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Contents

   



(Top)
 


1 Stratigraphic definitions  



1.1  Subdivision  







2 References  



2.1  Notes  





2.2  Literature  







3 External links  














Bajocian






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From Wikipedia, the free encyclopedia
 


Bajocian

170.9 ± 0.8 – 168.2 ± 1.2 Ma

O

S

D

C

P

T

J

K

Pg

N

Chronology

−200 —

−195 —

−190 —

−185 —

−180 —

−175 —

−170 —

−165 —

−160 —

−155 —

−150 —

−145 —

Mesozoic
T
K
 
 
 

Subdivision of the Jurassic according to the ICS, as of 2022.[1]
Vertical axis scale: millions of years ago.

Etymology

Name formality

Formal

Usage information

Celestial body

Earth

Regional usage

Global (ICS)

Time scale(s) used

ICS Time Scale

Definition

Chronological unit

Age

Stratigraphic unit

Stage

Time span formality

Formal

Lower boundary definition

FAD of the Ammonites Hyperlioceras mundum, Hyperlioceras furcatum, Braunsina aspera, and Braunsina elegantula

Lower boundary GSSP

Cabo Mondego, Portugal
40°11′57N 8°54′15W / 40.1992°N 8.9042°W / 40.1992; -8.9042

Lower GSSP ratified

1996[2]

Upper boundary definition

FAD of the Ammonite Gonolkites convergen

Upper boundary GSSP

Ravin du Bès, Bas-Auran, Alpes de Haute, France
43°57′38N 6°18′55E / 43.9606°N 6.3153°E / 43.9606; 6.3153

Upper GSSP ratified

July 2008[3]

In the geologic timescale, the Bajocian is an age and stage in the Middle Jurassic. It lasted from approximately 170.9 ±0.8 Ma to around 168.2 ±1.2 Ma (million years ago). The Bajocian Age succeeds the Aalenian Age and precedes the Bathonian Age.[4]

Stratigraphic definitions[edit]

The Bajocian Stage takes its name from the Latin name (Bajocae) of the town of Bayeux, in the region of NormandyinFrance. The stage was named and introduced in scientific literature by French palaeontologist Alcide d'Orbigny in 1842.

The base of the Bajocian stage is defined as the place in the stratigraphic column where fossils of the ammonite genus Hyperlioceras first appear. A global reference profile (aGSSP) for the base is located at Murtinheira, close to Cabo MondegoinPortugal.[5] The top of the Bajocian (the base of the Bathonian) is at the first appearance of ammonite species Parkinsonia convergens.

Subdivision[edit]

The Bajocian is often divided into Lower/Early and Upper/Late subages or substages.

In the Tethys domain, the Bajocian contains seven ammonite biozones:

References[edit]

Notes[edit]

  1. ^ "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy.
  • ^ Pavia, G.; Enay, R. (March 1997). "Definition of the Aalenian-Bajocian Stage boundary". Episodes. 20 (1): 16–22. doi:10.18814/epiiugs/1997/v20i1/004. Retrieved 23 December 2020.
  • ^ Fernández-López, Sixto Rafael; Pavia, Giulio; Erba, Elisabetta; Guiomar, Myette; Maria Helena Henriques; Lanza, Roberto; Mangold, Charles; Morton, Nicol; Olivero, Davide; Daniele Tiraboschi (2009). "The Global Boundary Stratotype Section and Point (GSSP) for base of the Bathonian Stage (Middle Jurassic), Ravin du Bès Section, SE France" (PDF). Episodes. 32 (4): 222–248. doi:10.18814/epiiugs/2009/v32i4/001.
  • ^ See for a detailed geologic timescale Gradstein et al. (2004)
  • ^ The GSSP is described by Pavia & Enay (1997)
  • Literature[edit]

    External links[edit]

  • Sinemurian
  • Pliensbachian
  • Toarcian
  • Bajocian
  • Bathonian
  • Callovian
  • Kimmeridgian
  • Tithonian
  • Cenozoic Era
    (present–66.0 Ma)

    Quaternary (present–2.58 Ma)

  • Pleistocene (11.7 ka–2.58 Ma)
  • Neogene (2.58–23.0 Ma)

  • Miocene (5.33–23.0 Ma)
  • Paleogene (23.0–66.0 Ma)

  • Eocene (33.9–56.0 Ma)
  • Paleocene (56.0–66.0 Ma)
  • Mesozoic Era
    (66.0–252 Ma)

    Cretaceous (66.0–145 Ma)

  • Early (100–145 Ma)
  • Jurassic (145–201 Ma)

  • Middle (164–174 Ma)
  • Early (174–201 Ma)
  • Triassic (201–252 Ma)

  • Middle (237–247 Ma)
  • Early (247–252 Ma)
  • Paleozoic Era
    (252–539 Ma)

    Permian (252–299 Ma)

  • Guadalupian (260–272 Ma)
  • Cisuralian (272–299 Ma)
  • Carboniferous (299–359 Ma)

  • Mississippian (323–359 Ma)
  • Devonian (359–419 Ma)

  • Middle (383–393 Ma)
  • Early (393–419 Ma)
  • Silurian (419–444 Ma)

  • Ludlow (423–427 Ma)
  • Wenlock (427–433 Ma)
  • Llandovery (433–444 Ma)
  • Ordovician (444–485 Ma)

  • Middle (458–470 Ma)
  • Early (470–485 Ma)
  • Cambrian (485–539 Ma)

  • Miaolingian (497–509 Ma)
  • Series 2 (509–521 Ma)
  • Terreneuvian (521–539 Ma)
  • Proterozoic Eon
    (539 Ma–2.5 Ga)

    Neoproterozoic (539 Ma–1 Ga)

  • Cryogenian (635–720 Ma)
  • Tonian (720 Ma–1 Ga)
  • Mesoproterozoic (1–1.6 Ga)

  • Ectasian (1.2–1.4 Ga)
  • Calymmian (1.4–1.6 Ga)
  • Paleoproterozoic (1.6–2.5 Ga)

  • Orosirian (1.8–2.05 Ga)
  • Rhyacian (2.05–2.3 Ga)
  • Siderian (2.3–2.5 Ga)
  • Archean Eon (2.5–4 Ga)

  • Mesoarchean (2.8–3.2 Ga)
  • Paleoarchean (3.2–3.6 Ga)
  • Eoarchean (3.6–4 Ga)
  • Hadean Eon (4–4.6 Ga)

     

    ka = kiloannum (thousands years ago); Ma = megaannum (millions years ago); Ga = gigaannum (billions years ago).
    See also: Geologic time scale  • icon Geology portal  • World portal


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    This page was last edited on 27 June 2023, at 09:21 (UTC).

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