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The Importance of Desert Margins as Indicators for Global Climatic Fluctuations (Introduction)

  • W. Smykatz-Kloss
  • P. Felix-Henningsen
Chapter
Part of the Lecture Notes in Earth Sciences book series (LNEARTH, volume 102)

Abstract

In various periods throughout the younger earth history comparable changes in climate occurred globally and simultaneously. Such global events can be reconstructed with the help of reliefs, sediments and palaeosoils and their specific morphological, chemical and mineralogical properties. Desert margins represent intersections between arid and humid ecosystems. Their geographical position will react very sensitively on climatic changes. The broad regions of transformation between recent humid ecosystems and the fully arid deserts are the proper areas where palaeoclimatically different phases will be remarkably recognized and interpreted.

Keywords

Geological Correlation Arid Desert Aeolian Sediment Mineralogical Property Marine Sediment Core 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2004

Authors and Affiliations

  • W. Smykatz-Kloss
    • 1
  • P. Felix-Henningsen
    • 2
  1. 1.Institute of Mineralogy and GeochemistryUniversity of KarlsruheKarlsruheGermany
  2. 2.Institute for GeologyUniversity of GöttingenGöttingenGermany

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