Calcaire d'eau douce de Soulce (USM)
Rappresentazione e statuto
- Colore CMYK
- (0%,4%,49%,4%)
- Colore RGB
- R: 245 G: 235 B: 125
- Rango
- Formazione litostratigrafica
- Uso
- Unità in uso.
- Status
- termine locale (informale)
- Discussione del statuto
Nomenclatura
- Deutsch
- Soulce-Süsswasserkalk (USM)
- Français
- Calcaire d'eau douce de Soulce (USM)
- Italiano
- Calcare d'acqua dolce di Soulce (USM)
- English
- Soulce Freshwater Limestone (USM)
- Origine del nome
-
Bordure nord du vallon de Soulce (JU), Haute-Sorne
- Varianti storiche
-
calcaires d'eau douce du Valon de Soulce-Undervelier (Fleury 1910), --- (Rollier 1910), calcaires oligocènes affleurant au NW de Soulce = gisement de Soulce (Gaudant 1979), Calcaires d'eau douce delémontiens (Pfirter 1997), Rupelian lacustrine lithographic limestones from Soulce (Mennecart et al 2011)
Links
- Non-synonimo
Descrizione
- Potenza
- 95 cm (Mennecart et al. 2011
Componenti
- vertebrati
- pesci
- molluschi
-
piante
:
Plantae
Iberomeryx (Mennecart et al. 2011)
Gerarchia e successione
- Limite inferiore
-
Molasse alsacienne s.s.
Età
- Geomorfologia
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- Rupeliano
- Età alla base
-
- Rupeliano
- Metodo di datazione
-
MP23 (Becker 2003, Mennecart et al. 2011, Mennecart 2012)
Paleogeografia e tettonica
-
- USM-J
- Termini generici
- Tipo di origine
-
- sedimentaria
- Condizioni di formazione
-
paléoécologie: cf. Gaudant 1979
Referenze
- Revisione
-
(2011) :
Iberomeryx minor (Mammalia, Artiodactyla) from the Early Oligocene of Soulce (Canton Jura, NW Switzerland): systematics and palaeodiet. Swiss J. Geosci. 104/Suppl.1, 115–132
p.117: According to the description of the outcrop (Fleury 1910; Rollier 1910) and in agreement with the geological map (Pfirter et al. 1996; Pfirter 1997) and the recent works on lithostratigraphy (Picot 2002; Berger et al. 2005a), the base of the short section is defined by Paleogene siderolitic fissure-fills and deposits (Bolustone, Ziegler 1956; Bohnerzkonglomerate, Greppin 1855) within and overlaying Mesozoic bedrock. The base of the overlying continental interval is formed by approximately 4 m of marly, calcareous and sandy deposits of the Molasse alsacienne sensu stricto (sensu Picot 2002). The Iberomeryx specimens were preserved in a 95 cm thick lacustrine lithographic limestone bed, extraordinarily rich in plant-, mollusk-, and vertebrate remains. Because of the many articulated fish skeletons (Esox, Umbra, Leuciscus) and two articulated amphibian specimens (Palaeobatrachus cf. diluvianus), this bed can be described as a conservation Lagersta¨tte.