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There have been significant changes in sea level over the past two million years, and a complete understanding of natural cycles of change as well as anthropogenic effects is imperative for future global development. This book reviews the history of research into these sea-level changes and summarises the methods and analytical approaches used to interpret evidence for sea-level changes. It provides an overview of changing climates during the Quaternary, examines processes responsible for global variability of sea-level records, and presents detailed reviews of sea-level changes for the Pleistocene and Holocene. The book concludes by discussing current trends in sea levels and likely future sea-level changes. This is an important and authoritative resource for academic researchers and graduate and advanced undergraduate students working in tectonics, stratigraphy, geomorphology, physical geography, environmental science and other aspects of Quaternary studies.
Sea level --- Paleoceanography --- Pleistocene-Holocene boundary --- Limite pléistocène-holocène --- History --- Pleistocene-Holocene boundary. --- History. --- Limite pléistocène-holocène --- Mer --- Paléo-océanographie --- Limite Pléistocène-Holocène --- Niveau --- Histoire. --- Boundary, Pleistocene-Holocene --- Holocene-Pleistocene boundary --- Pleistocene-Holocene transition --- Transition, Pleistocene-Holocene --- Geology, Stratigraphic --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch --- Mean sea level --- Sea level rise --- Oceanography --- Water levels --- Paléo-océanographie --- Limite Pléistocène-Holocène
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This eBook is a collection of articles from a Frontiers Research Topic. Frontiers Research Topics are very popular trademarks of the Frontiers Journals Series: they are collections of at least ten articles, all centered on a particular subject. With their unique mix of varied contributions from Original Research to Review Articles, Frontiers Research Topics unify the most influential researchers, the latest key findings and historical advances in a hot research area! Find out more on how to host your own Frontiers Research Topic or contribute to one as an author by contacting the Frontiers Editorial Office: frontiersin.org/about/contact
North Pacific --- Holocene-Pleistocene --- Paleoenvironment --- Paleoclimate --- Proxy reconstruction
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The Middle Holocene epoch (8,000 to 3,000 years ago) was a time of dramatic changes in the physical world and in human cultures. Across this span, climatic conditions changed rapidly, with cooling in the high to mid-latitudes and drying in the tropics. In many parts of the world, human groups became more complex, with early horticultural systems replaced by intensive agriculture and small-scale societies being replaced by larger, more hierarchical organizations. Climate Change and Cultural Dynamics explores the cause and effect relationship between climatic change and cultural transformation
Climatic changes --- Paleoclimatology --- Global warming --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch --- Research. --- Paleoclimatology - Holocene
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The fascinating story of how a harsh terrain that resembled modern Antarctica has been transformed gradually into the forests, grasslands, and wetlands we know today. "One of the best scientific books published in the last ten years."-Ottowa Journal "A valuable new synthesis of facts and ideas about climate, geography, and life during the past 20,000 years. More important, the book conveys an intimate appreciation of the rich variety of nature through time."-S. David Webb,Science
Paleobiogeography --- Paleontology --- Glacial epoch --- Paleoecology --- Palaeoecology --- Ecology --- Paleobiology --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch --- Ice Age --- Geology, Stratigraphic --- Geographical distribution of fossil animals and plants --- Biogeography --- Glacial epoch - North America --- Paleobiogeography - North America --- Paleoecology - Holocene
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Climate for the 21st century is expected to be considerably different from the present and recent past. Industrialization growth combined with the increasing CO2 concentration in the atmosphere and massive deforestation are well above the values over the past several decades and are expected to further grow. Air temperature is rising rapidly well as does the weather variability producing frequent extreme events. Six of the ten warmest years occurred in the 1990s. Temperatures predicted for the 21st century ranges well above the present day value. The time period of the last 100-200 years c
Paleoclimatology --- Methodology. --- Geologic climate --- Palaeoclimatology --- Paleoclimate --- Climatic changes --- Climatology --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch
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Geology, Stratigraphic --- Paleoclimatology. --- Geologic climate --- Palaeoclimatology --- Paleoclimate --- Climatic changes --- Climatology --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch
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Geology, Stratigraphic --- Paleogeography --- Historical geology --- Geology --- Palaeogeography --- Physical geography --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch
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Iceland provides an unique stage on which to study the natural environment, both past and present, and it is understanding both aspects of reconstructing the past and observing and interpreting the present that form the focus of the contributions to this volume. The papers are all written by active researchers and incorporate both reviews and new data. Although concentrating largely on the recent Quaternary timescale a wide range of topics is explored including subglacial volcanism, onshore and offshore evidence for the Last Glacial Maximum and subsequent deglaciation, current glaci
Geology. Earth sciences --- Geology, Stratigraphic --- Geodynamics --- Dynamic geology --- Tectonophysics --- Geophysics --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch
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This timely study is concerned with the current record of sea-level changes during the past 10,000 years; their rates, and our ability to estimate these changes accurately. The author begins with an extensive introduction to the subject, covering the historical background and the possible causes of sea-level changes and the main methods used to reconstruct former sea-level positions. The second and main part of the Atlas provides a worldwide review of Holocene sea level changes by assembling some 800 local relative sea-level curves, deduced from field data from all parts of the world, and comp
Geology, Stratigraphic --- Sea level --- Atlases --- Atlases. --- Issue --- Geology [Stratigraphic ] --- Holocene --- Sea level - Atlases. --- Geology, Stratigraphic - Holocene - Atlases. --- Mean sea level --- Sea level rise --- Oceanography --- Water levels --- Age of rocks --- Rocks --- Stratigraphic geology --- Physical geology --- Age --- Sea level - Atlases --- Geology, Stratigraphic - Holocene - Atlases
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From the traces of a devastating tsunami in Japan during the winter of 1700, scientists discover how it was recorded in Japanese history and then backtrack it to its origins via geological evidence in North America. Their work shows how tsunami research has evolved over three centuries and how this event impacts current warning systems.
Paleoseismology --- Subduction zones --- Zones, Subduction --- Plate tectonics --- Holocene Epoch --- Late Quaternary Period --- Postglacial Epoch --- Recent Epoch --- Historical seismicity --- Historical seismology --- Palaeoseismology --- Paleoseismicity --- Seismicity, Historical --- Paleogeophysics --- Seismology
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