Wenlock Epoch

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by InternetArchiveBot (talk | contribs) at 22:05, 14 June 2020 (Bluelink 1 book for verifiability (refca)) #IABot (v2.0.1) (GreenC bot). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Template:Geological epoch The Wenlock (sometimes referred to as the Wenlockian) is the second epoch of the Silurian. It is preceded by the Llandovery epoch and followed by the Ludlow epoch. Radiometric dates constrain the Wenlockian between 433.4 and 427.4 million years ago.[1]

Naming and history

The Wenlock is named after Wenlock Edge, an outcrop of rocks near the town of Much Wenlock in Shropshire (West Midlands, United Kingdom).[2] The name was first used in the term "Wenlock and Dudley rocks" by Roderick Murchison in 1834 to refer to the limestones and underlying shales that underlay what he termed the "Ludlow rocks".[3] He later modified this term to simply the "Wenlock rocks" in his book, The Silurian System in 1839.[4]

Definition and subdivision

The Wenlock's beginning is defined by the lower boundary (or GSSP) of the Sheinwoodian. The end is defined as the base (or GSSP) of the Gorstian.[5]

The Wenlock is divided into the older Sheinwoodian and the younger Homerian stage. The Sheinwoodian lasted from 433.4 to 430.5 million years ago. The Homerian lasted from 430.5 to 427.4 million years ago.[1]

Paleontology

Arthropods

Arthropods of the Wenlockian
Taxa Presence Location Description Images
Wenlock epoch Dudley, West Midlands, England Cephalon covered in nodular tubercles; the well known "strawberry-headed" trilobite of Dudley.
Balizoma variolaris (Murchison, 1839)

References

  1. ^ a b "International Chronostratigraphic Chart 2013/01" (PDF). International Commission on Stratigraphy. Retrieved 10 July 2013.
  2. ^ Gradstein, Felix M.; Ogg, James G.; Smith, Alan G. (2004). A Geologic Time Scale 2004. ISBN 9780521786737.
  3. ^ Murchison R.I. (1833–1834). "On the Structure and Classification of the Transition Rocks of Shropshire, Herefordshire and part of Wales and on the Lines of Disturbance which have affected that Series of Deposits, including the Valley of Elevation of Woolhope". Proceedings of the Geological Society of London. 2 (33): 14.
  4. ^ Murchison R.I. (1839). The Silurian System. Murray. p. 208.
  5. ^ The Geologic Time Scale 2012. Elsevier Science Ltd. ISBN 978-0-444-59425-9.