Rhuddanian

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Rhuddanian
443.8 ± 1.5 – 440.8 ± 1.2 Ma
Chronology

In the

Ma and ended 440.8 ± 1.2 Ma (million years ago). It succeeds the Himantian Age (the last age of the Ordovician Period) and precedes the Aeronian Age.[7]

GSSP

The GSSP for the Silurian is located in a section at Dob's Linn, Scotland, in an artificial excavation created just north of the Linn Branch Stream. Two lithological units (formations) occur near the boundary.[6] The lower is the Hartfell Shale (48 metres (157 ft) thick), consisting chiefly of pale gray mudstone with subordinate black shales and several interbedded meta-bentonites.[6] Above this is the 43 metres (141 ft) thick Birkhill Shale, which consist predominantly of black graptolitic shale with subordinate gray mudstones and meta-bentonites.[8]

See also

  • Ordovician-Silurian extinction events
  • Early Palaeozoic Icehouse

References

  1. .
  2. .
  3. ^ "Chart/Time Scale". www.stratigraphy.org. International Commission on Stratigraphy.
  4. .
  5. ^ . Retrieved 11 December 2020.
  6. ^ .
  7. ^ "GSSP Table - All Periods". International Commission on Stratigraphy. Retrieved 15 September 2018.
  8. ^ "GSSP for the Rhuddanian Stage". International Commission on Stratigraphy.