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The History of Flora and Vegetation During the Quaternary

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Progress in Botany / Fortschritte der Botanik

Part of the book series: Progress in Botany/Fortschritte der Botanik ((BOTANY,volume 42))

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Abstract

The pleistocene history of climate and the marine circulation patterns as well are strongly influenced by the evolution of the Antarctic ice cap. From this and from some recent atmospheric circulation patterns pointing to a situation in the near future when, thanks to the increasing CO2-content of the atmosphere, only Antarctica may be covered by ice, the history of Antarctica during the final part of the Tertiary has attracted much interest. So WEBB et al. (1979) stressed that at least Mary Bird Land has been glaciated since the middle oligocene. During miocene times this glaciation seems to have strengthened (STUMP et al., 1980), but since from these times appreciably rich photic plankton floras are known from the southern Ross Ice Self (WEBB et al., 1979) this ice can have been neither thick nor permanent. According to BRADY and MARTIN (1979) the appreciably rich pollen and spore flora, together with some 50 diatom species of the same age point to Nothofagus forests or stands at sheltered places within the valleys, surrounded by glaciers. These ice masses seem to have governed the deep-sea circulation pattern in the Pacific Ocean (KEIGWIN et al., 1979), and the Gulf Stream as well (KANEPS, 1979).

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  1. Botanisches Institut, Universität Hohenheim, D 7000, Stuttgart 70, Hohenheim, Germany

    Professor Dr. Burkhard Frenzel

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Frenzel, B. (1980). The History of Flora and Vegetation During the Quaternary. In: Progress in Botany / Fortschritte der Botanik. Progress in Botany/Fortschritte der Botanik, vol 42. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-67873-8_21

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  • DOI: https://doi.org/10.1007/978-3-642-67873-8_21

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-67875-2

  • Online ISBN: 978-3-642-67873-8

  • eBook Packages: Springer Book Archive

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