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The Pleistocene Boundary and the Beginning of the Quaternary [Paperback]

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  • Category: Books (Science)
  • ISBN-10:  0521617022
  • ISBN-10:  0521617022
  • ISBN-13:  9780521617024
  • ISBN-13:  9780521617024
  • Publisher:  Cambridge University Press
  • Publisher:  Cambridge University Press
  • Pages:  320
  • Pages:  320
  • Binding:  Paperback
  • Binding:  Paperback
  • Pub Date:  01-May-2004
  • Pub Date:  01-May-2004
  • SKU:  0521617022-11-MPOD
  • SKU:  0521617022-11-MPOD
  • Item ID: 100916746
  • Seller: ShopSpell
  • Ships in: 2 business days
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  • Delivery by: Jul 09 to Jul 11
  • Notes: Brand New Book. Order Now.
This book documents the agreed geological reference point for the Pleistocene boundary, and its worldwide correlation.The Pleistocene Boundary and the Beginning of the Quaternary documents the geology and palaeontology of the agreed physical reference point for the Pleistocene boundary, at 1.81 million years ago, found at Vrica in southern Italy. The book then describes the correlation of the boundary throughout the ocean basins and continents of the world.The Pleistocene Boundary and the Beginning of the Quaternary documents the geology and palaeontology of the agreed physical reference point for the Pleistocene boundary, at 1.81 million years ago, found at Vrica in southern Italy. The book then describes the correlation of the boundary throughout the ocean basins and continents of the world.The Pleistocene Boundary and the Beginning of the Quaternary presents the results of a forty-year international program to establish a precise definition for the most important boundary in geologic time  the beginning of the modern age of glacial climates. This book, the final report of International Geological Correlation Project 41, describes the selection of a fixed reference point in the sequence of deep-water marine strata exposed at Vrica, Italy. This point, dated to 1.81 million years before the present, coincides with the onset of the first of four major glacial phases. The opening chapters of the book document the geology and palaeontology of the agreed physical reference point, and the successful proposal of this point as the boundary-stratotype of the Pleistocene Epoch. The book then describes the correlation of the boundary throughout the ocean basins and continents of the world in terms of detailed stratigraphic criteria such as planktonic biostratigraphy, magnetostratigraphy and radiometric age determinations.List of contributors; Preface: the new Pleistocene; Foreword; Part I. Definition of the Base of the Quaternary: 1. International Geological Correlation Proglób
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