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  • Historical Geology  (86)
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  • 1
    Call number: M 99.0228/3 ; M 91.1205 (2/3) ; AWI Bio-99-0090
    In: Süßwasserflora von Mitteleuropa : Band 2: Bacillariophyceae, Teil 3
    Type of Medium: Monograph available for loan
    Pages: XIII, 576 Seiten , Illustrationen
    ISBN: 3437305417
    Classification:
    Historical Geology
    Language: German
    Note: Inhalt: I. Allgemeiner Teil. - 1. Terminologie. - II. Spezieller Teil. - A. Ordnung Centrales. - 1. Melosira Agardh [Krammer]. - 2. Orthoseira Thwaites [Krammer]. - 3. Ellerbeckia Crawford [Krammer]. - 4. Aulacoseira Thwaites [Krammer]. - 5. Cyclotella (Kützing) Brébisson [Håkansson]. - 6. Cyclostephanos Round [Håkansson]. - 7. Stephanodiscus Ehrenberg [Håkansson]. - 8. Thalassiosira Cleve [Håkansson]. - 9. Stephanocostis Genkai & Kuzmin [Håkansson]. - 10. Skeletonema Greville [Krammer]. - 11. Acanthoceras Honigmann [Krammer]. - 12. Chaetoceros Ehrenberg [Krammer]. - 13. Rhizosolenia Ehrenberg [Krammer]. - 14. Pleurosira (Meneghini) Trevisan [Krammer]. - 15. Actinocyclus Ehrenberg [Krammer]. - B. Ordnung Pennales. - Familie Fragilariaceae Hustedt. - 1. Tetracyclus Ralfs [Krammer]. - 2. Diatoma Bory [Krammer]. - 3. Meridion Agardh [Krammer]. - 4. Asterionella Hassall [Krammer]. - 5. Tabellaria Ehrenberg [Lange-Bertalot]. - 6. Synedra Ehrenberg [Lange-Bertalot]. - 7. Fragilaria Lyngbye [Lange-Bertalot]. - 1. Untergattung Fragilarias ensu Lange-Bertalot. - 2. Untergattung Alterasynedra Lange-Bertalot. - 3. Untergattung Ctenophora (Grunow) Lange-Bertalot. - 4. Untergattung Tabularia (Kützing) Lange-Bertalot. - 5. Untergattung Staurosira (Ehrenberg) Lange-Bertalot. - 8. Opephora Petit [Lange-Bertalot]. - 9. Hannaea Patrick [Lange-Bertalot]. - 10. Centronella Voigt [Lange-Bertalot]. - Familie Eunotiaceae Kützing [Lange-Bertalot unter Mitarb. v. Nörpel]. - 1. Eunotia Ehrenberg. - 2. Actinella Lewis. - 3. Peronia Brébisson & Arnott. - Tafeln 1-166. - Namenverzeichnis.
    Location: Upper compact magazine
    Location: Upper compact magazine
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    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Amsterdam : Elsevier
    Call number: M 17.90812
    Description / Table of Contents: Front Cover -- ADDRESSES/INSTITUTIONS -- A Concise Geologic Time Scale -- A Concise Geologic Time Scale -- Copyright -- CONTENTS -- 1 - Introduction -- Geologic time scale and this book -- International divisions of geologic time and their global boundaries (GSSPs) -- Biologic, chemical, sea-level, geomagnetic, and other events or zones -- Assigned numerical ages -- Time Scale Creator database and chart-making package -- Geologic Time Scale 2020 -- Selected publications and websites -- 2 - PLANETARY TIME SCALE -- Introduction -- The Moon -- Mars -- Mercury -- Venus
    Description / Table of Contents: Other solar system bodies -- Selected publications and websites -- 3 - Precambrian -- Status of international subdivisions -- Summary of Precambrian trends and events, and a potential revised time scale -- Hadean -- Archean -- Proterozoic -- Acknowledgments -- Selected publications and websites -- 4 - Cryogenian and Ediacaran -- Basal definitions and status of international subdivisions -- Cryogenian -- Selected main stratigraphic scales and events -- (1) Stable-isotope stratigraphy, magnetostratigraphy, and selected events -- (2) Biostratigraphy and major trends -- Numerical age model
    Description / Table of Contents: GTS2012 age model and potential future enhancements -- Revised ages compared to GTS2012 -- Acknowledgments -- Selected publications and websites -- 5 - CAMBRIAN -- Basal definition and status of international subdivisions -- Terreneuvian series -- Series 2 -- Series 3 -- Furongian series -- Selected main stratigraphic scales and events -- (1) Biostratigraphy and major trends -- (2) Stable-isotope stratigraphy, magnetostratigraphy, and selected events -- Numerical age model -- GTS2012 age model and potential future enhancements -- Revised ages compared to GTS2012
    Description / Table of Contents: Estimated uncertainties on assigned ages on stage boundaries -- Acknowledgments -- Selected publications and websites -- 6 - ORDOVICIAN -- Basal definition and international subdivisions -- Selected main stratigraphic scales and events -- (1) Biostratigraphy and major trends -- (2) Stable-isotope stratigraphy and selected events -- Numerical age model -- GTS2012 age model and potential future enhancements -- Estimated uncertainties on assigned ages on stage boundaries -- Acknowledgments -- Selected publications and websites -- 7 - SILURIAN -- Basal definition and international subdivisions
    Description / Table of Contents: Selected main stratigraphic scales and events -- (1) Biostratigraphy (marine -- terrestrial) -- (2) Stable-isotope stratigraphy, magnetostratigraphy, and selected events -- Numerical age model -- GTS2012 age model and potential future enhancements -- Estimated uncertainties on assigned ages on stage boundaries -- Acknowledgments -- Selected publications and websites -- 8 - DEVONIAN -- Basal definition and international subdivisions -- Selected main stratigraphic scales and events -- Biostratigraphy (marine -- terrestrial) -- Magnetostratigraphy -- Stable-isotope stratigraphy and selected events
    Description / Table of Contents: Numerical age model
    Type of Medium: Monograph available for loan
    Pages: 243 Seiten
    ISBN: 9780444637710 , 9780444594679
    Classification:
    Historical Geology
    Parallel Title: Print version A Concise Geologic Time Scale : 2016
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Cambridge :Cambridge University Press
    Call number: M 17.90784
    Description / Table of Contents: This work presents up-to-date research achievements from a region that displays unique interactions between climate, the environment and human evolution. Focusing on southeast Turkey, Lebanon, Syria, Jordan and Israel, it brings together over 80 contributions from leading researchers to review 2.5 million years of environmental change and human cultural evolution. Information from prehistoric sites and palaeoanthropological studies contributing to our understanding of 'out of Africa' migrations, Neanderthals, cultures of modern humans, and the origins of agriculture are assessed within the context of glacial-interglacial cycles, marine isotope cycles, plate tectonics, geochronology, geomorphology, palaeoecology and genetics. Complemented by overview summaries that draw together the findings of each chapter, the resulting coverage is wide-ranging and cohesive. The cross-disciplinary nature of the volume makes it an invaluable resource for academics and advanced students of Quaternary science and human prehistory, as well as being an important reference for archaeologists working in the region
    Type of Medium: Monograph available for loan
    Pages: XV, 771 Seiten
    ISBN: 9781107090460
    Classification:
    Historical Geology
    Language: English
    Location: Upper compact magazine
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  • 4
    Call number: M 16.90275
    Description / Table of Contents: Preface -- Contents -- Contributors -- Part I: Limnology, History and Comparative Legends -- 1: Pavin, the Birthplace of French Limnology (1770-2012), and Its Degassing Controversy (1986-2016) -- 1.1 Introduction -- 1.2 Analysis of Pavin Actors, History and Perception Through an Interdisciplinary and Intercomparative Approach -- 1.3 Pavin, a Typical Maar-Lake Above any Contamination Source -- 1.3.1 Pavin General Features -- 1.3.2 Pavin Compared to Other Lakes of the Cézallier Lake District -- 1.3.3 Pavin Compared to Other European Maar-Lakes -- 1.3.3.1 Eifel Lakes
    Description / Table of Contents: 1.3.3.2 Italian Lakes -- 1.4 Pavin Scientific Exploration (1770-1985) -- 1.4.1 Chevalier's Expedition (1770) -- 1.4.2 Lecoq, the Great Auvergne Naturalist, Normalizes Pavin… with Fishes (1847-1871) -- 1.4.3 The First Golden Age of Science at Pavin: Berthoule, Delebecque, Martel, Bruyant (1880-1914) -- 1.4.3.1 Clermont Botanists and Zoologists Establish the Limnological Station at Besse -- 1.4.3.2 André Delebecque at Pavin (1892) -- 1.4.3.3 Edouard-Alfred Martel at Creux de Soucy (1892) -- 1.4.4 Pavin Meromixis Discovery by Olivier and Pelletier (1950-1960s)
    Description / Table of Contents: 1.5 Pavin Acquires a Status of International Field Laboratory (1965-2000) -- 1.5.1 International Projects Select Pavin as a Pristine Lake (1965-1975) -- 1.5.2 Pavin, a Laboratory for Innovative Lake Research (1965-1986) -- 1.6 Maar Lakes Degassing Evidence in Cameroun and Italy -- 1.6.1 Nyos (21 August 1986) and Monoun (15 August 1984) Degassing Events and Their Effects on Populations -- 1.6.2 Ancient Degassing Events in Italian Maar-Lakes, Albano and Monticchio -- 1.6.2.1 The Albano Catastrophic Degassing and Spillover Event in Latium (398 BC)
    Description / Table of Contents: 1.6.2.2 Monticchio Lakes (Southern Italy) and Their Pioneer Degassing Studies, 1777-1838 -- 1.7 Sensory Grid of Degassing in Maar-Lakes -- 1.8 Pavin Degassing Controversy (1986-2016) -- 1.9 Conclusions -- References -- 2: Pavin, A Rich but Fragmented History (200 AD-2016) -- 2.1 Introduction -- 2.2 Finding Pavin Puzzle Pieces -- 2.3 Pavin's History Highlights -- 2.3.1 Antiquity: A Pompeian Millstone Retrieved from Pavin Waters in 1909 -- 2.3.2 Early Antique and Medieval Worship Near Pavin, on the Vassivière Mountain
    Description / Table of Contents: 2.3.3 Lacus pavens Terrifies the Whole Region Throughout the Sixteenth Century -- 2.3.3.1 The Terrible Explosion Witnessed at Vassivière by Besse People (28 August 1551 Pavin Event) -- 2.3.3.2 A Hazardous Abyss, Generating Storm, Thunder and Hail, Presented to Charles IX (1566) -- 2.3.3.3 Pavin Painted on the First Realistic Landscape Picture in France (1571-1579) -- 2.3.3.4 Pavin Marvelous Response to a Thrown Stone in Belleforest's Cosmographia Universalis (1575) -- 2.3.3.5 Lacus pavens, the Terrifying Lake, Is the Original Pavin Name (Banc 1605)
    Description / Table of Contents: 2.3.4 The Admirable and Terrifying Pavens Gets Famous During the Seventeenth Century
    Type of Medium: Monograph available for loan
    Pages: XV, 421 S.
    ISBN: 9783319399607
    Classification:
    Historical Geology
    Language: English
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  • 5
    Monograph available for loan
    Monograph available for loan
    Cham : Springer
    Call number: M 16.89836
    Type of Medium: Monograph available for loan
    ISBN: 9783319295367
    Series Statement: Quantitative archaeology and archaeological modelling
    Classification:
    Historical Geology
    Language: English
    Location: Upper compact magazine
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  • 6
    Call number: 12/ M 15.89487 ; AWI A3-15-89093
    Description / Table of Contents: This is the English translation (and German facsimile) of Wladimir Köppen and Alfred Wegener (1924): The Climates of the Geological Past (Die Klimate der geologischen Vorzeit), a landmark text of early paleoclimatological research. Wegener is best known for his theory of continental drift (The Origin of the Continents and Oceans, 1915). Less widely known, but equally important, are the studies he conducted on the climates of the past (with his colleague and father-in-law, Wladimir Köppen), which they jointly published (this book). Only one edition of the book was published, but unfortunately, all - save a few private copies - were destroyed during the second World War, rendering the book essentially unavailable. This English translation makes Köppen and Wegener's landmark text accessible to the international climate research community. It also includes the 'Supplements and Corrections' by Wladimir Köppen to this book, published in 1940, shortly before his death and a decade after Alfred Wegener's untimely death on Greenland. The discussion of the course and causal relationship of climates and climate change in the geological past are of principal scientific interest. Important elements of the discussions herein stem from the close collaboration with Milutin Milankovitch (who contributed entire sections of text, but is not named as an author). Building on the principles of the Milankovitch frequencies allowed Köppen and Wegener - for the first time, early in the last century - to establish a precise time scale of Late Cenozoic glacial-interglacial cycles. More recently, the orbital parameters originally calculated by Milankovitch were refined using time series data from deep-sea sediments and ice cores. Furthermore, Milankovitch's cycles may be extrapolated into the future to predict climate change. This very book, in which Köppen and Wegener roll out their theory, is therefore an important publication which has early on shaped our understanding of how climate has evolved and continuously evolves in the course of time. This translation affords non-German-speaking scientists and laypersons alike access to the full and compelling arguments of climate change, carefully and readably laid out and argued. It is a must-read for anybody interested in climate change, be it from a historic or present point of view.
    Type of Medium: Monograph available for loan
    Pages: IX, 657 S.
    Edition: Faksimilie-Nachdruck der dt. Originalausg. und komplette engl. Neuübersetzung
    ISSN: 9783443010881
    Classification:
    Historical Geology
    Note: Inhaltsverzeichnis / Contents: Preface 2015. - Note of the translator. - Die Klimate der geologischen Vorzeit. - Einleitung. - 1. Die fossilen Klimazeugen. - 2. Die Klimagürtel im Karbon und Perm. - 3. Die Klimagürtel im Mesozoikum. - 4. Die Klimagürtel in der Tertiärzeit. - 5. Die Klimate in den vorkarbonischen Zeiten. - 6. Polwege und Breitenänderungen in der Erdgeschichte. - 7. Die Klimate des Quartärs. - Index. - Die Klimate der geologischen Vorzeit - Ergänzungen und Berichtigungen. - The climates of the geological past. - Contents. - Table of figures. - Introduction. - 1. Fossil climate indicators. - 2. The climate belts of the carboniferous and permian. - 3. The climate belts of the Mesozoic. - 4. The climate belts of the tertiary. - 5. The climates of the pre-carboniferous periods. - 6. Pole migrations and latitude changes in earth's history. - 7. Climates of the quaternary. - Index. - The climates of the geological past - supplements and corrections.
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  • 7
    Call number: AWI G5-10-0074 ; M 11.0047
    In: Developments in paleoenvironmental research
    Description / Table of Contents: Chapter 1: High-resolution Paleoclimatology - R. Bradley What is high-resolution paleoclimatology? What are its major achievements? What opportunities and challenges does it now face? What should dendroclimatology's role be in this? Chapter 2: Dendroclimatology in high-resolution Paleoclimatology - M. K. Hughes, H. F. Diaz and Th. W. Swetnam An overview of the development of dendroclimatology and an introduction to the questions posed in this book. Scientific bases of dendroclimatology Chapter 3: How well understood are the processes that create tree-ring records? - G. Vaganov Starting at the most basic level of the environmental control of tree-ring formation, do we have the necessary biological and ecophysiological understanding of this to support inferences about climate variability from tree rings? What are the weak points of this understanding and how might they be strengthened? Chapter 4: The state of the art of quantitative methods in dendroclimatology - E. Cook How sound are the quantitative techniques commonly used in dendroclimatology, in chronology building, identification and reconstruction of climate variables and the checking of these reconstructions? Are they appropriate to the material being analyzed and to the climatological problems being addressed? How might they be improved? Chapter 5: Detecting low-frequency change using tree rings - K. Briffa What limits the ability of tree-ring records to faithfully record climate variability at low frequencies (multi-centennial to millennial)? How might those limitations be overcome, if at all? What are the advantages and limitations of older and more novel approaches? What are the implications of these limitations? Reconstruction of climate patterns and values relative to today's climate Chapter 6: Dendroclimatology at regional and continental scales - R. Villalba What have been the major contributions of dendroclimatology to climatology so far? In what regions and for which climate problems is exciting progress now being made? What next? Chapter 7: Dendroclimatology at hemispheric and global scales - M. K. Hughes and M. Mann What are the achievements of dendroclimatology as applied at hemispheric and global scales climate patterns, circulation indices and large-scale means? What are the limitations of this approach? How might they be overcome? How might dendroclimatology contribute to the study of central pressing problems such as "How big is climate sensitivity? How has the last century, and especially recent decades, compared with earlier centuries? How faithful a representation of variability in recent centuries does the 20th century instrumental record give? Particular attention will be given to: a) identifying the most robust findings; and b) the most serious limitations. Chapter 8: Dendroclimatology, dendrohydrology and water resources management - C. Woodhouse and D. Meko How may dendroclimatology contribute to the study of water resources? How may it be used to inform modern public and decision-maker expectations of climate variability? Chapter 9: Dendroclimatology and the ecosystem impacts of climate - Th. W. SwetnamHow has dendroclimatology contributed to disturbance ecology? What is the significance of the recent changes in tree-growth-climate relationships observed in some regions, not only for dendroclimatology, but also for the understanding of the impacts of climate variability and change on ecosystems? Chapter 10: Dendroclimatology and the understanding of the interactions between climate variability and ancient human societies - D. Stahle and J. DeanHow has dendroclimatology contributed to understanding of the relationships between climate variability and societies in ancient times? Chapter 11: Tree rings and climate- sharpening the focus - M. K. Hughes, H. F. Diaz and Th. W. Swetnam What has been learned, using tree rings, about natural climate variability and its environmental and social impacts? What are the most significant strengths and weaknesses of dendroclimatology and the needs of, and opportunities for, future work.
    Description / Table of Contents: This volume presents an overview of the current state of dendroclimatology, its contributions over the last 30 years, and its future potential. The material included is useful not only to those who generate tree-ring records of past climate-dendroclimatologists, but also to users of their results - climatologists, hydrologists, ecologists and archeologists.
    Type of Medium: Monograph available for loan
    Pages: xii, 365 S. : Ill., graph. Darst.
    ISBN: 9781402040108
    Series Statement: Developments in paleoenvironmental research 11
    Classification:
    Historical Geology
    Language: English
    Note: Contents: Part I Introductory Section. - 1 High-Resolution Paleoclimatology / Raymond S. Bradley. - 2 Dendroclimatology in High-Resolution Paleoclimatology / Malcolm K. Hughes. - Part II Scientific Bases of Dendroclimatology. - 3 How Well Understood Are the Processes that Create Dendroclimatic Records? A Mechanistic Model of the Climatic Control on Conifer Tree-Ring Growth Dynamics / Eugene A. Vaganov, Kevin J. Anchukaitis, and Michael N. Evans. - 4 Uncertainty, Emergence, and Statistics in Dendrochronology / Edward R. Cook and Neil Pederson. - 5 A Closer Look at Regional Curve Standardization of Tree-Ring Records: Justification of the Need, a Warning of Some Pitfalls, and Suggested Improvements in Its Application / Keith R. Briffa and Thomas M. Melvin. - 6 Stable Isotopes in Dendroclimatology: Moving Beyond ‘Potential’ / Mary Gagen, Danny McCarroll, Neil J. Loader, and Iain Robertson. - Part III Reconstruction of Climate Patterns and Values Relative to Today’s Climate. - 7 Dendroclimatology from Regional to Continental Scales: Understanding Regional Processes to Reconstruct Large-Scale Climatic Variations Across the Western Americas / Ricardo Villalba, Brian H. Luckman, Jose Boninsegna,Rosanne D. D’Arrigo, Antonio Lara, Jose Villanueva-Diaz, Mariano Masiokas, Jaime Argollo, Claudia Soliz, Carlos LeQuesne, David W. Stahle, Fidel Roig, Juan Carlos Aravena, Malcolm K. Hughes, Gregory Wiles, Gordon Jacoby, Peter Hartsough, Robert J.S. Wilson, Emma Watson, Edward R. Cook, Julian Cerano-Paredes, Matthew Therrell, Malcolm Cleaveland, Mariano S. Morales, Nicholas E. Graham, Jorge Moya, Jeanette Pacajes, Guillermina Massacchesi, Franco Biondi, Rocio Urrutia, and Guillermo Martinez Pastur. - Part IV Applications of Dendroclimatology. - 8 Application of Streamflow Reconstruction to Water Resources Management / David M. Meko and Connie A. Woodhouse. - 9 Climatic Inferences from Dendroecological Reconstructions / Thomas W. Swetnam and Peter M. Brown. - 10 North American Tree Rings, Climatic Extremes, and Social Disasters / David W. Stahle and Jeffrey S. Dean. - Part V Overview. - 11 Tree Rings and Climate: Sharpening the Focus / Malcolm K. Hughes, Henry F. Diaz, and Thomas W. Swetnam. - Index.
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  • 8
    Monograph available for loan
    Monograph available for loan
    San Diego : Society of Natural History
    Associated volumes
    Call number: M 98.0029
    In: The geology and paleontology of marine pliocene of San Diego, California
    Type of Medium: Monograph available for loan
    Classification:
    Historical Geology
    Language: English
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  • 9
    Call number: M 98.0239
    Type of Medium: Dissertations
    Pages: 115 S. + Anhänge
    Classification:
    Historical Geology
    Language: German
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  • 10
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Call number: M 98.0363 ; AWI G8-96-0626
    Type of Medium: Monograph available for loan
    Pages: XV, 433 Seiten , Illustrationen
    ISBN: 3540593489
    Classification:
    Historical Geology
    Language: English
    Note: Contents I Review of Current Concepts 1 Introduction 1.1 Sequence Stratigraphy: A New Paradigm? 1.2 From Sloss to Vail 1.3 Problems and Research Trends: The Current Status 1.4 Stratigraphic Terminology 2 Methods for Studying Sequence Stratigraphy 2.1 Introduction 2.2 Erecting a Sequence Framework 2.2.1 The Importance of Unconformities 2.2.2 Facies Cycles 2.2.3 Stratigraphic Architecture: The Seismic Method 2.3 Methods for Assessing Regional and Global Changes in Sea Level, Other Than Seismic Stratigraphy 2.3.1 Areas and Volumes of Stratigraphic Units 2.3.2 Hypsometric Curves 2.3.3 Backstripping 2.3.4 Sea-Level Estimation from Paleoshorelines and Other Fixed Points 2.3.5 Documentation of Meter-Scale Cycles 2.4 Integrated Tectonic-Stratigraphic Analysis 3 The Four Basic Types of Stratigraphic Cycle 3.1 Introduction 3.2 The Supercontinent Cycle 3.3 Cycles with Episodicities of Tens of Millions of Years 3.4 Cycles with Million-Year Episodicities 3.5 Cycles with Episodicities of Less Than One Million Years 4 The Basic Sequence Model 4.1 Introduction 4.2 Terminology 4.3 Depositional Systems and Systems Tracts 4.4 Sequence Boundaries 4.5 Other Sequence Concepts 5 The Global Cycle Chart II The Stratigraphic Framework 6 Cycles with Episodicities of Tens to Hundreds of Millions of Years 6.1 Climate, Sedimentation, and Biogenesis 6.2 The Supercontinent Cycle 6.2.1 The Tectonic-Stratigraphic Model 6.2.2 The Phanerozoic Record 6.3 Cycles with Episodicities of Tens of Millions of Years 6.3.1 Intercontinental Correlations 6.3.2 Tectonostratigraphic Sequences 6.4 Main Conclusions 7 Cycles with Million-Year Episodicities 7.1 Extensional and Rifted Clastic Continental Margins 7.2 Foreland Basin of the North American Western Interior 7.3 Other Foreland Basins 7.4 Forearc Basins 7.5 Backarc Basins 7.6 Cyclothems and Mesothems 7;7 Carbonate Cycles of Platforms and Craton Margins 7.8 Evidence of Cyclicity in the Deep Oceans 7.9 Main Conclusions 8 Cycles with Episodicities of Less Than One Million Years 8.1 Introduction 8.2 Neogene Clastic Cycles of Continental Margins 8.3 Pre-Neogene Marine Carbonate and Clastic Cycles 8.4 Late Paleozoic Cyclothems 8.5 Lacustrine elastic and Chemical Rhythms 8.6 Clastic Cycles of Foreland Basins 8.7 Main Conclusions III Mechanisms 9 Long-Term Eustasy and Epeirogeny 9.1 Mantle Processes and Dynamic Topography 9.2 Supercontinent Cycles 9.3 Cycles with Episodicities of Tens of Millions of Years 9.3.1 Eustasy 9.3.2 Dynamic Topography and Epeirogeny 9.4 Main Conclusions 10 Milankovitch Processes 10.1 Introduction 10.2 The Nature of Milankovitch Processes 10.2.1 Components of Orbital Forcing 10.2.2 Basic Climatology 10.2.3 Variations with Time in Orbital Periodicities 10.2.4 Isostasy and Geoid Changes 10.2.5 The Nature of the Cyclostratigraphic Data Base 10.2.6 The Sensitivity of the Earth to Glaciation 10.2.7 Glacioeustasy in the Mesozoic? 10.2.8 Nonglacial Milankovitch Cyclicity 10.3 The Cenozoic Record 10.4 Late Paleozoic Cyclothems 10.5 The End-Ordovician Glaciation 10.6 Main Conclusions 11 Tectonic Mechanisms 11.1 Introduction 11.2 Rifting and Thermal Evolution of Divergent Plate Margins 11.2.1 Basic Geophysical Models and Their Implications for Sea-Level Change 11.2.2 Some Results from the Analysis of Modern Data Sets 11.3 Tectonism on Convergent Plate Margins and in Collision Zones 11.3.1 Magmatic Arcs and Subduction 11.3.2 Tectonism Versus Eustasy in Foreland Basins 11.3.2.1 The North American Western Interior Basin 11.3.2.2 The Appalachian Foreland Basin 11.3.2.3 Pyrenean and Himalayan Basins 11.3.3 Rates of Uplift and Subsidence 11.3.4 Discussion 11.4 Intraplate Stress 11.4.1 The Pattern of Global Stress 11.4.2 In-Plane Stress as a Control of Sequence Architecture 11.4.3 In-Plane Stress and Regional Histories of Sea-Level Change 11.5 Basement Control 11.6 Other Speculative Tectonic Hypotheses 11.7 Sediment Supply and the Importance of Big Rivers 11.8 Environmental Change 11.9 Main Conclusions IV Chronostratigraphy and Correlation: Why the Global Cycle Chart Should Be Abandoned 12 Time in Sequence Stratigraphy 12.1 Introduction 12.2 Hierarchies of Time and the Completeness of the Stratigraphic Record 12.3 Main Conclusions 13 Correlation, and the Potential for Error 13.1 Introduction 13.2 The New Paradigm of Geological Time? 13.3 The Dating and Correlation of Stratigraphic Events: Potential Sources of Uncertainty 13.3.1 Identification of Sequence Boundaries 13.3.2 Chronostratigraphic Meaning of Unconformities 13.3.3 Determination of the Biostratigraphic Framework 13.3.3.1 The Problem of Incomplete Biostratigraphic Recovery 13.3.3.2 Diachroneity of the Biostratigraphic Record 13.3.4 The Value of Quantitative Biostratigraphic Methods 13.3.5 Assessment of Relative Biostratigraphic Precision 13.3.6 Correlation of Biozones with the Global Stage Framework 13.3.7 Assignment of Absolute Ages 13.3.8 Implications for the Exxon Global Cycle Chart 13.4 Correlating Regional Sequence Frameworks with the Global Cycle Chart 13.4.1 Circular Reasoning from Regional Data 13.4.2 A Rigorous Test of the Global Cycle Chart 13.4.3 A Correlation Experiment 13.4.4 Discussion 13.5 Main Conclusions 14 Sea-Level Curves Compared 14.1 Introduction 14.2 The Exxon Curves: Revisions, Errors, and Uncertainties 14.3 Other Sea-Level Curves 14.3.1 Cretaceous Sea-Level Curves 14.3.2 Jurassic Sea-Level Curves 14.3.3 Why Does the Exxon Global Cycle Chart Contain So Many More Events Than Other Sea-Level Curves? 14.4 Main Conclusions V Approaches to a Modern Sequence-Stratigraphic Framework 15 Elaboration of the Basic Sequence Model 15.1 Introduction 15.2 Definitions 15.2.1 The Hierarchy of Units and Bounding Surfaces 15.2.2 Systems Tracts and Sequence Boundaries 15.3 The Sequence Stratigraphy of Clastic Depositional Systems 15.3.1 Pluvial Deposits and Their Relationship to Sea-Level Change 15.3.2 The Concept of the Bayline 15.3.3 Deltas, Beach-Barrier Systems, and Estuaries 15.3.4 Shelf Systems: Sand Shoals and Condensed Sections 15.3.5 Slope and Rise Systems 15.4 The Sequence Stratigraphy of Carbonate Depositional Systems 15.4.1 Platform Carbonates: Catch-Up Versus Keep-Up 15.4.2 Carbonate Slopes 15.4.3 Pelagic Carbonate Environments 15.5 Main Conclusions 16 Numerical and Graphical Modeling of Sequences 16.1 Introduction 16.2 Model Design 16.3 Selected Examples of Model Results 16.4 Main Conclusions VI Discussion and Conclusions 17 Implications for Petroleum Geology 17.1 Introduction 17.2 Integrated Tectonic-Stratigraphic Analysis 17.2.1 The Basis of the Methodology 17.2.2 The Development of an Allostratigraphic Framework 17.2.3 Choice of Sequence-Stratigraphic Models 17.2.4 The Search for Mechanisms 17.2.5 Reservoir Characterization 17.3 Controversies in Practical Sequence Analysis 17.3.1 The Case of the Tocito Sandstone, New Mexico 17.3.2 The Case of Gippsland Basin, Australia 17.3.3 Conclusions: A Modified Approach to Sequence Analysis for Practicing Petroleum Geologists and Geophysicists 17.4 Main Conclusions 18 Conclusions and Recommendations 18.1 Sequences in the Stratigraphic Record 18.1.1 Long-Term Stratigraphic Cycles 18.1.2 Cycles with Million-Year Episodicities 18.1.3 Cycles with Episodicities of Less Than One Million Years 18.2 Mechanisms 18.2.1 Long-Term Eustasy and Epeirogeny 18.2.2 Milankovitch Processes 18.2.3 Tectonic Mechanisms 18.3 Chronostratigraphy and Correlation 18.3.1 Concepts of Time 18.3.2 Correlation Problems, and the Basis of the Global Cycle Chart 18.3.3 Comparison of Sea-Level Curves 18.4 Modern Sequence Analysis 18.4.1 Elaboration of the Basic Sequence Model 18.4.2 Numerical and Graphical Modeling of Stratigraphic Sequences 18.5 Implications for Petroleum Geology 18.6 The Global-Eustasy Paradigm: Working Backwards from the Answer? 18.6.1 The Exxon Factor 18.6.2 Conclusions . 18.7 Recommendations References Author Index Subject Index
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