System Series Stage Age (Ma) Paleogene Paleocene Danian younger Cretaceous Upper Maastrichtian 65.5–70.6 Campanian 70.6–83.5 Santonian 83.5–85.8 Coniacian 85.8–89.3 Turonian 89.3–93.5 Cenomanian 93.5–99.6 Lower Albian 99.6–112.0 Aptian 112.0–125.0 Barremian 125.0–130.0 Hauterivian 130.0–136.4 Valanginian 136.4–140.2 Berriasian 140.2–145.5 Jurassic Upper Tithonian older Subdivision of the Cretaceous system according to the IUGS, as of July 2009.
The Coniacian is an age or stage in the geologic timescale. It is a subdivision of the Late Cretaceous epoch or Upper Cretaceous series and spans the time between 89.3 ± 1 Ma and 85.8 ± 0.7 Ma (million years ago). The Coniacian is preceded by the Turonian and followed by the Santonian.
The base of the Coniacian stage is at the first appearance of the inoceramid bivalve species Cremnoceramus rotundatus. An official reference profile for the base (a GSSP) had in 2009 not yet been appointed.
The top of the Coniacian (the base of the Santonian stage) is defined by the appearance of the inoceramid bivalve Cladoceramus undulatoplicatus.
The Coniacian overlaps the regional Emscherian stage of Germany, which is roughly coeval with the Coniacian and Santonian stages. In magnetostratigraphy, the Coniacian is part of magnetic chronozone C34, the so called Cretaceous Magnetic Quiet Zone, a relatively long period with normal polarity.
Sequence stratigraphy and geochemistry
After a maximum of the global sea level during the early Turonian, the Coniacian was characterized by a gradual fall of the sea level. This cycle is in sequence stratigraphy seen as a first order cycle. During the middle Coniacian a shorter, second order cycle, caused a temporary rise of the sea level (and global transgressions) on top of the longer first order trend. The following regression (Co1, at 87,0 Ma) separates the Middle from the Upper Coniacian substage. An even shorter third order cycle caused a new transgression during the Late Coniacian.
Beginning in the Middle Coniacian, an anoxic event (OAE-3) occurred in the Atlantic Ocean, causing large scale deposition of black shales in the Atlantic domain. The anoxic event lasted till the Middle Santonian (from 87.3 to 84.6 Ma) and is the longest and last such event during the Cretaceous period.
- zone of Paratexanites serratomarginatus
- zone of Gauthiericeras margae
- zone of Peroniceras tridorsatum
In the boreal domain the Coniacian overlaps just one ammonite biozone: that of Forresteria petrocoriensis
Ornithopoda of the Coniacian Taxa Presence Location Description Images Turonian to Coniacian Gobi Desert, Mongolia and China Would have been 6 m (20 ft) long and 2 m (7 ft) high when in the quadrupedal stance, and weighed 1100 - 1500 kg (2400 - 3300 lb). Like many hadrosaurs, it could switch between bipedal and quadrupedal stances, but unusually it had large spines protruding from the vertebrae. Turonian to early Coniacian Portezuelo Formation, Argentina A genus of basal iguanodont, a large bipedal herbivore
- ^ See Gradstein et al. (2004) for a detailed version of the ICS' geologic timescale
- ^ See Meyers et al. (2006)
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- Meyers, P.A.; Bernasconi, S.M. & Forster, A.; 2006: Origins and accumulation of organic matter in expanded Albian to Santonian black shale sequences on the Demerara Rise, South American margin, Organic Geochemistry 37, pp 1816-1830.
- GeoWhen Database - Coniacian
- Late Cretaceous timescale, at the website of the subcommission for stratigraphic information of the ICS
- Stratigraphic chart of the Late Cretaceous, at the website of Norges Network of offshore records of geology and stratigraphy
Cretaceous Period Lower/Early Cretaceous Upper/Late Cretaceous Berriasian | Valanginian | Hauterivian
Barremian | Aptian | Albian
Cenomanian | Turonian | Coniacian
Santonian | Campanian | Maastrichtian
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