Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Cretaceous
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==Etymology and history== The Cretaceous as a separate period was first defined by Belgian geologist [[Jean Baptiste Julien d'Omalius d'Halloy|Jean d'Omalius d'Halloy]] in 1822 as the ''Terrain Crétacé'',<ref>{{cite journal | author = d’Halloy, d’O., J.-J. | year = 1822 | title = Observations sur un essai de carte géologique de la France, des Pays-Bas, et des contrées voisines |trans-title=Observations on a trial geological map of France, the Low Countries, and neighboring countries | journal = Annales des Mines | volume = 7 | pages = 353–376 | url = https://books.google.com/books?id=c-ocAQAAIAAJ&pg=PA353}} From page 373: "La troisième, qui correspond à ce qu'on a déja appelé formation de la craie, sera désigné par le nom de terrain crétacé." (The third, which corresponds to what was already called the "chalk formation", will be designated by the name "chalky terrain".)</ref> using [[stratum|strata]] in the [[Paris Basin]]<ref>{{cite book |trans-title=Great Soviet Encyclopedia |title=Sovetskaya Enciklopediya |publisher=Sovetskaya Enciklopediya |edition=3rd |pages=vol. 16, p. 50 |year=1974 |location=Moscow |language=ru |no-pp=true |title-link=Great Soviet Encyclopedia}}</ref> and named for the extensive beds of [[chalk]] ([[calcium carbonate]] deposited by the shells of marine [[invertebrate]]s, principally [[coccoliths]]), found in the upper Cretaceous of [[Western Europe]]. The name Cretaceous was derived from the [[Latin]] ''creta'', meaning ''chalk''.<ref>{{cite book|title=Glossary of Geology|publisher=American Geological Institute|edition=3rd|page= 165|year=1972|location=Washington, D.C.}}</ref> The twofold division of the Cretaceous was implemented by [[William Conybeare (geologist)|Conybeare]] and Phillips in 1822. [[Alcide d'Orbigny]] in 1840 divided the French Cretaceous into five ''étages'' (stages): the [[Neocomian]], Aptian, Albian, Turonian, and Senonian, later adding the ''Urgonian'' between Neocomian and Aptian and the Cenomanian between the Albian and Turonian.<ref>{{Citation|last1=Ogg|first1=J.G.|title=Cretaceous|date=2012|url=https://linkinghub.elsevier.com/retrieve/pii/B9780444594259000275|work=The Geologic Time Scale|pages=793–853|publisher=Elsevier|language=en|doi=10.1016/b978-0-444-59425-9.00027-5|isbn=978-0-444-59425-9|access-date=2021-01-08|last2=Hinnov|first2=L.A.|last3=Huang|first3=C.}}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)