Saint-Chinian Formation | |
---|---|
Stratigraphic range: | |
Type | Geologic formation |
Underlies | La Maurerie Formation |
Overlies | La Dentelle Formation |
Thickness | around 500 m |
Lithology | |
Primary | Shale |
Other | Sandstone |
Location | |
Coordinates | 43°25′07″N2°56′43″E / 43.418624°N 2.945366°E |
Region | Occitanie |
Country | France |
Type section | |
Named for | Saint-Chinian |
The Saint-Chinian Formation is a geological formation composed of shales with limestone inclusions, dating from the Lower Ordovician (Tremadocian).
It is one of the six geological formations from the Saint-Chinian Cambro-Ordovician basin, comprising, from the most ancient to the most recent : La Dentelle Formation, Saint-Chinian Formation, La Maurerie Formation, Cluse de l'Orb Formation and Setso member, Foulon Formation and Landeyran Formation. This formation outcrops on the southern flanks of the Montagne Noire in Southern France. [1]
The formation received its name from the small city of Saint-Chinian, a commune located in the Hérault department in Occitania.
It is dated from the biostratigraphic sub-zone characterized by Taihungshania miqueli and Asaphelina barroisi berardi. [1]
The thin nature of the silico-clastics deposits, the presence of slump, combined with a trilobite fauna dominated by members of the Asaphidae family indicates a marine environment of external distal platform. [2]
Shales of the Saint-Chinian Formation bears in certain areas accumulations of phosphated nodules, each potentially bearing a trilobite. Those are the so-called "schistes à gateaux" [3] ..
Genus | Species | Locality | Age | Notes | Images |
---|---|---|---|---|---|
Cyclostomiceras | C. thorali | Euloma filacovi Zone | Late Tremadocian | A cyclostomiceratid ellesmerocerid [4] | |
Saloceras | S. chinianense | Euloma filacovi Zone | Late Tremadocian | An eothinoceratid ellesmerocerid [4] | |
S. murvielense | Euloma filacovi Zone | Late Tremadocian | An eothinoceratid ellesmerocerid [4] | ||
S. pradense | Taihungshania miqueli acme Subzone | Late Tremadocian | An eothinoceratid ellesmerocerid [4] | ||
Rioceras | R. escandei | Euloma filacovi Zone ; Asaphelina barroisi berardi and Taihungshania miqueli Subzone | Late Tremadocian | A rioceratid ellesmerocerid [4] | |
Felinoceras | F. constrictum | Euloma filacovi Zone | Late Tremadocian | A rioceratid ellesmerocerid [4] | |
Annbactroceras | A. martyi | Euloma filacovi Zone | Late Tremadocian | A baltoceratid orthocerid [4] | |
A. felinense | Euloma filacovi Zone | Late Tremadocian | A baltoceratid orthocerid [4] | ||
Bactroceras | B. mourguesi | Euloma filacovi Zone | Late Tremadocian | A baltoceratid orthocerid [4] | |
Cochlioceras | C.? aff. roemeri | Euloma filacovi Zone ; Asaphelina barroisi berardi and Taihungshania miqueli Subzone | Late Tremadocian | A baltoceratid orthocerid [4] | |
Thoraloceras | T. bactroceroides | Euloma filacovi Zone ; Asaphelina barroisi berardi and Taihungshania miqueli Subzone | Late Tremadocian | A troedsonellid dissidocerid [4] | |
Lobendoceras | L. undulatum | Euloma filacovi Zone ; Asaphelina barroisi berardi and Taihungshania miqueli Subzone | Late Tremadocian | A protocameroceratid endocerid [4] | |
Genus | Species | Locality | Age | Notes | Images |
---|---|---|---|---|---|
Paramegalaspis | P. immarginata | Prades-sur-Vernazobre | Late Tremadocian-Early Arenig | An asaphid [5] | |
Asaphellus | A. frequens | Prades-sur-Vernazobre | Late Tremadocian-Early Arenig | An asaphid [5] | |
A.? sp. | Félines-Minervois | Late Tremadocian-Early Arenig | An asaphid [5] | ||
Aocaspis | A. macrophtalma | La Rouvelane, près de Prades-sur-Vernazobre | Late Tremadocian-Early Arenig | An nileid [6] | |
Geragnostus | G. occitanus | Saint-Chinian | Early Arenig | A geragnostid [7] | |
G. callavei | Saint-Chinian | Early Arenig | A geragnostid [7] | ||
G. pusio | Saint-Chinian | Early Arenig | A geragnostid [7] | ||
Micragnostus | M. languedocensis | Saint-Chinian | Early Arenig | A micragnostid [7] | |
Trinodus | T. chinianensis | Saint-Chinian | Early Arenig | A trinodid [7] | |
T. corpulentus | Saint-Chinian | Early Arenig | A trinodid [7] | ||
T. abruptus | Saint-Chinian | Early Arenig | A trinodid [7] | ||
T. oviformis | Saint-Chinian | Early Arenig | A trinodid [7] | ||
Other fossil remains of marine animals are known from the formation: [13]
Sagittariidae is a family of raptor with one living species—the secretarybird native to Africa—and a few fossil taxa.
Cothurnocystis is a genus of small enigmatic echinoderms that lived during the Ordovician. Individual animals had a flat boot-shaped body and a thin rod-shaped appendage that may be a stem, or analogous to a foot or a tail. Fossils of Cothurnocystis species have been found in Nevada, Scotland, Czech Republic, France and Morocco.
The Montagnes Noires, also known as the Montagne Noire and in Breton as Menez Du are an east–west oriented range of hills in Brittany centred on the town of Gourin. They culminate in the peak of Roc de Toullaeron which attains a height of either 318m or 326m. Other significant peaks include Ar Menez (304m) and Montagne Noir (307m) . They are composed from a range of Precambrian, Ordovician, Silurian and Devonian rocks forming a part of the Variscan orogen and include sandstones, quartzites and slates.
Iberosuchus is a genus of extinct sebecosuchian mesoeucrocodylian found in Western Europe from the Eocene. Remains from Portugal was described in 1975 by Antunes as a sebecosuchian crocodilian. This genus has one species: I. macrodon. Iberosuchus was a carnivore, unlike the crocodilians today, they are not aquatic and are instead terrestrial.
Congosaurus is an extinct genus of dyrosaurid mesoeucrocodylian. Fossils have been found from Lândana, in Angola and date back to the Paleocene epoch. In 1952 and 1964 Congosaurus was proposed to be synonymous with Dyrosaurus. The genus was later thought synonymous with Hyposaurus in 1976 and 1980. It has since been proven a distinct genus of dyrosaurid separate from both Dyrosaurus and Hyposaurus.
Miliolacea is one of five superfamilies belonging to the Miliolida,.
Velumbrella is a medusoid organism with tentacles known from the Middle Cambrian of Poland, and perhaps related to Rotadiscus; the fossils depict a scleritosed disk with a U-shaped gut. It was originally related to members of the Ediacara biota but is now thought to be related to the paropsonemids.
The Fezouata Formation or Fezouata Shale is a geological formation in Morocco which dates to the Early Ordovician. It was deposited in a marine environment, and is known for its exceptionally preserved fossils, filling an important preservational window beyond the earlier and more common Cambrian Burgess shale-type deposits.
The Canaveilles Group is the basal metasedimentary succession of late Neoproterozoic and Cambrian age outcropping in the Pyrenees.
Pierre Hupé was a French paleontologist.
Geragnostus is a genus of very small agnostid trilobites whose fossils are found Ordovician-aged marine strata from Eurasia, North America and Argentina.
Cynohyaenodon is an extinct paraphyletic genus of placental mammals from extinct family Hyaenodontidae that lived from the early to middle Eocene in Europe.
The Pissot Formation is a geologic formation in the Armorican Massif of Normandy, northwestern France. It preserves fossils dating back to the Darriwilian to Sandbian stages of the Ordovician period.
The Grand Auverné Formation is a geologic formation in France. It preserves fossils dating back to the Darriwilian to Sandbian stages of the Ordovician period.
Pseudocorax is an extinct genus of mackerel sharks that lived during the Late Cretaceous. It contains six valid species that have been found in Europe, the Middle East, North Africa, and North America. It was formerly assigned to the family Anacoracidae, but is now placed in its own family Pseudocoracidae along with Galeocorax. The former species "P." australis and "P." primulus have been reidentified as species of Echinorhinus and Squalicorax, respectively.
Bailiaspis Resser, 1936, is a Middle Cambrian (Miaolingian) trilobite genus belonging to the Family Conocoryphidae Angelin, 1854. Within the Acado-Baltic region, the genus ranges from Wuliuan into Guzhangian age strata.
Cambraster is an extinct genus of edrioasteroids with species that existed during the Cambrian.
Pelargopappus is an extinct genus of raptor related to the secretarybird that lived in early Miocene France. Only one species, the type species P. magnus is officially recognized. A second species, P. schlosseri from the mid-and late Oligocene, was split off into the genus Amphisagittarius.
Hemitragus bonali, the Bonal tahr, is an extinct species of bovid from the Pleistocene of Europe and the Caucasus mountains region.
Luc Bulot was a French paleontologist mainly known for his work on the biostratigraphy of West Africa and on the determination of Lower Cretaceous GSSP.
{{cite book}}
: CS1 maint: location missing publisher (link)