middle Pleistocene. - 6.7.1 Marine Isotope Stage 11. - 6.7.2 Marine Isotope Stage 9 - the pre-penultimate interglacial. - 6.7.3 Marine Isotope Stage 7 - the penultimate interglacial. - 6.8 Middle Pleistocene sea-level lowstands. - 6.9 Late Pleistocene sea-level changes. - 6.9.1 The last interglacial maximum (MIS 5e). - 6.9.2 Timing and duration of the last interglacial maximum. - 6.9.3 Global estimates of last interglacial sea Ievels - the sanctity of the 6 m APSL datum?. - 6.10 Interstadial sea Ievels of the last glacial cycle (MIS 5c and 5a). - 6.11 Interstadial sea Ievels during MIS 3. - 6.12 Late Pleistocene interstadial sea Ievels: Dansgaard-Oeschgerand Heinrich Events. - 6.13 Eustatic sea Ievels during the Last Glacial Maximum (MIS 2). - 6.14 Long records of Pleistocene sea-level highstands. - 6.14.1 Coorong Coastal Plain and Murray Basin, southern Australia. - 6.14.2 Wanganui Basin, New Zealand. - 6.14.3 Sumba Island, Indonesia. - 6.15 Synthesis and conclusions. - 7. Sea-level changes since the Last Glacial Maximum. - 7.1 Introduction. -