Late Eocene–Early Oligocene Evolution of Climate and Marine Circulation: Deep-Sea Clay Mineral Evidence

  1. Jemes P. Kennett and
  2. Detlef A. Warkne
  1. Christian Robert1 and
  2. Hervé Chamley2

Published Online: 21 MAR 2013

DOI: 10.1029/AR056p0097

The Antarctic Paleoenvironment: A Perspective on Global Change: Part One

The Antarctic Paleoenvironment: A Perspective on Global Change: Part One

How to Cite

Robert, C. and Chamley, H. (1992) Late Eocene–Early Oligocene Evolution of Climate and Marine Circulation: Deep-Sea Clay Mineral Evidence, in The Antarctic Paleoenvironment: A Perspective on Global Change: Part One (eds J. P. Kennett and D. A. Warkne), American Geophysical Union, Washington, D. C.. doi: 10.1029/AR056p0097

Author Information

  1. 1

    Géologie du Quaternaire, Centre National de la Recherche Scientifique—Luminy, Marseille, Cedex 9, France

  2. 2

    Dynamique Sedimentaire et Structurale, Centre National de la Recherche Scientifique, Université de Lille, d'Ascq Cedex, France

Publication History

  1. Published Online: 21 MAR 2013
  2. Published Print: 1 JAN 1992

ISBN Information

Print ISBN: 9780875908236

Online ISBN: 9781118667781

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Keywords:

  • Paleogeography—Antarctic regions—Congresses;
  • Paleoecology—Antarctic regions—Congresses

Summary

This chapter contains sections titled:

  • Introduction

  • Clay Mineral Associations of Late Eocene-Early Oligocene Age

  • Clay Mineral Variations in the South Atlantic and Southern Ocean

  • Clay Mineral Variations in the Northern Hemisphere

  • Global Evolution of Climate and Circulation at the Eocene/Oligocene Transition

  • Conclusion and Possible Scenario for Climatic and Oceanographic Development at the Eocene/Oligocene Transition