Paleobiota of the Posidonia Shale
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The Posidonia Shale or Posidonienschiefer Formation is a geological formation of southwestern Germany, northern Switzerland, western Czech Republic, northwestern Austria, southeast Luxembourg and the Netherlands, that spans about 3 million years during the Early Jurassic period (early Toarcian stage). It is known for its detailed fossils, especially sea fauna, listed below.[1] Composed mostly by black shale, the formation is a Lagerstätte, where fossils show exceptional preservation (Including exquisite soft tissues), with a thickness that varies from about 1 m to about 40 m on the Rhine level, being on the main quarry at Holzmaden between 5 and 14 m.[1] Some of the preserved material has been transformed into fossil hydrocarbon Jet, specially wood remains, used for jewelry.[2] The exceptional preservation seen on the Posidonia Shale has been studied since the late 1800s, finding that a cocktail of chemical and environmental factors let to such an impressive conservation of the marine fauna.[2] The most common theory is the changes on the oxygen level, where the different anoxic events of the Toarcian left oxygen-depleted bottom waters, with the biota dying and falling to the bottom without any predator able to eat the dead bodies.[3]
Microbial Activity
Color key
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Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Location | Material | Notes | Images |
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Traces of Microbial Activity |
Non-fenestrate stromatolite crusts formed in Aphotic deep-water environments during intervals of very low sedimentation.[4] Abundant on the Precambrian, but after it, and concretely on the Jurassic-Cretaceous, the appearance of the Corallinaceae algae and related biota forced the stromatolite-forming microbes to withdraw to extreme habitats such as hypersaline lagoons and possibly to deep-water settings. On the Posidonia Shale are related with plankton, mainly coccoliths and the problematic Schizosphaerella (A Haptophytan Alga), but also typical deep-sea forms including various groups of cephalopods, and articulated skeletons of fishes and reptiles.[4] The Stromatolites of this region have evidence of live on a deeper shelf environment with a quietwater deposit which suffered repeated phases of stagnant bottom waters, where a depth water habitat developed, probably at more than 100 meters depth.[4] There is a thin, southern widespread Stromatolite crust on the Top of the Posidonia Shale, called "Wittelshofener Bank", that has made rethink the depth of the major southern basin of the formation, where with the absence of phototrophic calcareous benthic organisms (probably due to the lack of light), shows the deph character of the Basin.[4] On the "Wittelshofener Bank" there is also the only occurrence of Ooids, presumably formed in the same deep-water environment.[4] |
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Possible traces of Microbial Activity |
Probably related with Archaea activity.[4] Altrought Frutexites is a cryptic microfossil and an important element of many deep water stromatolites, with an Inorganic origin proposed, where are interpreted as dendritic shrubs to purely inorganic growth of Aragonitic crystals, but also resemble shrubs of the cyanobacteria Angulocellularia.[4] On the Posidonia a cryptoendopelitic mode of life is assumed, being only possible for Heterotrophic bacteria or Fungi.[4] As seen on the Stromatolites of the Posidonia, Frutexites acted mainly as a dweller or secondary binder of the deep-water stromatolites, not as their major constructor.[4] |
Rhizaria
Foraminifera
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Shells |
A benthonic Foraminiferan, member of Vaginulinidae inside the family Vaginulinida (Lagenina). An extant genus. Its shell resemble a mixture between an ammonite conch, due to having a lower spiral, and a mussel. |
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Shells |
A benthonic Foraminiferan, member of Vaginulinidae inside the family Vaginulinida (Lagenina). Its conch has a Myriapod-like segmented built. |
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Shells |
A benthonic Foraminiferan, member of Vaginulinidae inside the family Vaginulinida (Lagenina). |
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Shells |
A benthonic Foraminiferan, type member of Vaginulinidae inside the family Vaginulinida (Lagenina). |
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Shells |
A benthonic Foraminiferan, member of Vaginulinidae inside the family Vaginulinida (Lagenina). |
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Shells |
A benthonic Foraminiferan, member of Marginulininae inside the family Vaginulinida (Lagenina). |
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Shells |
A benthonic Foraminiferan, member of Lenticulininae inside the family Vaginulinida (Lagenina). |
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Shells |
A benthonic Foraminiferan, type member of Cornuspiridae inside the family Cornuspirida (Lagenina). Round-spiral shell morphology |
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Shells |
A benthonic Foraminiferan, member of Nodosariidae inside the family Nodosariacea (Lagenina). Dentalina is an extant genus, with an elongated shell, that resemble a small worm. |
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Shells |
A benthonic Foraminiferan, member of Nodosariidae inside the family Nodosariacea (Lagenina). |
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Shells |
A benthonic Foraminiferan, type member of Ichthyolariidae inside the family Lagenina. Another genus with a Myriapod-like segmented built. |
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Shells |
A benthonic Foraminiferan, type member of Lingulininae inside the family Nodosariidae (Lagenina). Dentalina is an extant genus, with an elongated shell, that resemble a small worm. |
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Shells |
A benthonic Foraminiferan, member of Ceratobuliminidae inside the family Robertinida . It resembles a small ammonite. |
Dinoflagellata
Dinoflagellate cysts
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Millions of specimens |
A Dinoflagellate cyst, member of Dinophyceae of the family Nannoceratopsiaceae. On the Lias Epsylon Interval (Lowermost Toarcian), most of the assemblages are dominated by Nannoceratopsis gracilis. Nannoceratopsis senex becomes highly abundant until the uppermost Tenuicostatum.[7] |
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Millions of specimens |
A Dinoflagellate cyst from the family Comparodiniaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Comparodiniaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Apodiniaceae. An Ectoparasitic dinoflagellate, whose hosts are normally Tunicates |
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Millions of specimens |
A Dinoflagellate cyst from the family Scriniocassiaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Scriniocassiaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Scriniocassiaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Scriniocassiaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Heterocapsaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Heterocapsaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Heterocapsaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Heterocapsaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Gonyaulacaceae. |
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Millions of specimens |
A Dinoflagellate cyst from the family Peridiniphycidae. |
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Millions of specimens |
A Dinoflagellate cyst, type member of Mancodiniaceae. Dominant genera on some layers of the Lias Delta Stage.[7] |
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Millions of specimens |
A Dinoflagellate cyst, member of Mancodiniaceae. Commonly found along the genus Beaumontella.[8] |
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Millions of specimens |
A Dinoflagellate cyst, type member of Luehndeoideae. Luehndea spinosa is common on the medium layers of the lower Posidonia Shale, while restricted to some areas on the Lias delta.[7] |
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Millions of specimens |
A Dinoflagellate cyst, member of Suessiaceae. Common on Pliensbachian levels, become present but rare on lower Toarcian.[8] |
Algae
Includes abundant variety of algae, such as the genus of colonial Green algae Botryococcus,[13] or the unicellular algal bodies Tasmanites, and other small examples. Algae are a good reference for changes on the oxygen conditions along the Toarcian.[14]
Algae Acritarchs
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Millions of specimens |
An Acritarch probably from Algal origin. Veryhachium fossils represent open marine and transgressive conditions. It has high presence on most of the samples studied from the Posidonia Shale, being nearly the 50% of the Acritarch fraction on some locations. |
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Millions of specimens |
An Acritarch probably from Algal origin. Its fossils indicate nearshore or estuarine to shallow lagoon and/or slightly brackish-water environments. It is the dominant on the nearshore sections. |
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Millions of specimens |
An Acritarch probably from Algal origin. Related to estuarine deposits. |
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Millions of specimens |
An Acritarch probably from Algal origin. Related to open shelf deposits |
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Millions of specimens |
An Acritarch probably from Algal origin. Related to open shelf deposits |
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Millions of specimens |
An Acritarch probably from Algal origin. Related to open shelf deposits |
Haptophyta
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Millions of specimens |
A member of the family Parhabdolithaceae inside Stephanolithiales. Shore deposits genus. The abundance drop of M. jansae further characterise the T-OAE perturbation, where becomes the dominant Genus on most of the Saxony Basin. |
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Millions of specimens |
Type member of the family Parhabdolithaceae inside Stephanolithiales. |
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Millions of specimens |
Type member of the family Schizosphaerellaceae inside Parhabdolithaceae. Towards the Pliensbachian-Toarcian extincion this genus gets a decrease in abundance and size that shows the change and biotic crisis. |
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Millions of specimens |
Type member of the family Biscutaceae inside Parhabdolithaceae. |
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Millions of specimens |
A member of the family Chiastozygaceae inside Eiffellithales. |
Chlorophyta
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Millions of specimens |
A member of Dinophyceae. |
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Millions of specimens |
A member of Peridiniaceae inside Dinophyceae. |
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Millions of specimens |
A member of Gonyaulacaceae inside Dinophyceae. |
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Millions of specimens |
A member of Prasinophyceae. It the main genus present on silt and sand horizons, trending to be absent on black argillaceous layers. |
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Millions of specimens |
A member of Prasinophyceae. A genus common on green clays and other upper strata on the formation. |
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Millions of specimens |
A member of Prasinophyceae. A genus common on green clays and other upper strata on the formation. |
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Millions of specimens |
A member of Prasinophyceae. A genus common on green clays and other upper strata on the formation. |
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Millions of specimens |
A member of the Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the family Pyramimonadales inside Prasinophyceae. Basinal deposits genus |
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Millions of specimens |
A member of the family Halosphaeraceae inside Chlorodendrales. Basinal deposits genus |
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Millions of specimens |
Type member of the family Botryococcaceae inside Trebouxiales. Freshwater or Deltaic Genus |
Plantae
The macroflora of the Posidonia slate can be described as extremely poor in species.[19] Apart from the remains of Horsetails, it is without exception the remains of coarse branches and fronds from gymnosperms, in which one has a certain can assume transport resistance. Remains of Ferns are completely missing, except for tall arboreal ferns (Peltaspermales).[20] Mostly of the flora was reported from the area of Braunschweig.[19] The major explanation for the flora could be that the plants in question are mono-or oligotypic stands on the edge of the waters that flow into the Posidonienschiefer sea, probably tear away in the course of flood events, easily fragmented during transport and wave waves, possibly especially in the occasional storm events postulated.[21] In terms of taphonomy, this would result in a comparison with today's reed Phragmites, which can form extensive stocks on the edge of shallower and slowly flowing waters ("Reed belts").[19] The Wood remnants clearly indicate one higher diversity of Coniferous flora in the delivery area than the remains of leafy branches.[19] This fact is likely to be proportionate, similar to that frequent occurrence of charcoalized or gagged trunks, mostly of them are believed to be "driftwoods" that only take a long time drifting also suggests a frequent settlement with mussels and full-grown Sea Lilies.[19][21] The deposition settings are at large distance from the nearest coastline (for southern Germany about 100 kilometers), making only plants strong to transportation able to resist enougth to get deposited.[22][23]
Palynology
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Spores |
Affinities with Lycopsida. Most Abundant Pollen on the Bohemian realm |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopsida. |
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Spores |
Affinities with Lycopodiaceae. |
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Spores |
Affinities with Lycopodiaceae. |
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Spores |
Affinities with Isoetales. |
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Spores |
Affinities with Bryophyta. |
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Spores |
Affinities with Schizaeales. |
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Spores |
Affinities with Schizaeales. |
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Spores |
Affinities with Selaginellaceae. |
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Pollen |
Affinities with Gymnospermophyta. Non concreted affinities |
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Pollen |
Affinities with Gymnospermophyta. Non concreted affinities |
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Spores |
Affinities with Pteridopsida. |
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Spores |
Affinities with Pteridopsida. |
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Spores |
Affinities with Pteridopsida. |
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Spores |
Affinities with Pteridopsida. |
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Spores |
Affinities with Pteridopsida. |
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Spores |
Affinities with Ophioglossaceae. |
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Spores |
Affinities with Gleicheniaceae. |
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Pollen |
Affinities with Bennettitales. Abundant on the Lower Jurassic of NW Europe. |
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Pollen |
Affinities with Bennettitales. |
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Spores |
Affinities with Bennettitales. |
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Spores |
Affinities with Ginkgoopsida. |
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Spores |
Affinities with Pinopsida. |
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Pollen |
Affinities with Pinidae. Abundant on the Lower Jurassic of NW Europe, represents pollen of medium to large arboreal plants, specially coniferales. |
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Pollen |
Affinities with Cupressaceae inside Pinaceae. |
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Pollen |
Affinities with Cheirolepidiaceae. Abundant on the Lower Jurassic of North and Southern Europe, represents pollen of medium to large arboreal plants, specially coniferales. The abundance of pollen of Classopollis and other thermophile plants was observed in this region in the lower Toarcian from the end of the antiquum (= tenuicostatum) zone to the middle of commune zone.[27] |
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Pollen |
Affinities with Cheirolepidiaceae. Pollen of medium to large arboreal plants, specially coniferales. |
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Spores |
Affinities with Podocarpaceae. Pollen of medium to large arboreal plants, specially coniferales. |
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Pollen |
Shares morphology with Chloranthaceae pollen. Can be an example of primigenial Angiosperms pollen, more probably pollen related to genera such as Sanmiguelia and other primigenial Flower-Plant like flora. |
Equisetaceae
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Stems |
Affinities with Equisetaceae inside Equisetopsida. Number of mostly very fragmented and not particularly well preserved, but clear horsetail remains described. So far Recognizable, leaf sheaths were developed in most cases, but the state of preservation does not allow a more precise determination.[28] |
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Stems and incomplete axes |
Affinities with Equisetaceae inside Equisetopsida. Neocalamites is the most common more distributed of all the Posidonia Shale, being even found on Luxembourg Posidonia Strata.[30] Mostly of the Stems reported come from Aeolian-Dunar related deposits, or from nearshore-basinal deposition. Probably was related to the seashore.[30] Some stems are big, resembling the rates of growth seen on modern Bamboo specimens, suggesting +6–7 m tall Equisetopsids.[30] |
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Pollen Cones |
Affinities with Calamitaceae inside Equisetopsida. It was an approximately 2–3 m high shrub-like plant related to swamp environments. Calamitaceans are common in late Palaeozoic wetland plant communities, so the find of a jurassic specimen is rare.[31] Maybe is a mistaken new genera of Pollen cone, but definitely come from an Equisetalean. This genus is found associated with Annularia, being both part of the Calamites plant. It can be related with the Equisetites stems found on the formation. |
Pteridospermatophyta
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Affinities with Umkomasiaceae inside Corystospermaceae. Is based on bipinnate leaves, rachis longitudinally striated, with a long petiole and secondary rachises. It belongs to large tree ferns. Posidonia Shale Specimen is characterized for its large size and probably where attached to trunks similar in built to the Cretaceous genus Tempskya.[32] |
Cycadeoidophyta
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Affinities with Cycadeoidaceae inside Bennettitales. It is the most abundant medium-sized plant on the environment. Found specially on seashore depositional settings, but also on deltaic and lagoonar environments. It was a low arbustive-arboreal Bennetite related to arid environments, with a leave similar of that of the modern genus Encephalartos, specially Encephalartos munchii, but also Dioon mejiae. Otozamites has been considered synonym with Otopteris, but since the 1990s everybody used the name Otozamites, and Otopteris was forgotten.[35] |
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Affinities with Cycadeoidaceae inside Bennettitales. This Bennettitalean is related to Shrub built. Some specimens where assigned to Dioonites acutifolium (Junior synonym). Consits on leaves with pinnate, leaflets perpendicular or oblique to the rhachis, on the top of the leaf axis. It comes from fragments of fairly large fronds. In its external form it closely follows the modern genus Dioon, only the leaflets are of our kind wider and shorter, they are further apart, but the tendency to rhachis is the same. |
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Affinities with Williamsoniaceae inside Bennettitales. Arboreal Cycadaceans, some with the presence of flower-like structures. It resembles the leaf of the modern Microcycas calocoma, and probably had a similar arboreal built, being the leave of tall Bennetite trees such as Bucklandia, found on the middle jurassic of England. |
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A member of Williamsoniaceae inside Bennettitales. It has been interpreted as a cycad in the family Cycadaceae or a Bennettitalean plant. Leaflets somewhat removed, oval-oblong, a little narrower near the base, rounded at the tip, nerves partially diverging from the base towards the edge. It was assigned to Pterophyllum oblongifolium and on the genus Glossozamites. This genus was the leaf of arboreal Bennetites, similar in appearance to the modern Encephalartos woodii. |
Ginkgoales
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Affinities with Ginkgoaceae inside Ginkgoales. Various leaves are known from Ohmden, coming from marine deposits and where identified as Ginko digitata, identified originally as the only Ginko specimen reported on the Posidonia Shale. |
Pinophyta
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
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Affinities with Araucariaceae or Cheirolepidiaceae inside Pinales. Pagiophyllum araucarinum predominates among the two types of leafy coniferous branches that have become known from the Posidonia. However, there is no indication whether this fact reflects their respective share in the vegetation of the delivery area. Cheirolepidiaceae Pollen is the most abundant and diverse found on the formation, what is correlated with the abundance of this genus. Other factor that puts local Pagiophyllum on Cheirolepidiaceae is the dominance of an arid climate, the preferred for this type of conifers. |
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Affinities with Araucariaceae or Cheirolepidiaceae inside Pinales. Specimens whose spiral foliage of the branch, in which the individual leaves open about 2/3 of their length (without the tip) are fused with the branch they hold in their free part fits tightly, suggests belonging to the genus Brachyphyllum. |
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A possible ancestral member of the Sequoioideae or Callitroideae inside Cupressaceae. Was originally related to the genus "Quasisequoia" couttsiae, as a sister taxa to Sequoia jeholensis. The later studies suggest affinities with large modern redwoods, but others find relationships with the modern genus Fitzroya cupressoides. Both Genera are related with relatively humid ecosystems, while Widdringtonites is known from an Arid setting. |
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Fossil wood |
Affinities with the Taxodioideae family inside Cupressaceae. Resembles the modern genus Cryptomeria, but others resemble the southern genus Fitzroya, from the family Callitroideae. Large trees probably related to the coastal settings. |
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Fossil wood |
Affinities with the Taxaceae family inside Cupressaceae. Resembles the modern genus Austrotaxus. |
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Fossil wood |
Affinities with Sequoioideae inside Cupressaceae. Large wood with a morphology similar to the modern genus Sequoia sempervirens. Probably related to Widdringtonites liasinus, representing the earliest representatives of the Sequoia tribe. |
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Fossil wood |
Affinities with Podocarpaceae. It shares characters with modern Sciadopitys, Microcachrys, Dacrydium and Acmopyle. |
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Fossil Wood |
Affinities with Podocarpaceae, resembling modern genera such as Dacrycarpus, with other specimens resembling Juniperus. Includes wood more related to nearshore arbustive Conifers (columnar or low-spreading Shrubs with long, trailing branches), being the most abundant, but also medium to large arboreal conifers from nearshore forests. |
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Fossil wood |
Affinities with Podocarpaceae. Similar to the modern Phyllocladus aspleniifolius. |
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Fossil wood |
Affinities with Podocarpaceae. Resembles the modern Phyllocladus hypophyllus. |
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Fossil wood. |
Affinities with Araucariaceae. The largest known rafting wood on the fossil record is assigned to this genus, with a length of 18 m. The rafts were populated with Crinoid colonies, and a wide variety of organisms.[43] |
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Fossil wood |
Affinities with Araucariaceae, resembling the modern Wollemia. |
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Fossil wood |
Affinities with Araucariaceae, resembling the modern Agathis. |
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Fossil wood |
Affinities with Cheirolepidiaceae. Includes large sized trunks up to 1.7 m tall and 115 cm wide. Large medium to large sized trees (25 m) that extent along the coastal lines of the Vindelician land. The wood from tose trunks shows insect activity, such as wood Vasps and Beetles, that had been found on the Posidonia Shale. |
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Fossil wood |
Affinities with Cheirolepidiaceae |
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Fossil wood |
Dubious genera with possible affinities with the triassic wood Woodworthia. Protopinaceae is an invalid group of mostly Paleozoic Woods.[50] |
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Fossil wood |
Affinities with Coniferales, concretely is closer to the Podocarpaceae, Cupressaceae and in a lesser extend to the Cheirolepidiaceae. Finally can be a member of the extinct family Miroviaceae. It is the more abundant genus of wood present on the Bohemian Realm of the Posidonia Shale. |
Invertebrata
Ichnofossils
Genus | Species | Location | Material | Notes | Images |
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Burrowing and track ichnofossils |
Burrow-like ichnofossils, that can be related to Crustaceans, Annelids and Fishes.[54] The presence of this burrows changed along the different depositional layers, interpreted as result of relative magnitudes and durations of a series oxygenation events.[54] Increased Oxygen conditions eventually led to a level that permitted both the survival of larger Chondrites and Thalassinoides producing organisms, as well the depth of the Burrow-like structures.[54] The changes on the layers are detailed enough to know that oxygenation-change events duration was sufficient to allowe the migration and establishment of trace-producing organisms, establishing an "equilibrium" with bottom-water oxygen conditions.[54] |
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Burrowing and track ichnofossils |
Burrow-like ichnofossils. Interpreted as the feeding burrow of a sediment-ingesting animal.[56] A more recent study has find that Scoloplos armiger and Heteromastus filiformis, occurring in the German Wadden Sea in the lower parts of tidal flats, make burrows that are homonymous with numerous trace fossils of the ichnogenus.[57] |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. It consists commonly on a subhorizontal branching burrow system consisting of radiating tunnels filled with fecal pellets.[58] It has been interpreted as a product made by an Endobenthic deposit-feeding animal, specially a Fodinichnia, burrows produced by benthonic subsurface food-mining activity, as is proved by the tunnels and pelletal infill.[58] The study of the Fecal Pellets has revelated that the maker of this ichnogenus was an epicontinental shelf setting non-selective deposit feeder, ingesting particles on the sediment surface without selection. A mode of feeding common on aquatic Benthos, reported on modern animals such as Spionid Polychaete worms, tropical Holothurians and Spatangoid urchins.[59] |
||
|
|
Burrowing and track ichnofossils.[61] |
Burrow-like ichnofossils. It has been related to Echiuran annelids,[62] but also from moving and feeding polychaete worms.[63] |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. Considered an "Algae incertae sedis" fossil, it was recovered subdivided into 16 different groups, being in 1880 along certain ichnofossil genera, such as Cruziana with a massive nomenclatural complexity. Considered now a feeding burrow of a sediment-ingesting animal, sometimes synonymized with Chondrites. |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. It is controversial, since is considered a strictly a junior synonym of Palaeophycus.[65] |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. Palaeophycus is considered related with Planolites, being a litoral fodichnia, probably from a Priapulidan. |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. It is interpreted as a grazing trail or Fodinichnia, produced at shallow depth in sediment by Polychaetes and Priapulids.[66] |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. Gyrochorte is interpreted as a result of active digging on the sediment by deposit-feeding worm-like animal, probably an Annelid or similar kinds of creatures, such as Crustaceans, Sea Urchins, nearshore fishes, etc. |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. Cylindrichnus isp. was found only on seashore-related sections, and probably represents litoral Polychaete Burrows.[67] |
||
|
|
Burrowing and track ichnofossils. |
Burrow-like ichnofossils. Vertical or oblique complex trace fossil composed of a bunch of spindle-shaped structures and associated tubes, typical of a restricted environment (?estuarine/lagoonal). |
||
|
|
Burrows and associated traces |
Burrow-like ichnofossils. Spongeliomorpha is believed to come from the domicile of Crustaceans: Anomuras (Probably Eocarcinoidea) and Decapodans (Probably Glypheidae), created as they dig in a firm, semiconsolidated substrate. |
||
|
|
Burrows and associated traces |
Burrow-like ichnofossils. Most Diplocraterion show only protrusive spreit, like the local ones, produced under predominantly erosive conditions where the organism was constantly burrowing deeper into the substrate as sediment was eroded from the top. It can be Made by Crustaceans, Annelids or other benthic fauna.[66] |
Anthozoa
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Polyps |
A stone cora of the family Caryophylliidae inside Hexacorallia. Related to shallow waters, this genus is the main coral found on the Posidonia Shale, resembling the modern Polycyathus muellerae. Its fossils are related with near-land facies, Coralline Islands and relatively small landmases shuch as the Bohemian Massif. |
Porifera
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Specimens |
A sea sponge of the family Cribrospongiidae inside Sceptrulophora. Found on Shallow and basinal waters, some specimens get 22 cm wide, with a funnel-like morphology. It is relatively common on nearshore strata, but generally rare. |
||
|
|
Specimens |
A sea sponge (Glass sponge) of the family Staurodermatidae inside Hexactinellida. Found only on depth Basinal deposits, with a funnel like morphology attaining a diameter of at least 15 cm, with the exception of a large specimen of 30 cm diameter found on Dotternhausen. |
Annelida
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. Its affinities with the genus Serpula are controversial, since the genus is known mostly since Creataceus strata. Although there are other fossils assigned to the genus on same age deposits of France.[70] |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. It show the characteristic features to live on soft mud ground. |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. It show the characteristic features to live on soft mud ground. |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. Pentaditrupa managed to lie freely on the mud, as shows that its tube's curvature provides stability to its position. |
||
|
|
Multiple Specimens. |
A sessile, marine annelid tube worm of the family Serpulidae. Denominated "Serpula" segmentata, it lacks the two longitudinal edges characteristic on Mucroserpula. |
||
|
|
Multiple Specimens. |
A polychaete worm of the family Sabellidae. |
||
|
|
Leech cocoons |
Hirudinea cocoons, identified with palynological residues. The cocoons Dictyothylakos are common on flooded basin sediments, and implies not only the presence of parasitic leeches, but also the presence of large hosts nearby. |
Mollusca
Brachiopoda
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
A Discinidae rhynchonellatan. This genus was found had a planktotrophic larval stage, that adapted while growing to the local redox boundary, when this fluctuated near the sediment–water interface and oxygen availability prevailed, allowing benthic colonization. Is found on associations with Grammatodon and Pseudomytiloides.[85] |
||
|
|
Thousands of Specimens. |
A Lingulidae rhynchonellatan. Associations of bioturbation infauna are dominated on certain sections by Palaeonucula/Lingula agrupations, developed under longer-term oxygenated conditions within the substrate and bottom waters.[85] |
||
|
|
Thousands of Specimens. |
A Rhynchonellidae rhynchonellatan. Found assciated with Plicatula on long-term well-oxygenated conditions within the substrate and bottom waters.[85] |
Bivalvia
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
A propeamussiid mud scallop. |
||
|
|
Thousands of Specimens. |
A plicatulid mud scallop. |
||
|
|
20.000 specimens/m2 |
A "posidoniid" ostreoidan. It is the type fossil of the Posidonia Shale. Originally it was named "Posidonia bronni", thought to be a new genus, and the strata was denominated the Posidonia layers after it. Years later it turned out to be a junior synonym of Bositra, and thus, it was reassigned. However, the name of the layers was retained. The habitat and mode of life of Bositra has been debated for more than a century. There have been different interpretations, such as a pseudoplanktonic organism,[87] a benthic organism[88] related to open marine floor, where it was the main inhabitant of the basinal settings,[89][90] a free swimming mode of life filtering phytoplankton,[86] and a hybrid mode, where it has a life cycle with holopelagic reproduction controlled by the change on Oxygen levels,[91] and even a chemosymbiotic lifestile, related to the large crinoid rafts, being the main "Safe conduct" to evade anoxic events.[92] All the opinions along the years led to a large study in 1998, where the size/frequency distribution, the density of growth thanks to the lines related to the shell size and the position of the redox boundary by total organic carbon diagrams has revealed that Bositra probably had a benthic mode of life.[93] |
||
|
|
Thousands of Specimens. |
A "posidoniid" ostreoidan. Another Genera mistaken with "Posidonia bronni". |
||
|
|
Thousands of Specimens. |
A bakevelliid mud oyster. |
||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
An inoceramid clam. Being the second most common genera of Bivalve on the Formation, it had been object to several studies to find its ecological niche, like Bositra. Several opinions include a pseudoplanktonic-only organism, able to live in open sea,[90] or a benthonic-only organism.[89] On the 1998 evaluation with Bositra, was found that probably has a benthic early life that translated to a faculatively pseudoplanktonic mode of adult life.[93] |
||
|
|
Thousands of Specimens. |
An inoceramid clam. |
||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
A Clam, type member of the family Solemyidae inside Solemyida. |
||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
A cucullaeid clam. |
||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
A pholadomyid clam. |
||
|
|
Thousands of Specimens. |
A Grammatodontinae clam. This Genus had a lecithotrophic and planktotrophic larval development.[85] |
||
|
|
Thousands of Specimens. |
A mactromyid clam. |
||
|
|
Thousands of Specimens. |
A pleuromyid clam. |
||
|
|
Thousands of Specimens. |
|||
|
|
Thousands of Specimens. |
Gastropoda
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Docens of Specimens. |
A Coelodiscidae sea Snail. The is the oldest known holoplanktonic gastropod, thanks to a bilateral symmetrical shells as an adaption to active swimming. Also the most common of the sea snails of the Formation, it is also one of the most varied in size terms, with some of the biggest specimens of snail from the Lower Toarcian know.[96] It has been related to large floating driftwood as one of the primary settlers.[96] |
||
|
|
Docens of Specimens. |
A Coelodiscidae sea Snail. Possible holoplanktonic gastropod.[96] |
||
|
|
Docens of Specimens. |
A Procerithiidae sea Snail. |
||
|
|
Docens of Specimens. |
An Aporrhaidae sea Snail. Among the latest described from the formation, is one of the earliest certain aporrhaidae. Characterised by large spines growing at the head of the cunch. |
||
|
|
Docens of Specimens. |
A Cryptaulacidae sea Snail. |
||
|
|
Docens of Specimens. |
A Neritariidae sea Snail. |
||
|
|
Docens of Specimens. |
A Zygopleuridae sea Snail. |
||
|
|
Docens of Specimens. |
A Zygopleuridae sea Snail. |
||
|
|
Docens of Specimens. |
|||
|
|
Docens of Specimens. |
A Trochidae sea Snail. Characterised by a rhomboid scaly pattern on the teleoconch whorls. |
||
|
|
Docens of Specimens. |
A Pleurotomariidae sea Snail. |
||
|
|
Docens of Specimens. |
An Eotomariidae sea Snail. |
||
|
|
Various specimens. |
A Pterotracheidae sea Slug. Among the oldest pelagic floating Slugs, Pterotrachea liassica had a more extended larval period than modern extant Pterotrachea coronata, because one additional whorl is Present.[99] |
Cephalopoda
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Multiple Specimens. |
A Nautilidae Nautilidan. Includes the largest specimen of Cenoceras known, with 80 cm width. |
||
|
|
Multiple Specimens. |
A Lytoceratidae Ammonite. Lytoceras can get quite big, with nearly 50 cm in diameter. |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
A Dactylioceratidae Ammonite. Is common on the bituminous marls (incorrectly designated as “Wilder Schiefer”) of the Altdorf High. |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
Type Coeloceratidae Ammonite. |
||
|
|
Multiple Specimens. |
A Phylloceratidae Ammonite. The largest ammonite found in the Posidonienschiefer comes from the Ohmden quarry,and belongs to a Phylloceras heterophyllum with a diameter of 87 cm.[106] |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
A Loligosepiidae Loligosepiidan (Vampyromorpha).[111] The Loligosepiidae is believed to be ancestral to the Recent vampire squid, Vampyroteuthis infernalis.[112] |
||
|
|
Multiple Specimens. |
A Loligosepiidae Loligosepiidan (Vampyromorpha). Related to the modern Vampyroteuthis infernalis. Gladii of Loligosepia can be distinguished from Jeletzkyteuthis by the transition lateral field/hyperbolar zone. |
||
|
|
Multiple Specimens. |
A Geopeltidae Loligosepiidan (Vampyromorpha). Related to the modern Vampyroteuthis infernalis. Gladius with weakly arcuated hyperbolar zones. |
||
|
|
Multiple Specimens. |
A Geopeltidae Loligosepiidan (Vampyromorpha). Related to the modern Vampyroteuthis infernalis. It is distinguished from Geoteuthis and Loligosepia by its median rib: this rib forms a narrow ridge between two narrow grooves. |
||
|
|
Multiple Specimens. |
A Plesioteuthididae Prototeuthidinan (Vampyromorpha). was originally described as "Geoteuthis" sagittata. |
||
|
|
Multiple Specimens. |
A Belemnotheutidae Belemnite. Chitinobelus is an extrange fossil, sice the rostrum was composed of aragonite with organic material, while normal Belemnites had calcite. Has been suggested this rostrum was calcitic. |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
A Megateuthididae Belemnite. Includes some of the Biggest Know Belemnites, with stimated maximum up to 4.5 m long in life, although, most specimens would have been rather smaller. |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
A Megateuthididae Belemnite. Includes really large specimens |
||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
|||
|
|
Multiple Specimens. |
A Diplobelidae Coleoidean. It has been found adult individuals of Clarkeiteuthis which caught small teleost fish of the species Leptolepis bronni. Further indirect evidence for the hunting behaviour comes from their body orientation in the water during life.[123] |
||
|
|
Various Specimens. |
A Diplobelidae Coleoidean. Has been confused with Acrocoelites tripartitus, hence the species name. |
||
|
|
Various Specimens. |
A Diplobelidae Coleoidean. Some specimens belong to Clarkeiteuthis (=Phragmoteuthis) conocauda, but others are clearly different. |
||
|
|
Multiple Specimens. |
A Sueviteuthididae Coleoidean. Sueviteuthis had at least six arms with rather simple hooks, similar to the present of the genus Phragmoteuthis. |
||
|
|
Various Specimens. |
Type member of the Lioteuthididae Squid family. The taxonomic position of Lioteuthis is uncertain, although the wings reaching the proximal gladius section and the smooth median field suggest affinity to the Prototeuthididae[126] |
||
|
|
Various Specimens. |
A Teudopseina Squid. |
||
|
|
Various Specimens. |
A possible primigenial Cuttlefish. Is one of the most important fossils of Cephalopods on the Posidonia Shale, due to be one of the Earliest examples of Pigments found on any species, also one of the first historically.[129] The pigments are preserved on various specimens with Eumelanin related to its ink sacs and include even phosphatized musculature.[130] |
Arthropoda
Cycloidea
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Partial Specimens. |
The First Cycloid Arthropod from the Jurassic, from the family Cycloidae inside Cycloidea.[131] Cycloids are a group of maxillopod arthropods that span between the Paleozoic until the latest Cretaceous, probably related to the crustaceans and probably detritivores.[131] |
Ostracoda
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Cunchs |
A Marine Ostracodan of the family Protostomia. The specimens of this genus are rather fargmentary and of uncertain nature. |
||
|
|
Cunchs |
A marine Ostracodan, member of the family Healdiidae inside Podocopida. Rather abundant on the Toarcian profiles on Europe, this genus has a Mussel-like shape, with a very clean and round morphology. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Healdiidae inside Podocopida. This genus is the main reported on the marine facies of the Dobbertin Clay Pit. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Healdiidae inside Podocopida. This genus is the main reported on the marine facies of the Dobbertin Clay Pit. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Healdiidae inside Podocopida. The genus is rare on the layers. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Protocytheridae inside Podocopida. A genus related with Fish fossils and anoxic bottoms. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Praeschuleridea inside Podocopida. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Cytheruridae inside Podocopida. Is rare and the specimens found are rather incomplete. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Polycopidae inside Cladocopina. Scarce but well preserved specimens. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Cytherellidae inside Platycopida. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Bairdiidae inside Bairdioidea. Abundant and diverse, is found associated with Ammonite shells. |
||
|
|
Cunchs |
A Marine Ostracodan of the family Bairdiidae inside Bairdioidea. |
Malacostraca
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Partial Specimens. |
A hermit crab of the family Paguroidea. Hermit crabs are common of the marine layers of the lower Jurassic Europe, mostly on the Pliensbachian-Toarcian Boundary of France and Germany. Orthomalus is a small sized crab, probably inhabitant of nearshore waters, and even deltaic and beach environments, similar to modern genera. |
||
|
|
Single Specimen inside an Ammonite Shell. |
An hermit crab of the family Paguridae. |
||
|
|
Nearly complete & Partial Specimens. |
An Astacidea Decapodan of the family Uncinidae. Reaching large sizes of almost half a meter (39–47 cm), Uncina Posidoniae is among the largest know Jurassic Crustaceans. Uncina posidoniae is also the largest representative of the genus Uncina.[142] This large crustacean has been found associated with Ammonite and Bivalve filled Bentos, where probably hunted different kinds of prey.[142] Its large claws would have been perfect for hunt small invertebrates and vertebrates.[142] |
||
|
|
Partial Specimens and complete Specimens |
A gregarious Polychelidan Lobster. |
||
|
Partial Specimens. |
A Coleiidae Decapodan. The largest Coeloid from the formation, P. giganteus is a species reaching a larger size than most other polychelidans, with up to 15 cm. On the Posidonia Shale there is the most abundant variety of species from the genus, ranging from different sizes and morphologies, that indicate different habitat & feeding adaptations on the genus. Some like P. hartmani show less adaptations to hunt for small nectobenthic preys than other relatives, being abundant on Oyster-filled waters. There is a relatively abundance of the genus in deep-water settings from the Toarcian onward.[149] |
|||
|
|
Partial Specimens. |
A Penaeidae Decapodan. |
||
|
|
Partial Specimens. |
An Erymidae Decapodan. |
||
|
|
Complete Specimens. Includes specimens inside ammonites shells |
An Erymidae Decapodan. |
||
|
|
Complete Specimens |
Type genus of the Erymidae Decapodan family. Originally, was named Glyphea amalthei,informally used by Quenstedt and housed on the Museum Naturkunde in Württemberg. A series of posterior revisions probe it was a different genus.[158] |
||
|
|
Complete Specimens |
An Erymidae Decapodan. |
||
|
|
Single complete specimen in late larval stage |
The specimen reported represents the oldest fossil record of an achelatan lobster larva, and the first representative of achelatan lobsters in the Posidinia Shale. Shares similarities with the late jurassic genus Cancrinos. |
||
|
|
Single Incomplete Specimen |
A Stomatopoda Malacostracan. Its affinities haven't been tested. |
Thoracica
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Numerous disarticulated individuals, associated with fossil wood.[163] |
A phospatic-shelled Cirripede of the family Eolepadidae.[163] Toarcolepas is provisionally interpreted as the oldest epiplanktonic cirripede known, and is thought to have lived attached to floating driftwood.[163] |
Arachnida
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Single Incomplete Specimen. |
The type genus of the family Liassoscorpionididae, probably related to Mesophonoidea. Being the only Jurassic scorpion known, there is no evidence that L. schmidti was aquatic (which was suggested in the past) and in the absence of further, better preserved material it should be excluded from future considerations of broad patterns of scorpion evolution.[165] |
Insecta
Insects are a common terrestrial animals that where proabaly drifted to the sea due to Moonsonal conditions present on the Posidonia Shale.[166]
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Specimens |
A Dragonfly of the family Heterophlebiidae. A relative abundant genus, present on most of the pits of the Posidonia Shale, even on Holzmaden. |
||
|
|
Specimens |
A Dragonfly of the family Heterophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the family Liassogomphidae. Second most abundant genus of Odonatan in the Formation. |
||
|
|
Specimens |
A Dragonfly of the family Liassogomphidae. |
||
|
|
Specimens |
A Dragonfly of the family Liassogomphidae. |
||
|
|
Specimens |
A Dragonfly of the family Sphenophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the family Sphenophlebiidae. |
||
|
|
Specimens |
|||
|
|
Specimens |
A Dragonfly. |
||
|
|
Specimens |
A Dragonfly. |
||
|
|
Specimens |
A Dragonfly of the family Myopophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the family Myopophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the family Myopophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the Family Liassogomphidae. |
||
|
|
Specimens |
A Dragonfly of the family Campterophlebiidae.The largest Early Jurassic Insect Know, with a wings size up to 20 cm.[174] |
||
|
|
Specimens |
A Dragonfly of the family Campterophlebiidae. |
||
|
|
Specimens |
A Dragonfly of the family Henrotayiidae. |
||
|
|
Specimens |
A Cockroach of the family Raphidiomimidae. |
||
|
|
Specimens |
A Cockroach of the family Raphidiomimidae. |
||
|
|
Specimens |
A Cockroach of the family Caloblattinidae. |
||
|
|
Specimens |
A Cockroach of the family Blattulidae. |
||
|
|
Specimens |
A Stick insect. One of the described insects found more near the Bohemian Massif, where probably belong most of the terrestrial invertebrate fauna. |
||
|
|
Specimens |
A Stick insect of the family Aerophasmidae. |
||
|
|
Specimens |
A Grasshopper. |
||
|
|
Specimens |
A Grasshopper of the family Protogryllidae. |
||
|
|
Specimens |
A Grasshopper of the family Elcanidae. |
||
|
|
Specimens |
A Short-horned Grasshopper of the family Acrididae. |
||
|
|
Specimens |
A Grasshopper of the family Locustopsidae. |
||
|
|
Specimens |
A Grasshopper of the family Locustopsidae. |
||
|
|
Specimens |
A Planthopper of the family Archijassidae. |
||
|
|
Specimens |
A Planthopper. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Planthopper of the family Fulgoridiidae. |
||
|
|
Specimens |
A Froghopper of the family Procercopidae. |
||
|
|
Specimens |
A Shore bug. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A Shore bug of the family Archegocimicidae. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A False Ground Beetle of the family Trachypachidae. |
||
|
|
Specimens |
A False Ground Beetle of the family Trachypachidae. |
||
|
|
Specimens |
A Water Scavenger Beetle of the family Hydrophilidae. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle. |
||
|
|
Specimens |
A basal Beetle of the family Coptoclavidae. |
||
|
|
Specimens |
A basal Beetle of the family Coptoclavidae. |
||
|
|
Specimens |
A basal Beetle of the family Schizophoridae. |
||
|
|
Specimens |
A Giant Beetle. It is among the largest found on all the Jurassic. |
||
|
|
Specimens |
A Hangingfly of the family Bittacidae. |
||
|
|
Specimens |
A Hangingfly of the family Bittacidae. |
||
|
|
Specimens |
A Hangingfly of the family Bittacidae. |
||
|
|
Specimens |
A Hangingfly of the family Bittacidae. |
||
|
|
Specimens |
A Scorpionfly of the family Orthophlebiidae. |
||
|
|
Specimens |
A Scorpionfly of the family Orthophlebiidae. |
||
|
|
Specimens |
A Scorpionfly of the family Orthophlebiidae. |
||
|
|
Specimens |
A Scorpionfly of the family Pseudopolycentropodidae. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly of the family Protopleciidae. |
||
|
|
Specimens |
A Wood Gnat of the family Anisopodidae. |
||
|
|
Specimens |
A Snakefly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly. |
||
|
|
Specimens |
A Fly of the family Protorhyphidae. |
||
|
|
Specimens |
A primitive Crane fly of the family Tanyderidae. |
||
|
|
Specimens |
A primitive Crane fly of the family Tanyderidae. |
||
|
|
Specimens |
A Crane fly of the family Limoniidae. |
||
|
|
Specimens |
A Crane fly of the family Limoniidae. |
||
|
|
Specimens |
A Crane fly of the family Limoniidae. |
||
|
|
Specimens |
A Crane fly. |
||
|
|
Specimens |
A Crane fly. |
||
|
|
Specimens |
A Phantom Crane fly of the family Ptychopteridae. |
||
|
|
Specimens |
A Caddisfly. |
||
|
|
Specimens |
A Lacewing of the family Prohemerobiidae. |
||
|
|
Specimens |
A Lacewing of the family Prohemerobiidae. |
||
|
|
Specimens |
A Lacewing of the family Prohemerobiidae. |
||
|
|
Specimens |
A Lacewing of the family Panfiloviidae. A giant Lacewing, with forewing length more than 5 cm. |
||
|
|
Specimens |
A Giant Lacewing, type genus of the subfamily Liassopsychopinae inside Kalligrammatidae. It is one of the oldest known representatives of the Giant pollinator lacewings. The genus Liassopsychops was previously referred to Psychopsidae. Another specimen related, Ma 14504 is regarded here as Kalligrammatidae incertae sedis. This along the occurrence of two distantly-related genera of Kalligrammatidae in the lower Toarcian is unexpected.[185] |
||
|
|
Specimens |
A Giant Lacewing, genus of the subfamily Kallihemerobiidae inside Kalligrammatidae. Other of the oldest known representatives of the Giant pollinator lacewings. The Toarcian Kalligrammatidae lived in warm and dry conditions [185] |
||
|
|
Specimens |
A lance Lacewing of the family Osmylidae. The largest non-Kalligrammatidae lacewing of the Jurassic, with a forewing length of 470 mm and a wingspan stimated on 11 cm. |
||
|
|
Specimens |
A lance Lacewing of the family Mesochrysopidae. |
||
|
|
Specimens |
A Hairy Cicada of the family Tettigarctidae. |
||
|
|
Specimens |
A Hairy Cicada of the family Tettigarctidae. |
||
|
|
Specimens |
A Sternorrhynchan of the family Pincombeomorpha. It is curious for its peculiar venation on its wings. Has been proposed its own family, Xulsigiidae. |
||
|
|
Specimens |
A Coleorrhynchan of the family Progonocimicidae. |
||
|
|
Specimens |
A Wasp of the family Ephialtitidae. |
||
|
|
Specimens |
A Wasp of the family Ephialtitidae. |
||
|
|
Specimens |
A Wasp of the family Ephialtitidae. |
||
|
|
Specimens |
A Wood Wasp of the family Xyelotomidae. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A non classified Insect. |
||
|
|
Specimens |
A Dicondylian, from the family Protomyrmeleontidae. |
||
|
|
Specimens |
A basal Insect of the family Blattogryllidae. |
||
|
|
Specimens |
A basal Insect of the family Geinitziidae. |
||
|
|
Specimens |
A basal Insect of the family Pachymeridiidae. |
||
|
|
Specimens |
A basal Insect of the family Pachymeridiidae. |
Echinodermata
Asterozoa
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Few Specimens. |
An Ophiuridan of the family Ophiactidae. Very rare on the layers. |
||
|
|
Few Specimens. |
An Ophiuridan of the family Ophiolepididae. Very rare on the layers, being Mesophiomusium geisingense the most common of the two species present. |
||
|
|
Various Specimens. |
An Ophiuridan of the family Ophiacanthida. Very Common, related to non anoxic water sedimentation. |
||
|
|
Various Specimens. |
An Ophiuridan of the family Aplocomidae. Very Common. |
||
|
|
Few Specimens. |
An Ophiuridan of the family Ophiuridae. Its relationships haven't been confirmed and it is based on very fragmentary remains. |
||
|
|
Few Specimens. |
An Ophiuridan of the family Ophiuridae. Its relationships haven't been confirmed and it is based on very fragmentary remains. |
||
|
|
Few Specimens. |
An Asteroidean of the family Astropectinidae. It is very rare on the layers, and a few fragmentary specimens are known. Only a relatively complete specimen is known from Banz Abbey. |
Echinoidea
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Few Specimens. |
A sea urchin of the family Cidaridae. Common on several layers. Cidaris is genus that still alive today. A bottom dweller, is commonly found associated with Belemnnite fossils, probably due to eating its carcasses. |
||
|
|
Docens of Specimens |
A sea urchin of the family Pedinidae. It is the most common sea urchin in the formation, present on all the levels with specimens of various sizes. Vinculated to sea bottom sediments, before Gasteropods and Bivalves, Diademospsis was the tird major colonizer of the bottom, in between anoxic changes. |
||
|
|
Few Specimens. |
A sea urchin of the family Miocidaridae |
Crinoidea
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Multiple specimens. |
A Crinoidean of the family Plicatocrinidae. |
||
|
|
Multiple specimens. |
A Crinoidean of the family Millericrinidae. |
||
|
|
Multiple specimens. |
A Crinoidean of the family Isocrinida. |
||
|
|
Multiple specimens. |
Type genus of Crinoidean of the family Isocrinida. |
||
|
|
Multiple specimens. Fossilized rafts of +10 m long with complete colonies. |
The Largest Know Crinoidean, from the family Pentacrinitidae. Among the tallest animals of its period, Seirocrinus is also one of the most famous fossils from the Posidonia Shale. It consists of fossils of colonies along large wood trunks, with specimens up to 14 m long, with the largest specimen reaching 26 m long,[200] what makes it among the tallest know Mesozoic organisms, one of the largest invertebrates know on the fossil record and one of the tallest know animals. It was an open ocean organism that lived in rafting woods, probably filtering food and serving as a refuge for other animals, such as ammonites.[201] The crinoids had a large colonization process, based on the status of the fossil wood found.[202][203] The large rafts where the home for a high variety of marine organisms, such as Balanoideans, Ammonites and other. It has been stimated that without the presence of modern raft wood predators (that apperared on the Bathonian) those rafts can last up to 5 years, being that the main reason the crinoids where able to attach such huge sizes. The large rafts where also proabaly essential to distribute animals along the Early Jurassic Seas.[204] |
||
|
|
Multiple specimens. Fossilized rafts of +10 m long with complete colonies. |
Type genus of Crinoidean from the family Pentacrinitidae. Like Seirocrinus, Pentacrinites formed colonies on rafting wood, getting a different role than bigger crinoid and appearing on the first stages of the descomposition of the rafting wood. Was a smaller genus, with specimens of no more than 1 meter long, usually measuring 40–70 cm. |
Vertebrata
Fishes
Chondrichthyes
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Teeth |
A non classified Elasmobranch. |
||
|
|
Teeth |
Thype shark of the family Synechodontiformes. |
||
|
|
Teeth |
A shark of the family Synechodontiformes. |
||
|
|
Teeth |
A member of the family Protospinacidae. |
||
|
|
Articulated vertebral column, girdles, both fin spines and clasper organ |
A member of the family Palaeospinacidae. |
||
|
|
Anterior part of body with basicranium, palatoquadrates, Meckel's cartilage, ceratohyals, epihyals, teeth, traces of the branchial arches and the anterior finspine |
Type member of the family Palaeospinacidae. |
||
|
|
Teeth |
A Carpet shark of the family Orectolobiformes. |
||
|
|
Teeth |
A Carpet shark of the family Hemiscylliidae. |
||
|
|
Teeth |
A Carpet shark of the family Orectolobiformes. |
||
|
|
Teeth |
A Carpet shark of the family Orectolobiformes. |
||
|
|
Teeth |
A Carpet shark of the family Orectolobiformes. |
||
|
|
Teeth |
A Bullhead Shark of the family Heterodontidae. |
||
|
|
Teeth. |
A Bullhead Shark of the family Heterodontidae. |
||
|
|
Teeth |
A shark of the family Agaleidae. |
||
|
|
Teeth |
A shark of the family Acrodontidae. |
||
|
|
Teeth |
A shark of the family Hybodontiformes. |
||
|
|
Meckelian Cartilages, Jaws, teeth, Palatoquadrates, placoid scales and desarticualted parts of the labial, hyoid and branchial skeleton. |
A shark of the family Hybodontidae. The Type specimen belongs to a large hybodontid, with an estimated total length of up to 3 m.[212] It has a Meckelian Cartilage more robust than Hybodus hauffianus and an acrodontine dentition, as seen on Bdellodus.[212] Probably is related with "Hybodus" delabechei, very likely a junior synonym of Crassodus.[212] |
||
|
|
Teeth. |
A shark of the family Hybodontidae. |
||
|
|
Complete Specimens and fragments, including Teeth, scales, jaws and Cartilage. |
Type shark of the family Hybodontidae. It is the most abundant shark on the layers of the Posidonia Shale, with some of the best preserved specimens of the genus known. It was probably an open ocean hunter, with small horns over the eyes. With a size around 2 m, it was also one of the largest representatives of the Chondrichthyes on the formation.[216][217] |
||
|
|
Fragmentary and Complete Specimens |
A shark of the family Hexanchiformes. |
||
|
|
Partially Complete Specimen, with associated teeth |
A member of Callorhynchidae inside Chimaeriformes. Similar to Callorhinchus, among the oldest known of its type. |
||
|
|
Head and postcranial remains |
A member of Myriacanthidae inside Chimaeriformes. An aberrant Chimaera with an extrange elongated nose and horns over the skull. |
||
|
|
Head and several postcranial remains |
A member of Myriacanthidae inside Chimaeriformes. An aberrant Chimaera with a second jaw-like structure on its head. |
||
|
|
Teeth |
A Basal member of the Rajiformes of the family Archaeobatidae. |
||
|
|
Teeth |
A Basal member of the Rajiformes of the family Archaeobatidae. |
||
|
|
Teeth |
A Basal member of the Rajiformes of the family Archaeobatidae. |
||
|
|
Teeth |
A Basal member of the Rajiformes. |
Actinopteri
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Complete Specimen |
First ganoin-scaled Ophiopsiformes (Halecomorphi) from the Posidonienschiefer. The type specimen measures 51 cm, and has elongated and serrated body scales before the dorsal fin and tiny ganoid scales after it.[223] |
||
|
|
Nearly complete specimen with broken skull |
First ganoin-scaled Ophiopsiformes (Halecomorphi) from the Posidonienschiefer. Elongated morphology, with a length of ~39 cm, covered by smooth, masive ganoin scales.[223] |
||
|
|
Various Complete and nearly complete Specimens |
Type Genus of the family Caturidae inside Amiiformes |
||
|
|
Multiple specimens. |
The youngest representative of the family Saurichthyidae, known for its large jaws, similar to modern Belonidae. |
||
|
|
Multiple specimens. |
Type member of the family Ptycholepididae inside Ptycholepiformes. It is one of the Youngest representatives of its Family. |
||
|
|
Multiple specimens. |
A member of the family Pholidophoridae. Is among the most abundant fishes on the late liassic of Europe, present on the sub-mediterranean boreal, with specimens of several sizes. |
||
|
|
Multiple specimens. |
A member of the family Pholidophoridae. |
||
|
|
Multiple specimens. |
A member of the family Leptolepididae. The most common member of its family, Leptolepis is commonly associated with Crustaceans and small marine invertebrates, probably main creatures on its diet. One on the most predated vertebrates on the formation, with abundance of larger fishes and reptiles with specimens associated. |
||
|
|
MB. f.7612, nearly complete specimen. |
A member of the family Leptolepididae. It differs from Leptolepis coryphaenoides in the presence of a few autapomorphics and also in the retention of several primitive features not present on the last one.[230] Small genus, of about 14 cm length.[230] |
||
|
|
Multiple specimens. |
A member of the family Pachycormidae. |
||
|
|
Multiple specimens. |
A member of the family Pachycormidae. Large representative of the family, reaching sizes up to 2.3 m. |
||
|
|
Multiple specimens. |
Type member of the family Pachycormidae. Large representative of its family, with a size up to 1.5 m. One specimen preserved the alimentary canal, with the stomach filled by numerous hooklets that can be referred to the coleoid cephalopod Phragmoteuthis, impliying a diet of cephalopods from this genus.[235] |
||
|
|
Multiple specimens. |
A large member of the family Pachycormidae. |
||
|
|
Partial specimen. |
A large member of the family Pachycormidae, with up to 2.5–3 m long and an estimated weight over 200 kg.[238][239] Considered originally a junior synonym of Pachycormus, although the craneal bones suggest a new genus. Among the largest fish found on the formation it is a key fossil on the transition to large filter feeding fishes.[239] Being Coeval with another basal Pachycormiformes show the specialization of the group during the late lower jurassic.[239] Ohmdenia is the sister taxa to group of suspension-feeding Giant Middle-Late Jurassic Fishes (Including the famous Leedsichthys), showing alterations on its dental structure, with jaw indicates a diet based on soft body prey.[239] Its evolutionary significance is equiparable to that of the genus Aetiocetus for the modern Baleen whale.[239] |
||
|
Multiple specimens. |
A deep-bodied neopterygian, Type member of the family Dapediidae. Unpublished material indicates the presence of one or even two more still undescribed species of Dapedium in the Lower Toarcian.[241] |
|||
|
|
Multiple specimens. |
A common member of the Lepisosteiformes. |
||
|
|
Multiple specimens. |
A common member of the Semionotidae. |
||
|
|
Various Specimens |
A large member of the Chondrosteidae and the largest non reptilian marine vertebrate of the Posidonia shale, with a size between 3 and 4.5 m, and an estimated weight over 800 kg to 1 tonne.[245] Has been suggested as a junior Synonym of Chrondrosteus, although there haven't been any new revision about the status of the genus. It is related to modern sturgeons, but with a different kind of mouth than common species, made for hunting prey in open waters, with a strong lower jaw, similar to modern Beluga Sturgeons.[247] |
Sarcopterygii
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Various Specimens with diverse degree of preservation. |
A large coelacanth of the family Mawsoniidae, related with the genera Axelrodichthys, Chinlea, Diplurus and the type Mawsonia.[249] The largest specimen know from the Posidonia Shale is GPIT.OS.770 (Holotype), with a length over 1.6 m.[248] The specimen presents an ossified lung inside the abdominal cavity, and most of the body, being also one of the most complete Coelacanths of the Jurassic found.[248][249] Some recent discoveries from the Middle Jurassic show specimens of up to 3.5 m long.[250] Trachymetopon precedes the presence of the family Mawsoniidae in Europe by about 120 Ma and the northernmost occurrence of a member of the group, impliying an extensive geographical range during the Early Jurassic.[249] Due to the specimens being found on pelagic deposits suggest that probably was an open ocean swimmer.[248][249] |
Reptiles
Ichthyosauria
Inderminate specimens are known.[6]
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Multiple specimens with different degree of preservation. |
Type genus of the family Temnodontosauridae. A large Macroraptorial Ichthyosaur, apex predator of its environment. It range on sizes between the 9 and the 12 m, being one of the largest know ichthyosaurs, characterized by skulls and jaws over 1 m in length, with the largest being over 1.9 m long. It has been found with fragments of young icthyosaur on his stomach.[253] Of 39 specimens of Temnodontosaurus studied, a 21% (8 Specimens) show pathologies along their body, with several injuries post traumatic, probably done by other marine reptiles.[254] |
||
|
|
Multiple specimens. Some of them are among the best preserved Ichthyosaur remains known.[255][256][257][258] |
Type genus of the family Stenopterygiidae. A common Toarcian Ichthyosaur, present on multiple layers. The rather exquisite level of preservation has led to know even the coloration, that exposes a clear countershading, with an upper part being more obscure than the lower, similar to modern Killer Whales, the Heaviside's dolphin or the Dall's porpoise. There is also evidence of changes in color with ontogenic chnges, going from dark juveniles to countershaded adults. The skin was flexible & Scaless, as in Dolphins.[259] |
||
|
|
Multiple specimens. |
Type genus of the family Suevoleviathanidae. Includes specimens up to 4 m long. |
||
|
|
Complete Specimen. |
Small sized Ichthyosaur, probably a member of Parvipelvia, sister group to Stenopterygius + Ophthalmosauridae.[265] A small- to mid-sized ichthyosaur, 2–3 m in length, with relatively short and slender antorbital rostrum.[264] |
||
|
|
Complete and partial Specimens. |
A large ichthyosaur of the family Leptonectidae with convergent evolution with modern Swordfish. Like this fishes, Eurhinosaurus is believed to be a fast swimming predator, able to hunt fish schools on same way. Large specimens of up to 6 m are known. |
Plesiosauria
Genus | Species | Location | Material | Notes | Images |
---|---|---|---|---|---|
|
|
Nearly complete specimen. |
A Rhomaleosauridae Plesiosaur. Its detailed fossils have helped to study plesiosaur movement.[270] |
||
|
|
Complete specimen. |
A Rhomaleosauridae Plesiosaur. A moderately sized (3.4 m) Rhomaleaosaurid, ecologically adapted to fish hunt, as has been observed due to comparing the long snouted skull with that of Peloneustes, Gharial Crocodiles or Dolphins.[271] |
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Complete Specimen. |
A basal Plesiosaur that has been linked with Cryptoclididae. It is one of the smallest from the Posidonia, with a complete skeleton measuring less than 2.5 m. It is considered a possible junior synonym of Seeleyosaurus[274] |
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Complete Specimens. |
A Plesiosaur of the family Microcleididae. It was named originally "Plesiosaurus guilelmiimperatoris". It was a moderate‐sized plesiosauroid, measuring up to 3,5 m in length with a skull length of 170 mm.[276] |
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Several Complete Specimens. |
Type member of the Plesiosaur family Microcleididae. Small Plesiosaur, with a length of less than 3 m. Possible Junior synonym of Hydrorion |
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Complete Specimen. |
A Plesiosaur of the family Plesiosauridae. It is characterised by a really enlongated neck, was probably an ichthyophagous form that occurred rarely in the Posidonienschiefer fauna. |
Sphenodontia
Genus | Species | Location | Material | Notes | Images |
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Complete specimens. |
An aquatic sphenodont of the family Pleurosauridae. Palaeopleurosaurus evidences that there was a slightly skeletal specialization for an aquatic lifestyle, achieved trougth the Jurassic gradually on pleurosaurs.[280] It has similarities with other marine reptiles, such with members of Sauropterygia the presence of a defined suture between the centrum and the neural arch, along with reducted sternum.[281] Probably had a semiaquatic style of life, altrought not as adapted as Pleurosaurus, as show limited morphological evidence of adaptation to a complete aquatic lifestyle, defined by no Osteosclerosis and the lack of Pachyostosis, except for a thicker shaft region in the humerus, that is as narrow as in terrestrial rhynchocephalians, such as the terrestrial Clevosaurus.[281] Palaeopleurosaurus probably was still able to walk on land, for example for Oviposition.[281] Recent studies suggest a shorter lifespan than modern Tuatara, based on irregular spacing of growth marks.[282] |
Testudinata
Genus | Species | Location | Material | Notes | Images |
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Various partial specimens, mostly pleurals. |
Unclassified Testudine. Münster (1834) cited: " there were also rare things at the quarries of Altdorf, among other remains there where ones of a turtle on lias limestone"". The remains are not cataloged.[286] |
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Various partial specimens, mostly pleurals. Includes a left partial shell. |
Assigned to Mesochelydia(?) due to resemblances for the authors to modern turtles. Unclassified and non cataloged.[286] |
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Fragmentary Remains |
Can be a more basal taxon or even not a turtle. If it is, can be the first Turtle remains found on the Posidonia Shale since the late 1800s. Now on a private collection.[288] |
Crocodrylomorpha
Genus | Species | Location | Material | Notes | Images |
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Complete specimens. |
A marine crocodrylomorph with a diet probably based on fish.[290] It is the best known member of the family Teleosauriade. The Genus was declared Invalid in 2020. |
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Series of Complete specimens, including skin impressions |
A Thalattosuchian of the family Teleosauridae. Was considered synonymous with Steneosaurus until in 2020 this last was recovered as invalid.[292] Includes 5 m specimens. |
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Complete specimen. |
A Thalattosuchian of the family Teleosauridae. A marine crocodrylomorph with a diet probably based on fish. Was considered synonymous with Steneosaurus until recently.[295] |
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Complete specimen. |
A Thalattosuchian of the family Teleosauridae. Platysuchus was slightly more robust than its contemporaneous relatives, being probably adapted to hunt more voluminous fish. |
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Complete specimen. |
A Thalattosuchian with a complex assignation, where can be a member of the family Teleosauridae or the basalmost Metriorhynchoidean. With a less heavy built, bigger skull and more visible marine adaptation, its diet probably based completely on fish (one fossil specimen was found with a Leptolepis in its stomach contents). Has been considered a basal Metriorhynchidae[299] or sister taxon to both Teleosauridae and Metriorhynchidae.[300] |
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Partial specimen. |
A possible Pholidosauridae Neosuchian. A marine crocodrylomorph, that can be a mistaken Teleosaurian as has been included on Cf. Platysuchus, although has characters that align it with Anglosuchus, that was also confused with a Teleosaurid.[289] |
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Frontal Snout |
A Possible Goniopholid Neosuchian. Classified as "?Steneosaurus" sp., it was noted initially a morphology more similar to Goniopholis simus and specially Amphicotylus lucasii, being a possible early member of the group.[105] |
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Fragmentary remains |
Possible member of the Protosuchia inside Crocodyliformes. If is confirmed as a member of the family it would be a terrestrial, maybe semi-acuatic crocodrylomorph. Can be a mistaken juvenile Teleosaurian.[288] |
Pterosauria
Genus | Species | Location | Material | Notes | Images |
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Several specimens with different degrees of preservation. |
A Novialoidean Pterosaur, type genus of the family Campylognathoidea. Mark Witton suggests the construction of Campylognathoides' extremely robust forelimbs, with proportionally long wing fingers, could be a specialization for a fast aerial lifestyle comparable to those of Falcons and mastiff bats, being more probably an insect & vertebrate hunter and living on nearshore environments.[304] |
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Pelvis and several vertebrae. |
A Novialoidean Pterosaur, probably a member of the family Campylognathoidea. Has been assigned to the genus Campylognathoides, although it is clearly different than any other pterosaur from the Posidonia Shale.[305] The name "Schandelopterus" is invalid and lacks any study, assigned without species to refer to the specimen on private German Fossil Groups. The pelvis indicates a laterally, slightly upwardly directed orientation of the acetabula which does not support a bird-like bipedal locomotion of this pterosaur as has been suggested on the past.[305] |
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Skull |
A Rhamphorhynchinae Pterosaur. Has been assigned to the genus Dorygnathus. It has a really complete skull that can help to explain the estatus of the genus Parapsicephalus.[306] |
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Multiple specimens with different degree of preservation.[311] |
A Rhamphorhynchinae Pterosaur. It is one of the best known Early Jurassic Pterosaurs.[307] Unlike Campylognthoides, Dorygnathus was an oceanic hunter, with teeth disposed to catch marine prey, such as Belemnittes and several species of fishes. Dorygnathus mistelgauensis is considered a junior synonym until more data can be recovered from the specimen, held on a private collection.[307] |
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Femur and a broken tibia-fibula. |
A possible Rhamphorhynchinae Pterosaur. Like "Schandelopterus", "Ohmdenodraco" is an invalid name, used on private fossil groups to refer to SMNS 80439, assigned as "?Dorygnathus sp." originally, altrougth characters on the tibia and femur are distinct to any Pterosaur found on the Posidonia.[307] |
Dinosauria
Possible teeth from Dinosaurs are known from the Lias Clay pit of Unterstürmig (Referred as "Various Archosaur teeth").[6]
Genus | Species | Location | Material | Notes | Images |
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An indeterminate possible Theropod dinosaur, possibly Neotheropoda. Hasn't been revised since 1984. The Cervical Vertebrae can be alternatively from a Plesiosaur, although the teeth show a clear theropod morphology. |
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3 cm long, tooth-studded fragment of a lower jaw |
An indeterminate possible Sauropodomorph dinosaur, possibly a member of Sauropodiformes (Resemble Yunnanosaurus teeth).[313] The Fossil was reported from the Lias Epsilon level, that on Oedhof is occupied by the Posidonia Shale.[313] It was found with abundant Plant debris and Belemnite remains.[313] Hasn't been revised since 1956 |
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Tibia and astragalus |
A Gravisaurian Sauropod. One of the few formally described from the Toarcian. Has been related with Vulcanodon, although more recent studies placed it as a relative of Rhoetosaurus.[315] It has been claimed to be a small sauropod with a size of 4 m, altrought the tibia measures 405 to 410 mm, leading to a 6.7 m long sauropod. Molina Pérez & Larramendi, stimated a modern size of 6.2 to 6.7 m long, with a weight of 1.3 tonnes.[316] |
Synapsida
Genus | Species | Location | Material | Notes | Images |
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3 Teeth |
The specimens were listed on several notes on the 1800s (As "mammal teeth"), although its existence has not been proved. Can be related to the Trithelodontidae or other late surviving Cynodonts by related characters, such as Irajatherium, but also to the Mammaliformes. If its presence is proved, it would be the first Synapsid found on the Posidonia Shale. |
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