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Paläozoikum I – Das Kambrium

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Die Entwicklung des Systems Erde

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Notes

  1. 1.

    Im Gegensatz zur „wahren Wanderung“ des geografischen Pols, verursacht durch Massenverlagerungen auf und in der Erde

  2. 2.

    Messungen an jungen Sedimentkernen zeigen, dass die Deklination, innerhalb von 1–2 ka gemittelt, die Richtung des geografischen Pols ergibt.

  3. 3.

    http://www.fossilmuseum.net/Fossil_Sites/Chengjiang.htm

  4. 4.

    http://paleobiology.si.edu/burgess/index.html

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Author information

Authors and Affiliations

  1. Geologisches Institut, Technische Universität Bergakademie Freiberg, Freiberg, Deutschland

    Olaf Elicki

  2. Geologisches Institut, Technische Universität Bergakademie Freiberg, Freiberg, Deutschland

    Christoph Breitkreuz

Authors
  1. Olaf Elicki
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  2. Christoph Breitkreuz
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Correspondence to Olaf Elicki .

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Elicki, O., Breitkreuz, C. (2016). Paläozoikum I – Das Kambrium. In: Die Entwicklung des Systems Erde. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-47192-0_4

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