Schlagwort(e):
Paleogeography -- Quaternary.
;
Electronic books.
Beschreibung / Inhaltsverzeichnis:
The years since the second edition of Reconstructing Quaternary Environments have seen an exponential increase in the volume of literature written on the Quaternary. New methods and technological advances have given rise to a number of multi-disciplinary and interdisciplinary research groups able to offer startling insights in to short- and long- term climatic changes. This third edition has been revised and updated to address these developments and to freshly examine the various forms of evidence that can be used to establish the history and scale of environmental changes during the Quaternary. Building on the format previously established it reviews the geomorphological, lithological and biological evidence that compromises the Quaternary record, describes and evaluates dating methods and considers how these elements can be bought together in a robust stratigraphic framework. A new final chapter demonstrates how results using these different methods and approaches can by synergised to provide an overview of global environmental change. Compelling new evidence from the integration of polar ice and marine isotopes records allow the authors to examine a series of themes relating to climate change at a number of spatial scales and over a series of time intervals that become progressively shorter towards the present day. Clearly Illustrated to demonstrate key concepts and with progressive learning techniques employed throughout this new edition will be of interest to undergraduate students and professionals of Earth Science, Environmental Science, Physical Geography, Geology, Botany, Zoology, Ecology, Archaeology and Anthropology.
Materialart:
Online-Ressource
Seiten:
1 online resource (569 pages)
Ausgabe:
3rd ed.
ISBN:
9781317753711
URL:
https://ebookcentral.proquest.com/lib/geomar/detail.action?docID=1783956
DDC:
551.7/9
Sprache:
Englisch
Anmerkung:
Cover -- Half Title -- Dedication -- Title Page -- Copyright Page -- Table of Contents -- List of figures and tables -- Preface to the third edition -- Acknowledgements -- Cover image details -- 1 The Quaternary record -- 1.1 Introduction -- 1.2 Interpreting the Quaternary record -- 1.3 The status of the Quaternary in the geological timescale -- 1.4 The duration of the Quaternary -- 1.5 The development of Quaternary studies -- 1.5.1 Historical developments -- 1.5.2 Recent developments -- 1.6 The framework of the Quaternary -- 1.7 The causes of climatic change -- 1.8 The scope of this book -- Notes -- 2 Geomorphological evidence -- 2.1 Introduction -- 2.2 Methods -- 2.2.1 Field methods -- 2.2.1.1 Field mapping -- 2.2.1.2 Instrumental levelling -- 2.2.2 Remote sensing -- 2.2.2.1 Aerial photography -- 2.2.2.2 Satellite imagery -- 2.2.2.3 Radar -- 2.2.2.4 Sonar and seismic sensing -- 2.2.2.5 Digital elevation/terrain modelling -- 2.3 Glacial landforms -- 2.3.1 Extent of ice cover -- 2.3.2 Geomorphological evidence and the extent of ice sheets and glaciers during the last cold stage -- 2.3.2.1 Northern Europe -- 2.3.2.2 Britain and Ireland -- 2.3.2.3 North America -- 2.3.3 Direction of ice movement -- 2.3.3.1 Striations -- 2.3.3.2 Friction cracks -- 2.3.3.3 Ice-moulded (streamlined) bedrock -- 2.3.3.4 Streamlined glacial deposits -- 2.3.4 Reconstruction of former ice masses -- 2.3.4.1 Ice sheet modelling -- 2.3.4.2 Ice caps and glaciers -- 2.3.5 Palaeoclimatic inferences using former glacier elevations -- 2.3.5.1 Cirque floor altitude (CFA) and toe-to-headwall (THAR) methods -- 2.3.5.2 ELA/FLA method -- 2.4 Periglacial landforms -- 2.4.1 Palaeoclimatic inferences based on periglacial evidence -- 2.4.1.1 Rock glaciers -- 2.4.1.2 Pingos and palsas -- 2.4.1.3 Pronival ('protalus') ramparts -- 2.5 Sea-level change.
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2.5.1 Relative and 'absolute' sea-level changes -- 2.5.2 Eustatic changes in sea level -- 2.5.2.1 Pre-Quaternary eustatic changes -- 2.5.2.2 Quaternary eustatic changes -- 2.5.3 Tectonic influences -- 2.5.4 Glacio-and hydro-isostasy -- 2.5.5 Shoreline sequences in areas affected by glacio-isostasy -- 2.5.6 Palaeoenvironmental significance of sea-level changes -- 2.6 River terraces -- 2.6.1 Origins of river terraces -- 2.6.1.1 Eustatic changes in sea level -- 2.6.1.2 Climatic change -- 2.6.1.3 Glaciation -- 2.6.1.4 Tectonic changes -- 2.6.1.5 Human activity -- 2.6.2 River terraces and palaeoenvironmental reconstruction -- 2.6.3 The terraces of the River Thames -- 2.7 Quaternary landforms in low latitudes -- 2.7.1 Pluvial lakes -- 2.7.2 Dunefields -- 2.7.3 Fluvial landforms -- 2.7.4 Weathering crusts -- 2.8 Conclusions -- Notes -- 3 Lithological evidence -- 3.1 Introduction -- 3.2 Field and laboratory methods -- 3.2.1 Sediment sections -- 3.2.2 Coring -- 3.2.3 Laboratory methods -- 3.2.3.1 Particle size measurements -- 3.2.3.2 Particle shape -- 3.2.3.3 Surface textures of quartz particles -- 3.2.3.4 Organic carbon content -- 3.2.3.5 Metallic elements -- 3.2.3.6 Heavy minerals -- 3.2.3.7 Clay mineralogy -- 3.2.3.8 Mineral magnetic analysis -- 3.2.3.9 Stable isotope analysis -- 3.3. Glacial sediments -- 3.3.1 Introduction -- 3.3.2 The nature of glacial sediments -- 3.3.2.1 Unstratified and stratified sediments -- 3.3.2.2 Glacigenic facies -- 3.3.3 The classification of tills -- 3.3.3.1 Lodgement, melt-out and 'flow' tills -- 3.3.3.2 Deformation tills -- 3.3.3.3 Paraglacial deposits -- 3.3.4 The influence of the thermal regime of glacier ice -- 3.3.5 Analysis of glacigenic sequences -- 3.3.5.1 Particle size and shape analysis -- 3.3.5.2 Lithofacies interpretations -- 3.3.6 Ice-directional indicators -- 3.3.6.1 Erratics -- 3.3.6.2 Till fabrics.
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3.3.6.3 Properties of the till matrix -- 3.4 Periglacial sediments -- 3.4.1 Introduction -- 3.4.2 Structures associated with permafrost -- 3.4.3 Palaeoclimatic significance of periglacial structures -- 3.5 Palaeosols -- 3.5.1 Introduction -- 3.5.2 The nature of palaeosols -- 3.5.3 Analysis of palaeosols -- 3.5.4 Palaeosols and Quaternary environments -- 3.6 Wind-blown sediments -- 3.6.1 Introduction -- 3.6.2 Loess stratigraphy -- 3.6.3 Mid-latitude sand belts (coversands) -- 3.6.4 Low-latitude 'sand seas' -- 3.6.5 Wind-blown sediments and palaeoenvironmental reconstructions -- 3.7 Lake-level records from low-latitude regions -- 3.7.1 Introduction -- 3.7.2 Pluvial lake sediment sequences -- 3.7.3 Lake-level changes and Quaternary palaeoclimates -- 3.8 Cave sediments and carbonate deposits -- 3.8.1 Introduction -- 3.8.2 Detrital sediment in caves -- 3.8.3 Speleothem -- 3.8.4 Speleothem growth and environmental reconstruction -- 3.8.4.1 Speleothem growth and climatic change -- 3.8.4.2 Stable isotope ratios in cave speleothem -- 3.8.4.3 Trace elements in cave speleothem -- 3.8.4.4 Speleothem formation and sea-level variations -- 3.8.4.5 Speleothem formation and tectonic activity -- 3.8.4.6 Speleothem formation and rates of denudation -- 3.8.5 Other carbonate deposits -- 3.9 Lake, mire and bog sediments -- 3.9.1 Introduction -- 3.9.2 The nature of lake and bog sediments -- 3.9.3 Palaeoenvironmental evidence from lake sediments -- 3.9.3.1 Lake sediments and landscape changes -- 3.9.3.2 Lake-level variations and climatic changes -- 3.9.3.3 Lake sediments and palaeotemperatures -- 3.9.4 Palaeoenvironmental evidence from mire and bog sediments -- 3.9.4.1 Palaeoprecipitation records from ombrotrophic peats -- 3.9.4.2 Stable isotope records from ombrotrophic peats -- 3.9.4.3 Human impact recorded in ombrotrophic peat -- 3.10 The deep-sea sediment record.
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3.10.1 The nature and origin of ocean sediments -- 3.10.2 Oxygen isotope ratios and the ocean sediment record -- 3.10.2.1 General principles -- 3.10.2.2 Glacial ice storage and the marine oxygen isotope record -- 3.10.2.3 Ice volumes, sea level and the marine oxygen isotope record -- 3.10.2.4 Sea-surface temperatures and the marine oxygen isotope record -- 3.10.3 Limitations of oxygen isotope analysis -- 3.10.3.1 Stratigraphic resolution -- 3.10.3.2 Sediment mixing -- 3.10.3.3 Isotopic equilibrium between test carbonate and ocean water -- 3.10.3.4 Carbonate dissolution and diagenesis -- 3.10.4 Carbon isotopes in marine sediments -- 3.11 Ice-core stratigraphy -- 3.11.1 A brief history of deep-ice coring -- 3.11.2 Ice masses as palaeoenvironmental archives -- 3.11.3 Analysis of ice cores -- 3.11.3.1 Annual ice increments -- 3.11.3.2 Dust content -- 3.11.3.3 Chemical content -- 3.11.3.4 Stable isotope records -- 3.11.3.5 Other trace substances -- 3.11.4 Palaeoenvironmental significance of ice cores -- 3.12 Conclusions -- Notes -- 4 Biological evidence -- 4.1 Introduction -- 4.1.1 The nature of the Quaternary fossil record -- 4.1.2 The taphonomy of Quaternary fossil assemblages -- 4.1.3 The interpretation of Quaternary fossil assemblages -- 4.2 Pollen analysis -- 4.2.1 Introduction -- 4.2.2 The nature of pollen and spores -- 4.2.3 Field and laboratory work -- 4.2.4 Pollen diagrams -- 4.2.5 The interpretation of pollen diagrams -- 4.2.6 Applications of pollen stratigraphy -- 4.2.6.1 Local vegetation reconstructions -- 4.2.6.2 Regional vegetation reconstructions -- 4.2.6.3 Space-time reconstructions -- 4.2.6.4 Human impact on vegetation cover -- 4.2.6.5 Pollen data and climatic reconstructions -- 4.3 Diatom analysis -- 4.3.1 Introduction -- 4.3.2 The nature and ecology of diatoms -- 4.3.3 Field and laboratory methods.
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4.3.4 The interpretation of Quaternary diatom records -- 4.3.5 Applications of diatom analysis -- 4.3.5.1 Diatoms as salinity indicators -- 4.3.5.2 Diatoms and pH -- 4.3.5.3 Diatoms and trophic status -- 4.3.5.4 Diatoms and the archaeological record -- 4.3.5.5 Other environmental applications -- 4.4 Plant macrofossil analysis -- 4.4.1 Introduction -- 4.4.2 The nature of plant macrofossils -- 4.4.3 Field and laboratory work -- 4.4.4 Data presentation -- 4.4.5 The interpretation of plant macrofossil data -- 4.4.6 Palaeoenvironmental applications of plant macrofossil studies -- 4.4.6.1 Palaeoclimatic reconstructions -- 4.4.6.2 Forest history -- 4.4.6.3 Charcoal and fire history -- 4.4.6.4 Archaeological records -- 4.5 Fossil insect remains -- 4.5.1 Introduction -- 4.5.2 Coleoptera -- 4.5.3 Laboratory methods -- 4.5.4 Coleopteran analysis and Quaternary environments -- 4.5.4.1 Habitat preferences -- 4.5.4.2 Palaeoclimatic inferences based on coleopteran assemblages -- 4.5.4.3 Insect fossils and archaeology -- 4.5.5 Chironomidae -- 4.6 Non-marine Mollusca -- 4.6.1 Introduction -- 4.6.2 The nature and distribution of molluscs -- 4.6.3 Field and laboratory work -- 4.6.4 Taphonomy of non-marine molluscan assemblages -- 4.6.5 Interpretation of non-marine molluscan assemblages: habitat groups and indices of species diversity -- 4.6.6 Applications of Quaternary non-marine molluscan records -- 4.6.6.1 Biostratigraphic correlation -- 4.6.6.2 Palaeoclimatic reconstructions -- 4.6.6.3 Archaeological relevance -- 4.7 Marine Mollusca -- 4.7.1 Introduction -- 4.7.2 Analysis of marine molluscan assemblages -- 4.7.3 Marine Mollusca and palaeoclimatic inferences -- 4.7.4 Other applications of fossil marine molluscan records -- 4.8 Ostracod analysis -- 4.8.1 The nature and distribution of ostracods -- 4.8.2 Collection and identification.
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4.8.3 Ostracoda in Quaternary studies.
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