Gauss-Matuyama reversal

From Wikipedia, the free encyclopedia

The Gauss-Matuyama Reversal was a geologic event approximately 2.588 million years ago when the Earth's magnetic field underwent reversal.

This event, which separates the Piacenzian from the Gelasian and marks the start of the Quaternary,[1] is useful in dating sediments.

Biological effects

The event is marked by the extinction of calcareous nannofossils Discoaster pentaradiatus and D. surculus, among others.

References

  1. ↑ Clague, John et al. (2006) "Open Letter by INQUA Executive Committee" Quaternary Perspective, the INQUA Newsletter International Union for Quaternary Research 16(1):

See also


This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.