Search the Archive
  Home
  Welcome to
  Station Information
  Mathematical and
  Natural Sciences

  Astronomy
  Biology
  Chemistry
  Computer science
  Earth science
  Ecology
  Health science
  Mathematics
  Physics
  Statistics
  Applied Arts
  and Sciences

  Agriculture
 
Architecture
  Business
  Communication
  Education
  Engineering
  Family and
  consumer science

  Government
  Law
  Library and information
  science

  Medicine
  Politics
  Public affairs
  Software engineering
  Technology
  Transport
  Social Sciences
  and Philosophy

  Archaeology
  Economics
  Geography
  History
  History of science
  and technology

  Language
  Linguistics
  Mythology
  Philosophy
  Political science
  Psychology
  Sociology
  Culture and
  Fine Arts

  Classics
  Cooking
  Dance
  Entertainment
  Film
  Games
  Gardening
  Handicraft
  Hobbies
  Holidays
  Internet
  Literature
  Music
  Opera
  Painting
  Poetry
  Radio
  Recreation
  Religion
  Sculpture
  Sports
  Television
  Theater
  Tourism
  Visual arts and design

Silurian


 

 This period is part of the
Paleozoic era.
 Cambrian
 Ordovician
 Silurian
 Devonian
 Carboniferous
 Permian

Table of contents
1 Silurian naming
2 Silurian dating
3 Silurian subdivisions
4 Silurian paleogeography
5 Silurian fauna

Silurian naming

The Silurian system was first described by Sir Roderick Murchison in the 1830s based on rocks in South Wales. It is named for a Welsh Celtic tribe -- the Silures. The series quickly came to overlap Adam Sedgwick's Cambrian sequence. Lapworth eventually resolved the conflict by defining a new Ordovician system including the contended beds.

Silurian dating

The Silurian is a Geologic Period that extends from about 408.5 to 443.5 million Years before the present. As with most other geologic periods, the rock beds that define the start and end are well identified, but the exact dates of the start and end of the period are uncertain by 5-10 million years. The Silurian period follows the Ordovician and is followed by the Devonian period. The base of the Silurian is set at a major extinction event where 60% of marine species were wiped out.

Silurian subdivisions

The Silurian is usually broken into Lower and Upper subdivisions, however some workers do use a Lower/Middle/Upper breakdown. The Faunal stages from youngest to oldest are:

  • no stage defined? (Upper-Pridoli)
  • Cayugan (Upper- Ludlow)
  • Ludfordian (Upper- Ludlow)
  • Gorstian (Upper- Ludlow)

  • Homerian/Lockportian (Middle-Wenlock)
  • Sheinwoodian/Tonawandan (Middle-Wenlock)

  • Telychian/Ontarian (Lower-Llandovery)
  • Aeronian/Alexandrian (Lower-Llandovery)
  • Rhuddanian/Alexandrian (Lower-Llandovery)

Silurian paleogeography

During the Silurian,
Gondwana remained in high Southern latitudes, but there is evidence that the Silurian icecaps were less extensive than those of the late Ordovician. The other continents drifted together near the equator starting the formation of a second supercontinent known as Laurasia.

Silurian fauna

Life was abundant in the Silurian. Silurian beds are oil and gas producers in some areas. Extensive beds of Silurian hematite -- an iron ore -- in Eastern North America were important to the colonial economy.

The Silurian was a time of high sea levels in Eastern North America and Europe. Primitive multicelled land plants are found from the Silurian. A few arthropods seem to have invaded the land during the Silurian. Fish reached considerable diversity and developed movable jaws. A diverse fauna of Sea Scorpions -- some of them several meters in length -- graces the Silurian of North America. Brachiopods, bryozoa, mollusks, etc were abundant and diverse








Site Partners

Easy Encyclopedia
Small Business Forum
Free Web Templates
Free Mortgage Quote

  This content from wikipedia is licensed under the GNU Free Documentation License