The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous epoch, or a stage in the Upper Cretaceous series. It spans the time between 93.5 Β± 0.8 Ma and 89.3 Β± 1 Ma (million years ago). The Turonian is preceded by the Cenomanian stage and underlies the Coniacian stage.[1]
At the beginning of the Turonian an anoxic event took place which is called the Cenomanian-Turonian boundary event or the "Bonarelli Event".
Stratigraphic definition
The Turonian (French: Turonien) was definied by the French paleontologist Alcide d'Orbigny (1802β1857) in 1842. Orbigny named it after the French city of Tours in the region of Touraine (department Indre-et-Loire), which is the original type locality.
The base of the Turonian stage is defined as the place where the ammonite species Watinoceras devonense first appears in the stratigraphic column. The official reference profile (the GSSP) for the base of the Turonian is located in the Rock Canyon anticline near Pueblo, Colorado (USA, coordinates: 38Β° 16' 56" N, 104Β° 43' 39" W).[2]
The top of the Turonian stage (the base of the Coniacian) is defined as the place in the stratigraphic column where the inoceramid bivalve species Cremnoceramus rotundatus first appears.
Subdivision
The Turonian is sometimes subdivided in Lower/Early, Middle and Upper/Late substages or subages. In the Tethys domain, it contains the following ammonite biozones:
- zone of Subprionocyclus neptuni (in the Upper Turonian)
- zone of Collignoniceras woollgari (in the Middle Turonian)
- zone of Mammites nodosoides
- zone of Watinoceras coloradoense or Watinoceras devonense (last two both in the Lower Turonian)
Other important index fossils are species of the inoceramid genus Inoceramus (I. schloenbachi, I. lamarcki and I. labiatus). Inoceramids are bivalve Mollusca related to today's mussels.
Palaeontology
β Ankylosaurs
Ankylosaurs of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
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Bayn Shire Formation, Mongolia |
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Birds (avian theropods)
Aves of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Catenoleimus |
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Bissekty Formation, Uzbekistan |
A mid-sized enantiornithine, perhaps 20β25 cm long in life |
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Explorornis |
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Bissekty Formation, Uzbekistan |
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Ichthyornis |
Turonian - Campanian |
Alberta and Saskatchewan, Canada; Alabama, Kansas, New Mexico and Texas, USA; Argentina; Central Asia |
The Cretaceous ecological equivalent of modern seabirds such as gulls, petrels, and skimmers. At 60 cm (2 ft), it was the size of a gull. Although the wings and breastbone are very modern in appearance (suggesting strong flight ability), the jaws retained numerous small, sharp teeth |
β Ceratopsians
Ceratopsia of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Zuniceratops |
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Moreno Hill Formation, New Mexico, USA |
The earliest-known ceratopsian to have eyebrow horns and the oldest-known ceratopsian from North America, appears to have been roughly 3 to 3.5 meters long (10β11 ft) and 1 meter (3 ft) tall at the hips. |
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Crocodylomorphs
Mammals
Mammalia of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Bryceomys |
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β Ornithopods
Ornithopoda of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Bactrosaurus |
Turonian to Coniacian |
Gobi Desert, Mongolia and China |
Would have been 6 m (20 ft) long[1] and 2 m (7 ft) high when in the quadrupedal stance, and weighed 1100 β 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. |
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Macrogryphosaurus |
Turonian to early Coniacian |
Portezuelo Formation, Argentina |
A genus of basal iguanodont, a large bipedal herbivor |
Notohypsilophodon |
Cenomanian-Turonian |
Bajo Barreal Formation, Chubut, Argentina |
A hypsilophodontid or other basal ornithopod, Notohypsilophodon would have been a bipedal herbivore. Its size has not been estimated |
Shuangmiaosaurus |
Cenomanian-Turonian |
China |
A poorly known iguanodont |
β Plesiosaurs
Plesiosauria of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Libonectes |
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Britton Formation (Cedar Hill), Texas, USA |
A 7β14 m (23β47 ft) long creature, was very similar to the related Elasmosaurus. It had a compact body with a short tail and large flippers. Its small skull had long, forward-facing teeth ideal for catching slippery fish and squid that came together outside of its mouth when the mouth was closed, and was placed atop a very long neck. |
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Manemergus |
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Morocco |
A genus of polycotylid plesiosaur |
Polyptychodon hudsoni |
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Texas, USA |
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Thililua |
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High Atlas, Morocco |
A genus of polycotylid plesiosaur, the estimated total length of Thililua is 5.5 to 6 metres. |
Squamats
Squamata of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
Dallasaurus |
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Arcadia Park Shale, Texas, USA |
A basal, small, plesiopedal mososauroid |
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Russellosaurus |
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Arcadia Park Shale, Texas, USA |
A basal, small, lightly built mosasaur |
β Theropods (non-avian)
Theropods of the Turonian |
Taxa |
Presence |
Location |
Description |
Images |
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Rio Limay, Argentina |
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References
Notes
- β See Gradstein et al. (2004) for a detailed description of the ICS' timescale
- β The GSSP was established by Kennedy et al. (2005)
Literature
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- Kennedy, W.J.; Walaszczyk, I. & Cobban, W.A.; 2005: The Global Boundary Stratotype Section and Point for the base of the Turonian Stage of the Cretaceous: Pueblo, Colorado, U.S.A., Episodes 28(2): pp 93β104.
External links
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In left column are eons; right column: bold are eras; not bold are periods: | | Hadean (4.6 β 3.8 Gya) |
- Paleohadean (4.6 β 4.3 Gya)
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- Mesohadean (4.3 β 4.1 Gya)
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- Neohadean (4.1 β 3.8 Gya)
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| Archean (3.8 β 2.5 Gya) |
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| Proterozoic (2.5 Gya β 542 Mya) |
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Mya = millions years ago. Gya = billions years ago. |
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In horizontal bars are eras; in left column are periods; right column: bold are epochs; not bold not italic are ages; italic are chrons: | |
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- Llandovery (443 β 433 Mya): Rhuddanian (443 β 441 Mya)
- Aeronian (441 β 439 Mya)
- Telychian (439 β 434 Mya)
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- Ludlow (427 β 423 Mya): Gorstian (427 β 426 Mya)
- Ludfordian (426 β 423 Mya)
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- Pridoli (423 β 419 Mya)
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- Early Devonian (419 β 393 Mya): Lochkovian (419 β 411 Mya)
- Pragian (411 β 408 Mya)
- Emsian (408 β 393 Mya)
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kya = thousands years ago. Mya = millions years ago. * Not officially recognized by the I.C.S. |
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