Encyclopedia of Paleoclimatology and Ancient Environments
(Sprache: Englisch)
One of Springer's Major Reference Works, this book gives the reader a truly global perspective. Paleoclimate topics covered in the encyclopedia give the reader the capability to place the observations of recent global warming in the context of longer-term natural climate fluctuations.
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One of Springer's Major Reference Works, this book gives the reader a truly global perspective. Paleoclimate topics covered in the encyclopedia give the reader the capability to place the observations of recent global warming in the context of longer-term natural climate fluctuations.
Klappentext zu „Encyclopedia of Paleoclimatology and Ancient Environments “
Concern exists over human-generated increases in atmospheric greenhouse gases and their potential consequences to society. The Intergovernmental Panel on Climate Change (IPCC) in 2007 finds that global temperatures have increased by 0.8ºC since 1850 and that climate warming is now 'unequivocal'. While the human imprint is becoming increasingly apparent, Earth¿s climate has shifted dramatically and frequently during the last few million years, alternating between ice ages, when vast glaciers covered Northern Europe and much of North America, and interglacials¿warm periods much like today. Farther back in geologic time, climates have differed even more from the present. Thus, to fully understand the unusual changes of the 20th century and possible future trends, these must be placed in a longer-term context extending beyond the period of instrumental records.The Encyclopedia of Paleoclimatology and Ancient Environments, a companion volume to the recently-published Encyclopedia of World Climatology, provides the reader with an entry point to the rapidly expanding field of paleoclimatology¿the study of climates of the past. Highly interdisciplinary in nature, paleoclimatology integrates information from a broad array of disciplines in the geosciences, ranging from stratigraphy, geomorphology, glaciology, paleoecology, paleobotany to geochemistry and geophysics, among others. The encyclopedia offers 230 informative articles written by over 200 well known international experts on numerous subjects, ranging from classical geological evidence to the latest research. The volume is abundantly illustrated with line-drawings, black-white and color photographs. Articles are arranged alphabetically, with extensive bibliographies and cross-references.
Volume Editor:
Vivien Gornitz is a Senior Research Scientist, Center for Climate Systems Research Columbia University and NASA Goddard Institute for Space Studies. She holds a B.A. from Barnard College and
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a Ph.D. from Columbia University. Her research interests include global sea level rise--past, present, and future, coastal hazards, climatic implications of land cover transformations, and planetary geology, including Mars. In addition to numerous scientific publications, she has edited Geology of the Planet Mars (Benchmark Papers in Geology, v. 48, Dowden, Hutchinson & Ross, Inc., 1979) and has contributed articles to several of the encyclopedias in the Earth Sciences Series. She was a Contributing Author for the IPCC in 1990, 1995, 2001, and 2007.
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Inhaltsverzeichnis zu „Encyclopedia of Paleoclimatology and Ancient Environments “
- List of Contributors- Preface
- Acknowledgments
- Abrupt climate change
- Aerosols (mineral)
- Albedo (feedbacks)
- Alkenones
- Animal proxies, invertebrates
- Animal proxies, vertebrates
- Anoxic events
- Antarctica, glaciation history
- Antarctic Bottom Water and climate change
- Antarctic Cold Reversal
- Antarctic sea ice history, Late Quaternary
- Archean environments
- Archeological data and climate change
- Arctic sea ice
- Arid climates and indicators
- Astronomical theory of climate change
- Atmospheric circulation during the Last Glacial Maximum
- Atmospheric evolution, Earth
- Atmospheric evolution, Mars
- Atmospheric evolution, Venus
- Banded iron formations and the early atmosphere
- Basal ice
- Beachrock
- Beetles as Quaternary and Late Tertiary climate indicators
- Beryllium-10
- Binge/purge model of ice sheet dynamics
- Bolide impacts and climate
- Blling-Allerd interstadial
- Borehole climatology: climate change from geothermal data
- Carbon cycle
- Carbon dioxide, dissolved (ocean)
- Carbon dioxide and methane, Quaternary variations
- Carbon isotopes, stable
- Carbon isotope variations over geologic time
- Carbonate compensation depth
- Carbonates, cool water
- Carbonates, warm water
- Cenozoic climate and long-term cooling
- Cirques
- CLAMP (Climate Leaf Analysis Multivariate Program)
- CLIMAP
- Climate change, causes
- Climate forcing
- Climate variability, last 1000 years
- Coal beds, origin and climate
- Coastal environments
- Coccoliths
- COHMAP
- Continental sediments
- Corals and coral reefs
- Cordilleran ice sheet
- Cosmogenic radionuclides
- Cretaceous-Tertiary (K-T) boundary
- Cretaceous warm climates
- Cryosphere
- Cyclic sedimentation (cyclothems)
- Dansgaard-Oeschger cycles
- Dating, amino acid geochronology
- Dating, biostratigraphic methods
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Dating, dendrochronology
- Dating, fission tracks
- Dating, luminescence techniques
- Dating, magnetostratigraphy
- Dating, radiometric methods
- Deep Sea Drilling Project (DSDP)
- Deltaic sediments, climate records
- Dendroclimatology
- Desert varnish as climate proxy
- Deuterium, deuterium excess
- Diamicton
- Diatoms
- Dinoflagellates
- Dole effect
- Drumlins
- Duricrusts
- Dust transport, Quaternary
- Earth laws and climatology
- Early Paleozoic climates (Cambrian-Devonian)
- Eccentricity, earth's orbit
- Eemian (Sangamonian) interglacial
- Electrical conductivity
- Eolian dust, marine sediments
- Eolian sediments and processes
- Eolianite
- Eskers
- Evaporites
- Evolution and climate change
- Faint Young Sun Paradox
- Flood basalts, climatic implications
- Foraminifera
- Geochemical proxies (non-isotopic)
- Glacial erratic
- Glacial eustasy
- Glacial geomorphology
- Glacial isostasy
- Glacial
- megalakes
- Glacial sediments
- Glaciations, pre-Quaternary
- Glaciations, Quaternary
- Glaciofluvial sediments
- Glaciomarine sediments
- Glendonite/ikaite
- "Greenhouse" (warm) climates
- Heat transports, oceanic and atmospheric
- Heinrich events
- History of Paleoclimatology
- Holocene climates
- Holocene treeline fluctuations
- Hypsithermal
- Human evolution and climate change
- Ice cores, Antarctica and Greenland
- Ice cores, mountain glaciers
- "Icehouse" (cold) climates
- Ice-rafted debris (IRD)
- Integrated Ocean Drilling Program (IODP)
- Interstadials
- Iron and climate change
- Isotopic fractionation
- Kames
- Kettles
- Lacustrine sediments
- Lake level variations
- Late Glacial Maximum
- Last Glacial Termination
- Laterite
- Late Paleozoic climates
- Late Quaternary-Holocene vegetation modeling
- Late Quaternary megafloods
- Laurentide ice sheet
- Little Ice Age
- Loess deposits
- Marine biogenic sediments
- Marine carbon geochemistry
- Marine clay minerals
- Marine non-biogenic (inorganic) sediments
- Mars: water and past climates
- Mass extinctions: role of Climate
- Maunder minimum
- Medieval warm period
- Mesozoic climates
- Messinian salinity crisis
- Methane hydrates, carbon cycling, and environmental change
- Mid-Pliocene warming
- Millennial climate variability
- Mineral indicators of past climates
- Monsoons, Pre-Quaternary
- Monsoons, Quaternary
- Moraines
- Mountain
- glaciers,
- Mountain uplift and climate change
- Nearest-living-relative method
- Neogene climates
- Nitrogen isotopes
- North Atlantic Oscillation (NAO) records
- North Atlantic Deep Water and climate change
- Obliquity, earth's orbit
- Ocean Drilling Program (ODP)
- Ocean paleocirculation
- Ocean paleoproductivity
- Ocean paleotemperatures
- Organic geochemical proxies
- Ostracodes
- Outwash plains
- Oxygen isotopes
- PAGES
- aleobotany
- Paleocene-Eocene Thermal Maximum
- Paleoclimate modeling, Quaternary
- Paleoclimate modeling, pre-Quaternary
- Paleoclimate proxies, an introduction
- Paleo-El Nino-Southern Oscillation (ENSO) records
- Paleogene climates
- Paleohydrology
- Paleo-ocean modeling
- Paleo-ocean pH
- Paleoceanography
- Paleolimnology
- Paleo-precipitation indicators
- Paleosols-pre-Quaternary
- Paleosols-Quaternary
- Paleotemperatures, proxy reconstructions
- Paleotempestology-sedimentary record of intense hurricanes
- Palynology
- Patterned ground
- Periglacial geomorphology
- Phosphorite
- Phosphorus cycle
- Pingo
- Plate tectonics and climate change
- Pleistocene climates
- Pliocene climates
- Pollen analysis
- Potassium-Argon/argon-argon dating
- Precession, earth's orbit
- Pre-Quaternary Milankovitch cycles and climate
- Proglacial lacustrine sediments
- Proterozoic climates
- Quaternary climate transitions and cycles
- Quaternary vegetation distribution
- Radiocarbon dating
- Radiolaria
- Red beds
- Roche moutonne
- Sapropels (organic-rich muds)
- Scandinavian ice sheet
- Sea level change, Holocene
- Sea level change, Quaternary
- Sea level change, last 250 million years
- Sea level indicators
- Sedimentary indicators of climate change
- Snowball Earth hypothesis
- SPECMAP
- Speleothems
- Stable isotope analysis
- Strontium isotopes
- Sulfur isotopes
- Sun-climate style='mso-spacerun:yes'>connections
- Tephrochronology
- The 8200 year BP cold event
- Thermohaline circulation
- Time series analysis
- Till and Tillites
- Transfer functions
- Triassic-Jurassic climates
- Uranium-series dating
- Varved sediments
- Volcanic eruptions and climate change
- Weathering and climate
- Wisconsinan (Weichselian, Wurm) glaciation
- Younger Dryas
- Author index
- Subject index
- Dating, fission tracks
- Dating, luminescence techniques
- Dating, magnetostratigraphy
- Dating, radiometric methods
- Deep Sea Drilling Project (DSDP)
- Deltaic sediments, climate records
- Dendroclimatology
- Desert varnish as climate proxy
- Deuterium, deuterium excess
- Diamicton
- Diatoms
- Dinoflagellates
- Dole effect
- Drumlins
- Duricrusts
- Dust transport, Quaternary
- Earth laws and climatology
- Early Paleozoic climates (Cambrian-Devonian)
- Eccentricity, earth's orbit
- Eemian (Sangamonian) interglacial
- Electrical conductivity
- Eolian dust, marine sediments
- Eolian sediments and processes
- Eolianite
- Eskers
- Evaporites
- Evolution and climate change
- Faint Young Sun Paradox
- Flood basalts, climatic implications
- Foraminifera
- Geochemical proxies (non-isotopic)
- Glacial erratic
- Glacial eustasy
- Glacial geomorphology
- Glacial isostasy
- Glacial
- megalakes
- Glacial sediments
- Glaciations, pre-Quaternary
- Glaciations, Quaternary
- Glaciofluvial sediments
- Glaciomarine sediments
- Glendonite/ikaite
- "Greenhouse" (warm) climates
- Heat transports, oceanic and atmospheric
- Heinrich events
- History of Paleoclimatology
- Holocene climates
- Holocene treeline fluctuations
- Hypsithermal
- Human evolution and climate change
- Ice cores, Antarctica and Greenland
- Ice cores, mountain glaciers
- "Icehouse" (cold) climates
- Ice-rafted debris (IRD)
- Integrated Ocean Drilling Program (IODP)
- Interstadials
- Iron and climate change
- Isotopic fractionation
- Kames
- Kettles
- Lacustrine sediments
- Lake level variations
- Late Glacial Maximum
- Last Glacial Termination
- Laterite
- Late Paleozoic climates
- Late Quaternary-Holocene vegetation modeling
- Late Quaternary megafloods
- Laurentide ice sheet
- Little Ice Age
- Loess deposits
- Marine biogenic sediments
- Marine carbon geochemistry
- Marine clay minerals
- Marine non-biogenic (inorganic) sediments
- Mars: water and past climates
- Mass extinctions: role of Climate
- Maunder minimum
- Medieval warm period
- Mesozoic climates
- Messinian salinity crisis
- Methane hydrates, carbon cycling, and environmental change
- Mid-Pliocene warming
- Millennial climate variability
- Mineral indicators of past climates
- Monsoons, Pre-Quaternary
- Monsoons, Quaternary
- Moraines
- Mountain
- glaciers,
- Mountain uplift and climate change
- Nearest-living-relative method
- Neogene climates
- Nitrogen isotopes
- North Atlantic Oscillation (NAO) records
- North Atlantic Deep Water and climate change
- Obliquity, earth's orbit
- Ocean Drilling Program (ODP)
- Ocean paleocirculation
- Ocean paleoproductivity
- Ocean paleotemperatures
- Organic geochemical proxies
- Ostracodes
- Outwash plains
- Oxygen isotopes
- PAGES
- aleobotany
- Paleocene-Eocene Thermal Maximum
- Paleoclimate modeling, Quaternary
- Paleoclimate modeling, pre-Quaternary
- Paleoclimate proxies, an introduction
- Paleo-El Nino-Southern Oscillation (ENSO) records
- Paleogene climates
- Paleohydrology
- Paleo-ocean modeling
- Paleo-ocean pH
- Paleoceanography
- Paleolimnology
- Paleo-precipitation indicators
- Paleosols-pre-Quaternary
- Paleosols-Quaternary
- Paleotemperatures, proxy reconstructions
- Paleotempestology-sedimentary record of intense hurricanes
- Palynology
- Patterned ground
- Periglacial geomorphology
- Phosphorite
- Phosphorus cycle
- Pingo
- Plate tectonics and climate change
- Pleistocene climates
- Pliocene climates
- Pollen analysis
- Potassium-Argon/argon-argon dating
- Precession, earth's orbit
- Pre-Quaternary Milankovitch cycles and climate
- Proglacial lacustrine sediments
- Proterozoic climates
- Quaternary climate transitions and cycles
- Quaternary vegetation distribution
- Radiocarbon dating
- Radiolaria
- Red beds
- Roche moutonne
- Sapropels (organic-rich muds)
- Scandinavian ice sheet
- Sea level change, Holocene
- Sea level change, Quaternary
- Sea level change, last 250 million years
- Sea level indicators
- Sedimentary indicators of climate change
- Snowball Earth hypothesis
- SPECMAP
- Speleothems
- Stable isotope analysis
- Strontium isotopes
- Sulfur isotopes
- Sun-climate style='mso-spacerun:yes'>connections
- Tephrochronology
- The 8200 year BP cold event
- Thermohaline circulation
- Time series analysis
- Till and Tillites
- Transfer functions
- Triassic-Jurassic climates
- Uranium-series dating
- Varved sediments
- Volcanic eruptions and climate change
- Weathering and climate
- Wisconsinan (Weichselian, Wurm) glaciation
- Younger Dryas
- Author index
- Subject index
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Bibliographische Angaben
- 2008, 1049 Seiten, 38 farbige Abbildungen, Masse: 23,1 x 28,9 cm, Gebunden, Englisch
- Herausgegeben: Vivien Gornitz
- Verlag: Springer Netherlands
- ISBN-10: 1402045514
- ISBN-13: 9781402045516
Sprache:
Englisch
Rezension zu „Encyclopedia of Paleoclimatology and Ancient Environments “
From the reviews: "This book is an A-Z series of entries on paleoclimatology and ancient environments. ... offers a good overview of its subject matter and would be a suitable reference for any academic library that supports research in paleoclimatology and ancient environments or related fields. It would also be of interest to the general public who were interested in this subject area. ... here is a chronological list of the geological time-periods as an appendix. This makes the text more accessible to the non-specialist ... ." (Clari Hunt, Reference Reviews, Vol. 23 (8), 2009)
"I was very impressed by the sedimentology encyclopedia ... and I had therefore great expectations of this new title. ... seems to be more interesting for Quaternary geologists and climatologists ... . I must conclude that the volume comprises a wealth of valuable information, and that most chapters are truly useful. ... the book is well printed, most figures are instructive and well-readable, and the binding has the quality that is required for such a huge work." (A. J. Tom van Loon, Journal of Sedimentary Research, February, 2010)
"This companion volume focuses on paleoclimatology and spans Earth's climate history from the early Precambrian to the Little Ice Age, which ran from the 16th to the mid-19th centuries. ... All articles contain excellent bibliographies leading to additional information. The work is well indexed, entries are cross-referenced, and the text is profusely illustrated with maps, graphs, and charts. Summing Up: Essential. Reference collections supporting programs in climate studies, lower-level undergraduates through professionals/practitioners, and general readers." (J. C. Stachacz, Choice, Vol. 47 (6), February, 2010)
"The chapters of the encyclopaedia are informative ... . Palaeoclimatology, palaeogeography, geomorphology, geochemistry, and several more disciplines that are important for the climatological reconstruction of the
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geological past form a wide spectrum, and the encyclopaedia is, therefore, truly comprehensive. ... easy to use. ... Each chapter ends with cross-references, which indicate relevant chapters on related topics. ... very useful for all geoscientists. It belongs in each geoscience library." (Dmitry A. Ruban, Geologos, Vol. 16 (2), 2010)
"The first major reference work covering the field of palaeoclimatology through the whole of Earth's history from the early Precambrian to recent times. ... the authors and editor have done a great job in making each entry accessible, creating a work that is extremely useful for providing introductions to undergraduate students approaching palaeoclimatology for the first time, or to postgraduates and academics wanting a quick explanation of an area outside of their area of expertise or an insight into how theories have developed over time." (Jonathan R. Dean, Journal of Paleolimnology, Vol. 47, 2012)
"The first major reference work covering the field of palaeoclimatology through the whole of Earth's history from the early Precambrian to recent times. ... the authors and editor have done a great job in making each entry accessible, creating a work that is extremely useful for providing introductions to undergraduate students approaching palaeoclimatology for the first time, or to postgraduates and academics wanting a quick explanation of an area outside of their area of expertise or an insight into how theories have developed over time." (Jonathan R. Dean, Journal of Paleolimnology, Vol. 47, 2012)
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