The Last Deglaciation: Absolute and Radiocarbon Chronologies (Nato ASI Series (closed) / Nato ASI Subseries I: (closed)) (Nato ASI Subseries I:, 2, Band 2) - Softcover

Name: The Last Deglaciation: Absolute and Radiocarbon Chronologies (Nato ASI Series (closed) / Nato ASI Subseries I: (closed)) (Nato ASI Subseries I:, 2, Band 2)
Author: Bard, Edouard
ISBN: 9783642760617

Bard, Edouard

9783642760617: The Last Deglaciation: Absolute and Radiocarbon Chronologies (Nato ASI Series (closed) / Nato ASI Subseries I: (closed)) (Nato ASI Subseries I:, 2, Band 2)

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ISBN 10: 3642760619 ISBN 13: 9783642760617

Verlag: Springer, 2012

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The main focus of the book is the last deglaciation - a period of intense and rapid climatic changes which affected the global climate approximately 20,000 to 50,000 years ago. Special emphasis is placed on the timing of the last deglaciation in order to provide a common absolute chronological framework for the numerous researchers in the field. Accordingly, results obtained from the various scientific disciplines, relevant for the chronological problem, are reviewed and discussed: from glaciology, varved clay sedimentology, paleomagnetism, dendrochronology and radiochronology (14C and U/Th).

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Verlag: Springer
Erscheinungsdatum: 2012
Sprache: Englisch
ISBN 10: 3642760619
ISBN 13: 9783642760617
Einband: Taschenbuch
Anzahl der Seiten: 364
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The Last Deglaciation: Absolute and Radiocarbon Chronologies (eng)

Broecker, Wallace S.

Verlag: Springer, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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The Last Deglaciation: Absolute and Radiocarbon Chronologies

Wallace S. Broecker

Verlag: Springer Berlin Heidelberg, Springer Berlin Heidelberg Feb 2012, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Time is a major factor in Quaternary science. Without a trustworthy chronometer any interpretation of changes in proxy data of stratigraphical origin is on weak ground. In fact, any attempt at a sound reconstruction of timing and rates of past climatic change as well as the response of the biosphere can only be achieved on the basis of a reliable chronology. Moreover, all correlations and comparisons through time on a continental or global scale depend heavily on the reliability of the time-scale used. Therefore the establishment of an absolute time-scale is a fundamental goal. In this contribution we refer to the term 'absolute time-scale' as a time-scale consisting of ages determined on the basis of sidereal years. Traditional stratigraphical methods of absolute dating include the Swedish glacial varve chronology, already developed early in this century by De Geer (1912) and since then continuously improved (e.g. Stromberg 1985; Cato 1987). Unfortunately, however, a spatial correlation with other stratigraphies outside Fennoscandia is difficult. 364 pp. Englisch. Bestandsnummer des Verk�ufers 9783642760617

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The Last Deglaciation: Absolute and Radiocarbon Chronologies

Bard, Edouard|Broecker, Wallace S.

Verlag: Springer Berlin Heidelberg, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Time is a major factor in Quaternary science. Without a trustworthy chronometer any interpretation of changes in proxy data of stratigraphical origin is on weak ground. In fact, any attempt at a sound reconstruction of timing and rates of past climatic chan. Bestandsnummer des Verk�ufers 5069951

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The Last Deglaciation: Absolute and Radiocarbon Chronologies (Nato ASI Subseries I:, 2)

Bard, Edouard

Verlag: Springer, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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The Last Deglaciation: Absolute and Radiocarbon Chronologies

Wallace S. Broecker

Verlag: Springer Berlin Heidelberg, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Time is a major factor in Quaternary science. Without a trustworthy chronometer any interpretation of changes in proxy data of stratigraphical origin is on weak ground. In fact, any attempt at a sound reconstruction of timing and rates of past climatic change as well as the response of the biosphere can only be achieved on the basis of a reliable chronology. Moreover, all correlations and comparisons through time on a continental or global scale depend heavily on the reliability of the time-scale used. Therefore the establishment of an absolute time-scale is a fundamental goal. In this contribution we refer to the term 'absolute time-scale' as a time-scale consisting of ages determined on the basis of sidereal years. Traditional stratigraphical methods of absolute dating include the Swedish glacial varve chronology, already developed early in this century by De Geer (1912) and since then continuously improved (e.g. Stromberg 1985; Cato 1987). Unfortunately, however, a spatial correlation with other stratigraphies outside Fennoscandia is difficult. Bestandsnummer des Verk�ufers 9783642760617

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The Last Deglaciation: Absolute and Radiocarbon Chronologies

Wallace S. Broecker

Verlag: Springer Berlin Heidelberg, Springer Feb 2012, 2012

ISBN 10: 3642760619 ISBN 13: 9783642760617

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Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Time is a major factor in Quaternary science. Without a trustworthy chronometer any interpretation of changes in proxy data of stratigraphical origin is on weak ground. In fact, any attempt at a sound reconstruction of timing and rates of past climatic change as well as the response of the biosphere can only be achieved on the basis of a reliable chronology. Moreover, all correlations and comparisons through time on a continental or global scale depend heavily on the reliability of the time-scale used. Therefore the establishment of an absolute time-scale is a fundamental goal. In this contribution we refer to the term 'absolute time-scale' as a time-scale consisting of ages determined on the basis of sidereal years. Traditional stratigraphical methods of absolute dating include the Swedish glacial varve chronology, already developed early in this century by De Geer (1912) and since then continuously improved (e.g. Stromberg 1985; Cato 1987). Unfortunately, however, a spatial correlation with other stratigraphies outside Fennoscandia is difficult.Springer-Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 364 pp. Englisch. Bestandsnummer des Verk�ufers 9783642760617

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