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Cambrian to Silurian Non-Marine Palynology

  • Traverse A
Springer Netherlands, (2007), 189-197
DOI: 10.1007/978-1-4020-5610-9_7
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Abstract

CAMBRIAN TO SILURIAN NON-MARINE In late Silurian time, more or less at the Ludlow/Downton (or Pridoli) boundary, about 405 million years ago ( , 1977), after the arrival of the tiny vascular plant, Cooksonia, vascular vegetation developed on land.

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APA

Traverse, A. (2007). Cambrian to Silurian Non-Marine Palynology. In Paleopalynology (pp. 189–197). Springer Netherlands. https://doi.org/10.1007/978-1-4020-5610-9_7

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