Fern spike

From Wikipedia, the free encyclopedia

In paleontology, a fern spike is the occurrence of abundant fern spores in the fossil record, usually immediately (in a geological sense) after an extinction event. The spikes are believed to represent a large, temporary increase in the number of ferns relative to other terrestrial plants after the extinction or thinning of the latter, probably because fern dispersal is more rapid over large geographic areas, since single-celled fern spores are more easily distributed by the wind than are seeds[citation needed]. Fern spikes are most associated with the Cretaceous-Tertiary extinction event[1][2], although they have been found at other events such as at the Triassic-Jurassic boundary[3][4]. Away from the fossil record, fern spikes have also been observed to occur in response to local extinction events, for instance the 1980 Mount St. Helens eruption.

[edit] References

  1. ^ Schultz, P.H. and D'Hondt, S. (1996) Cretaceous-Tertiary (Chicxulub) impact angle and its consequences. Geology 24, 963-967
  2. ^ Vajda, V., Raine, J.I. and Hollis, C.J. (2001) Indication of global deforestation at the Creataceous-Tertiary boundary by New Zealand fern spike. Science 294, 1700-1702
  3. ^ Fowell, S.J. and Olsen, P.E. (1993) Time calibration of Triassic-Jurassic microfloral turnover, eastern North-America. Tectonophysics 222, 361-369
  4. ^ Olsen, P. E., Kent, D.V., Sues, H.D., Koeberl, C., Huber, H., Montanari, A., Rainforth, E.C., Fowell, S.J., Szajna, M.J. and Hartline, B.W. (2002) Ascent of dinosaurs linked to an iridium anomaly at the Triassic-Jurassic boundary. Science 296, 1305-1307
 This fern-related article is a stub. You can help Wikipedia by expanding it.