Sables du Castrais Formation

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Sables du Castrais Formation
Stratigraphic range: Eocene, Ypresian–Bartonian
Type Geological formation
Sub-units
  • Lophiodon lautricense and Paleotherium zone
  • Issel Member
  • Villeneuve-la-Comptal Member
  • Grès de Carcassonne Member
  • Argiles rutilants d'Issel et de Saint-Papoul
  • Grès d'Issel
  • Molasses de Castelnaudary
  • Issel Sandstones
Underlies Molasses de Saix et de Lautrec Formation
Overlies Danian rocks
Thickness15–40 metres (49–131 ft) at the base and at Castelnaudary. 50–100 metres (160–330 ft) at Issel.
Lithology
Primary Sandstone, molasse and conglomerate
Other Gravel clays
Location
Coordinates 43°22′05″N1°59′26″E / 43.3681°N 1.9906°E / 43.3681; 1.9906
Region Montagne-Noire
Country France
Extent Carcassonne, Castelnaudary, Issel, Réalmont and Saint-Papoul
Type section
Named byM. Richard (1946) [1]
France relief location map.jpg
Lightgreen pog.svg
Sables du Castrais Formation (France)

The Sables du Castrais Formation, also known as the Molasses du Castrais, is a geologic formation of Eocene (Ypresian to Bartonian) age, [2] [3] outcropping in the Montagne-Noire region of France. [3] [4]

Contents

History

"Petrified fossil remains" were known from the Sables du Castrais Formation since at least the 18th century, [5] and several of these fossils were described by Cuvier (1804) and Cuvier (1822) as belonging to Palaeotherium and Lophiodon . [6] [7]

In 1845, a jaw assigned to Lophiodon lautricensis was discovered in the formation and was described by Noulet (1851); [8] Noulet also mentioned that he had himself collected fossils from the formation alongside pharmacist J. Parayre as early as c.1843. [9]

Léonce Roux du Carla discovered several more fossils from the Grès d'Issel Mermber of the Sables du Castrais formation from February 1855 until his death in 1859, and this helped Noulet (1858) to confirm the Eocene age of the deposit. [4] Despite this, all that remains today of du Carla's collection is a single jaw of Palaeotherium castrense from the Sables du Castrais Formation. [5]

Between 1850 and 1868, during the construction of the Castres - Albi railroad, several more fossils were recovered from the Sables du Castrais Formation, [5] including M. Zebrowsky's 1868 discovery of fossils within the area. [10]

The Grès d'Issel Member was identified by Henri de Sévérac in 1873, [11] and the Sables du Castrais Formation was first described by M. Richard in 1946. [1]

The Grès d'Issel Member is located in a quarry which closed around 1966 and is now inaccessible due to it currently being located underneath a private garden. [12]

Age of the formation

The age of the Sables du Castrais Formation was listed as Eocene by Noulet (1858) [4] and in 1867, Gervais noted that the Issel Member likely dated to the Early Eocene, while the Villeneuve-la-Comptal Member likely dated to the Middle Eocene. [13]

Caraven-Cachin (1898) was the first to assign the Sables du Castrais Formation to the Bartonian. [14] Stehlin (1910) and Escarguel (1999) dated the formation to the Lutetian-Bartonian and found it to overlie the Molasses de Saix et de Lautrec Formation. [15] [16] Fauré (2011) agreed with the more recent dating of the formation to the Ypresian-Bartonian. [5]

Geology

The base of the Sables du Castrais Formation, which overlies Danian rocks, [12] is made up of Ypresian gravel clays and the Issel Sandstones, which range from 15–40 metres (49–131 ft), and the Argiles rutilants d'Issel et de Saint-Papoul Member is deposited within the gravel clays, and is between 20–30 metres (66–98 ft) thick. [12]

The Argiles rutilants d'Issel et de Saint-Papoul Member is overlain by the Lutetian Grès d'Issel Member, which is between 50–100 metres (160–330 ft) thick, [17] and is overlain by the Bartonian Molasses du Castelnaudary Member. [12] [18] [19] The whole formation underlies the Molasses de Saix et de Lautrec Formation. [5]

The Grès de Carcassonne Member also appears to be slightly younger than the Grès d'Issel Member, likely dating to the late Lutetian or early Bartonian. [20] [17]

The Sables du Castrais Formation was described by Capera and Baillet (2014) as a typical fluviatile formation, with lenticular channels, formed by conglomerates and sandstones, with calcareous cement and large trough cross-strata. [21]

Paleofauna

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Mammals

Artiodactyl
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Catadontherium C ? paquieri
Cebochoerus C.(Gervachoerus) campichii
C.(Cebochoerus) helveticus
Choeropotamus C. lautricensis
Dacrytherium D. elegans
Pseudoamphimeryx P. sp.
Robiacina R. minuta
Tapirulus Tapirulus cf. schlosseri
Xiphodon X. castrense
Lipotyphia
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Saturninia S. sp.
Marsupial
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Paratherium P. sp.
Pan-Carnivora
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Hyaenodon H. nouleti
H. sp
Quercygale Q. angustidens
Perissodactyl
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Anchylophus A. cf. desmaresti
A. cf. gaudini
Eurohippus E. parvulus
Eurohippus parvulus.jpg
Lophiodon L. isselense .
Lophiodon NT.jpg
L. lautricense .
L. sp.
Plagiolophus P. cartailhaci
P. cf. minor
Leptolophus L. nouleti
Lophiaspis L. occitanicus
Paralophiodon [12] P. isselense [12]
Palaeotherium P. castrense
Paleotherium 2.jpg
P. (Frantzenitherium) lautricense
P. isselanum [7]
P. rhinocerodes
P. siderolithicum
P. pomeli
Propalaeotherium P. sp.
Primates
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Adapis A. aff. parisiensis
A. rouxii
Necrolemur N. sp.
Rodent
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Gliravus G. sp.
Suevoscurius S. sp.
Pseudoltinomys P. sp.

Reptiles

Crocodilians
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Asiatosuchus A. depressifrons [12] Crocodylus depressifrons.jpg
Atacisaurus A. glareae [17]
A. cf. sp. [17]
Crocodylus C. rouxii
Dentaneosuchus D. crassiproratus [17] [3] A mandibular symphysis.A giant sebecid crocodile.
Dentaneosuchus crassiproratus.png
Iberosuchus I. cf. macrodon
Kentisuchus [12] K. astrei [12]
Pristichampsus P. rollinati
Pristichampsus restoration.png
Turtles
TaxaSpeciesLocalityStratigraphic positionMaterialNotesImages
Allaeochelys A. pareyrei
A. nouleti
A. castrensis
Hadrianus H. castrensis
Neochelys N. mengauti
N. sp. [22]
Trionyx T. filholi
T. sp. [23]

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References

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