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This comprehensive synthesis of our knowledge of the biostratigraphy of marine plankton is the work of an international team of eighteen authors. It covers all the major fossil groups that can be used to date sediments and rocks in the time interval Late Mesozoic to Holocene. Altogether more than 3200 taxa are considered, almost all of which are illustrated and depicted on range charts, making the book a valuable work of reference in the earth sciences. For ease of reference by specialists interested in either calcareous or non-calcareous microfossils, the original work is now divided into two independent volumes. Volume 2 describes siliceous and other non-calcareous microfossils, covering radiolaria, diatoms, silicoflagellates, dinoflagellates and ichthyoliths.
This comprehensive synthesis of our knowledge of the biostratigraphy of marine plankton is the work of an international team of eighteen authors. It covers all the major fossil groups that can be used to date sediments and rocks in the time interval Late Mesozoic to Holocene. Altogether more than 3200 taxa are considered, almost all of which are illustrated and depicted on range charts, making the book a valuable work of reference in the earth sciences. For ease of reference by specialists interested in either calcareous or non-calcareous microfossils, the original work is now divided into two independent volumes. Volume I covers the calcareous microfossils and includes planktic foraminifers, calcareous nannofossils and calpionellids.
Geologic Time Scale 2020 (2 volume set) contains contributions from 80+ leading scientists who present syntheses in an easy-to-understand format that includes numerous color charts, maps and photographs. In addition to detailed overviews of chronostratigraphy, evolution, geochemistry, sequence stratigraphy and planetary geology, the GTS2020 volumes have separate chapters on each geologic period with compilations of the history of divisions, the current GSSPs (global boundary stratotypes), detailed bio-geochem-sequence correlation charts, and derivation of the age models. The authors are on the forefront of chronostratigraphic research and initiatives surrounding the creation of an international geologic time scale. The included charts display the most up-to-date, international standard as ratified by the International Commission on Stratigraphy and the International Union of Geological Sciences. As the framework for deciphering the history of our planet Earth, this book is essential for practicing Earth Scientists and academics. - Completely updated geologic time scale - Provides the most detailed integrated geologic time scale available that compiles and synthesize information in one reference - Gives insights on the construction, strengths and limitations of the geological time scale that greatly enhances its function and its utility
This book provides a benchmark study of southern African landscape evolution during the Quaternary, for researchers, professionals and policymakers.
Each issue contains a "Bibliography and taxa of calcareous nannoplankton."
This monumental synthesis of our knowledge of the biostratigraphy of marine plankton is the work of an international team of thirteen authors, who have contributed nineteen chapters in all. The book covers every aspect of the stratigraphy of plankton, starting with the fossil schemes and then systematically examining the identification of the groups through geological time (from the present to the Cretaceous era). A particular strength of the work is the provision of thousands of photographs and diagrams of particular planktic fossils, making the book an indispensable work of reference in the earth sciences.
There has been a recent upsurge in research into structural geology and sedimentology of Wales. The breadth and the quantity of the activity, particularly in previously under-researched areas, is reflected. Chapters are arranged in approximate time order of the events described and new field data are set in their local tectonic context. Speculation on models for the plate tectonic setting of Early Palaeozoic Wales is included, with an examination of the necessary components.