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Author: Michael Montenari Publisher: Academic Press ISBN: 0128155183 Category : Science Languages : en Pages : 400
Book Description
Stratigraphy and Time Scale, Volume Three in the Advances in Sequence Stratigraphy series, covers current research across many stratigraphic disciplines, providing information on the most recent developments for the geoscientific research community. This fully commissioned review publication aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, isotope stratigraphy, astrochronology, climatostratigraphy, seismic stratigraphy, biostratigraphy, ice core chronology, cyclostratigraphy, palaeoceanography, sequence stratigraphy, and more. Updated chapters include topics such as the Cyclostratigraphy of shallow-water carbonates – limitations and opportunities, Muschelkalk ramp cycles, Orbital Control on Paleozoic Source Rock Formation, and Cyclostratigraphy in different Jurassic carbonate ramps (Iberian Basin, NE Spain). Contains contributions from leading authorities in the field Informs and updates on all the latest developments in the field Aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, and more
Author: Michael Montenari Publisher: Academic Press ISBN: 0128155183 Category : Science Languages : en Pages : 400
Book Description
Stratigraphy and Time Scale, Volume Three in the Advances in Sequence Stratigraphy series, covers current research across many stratigraphic disciplines, providing information on the most recent developments for the geoscientific research community. This fully commissioned review publication aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, isotope stratigraphy, astrochronology, climatostratigraphy, seismic stratigraphy, biostratigraphy, ice core chronology, cyclostratigraphy, palaeoceanography, sequence stratigraphy, and more. Updated chapters include topics such as the Cyclostratigraphy of shallow-water carbonates – limitations and opportunities, Muschelkalk ramp cycles, Orbital Control on Paleozoic Source Rock Formation, and Cyclostratigraphy in different Jurassic carbonate ramps (Iberian Basin, NE Spain). Contains contributions from leading authorities in the field Informs and updates on all the latest developments in the field Aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, and more
Author: Graham P. Weedon Publisher: Cambridge University Press ISBN: 1139435175 Category : Science Languages : en Pages : 275
Book Description
Increasingly environmental scientists, palaeoceanographers and geologists are collecting quantitative records of environmental changes (time-series) from sediments, ice cores, cave calcite, corals and trees. This book explains how to analyse these records, using straightforward explanations and diagrams rather than formal mathematical derivations. All the main cyclostratigraphic methods are covered including spectral analysis, cross-spectral analysis, filtering, complex demodulation, wavelet and singular spectrum analysis. Practical problems of time-series analysis, including those of distortions of environmental signals during stratigraphic encoding, are considered in detail. Recent research into various types of tidal and climatic cycles is summarised. The book ends with an extensive reference section, and an appendix listing sources of computer algorithms. This book provides the ideal reference for all those using time-series analysis to study the nature and history of climatic and tidal cycles. It is suitable for senior undergraduate and graduate courses in environmental science, palaeoceanography and geology.
Author: Felix Gradstein Publisher: Elsevier ISBN: 0444594485 Category : Science Languages : en Pages : 1175
Book Description
The Geologic Time Scale 2012, winner of a 2012 PROSE Award Honorable Mention for Best Multi-volume Reference in Science from the Association of American Publishers, is the framework for deciphering the history of our planet Earth. The authors have been at the forefront of chronostratigraphic research and initiatives to create an international geologic time scale for many years, and the charts in this book present the most up-to-date, international standard, as ratified by the International Commission on Stratigraphy and the International Union of Geological Sciences. This 2012 geologic time scale is an enhanced, improved and expanded version of the GTS2004, including chapters on planetary scales, the Cryogenian-Ediacaran periods/systems, a prehistory scale of human development, a survey of sequence stratigraphy, and an extensive compilation of stable-isotope chemostratigraphy. This book is an essential reference for all geoscientists, including researchers, students, and petroleum and mining professionals. The presentation is non-technical and illustrated with numerous colour charts, maps and photographs. The book also includes a detachable wall chart of the complete time scale for use as a handy reference in the office, laboratory or field. The most detailed international geologic time scale available that contextualizes information in one single reference for quick desktop access Gives insights in the construction, strengths, and limitations of the geological time scale that greatly enhances its function and its utility Aids understanding by combining with the mathematical and statistical methods to scaled composites of global succession of events Meets the needs of a range of users at various points in the workflow (researchers extracting linear time from rock records, students recognizing the geologic stage by their content)
Author: Kenneth P. Kodama Publisher: John Wiley & Sons ISBN: 1118561287 Category : Science Languages : en Pages : 176
Book Description
Rock magnetic cyclostratigraphy merges environmental magnetism, in which rock magnetic measurements are used to detect past environmental change, and cyclostratigraphy, in which cyclic variations of lithology or a sedimentary rock’s physical properties are related to astronomically-forced paleoclimate change. In addition to providing paleoclimate data, cyclostratigraphy can establish high-resolution chronostratigraphy for a sequence of sedimentary rocks, even at distant times in Earth’s history. This book provides an overview of concepts underlying these two techniques, recipes for the time series analysis of cyclostratigraphy, and case studies to illustrate the variety and breadth of problems addressed by rock magnetic cyclostratigraphy. New Analytical Methods in Earth and Environmental Science Because of the plethora of analytical techniques now available, and the acceleration of technological advance, many earth scientists find it difficult to know where to turn for reliable information on the latest tools at their disposal, and may lack the expertise to assess the relative strengths or limitations of a particular technique. This new series will address these difficulties by providing accessible introductions to important new techniques, lab and field protocols, suggestions for data handling and interpretation, and useful case studies. The series represents an invaluable and trusted source of information for researchers, advanced students and applied earth scientists wishing to familiarise themselves with emerging techniques in their field. All titles in this series are available in a variety of full-colour, searchable e-book formats.
Author: Michael Robert House Publisher: Geological Society Publishing House ISBN: Category : Science Languages : en Pages : 224
Book Description
The metronomic variations of the Earth-Moon system and of the Earth-Sun orbital patterns produce gravitational and temperature effects that alter the physical environment on the Earth's surface. These give an interpenetrating effect of forcing cycles ranging from twice-daily tides, day-night alternations, various tidal patterns and the annual solar pattern. All of these have been used palaeontologically to give precision to short-term age determination in the past. It is cycles of the Milankovitch band that are showing promise of enabling new practical timescales to be established for parts of the geological record. These depend on changes in the Earth-Sun distance and changes in the tilt of the Earth's axis with respect to the Earth's orbit round the Sun. There is increasing evidence that small-scale sedimentary rhythmic couplets may represent the effect of such changes. The disentangling of the interpenetrating cycles to produce an orbital forcing timescale is an exciting problem and challenge for palaeobiology and sedimentology. These should enable numerical dates to be given to bio- and chronostratigraphical timescales and eventually enable many Earth processes to be analysed in real time. The papers in this volume represent major new developments in sedimentological, paIaeontological, geochemical and stratigraphical research being undertaken in this field.--Provided by publisher.--Provided by publisher.
Author: Nicholas Benetti Sullivan Publisher: ISBN: Category : Languages : en Pages : 0
Book Description
The study of deep time is crucial for contextualizing present and future environmental change. This is particularly true for the high southern latitudes, a linchpin of the global climate system. However, assembling and compositing a complete, high-resolution sedimentary archive in these regions is often difficult, owing to a range of logistical, environmental, and stratigraphic challenges. Two quantitative methodologies are brought to bear on these problems. The first is stratigraphic constrained optimization (CONOP), a tool for compiling individual, imperfect, local stratigraphic sections into a parsimonious composite succession. The second is astrochronology, a branch of cyclostratigraphy focused on the recognition of astronomically influenced climate rhythms (Milankovitch Cycles) in the stratigraphic record. The findings presented here, using these approaches, provide insight into past environmental and oceanographic change occurring at timescales ranging from millennia to millions of years. Chapter 1 of this dissertation presents strategies for calibrating timescales generated by CONOP with the geochronological information encoded in astrochronology. A synthesis of new and published cyclostratigraphic records in the Southern Ocean are reviewed. These are then used to help refine and calibrate a CONOP output, and four strategies for integrating these interpretations are discussed. Various case studies are used to build a refined composite history for the Southern Ocean. Chapter 2 presents a new Early Miocene cyclostratigraphic analysis of Miocene strata at two ice-proximal sites, IODP U1521 and AND-2A, in the Ross Sea in the Southern Ocean. Astrochronological analysis was conducted on clast abundance data that reflect the proportion of ice-rafted debris. The variable strength of observed obliquity and eccentricity forcing in data across two distinct time intervals (17.4-17.7 Ma and 18.0-18.5 Ma) informs our uncertainty of ice sheet dynamics during the warm climate of the Miocene and helps characterize the different responses of marine influenced versus terrestrial-based ice sheets. These interpretations are then used to inform and develop a new hypothesis relating the evolution of the Antarctic cryosphere to multi-million year "grand cycles" in eccentricity and obliquity. Finally, chapter 3 presents the discovery of astronomically-influenced millennial (1-15 kyr) cycles in early Miocene strata in the core AND-2A from McMurdo Sound. This discovery shows the ubiquity of millennial-scale cyclicity in the southern cryosphere, even during the comparatively warmer Miocene climates that predate a large Northern Hemisphere ice sheet. These findings help us understand the intrinsic behavior of the Antarctic ice sheet and its response to external forcing at a range of temporal scales. The chapters of this dissertation contribute to a better understanding of the temporal dynamics of the Southern Ocean and the Antarctic cryosphere, a complex and dynamic system that may respond to modern climate change in unexpected ways. This has been achieved with the development of new ways of using astrochronology and CONOP together, a methodological advancement that shows promise for application at all levels of the geologic timescale.
Book Description
Stratigraphy and Timescales covers current research across a wide range of stratigraphic disciplines, providing information on recent developments for the geoscientific research community. This fully commissioned review publication aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, isotope stratigraphy, astrochronology, climatostratigraphy, seismic stratigraphy, biostratigraphy, ice core chronology, cyclostratigraphy, palaeoceanography, sequence stratigraphy, and more. Contains contributions from leading authorities in the field Informs and updates on all the latest developments in the field Aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, and more
Author: Andrew D. Miall Publisher: Springer Science & Business Media ISBN: 3662033801 Category : Science Languages : en Pages : 436
Book Description
Sequence stratigraphy represents a new paradigm in geology. The principal hypothesis is that stratigraphie successions may be subdivided into discrete sequences bounded by widespread unconformities. There are two parts to this hypothesis. First, it suggests that the driving forces which generate sequences and their bounding unconformities also generate predietable three-dimensional stratigraphies. In re cent years stratigraphie research guided by sequence models has brought about fundamental im provements in our understanding of stratigraphie processes and the controls of basin architecture. Sequence models have provided a powerful framework for mapping and numerieal modeling, enabling the science of stratigraphy to advance with rapid strides. This research has demonstrated the importance of a wide range of processes for the generation of cyclie sequences, including eustasy, tectonics, and orbital forcing of climate change. The main objective of this book is to document the sequence record and to discuss our current state of knowledge about sequence-generating processes.
Author: Publisher: Academic Press ISBN: 0128130784 Category : Science Languages : en Pages : 456
Book Description
Advances in Sequence Stratigraphy, Volume Two covers current research across a wide range of stratigraphic disciplines, providing information on the most recent developments for the geoscientific research community. Chapters in this volume include Sequence Stratigraphy – Oman, Sequence Stratigraphy and diagenesis, Sequence Stratigraphy of Siliciclastic Systems, Upper Devonian Biostratigraphy, Event Stratigraphy and Late Fransian Kellwasser Extinction Bio-events in the Iowa Basin: Western Euramerica, Sea-level change and Sequence Stratigraphy, Sequence Stratigraphy: A Material-based Approach Versus A Time-Based Approach, and Anisian-Ladinian marker horizon: Implications for sequence stratigraphy and intra-tethyan correlation. This fully commissioned review publication aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, isotope stratigraphy, astrochronology, climatostratigraphy, seismic stratigraphy, biostratigraphy, ice core chronology, cyclostratigraphy, palaeoceanography, sequence stratigraphy, and more. Contains contributions from leading authorities in the field Informs and updates on all the latest developments in the field Aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, and more
Author: Meil D. Opdyke Publisher: Academic Press ISBN: 0080535720 Category : Science Languages : en Pages : 361
Book Description
Magnetic Stratigraphy is the most comprehensive book written in the English language on the subject of magnetic polarity stratigraphy and time scales. This volume presents the entirety of the known geomagneticrecord, which now extends back about 300 million years. The book includes the results of current research on sea floor spreading, magnetic stratigraphy of the Pliocene and Pleistocene, and postulations on the Paleozoic. Also included are both historicalbackground and applications of magnetostratigraphy. Individual chapters on correlation are presented, using changes in magnetic properties and secular variation. Key Features* Discusses pioneering work in the use of marine sediments to investigate the Earths magnetic field* Serves as a guide for students wishing to begin studies in magnetostratigraphy* Provides a comprehensive guide to magnetic polarity stratigraphy including up-to-date geomagnetic polarity time scales* Correlates magnetic stratigraphics from marine and non-marine Cenozoic sequences* Details reversal history of the magnetic field for the last 350 million years* Discusses correlation using magnetic dipole intensity changes* Up-to-date correlation of biostratigraphy with magnetic stratigraphy through the late Jurassic