Encyclopedia of Paleoclimatology and Ancient Environments

2009 Edition
| Editors: Vivien Gornitz

Mineral Indicators Of Past Climates

  • Vivien Gornitz
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-4411-3_143

Introduction

A mineral is a naturally occurring crystalline solid created by geological or biogenic processes (e.g., calcite/aragonite in mollusk shells or coral). Minerals that form at or near the Earth’s surface are products of chemical weathering, evaporation, authigenic crystallization, and bio-mineralization. They reflect ambient conditions at the Earth-atmosphere interface. Therefore they can furnish important clues about former climates. Minerals are utilized as paleoclimate indicators or proxies in several different ways:
  1. 1.

    To infer past climates and changes over time.

     
  2. 2.

    To deduce changes in atmospheric composition.

     
  3. 3.

    As mineralogical “markers” in provenance studies.

     
  4. 4.

    As “hosts” for climate-sensitive stable isotopes and trace elements.

     

The most direct mineral indicators or proxies are those that are generated under relatively narrow climatic ranges or within restricted environmental settings. Examples include chemical precipitates such as evaporites, low...

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© Springer-Verlag 2009

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  • Vivien Gornitz

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