Sainte-Barbe Clays Formation

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UnderliesAlbian aged "Meules"
ThicknessVariable, 50 m (160 ft) at Bernissart
Sainte-Barbe Clays Formation
Stratigraphic range: Barremian-early Aptian
~126–124 Ma
TypeGeological formation
UnderliesAlbian aged "Meules"
OverliesBreccia, Pennsylvanian basement
ThicknessVariable, 50 m (160 ft) at Bernissart
Lithology
PrimaryClay
OtherLignite
Location
Coordinates50°30′N 3°36′E / 50.5°N 3.6°E / 50.5; 3.6
Approximate paleocoordinates40°42′N 13°42′E / 40.7°N 13.7°E / 40.7; 13.7
CountryBelgium
ExtentLocalised within the northern margins of the Mons Basin
Sainte-Barbe Clays Formation is located in Belgium
Sainte-Barbe Clays Formation
Sainte-Barbe Clays Formation (Belgium)

The Sainte-Barbe Clays Formation is a geological formation in Belgium. It is found in localised areas of the northern margin of the Mons Basin, alongside the equivalently aged Hautrage and Baudour Clay Formations.[1] It is Upper Barremian-Lower Aptian in age.[2] It predominantly consists of laminated clay, with some lignite.[3] It is well known for the "Iguanodon sinkhole" locality near Bernissart where many specimens of Iguanodon bernissartensis were described by Louis Dollo in the late 19th century.

The Sainte-Barbe Clays Formation are part of the stratigraphy of the Mons Basin, a Cretaceous-Cenozoic sedimentary basin in western Belgium. The subsidence of the basin floor is caused by the dissolution of anhydrite in the Carboniferous basement. Wealden facies are the oldest units within the basin, and are only found on the northern margin of the basin, being absent from the central and southern parts of the basin. Localised areas of significant subsidence, referred to as "sinkholes" are observed. The Wealden facies are overlain by "mixed siliciclasticcarbonate formations" called Meules dating to the Albian.[1]

Fossil content

Tetrapods

Tetrapods of the Sainte-Barbe Clays Formation
GenusSpeciesLocationStratigraphic positionAbundanceNotesImages
Anteophthalmosuchus A. epikrator[4] Bernissart "Two ... fully articulated skeletons, one missing the skull and mandible."[5] Goniopholidid crocodyliform
Bernissartia B. fagesii IRSNB R46, mostly complete skeleton Bernissartiid crocodyliform
Chitracephalus C. dumonii Carapace with preserved limbs Cryptodiran turtle[6]
Iguanodon I. bernissartensis Multiple skeletons Iguanodontian dinosaur
Mantellisaurus M. atherfieldensis IRSNB 1551, single mostly complete skeleton Iguanodontian dinosaur, formerly considered holotype of "Dollodon bampingi"[7]
Hylaeobatrachus H. croyii Slab and counterslab of a complete skeleton Salamander
Peltochelys P. duchastelii Shell fragments Paracryptodire, probable close relative of Compsemys[8]
Theropoda Indeterminate Phalanx

Fish

Fish of the Sainte-Barbe Clays Formation
GenusSpeciesLocationStratigraphic positionAbundanceNotesImages
Aethalionopsis A. robustus Bernissart Formerly referred to Anaethalion
Amiopsis A. dolloi
Barbalepis B. macroptera Coccolepid fish, formerly referred to Coccolepis[9]
Pleuropholis P. germinalis Pleuropholid fish[10]
Callopterus C. insignis Genus is later considered as nomen nudum and Ainia is used for Jurassic species, but validity of this species is not discussed[11]
Pattersonella P. formosa Formerly referred to Leptolepis
Scheenstia S. bernissartensis Multiple specimens Previously referred to Lepidotes, L. brevifulcratus is a junior synonym.[12]
Turbomesodon T. bernissartensis Multiple specimens Previously referred to Mesodon and Macromesodon.[13]
Other fish

Insects

The Tettigarctid cicada Hylaeoneura lignei is known from the formation.[19]

Parasites

Flora

Ichnofossils

See also

References

Further reading

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