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Moltrasio Formation

The Moltrasio Formation also known as the Lombardische Kieselkalk Formation is a geological formation in Italy and Switzerland. This Formation mostly developed in the Lower or Middle Sinemurian stage of the Lower Jurassic, where on the Lombardian basin tectonic activity modified the current marine and terrestrial habitats.[2] Here it developed a series of marine-related depositional settings, represented by an outcrop of 550–600 m of grey Calcarenites and Calcilutites with chert lenses and marly interbeds, that recovers the Sedrina, Moltrasio and Domaro Formations.[2] This was mostly due to the post-Triassic crisis, that was linked locally to tectonics.[3] The Moltrasio Formation is considered a continuation of the Sedrina Limestone and the Hettangian Albenza Formation, and was probably a shallow water succession, developed on the passive margin of the westernmost Southern Alps.[3][4] It is known due to the exquisite preservation observed on the Outcrop in Osteno, where several kinds of marine biota have been recovered.[5]

Moltrasio Formation
Stratigraphic range: Middle Sinemurian-Lower Pliensbachian
~196–188 Ma
Outcrop
TypeGeological formation
Unit ofMonte Generoso Basin
Sub-unitsOsteno Outcrop
UnderliesDomaro Formation
OverliesSedrina Limestone
Thickness200 m
Lithology
PrimaryLimestone
Location
Coordinates46°00′N 9°06′E / 46.0°N 9.1°E / 46.0; 9.1
Approximate paleocoordinates33°12′N 15°36′E / 33.2°N 15.6°E / 33.2; 15.6
RegionLombardy
Country
Type section
Named forMoltrasio
Named byAntonio Stoppani[1]
Year defined1857
Moltrasio Formation (Italy)
Moltrasio Formation (Lombardy)

Fossils edit

Exceptional fossilization edit

 
Exposed Moltrasio Fm in Southern Switzerland

Apart from the Eocene of Monte Bolca, the Sinemurian of Osteno is the only fossil deposit in Italy in which soft bodies are preserved. The Osteno site was discovered in 1964. It was recovered from a series of 6 metres (20 ft) package of fine laminated, gray, spongiolitic, micritic limestone.[6] Coroniceras bisulcatum allowed to date the outcrop as the Bucklandi zone, lower Sinemurian.[6] The outcrop is a good documentation of a particularly complete fauna and flora of the Lower Jurassic which is not exactly common in the Southern Alps.[6] The Osteno outcrop, part of the formation, is worldwide known due to the exceptional preservation of mostly marine biota, including rare fossilized components, helping to understand the ecosystems of the local Sinemurian margin of the Monte Generoso Basin.[7] The high local variety of fossils found is most likely due to unique conditions of preservation, where phosphatized soft tissues have not been observed in any fish or polychaetes, but they are common in crustaceans (33%) and also occur in a smaller percentage of teuthids (14%).[8] Soft part preservation through phosphatization in this deposit includes the muscles and branchia of Crustaceans, fish tissues, and the digestive tracts of coleoids, polychaetes, and nematodes. These fossils are interpreted as having been preserved in a stagnant, restricted basin with anoxic conditions likely within the sediment pore waters.[5]

Nematoida edit

Genus Species Material Location Notes Images

Eophasma[6][9]

Eophasma jurasicum

  • A complete specimen

Osteno Outcrop

A nematode, type member of the family Eophasmidae inside Desmoscolecida.[10] A rare find, since nematode fossils are absent in most Mesozoic marine rocks.[9]

 

Annelida edit

Genus Species Material Location Notes Images

Melanoraphia[5][6][11]

Melanoraphia maculata

  • A nearly complete specimen

Osteno Outcrop

A polychaete, member of the group Phyllodocemorpha with incertae sedis assignation. This polychaete was probably an open swimmer more than a subtrate dweller.[11]

 

Crustacea edit

Genus Species Material Location Notes Images

Aeger[5][6][12][13]

  • Aeger foesteri
  • Aeger muensteri
  • Aeger robustus
  • Aeger rostrospinatus
  • Aeger elongatus
  • Aeger macropus

Multiple specimens fairly preserved

Osteno Outcrop

A decapod, type member of the family Aegeridae. This genus is the most abundant local crustacean, and was a shrimp-like creature that was probably necrophagous.[13]

 

Coleia[5][6][12][14][15][16]

  • Coleia vialiii
  • Coleia medilerranea
  • Coleia cf. antiqua
  • Coleia pinnnai

Multiple specimens fairly preserved

Osteno Outcrop

A decapod, type member of the family Coleiidae. Probably a bottom dweller predatory crustacean.[14]

 

Eryma[17][18]

  • Eryma sinemuriana

41 specimens, fairly preserved

Osteno Outcrop

A decapod, type member of the family Erymidae. The species was originally identified as Pustulina sinemuriana.[19]

Glyphea[17]

  • Glyphea tricarinata

137 complete and fragmentary specimens

Osteno Outcrop

A decapod, type member of the family Erymidae. The species was originally identified as Pustulina sinemuriana.[19]

Mecochirus[17]

  • Mecochirus germari

81 complete and fragmentary specimens,

Osteno Outcrop

A decapod, member of the family Mecochiridae. Rather rare compared to other local crustacean genera.

Ostenosculda[20]

Ostenosculda teruzzii

Single Specimen fairly preserved

Osteno Outcrop

A mantis shrimp

Palaeastacus[17][19]

  • Palaeastacus meyeri

Multiple specimens fairly preserved

Osteno Outcrop

A decapod, member of the family Erymidae. The species was originally included in the genus Eryma as E. meyeri, although the specimens reveal morphological characters diagnostic of Palaeastacus.[19]

Phlyctisoma[17]

  • Phlyctisoma sinemuriana

10 specimens, in a fairly good state of preservation

Osteno Outcrop

A decapod, type member of the family Erymidae. The species was originally identified as Pustulina sinemuriana.[19]

Pseudoglyphea[5][12][16]

  • Pseudoglyphea amylochelis

7 complete specimens, in a fairly good state

Osteno Outcrop

A decapod, member of the family Litogastroidae. Probably a bottom dweller predatory crustacean.[14]

Teruzzicheles[21] Teruzzicheles popeyei

Various specimens fairly preserved

Osteno Outcrop

A decapod belonging to the family Polychelidae

Xiphosurida edit

Genus Species Material Location Notes Images

Ostenolimulus[22]

  • Ostenolimulus latus
  • A nearly complete specimen

Osteno Outcrop

A horseshoe crab, member of the family Limulidae. This genus represents the oldest Jurassic limulid and only the second xiphosuran known from Italy.[22] Also indicates that this family were a diverse and widespread clade during the Jurassic.[22]

Thylacocephala edit

Genus Species Material Location Notes Images

Ostenocaris[5][6][23][24]

Ostenocaris cypriformis

  • Multiple specimens, complete and incomplete

Osteno Outcrop

A thylacocephalan, type member of the family Ostenocarididae inside Conchyliocarida. Originally Interpreted as a bizarre Cirriped. Ostenocaris is the most common fossil of the formation, and the main identified thylacocephalan from the formation. In the first interpretations, the genus was shown as a filter-feeding organism, which used the cephalic sac as a burrowing organ to ensure adhesion to the substrate. Based on the presence of Coprolites associated to the genus, with abundant masses of alimentary residues (hooks of cephalopods, vertebrates, remains of Crustacea) in the stomach of these organisms, Ostenocaris cypriformis was probably a necrophagous organism, and the cephalic sac can be tentatively interpreted as being a burrowing organ employed during the search for food, or as an organ of locomotion with intrinsic motility.[25]

 

Cephalopoda edit

Genus Species Material Location Notes Images

Arietites[5][6]

  • Arietites bucklandi

Shells

Osteno outcrop

An ammonitidan, type member of the family Arietitidae inside Psiloceratoidea. The main ammonite identified locally.

Angulaticeras[5][6][16]

  • Angulaticeras sp.

Shells

Osteno outcrop

An ammonitidan, member of the family Schlotheimiidae inside Psiloceratoidea. It was not the most abundant ammonite, but was rather common.

Coroniceras[5][6][16]

  • Coroniceras bisulcatum

Shells

Osteno outcrop

An ammonitidan, member of the family Arietitidae inside Psiloceratoidea. It was less common than other ammonites, although index for some locations.

Ectocentrites[5][6][16]

  • Ectocentrites sp.

Shells

Osteno outcrop

An ammonitidan, member of the family Lytoceratidae inside Lytoceratina. It was not the most abundant ammonite, but was rather common.

Ostenoteuthis[5][6][16][26][27]

  • Ostenoteuthis siroi

Several specimens with decent preservation

Osteno outcrop

A coleoid, type member of the family Ostenoteuthidae. A unique group of coeloids, only found at this location. Coleoids with ten arms each bearing pairs of hooks, Ostenoteuthis measure between 18 and 30 cm length.[27]

 

Oxynoticeras[5][6]

  • Oxynoticeras oxynotum

Shells

Osteno outcrop

An ammonitidan, type member of the family Oxynoticeratidae inside Ammonitida. It was not the most abundant ammonite, but was rather common.

Uncinoteuthis[6][27]

  • Uncinoteuthis cuvieri

An incomplete specimen consisting of the arm crown only

Osteno outcrop

A coleoid, member of the family Ostenoteuthidae. A unique group of coeloids, only found at this location.[27]

 

Echinoderms edit

Genus Species Material Location Notes Images

Hispidocrinus[28]

  • Hispidocrinus scalaris

Multiple ossicles

Pradalunga

An Crinoidean, member of the family Isocrininae inside Isocrinida.

Isocrinus[28]

  • Isocrinus sp.

Multiple ossicles

Ubiale - Clanezzo

An Crinoidean, member of the family Isocrininae inside Isocrinida.

Millericrinus[28]

  • Millericrinus cf. adneticus

Multiple ossicles

M. di Grone

An Crinoidean, member of the family Millericrinidae inside Millericrinida.

Palaeocoma[6][16]

  • Palaeocoma milleri

Multiple specimens

Ubiale - Clanezzo

An ophiuridan, member of the family Ophiodermatidae inside Ophiodermatina. Extant tropical species like Ophioderma are benthic predators and scavengers that show the same short spines seen in Palaeocoma.[6]

 

Hemichordata edit

Genus Species Material Location Notes Images

Megaderaion[29]

Megaderaion sinemuriense

  • A nearly complete specimen with soft tissue

Osteno Outcrop

An acorn worm, member of the family Harrimaniidae inside Enteropneusta. It was a large sized member of its family. This genus probably lived linked to sand bottoms, where it made burrows to hide and find food.[29]

Chondrichthyes edit

Genus Species Material Location Notes Images

Hybodontiformes[30]

Hybodontiformes indet

Teeth

Osteno Outcrop

A shark, member of the family Hybodontiformes.

Myriacanthidae[30]

Gen et sp. nov

Virtually complete skull with associated parts of the branchial skeleton

Osteno Outcrop

A chimaerid, member of the family Myriacanthidae inside Chimaeriformes.

Ostenoselache[6][16]

Ostenoselache stenosoma

One complete articulated specimen

Osteno Outcrop

An euselachiian, type member of the family Ostenoselachidae inside Elasmobranchii. A unique genus of shark, only found in the Osteno Formation. With an elongated eel-shaped morphology, the specimens found measure at least 240 mm in length, with a neurocranium with a long, complex rostrum.[16] It has been suggested it was an animal able to produce electric shocks, probably to kill prey.[16]

 

Palaeospinax[16][31]

Palaeospinax pinnai

A single specimen in four contiguous pieces and including parts of the dentition and squamation

Osteno Outcrop

A Shark, type member of the family Palaeospinacidae inside Synechodontiformes. Open water swimmer.

Squaloraja[16][30][32]

Squaloraja sp.

One complete articulated specimen

Osteno Outcrop

A chimaerid, type member of the family Squalorajidae inside Squalorajoidei. This genus belongs to a lineage of ray-like chimaeras.

 

Actinopterygii edit

Genus Species Material Location Notes Images

Cosmolepis[33]

Cosmolepis ornatus

  • MSNM V617, complete specimen

Osteno Outcrop

A primitive actinopterygiian, member of the order Palaeonisciformes. A late surviving representative of the family.

 

Dapedium[33]

Dapedium sp.

  • MSNM V630, caudal fin with associated scales

Osteno Outcrop

A primitive actinopterygiian, type member of the family Dapediidae inside Holostei. Probably a Coral Environment wanderer.

 

Furo[33]

Furo ("Eugnathus") sp.

  • MSNM V659, skull & anterior truncal body

Osteno Outcrop

A primitive actinopterygiian, type member of the family Furidae inside Ionoscopiformes. An enlongated Gar-alike taxon.

 

Pholidophorus[33]

Pholidophorus cf.bechei

  • MSNM V621, complete specimen
  • MSNM V556, isolated complete skull
  • Multiple referred specimens

Osteno Outcrop

A primitive actinopterygiian, type member of the family Pholidophoridae inside Teleostei. Open water swimmer, probably forming schools. It is the main fish recovered on the formation.

 

Pholidolepis[33]

Pholidolepis sp.

  • MSNM V409, complete specimen
  • MSNM V594, isolated complete skull
  • Multiple referred specimens

Osteno Outcrop

A primitive Actinopterygiian, member of the family Pholidophoridae inside Teleostei. Open water swimmer, probably forming schools.

 

Peripeltopleurus?[33][34]

Peripeltopleurus sp.

  • MSNM V659, almost complete specimen lacking the tail

Osteno Outcrop

A primitive actinopterygiian, member of the family Peltopleuridae inside Neopterygii. Probably represents the only known Jurassic survivor of the order Peltopleuriformes

 

Pteroniscus[33]

Cf.Pteroniscus sp.

  • MSNM V618-19, skull & toracic section specimen

Osteno Outcrop

A primitive actinopterygiian, member of the order Palaeonisciformes. A complicated genus know from younger-aged freshwater deposits, whose modern status is rather dubious.

Sarcopterygii edit

Genus Species Material Location Notes Images

Undina[6][33]

Undina (Holophagus) cf. gulo

  • MSNM V587, isolated scales

Osteno Outcrop

A Coelacanth, member of the family Latimeriidae inside Coelacanthiformes. Isolated 20 mm scales of coelacanths analogous to the genus Holophagus are quite frequent on the Osteno deposits, suggesting a taxon up to 75 cm long.

 

Plants edit

Genus Species Material Location Notes Images

Brachyphyllum[6][35]

  • Brachyphyllum sp. A
  • Brachyphyllum sp. B
  • Brachyphyllum sp. C
  • Fronds

Osteno Outcrop.[33]

A coniferophytan, member of the family Cheirolepidiaceae inside Pinopsida.

Equisitites[6][35]

Equisitites bunburyanus

  • Stems

Osteno Outcrop.[33]

A Horsetail, member of the family Equisetaceae inside Equisetales. A freshwater-related plant, that grew as fast as modern bamboo on tropical settings.

Otozamites[6][35]

  • Otozamites bunburyanus
  • Otozamites sp.
  • Fronds

Osteno Outcrop.[33]

A spermatopsidan, member of the family Bennettitales inside Bennettitopsida. Cycad-like flora, common on dry settings.

Pachypteris[6][35]

Pachypteris cf. rhomboidalis

  • Fronds

Osteno Outcrop.[33]

A tree fern, member of the family Umkomasiaceae inside Peltaspermales. Fronds of large tree ferns, related to humid ecosystems.

Pagiophyllum[6][35]

  • Pagiophyllum sp. A
  • Pagiophyllum sp. B
  • Fronds

Osteno Outcrop.[33]

A coniferophytan, member of the family Araucariaceae inside Pinopsida.

Williamsonia[6][35]

Williamsonia sp.

  • Fronds

Osteno Outcrop.[33]

A spermatopsidan, member of the family Bennettitales inside Bennettitopsida. Cycad-like flora, common on dry settings.

 

Zamites[6][35]

Zamites sp.

  • Fronds

Osteno Outcrop.[33]

A spermatopsidan, member of the family Bennettitales inside Bennettitopsida. Cycad-like flora, common on dry settings.

 

See also edit

References edit

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  2. ^ a b Muttoni, G.; Erba, E.; Kent, D. V.; Bachtadse, V. (2005). "Mesozoic Alpine facies deposition as a result of past latitudinal plate motion". Nature. 434 (7029): 59–63. Bibcode:2005Natur.434...59M. doi:10.1038/nature03378. hdl:2434/30440. PMID 15744297. S2CID 4316860.
  3. ^ a b Jadoul, F.; Galli, M. T. (2008). "The Hettangian shallow water carbonates after the Triassic-Jurassic biocalcification crisis: The Albenza Formation in the western Southern Alps". Rivista Italiana di Paleontologia e Stratigrafia. 114 (3): 453–470. Retrieved 2 May 2023.
  4. ^ Sarti, M.; Bosellini, A.; Winterer, E. L. (1992). "Basin Geometry and Architecture of a Tethyan Passive Margin, Southern Alps, Italy: Implications for Rifting Mechanisms: Chapter 13: African and Mediterranean Margins". AAPG Special Volumes. 115 (5): 241–258. Retrieved 2 May 2023.
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  6. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z Pinna, G. (2000). "Die Fossillagerstätte im Sinemurium (Lias) von Osteno, Italien". Europäische Fossillagerstätten, Springer, Berlin, Heidelberg. 3 (7): 91–136. doi:10.1007/978-3-642-57198-5_13. ISBN 978-3-642-62975-4. Retrieved 2 May 2023.
  7. ^ Bottjer, D. J.; Etter, W.; Tang, C. M.; Hagadorn, J. W. (2002). Exceptional fossil preservation: a unique view on the evolution of marine life. Columbia University Press. p. 421. ISBN 9780231102544. Retrieved 2 May 2023.
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  34. ^ Franceschi, F.; Marramà, G.; Carnevale, G. (2023). "Reassessment of a putative peltopleurid fish from the Sinemurian (Lower Jurassic) of Osteno (Como, Italy): preliminary results" (PDF). PALEODAYS-Abstract Book. XXIII Edizione delle Giornate di Paleontologia-2023. 23 (1): 51–51.
  35. ^ a b c d e f g Bonci, M. C.; Vanucci, G. (1986). "I vegetali sinemuriani di Osteno (Lombardia)". Atti della Società italiana di scienze naturali e del museo civico di storia naturale di Milano. 127 (2): 107–127.

moltrasio, formation, also, known, lombardische, kieselkalk, formation, geological, formation, italy, switzerland, this, formation, mostly, developed, lower, middle, sinemurian, stage, lower, jurassic, where, lombardian, basin, tectonic, activity, modified, cu. The Moltrasio Formation also known as the Lombardische Kieselkalk Formation is a geological formation in Italy and Switzerland This Formation mostly developed in the Lower or Middle Sinemurian stage of the Lower Jurassic where on the Lombardian basin tectonic activity modified the current marine and terrestrial habitats 2 Here it developed a series of marine related depositional settings represented by an outcrop of 550 600 m of grey Calcarenites and Calcilutites with chert lenses and marly interbeds that recovers the Sedrina Moltrasio and Domaro Formations 2 This was mostly due to the post Triassic crisis that was linked locally to tectonics 3 The Moltrasio Formation is considered a continuation of the Sedrina Limestone and the Hettangian Albenza Formation and was probably a shallow water succession developed on the passive margin of the westernmost Southern Alps 3 4 It is known due to the exquisite preservation observed on the Outcrop in Osteno where several kinds of marine biota have been recovered 5 Moltrasio FormationStratigraphic range Middle Sinemurian Lower Pliensbachian 196 188 Ma PreꞒ Ꞓ O S D C P T J K Pg NOutcropTypeGeological formationUnit ofMonte Generoso BasinSub unitsOsteno OutcropUnderliesDomaro FormationOverliesSedrina LimestoneThickness200 mLithologyPrimaryLimestoneLocationCoordinates46 00 N 9 06 E 46 0 N 9 1 E 46 0 9 1Approximate paleocoordinates33 12 N 15 36 E 33 2 N 15 6 E 33 2 15 6RegionLombardyCountry Italy SwitzerlandType sectionNamed forMoltrasioNamed byAntonio Stoppani 1 Year defined1857Moltrasio Formation Italy Show map of ItalyMoltrasio Formation Lombardy Show map of Lombardy Contents 1 Fossils 1 1 Exceptional fossilization 1 2 Nematoida 1 3 Annelida 1 4 Crustacea 1 5 Xiphosurida 1 6 Thylacocephala 1 7 Cephalopoda 1 8 Echinoderms 1 9 Hemichordata 1 10 Chondrichthyes 1 11 Actinopterygii 1 12 Sarcopterygii 1 13 Plants 2 See also 3 ReferencesFossils editExceptional fossilization edit nbsp Exposed Moltrasio Fm in Southern Switzerland Apart from the Eocene of Monte Bolca the Sinemurian of Osteno is the only fossil deposit in Italy in which soft bodies are preserved The Osteno site was discovered in 1964 It was recovered from a series of 6 metres 20 ft package of fine laminated gray spongiolitic micritic limestone 6 Coroniceras bisulcatum allowed to date the outcrop as the Bucklandi zone lower Sinemurian 6 The outcrop is a good documentation of a particularly complete fauna and flora of the Lower Jurassic which is not exactly common in the Southern Alps 6 The Osteno outcrop part of the formation is worldwide known due to the exceptional preservation of mostly marine biota including rare fossilized components helping to understand the ecosystems of the local Sinemurian margin of the Monte Generoso Basin 7 The high local variety of fossils found is most likely due to unique conditions of preservation where phosphatized soft tissues have not been observed in any fish or polychaetes but they are common in crustaceans 33 and also occur in a smaller percentage of teuthids 14 8 Soft part preservation through phosphatization in this deposit includes the muscles and branchia of Crustaceans fish tissues and the digestive tracts of coleoids polychaetes and nematodes These fossils are interpreted as having been preserved in a stagnant restricted basin with anoxic conditions likely within the sediment pore waters 5 Nematoida edit Genus Species Material Location Notes Images Eophasma 6 9 Eophasma jurasicum A complete specimen Osteno Outcrop A nematode type member of the family Eophasmidae inside Desmoscolecida 10 A rare find since nematode fossils are absent in most Mesozoic marine rocks 9 nbsp Annelida edit Genus Species Material Location Notes Images Melanoraphia 5 6 11 Melanoraphia maculata A nearly complete specimen Osteno Outcrop A polychaete member of the group Phyllodocemorpha with incertae sedis assignation This polychaete was probably an open swimmer more than a subtrate dweller 11 nbsp Crustacea edit Genus Species Material Location Notes Images Aeger 5 6 12 13 Aeger foesteri Aeger muensteri Aeger robustus Aeger rostrospinatus Aeger elongatus Aeger macropus Multiple specimens fairly preserved Osteno Outcrop A decapod type member of the family Aegeridae This genus is the most abundant local crustacean and was a shrimp like creature that was probably necrophagous 13 nbsp Coleia 5 6 12 14 15 16 Coleia vialiii Coleia medilerranea Coleia cf antiqua Coleia pinnnai Multiple specimens fairly preserved Osteno Outcrop A decapod type member of the family Coleiidae Probably a bottom dweller predatory crustacean 14 nbsp Eryma 17 18 Eryma sinemuriana 41 specimens fairly preserved Osteno Outcrop A decapod type member of the family Erymidae The species was originally identified as Pustulina sinemuriana 19 Glyphea 17 Glyphea tricarinata 137 complete and fragmentary specimens Osteno Outcrop A decapod type member of the family Erymidae The species was originally identified as Pustulina sinemuriana 19 Mecochirus 17 Mecochirus germari 81 complete and fragmentary specimens Osteno Outcrop A decapod member of the family Mecochiridae Rather rare compared to other local crustacean genera Ostenosculda 20 Ostenosculda teruzzii Single Specimen fairly preserved Osteno Outcrop A mantis shrimp Palaeastacus 17 19 Palaeastacus meyeri Multiple specimens fairly preserved Osteno Outcrop A decapod member of the family Erymidae The species was originally included in the genus Eryma as E meyeri although the specimens reveal morphological characters diagnostic of Palaeastacus 19 Phlyctisoma 17 Phlyctisoma sinemuriana 10 specimens in a fairly good state of preservation Osteno Outcrop A decapod type member of the family Erymidae The species was originally identified as Pustulina sinemuriana 19 Pseudoglyphea 5 12 16 Pseudoglyphea amylochelis 7 complete specimens in a fairly good state Osteno Outcrop A decapod member of the family Litogastroidae Probably a bottom dweller predatory crustacean 14 Teruzzicheles 21 Teruzzicheles popeyei Various specimens fairly preserved Osteno Outcrop A decapod belonging to the family Polychelidae Xiphosurida edit Genus Species Material Location Notes Images Ostenolimulus 22 Ostenolimulus latus A nearly complete specimen Osteno Outcrop A horseshoe crab member of the family Limulidae This genus represents the oldest Jurassic limulid and only the second xiphosuran known from Italy 22 Also indicates that this family were a diverse and widespread clade during the Jurassic 22 Thylacocephala edit Genus Species Material Location Notes Images Ostenocaris 5 6 23 24 Ostenocaris cypriformis Multiple specimens complete and incomplete Osteno Outcrop A thylacocephalan type member of the family Ostenocarididae inside Conchyliocarida Originally Interpreted as a bizarre Cirriped Ostenocaris is the most common fossil of the formation and the main identified thylacocephalan from the formation In the first interpretations the genus was shown as a filter feeding organism which used the cephalic sac as a burrowing organ to ensure adhesion to the substrate Based on the presence of Coprolites associated to the genus with abundant masses of alimentary residues hooks of cephalopods vertebrates remains of Crustacea in the stomach of these organisms Ostenocaris cypriformis was probably a necrophagous organism and the cephalic sac can be tentatively interpreted as being a burrowing organ employed during the search for food or as an organ of locomotion with intrinsic motility 25 nbsp Cephalopoda edit Genus Species Material Location Notes Images Arietites 5 6 Arietites bucklandi Shells Osteno outcrop An ammonitidan type member of the family Arietitidae inside Psiloceratoidea The main ammonite identified locally Angulaticeras 5 6 16 Angulaticeras sp Shells Osteno outcrop An ammonitidan member of the family Schlotheimiidae inside Psiloceratoidea It was not the most abundant ammonite but was rather common Coroniceras 5 6 16 Coroniceras bisulcatum Shells Osteno outcrop An ammonitidan member of the family Arietitidae inside Psiloceratoidea It was less common than other ammonites although index for some locations Ectocentrites 5 6 16 Ectocentrites sp Shells Osteno outcrop An ammonitidan member of the family Lytoceratidae inside Lytoceratina It was not the most abundant ammonite but was rather common Ostenoteuthis 5 6 16 26 27 Ostenoteuthis siroi Several specimens with decent preservation Osteno outcrop A coleoid type member of the family Ostenoteuthidae A unique group of coeloids only found at this location Coleoids with ten arms each bearing pairs of hooks Ostenoteuthis measure between 18 and 30 cm length 27 nbsp Oxynoticeras 5 6 Oxynoticeras oxynotum Shells Osteno outcrop An ammonitidan type member of the family Oxynoticeratidae inside Ammonitida It was not the most abundant ammonite but was rather common Uncinoteuthis 6 27 Uncinoteuthis cuvieri An incomplete specimen consisting of the arm crown only Osteno outcrop A coleoid member of the family Ostenoteuthidae A unique group of coeloids only found at this location 27 nbsp Echinoderms edit Genus Species Material Location Notes Images Hispidocrinus 28 Hispidocrinus scalaris Multiple ossicles Pradalunga An Crinoidean member of the family Isocrininae inside Isocrinida Isocrinus 28 Isocrinus sp Multiple ossicles Ubiale Clanezzo An Crinoidean member of the family Isocrininae inside Isocrinida Millericrinus 28 Millericrinus cf adneticus Multiple ossicles M di Grone An Crinoidean member of the family Millericrinidae inside Millericrinida Palaeocoma 6 16 Palaeocoma milleri Multiple specimens Ubiale Clanezzo An ophiuridan member of the family Ophiodermatidae inside Ophiodermatina Extant tropical species like Ophioderma are benthic predators and scavengers that show the same short spines seen in Palaeocoma 6 nbsp Hemichordata edit Genus Species Material Location Notes Images Megaderaion 29 Megaderaion sinemuriense A nearly complete specimen with soft tissue Osteno Outcrop An acorn worm member of the family Harrimaniidae inside Enteropneusta It was a large sized member of its family This genus probably lived linked to sand bottoms where it made burrows to hide and find food 29 Chondrichthyes edit Genus Species Material Location Notes Images Hybodontiformes 30 Hybodontiformes indet Teeth Osteno Outcrop A shark member of the family Hybodontiformes Myriacanthidae 30 Gen et sp nov Virtually complete skull with associated parts of the branchial skeleton Osteno Outcrop A chimaerid member of the family Myriacanthidae inside Chimaeriformes Ostenoselache 6 16 Ostenoselache stenosoma One complete articulated specimen Osteno Outcrop An euselachiian type member of the family Ostenoselachidae inside Elasmobranchii A unique genus of shark only found in the Osteno Formation With an elongated eel shaped morphology the specimens found measure at least 240 mm in length with a neurocranium with a long complex rostrum 16 It has been suggested it was an animal able to produce electric shocks probably to kill prey 16 nbsp Palaeospinax 16 31 Palaeospinax pinnai A single specimen in four contiguous pieces and including parts of the dentition and squamation Osteno Outcrop A Shark type member of the family Palaeospinacidae inside Synechodontiformes Open water swimmer Squaloraja 16 30 32 Squaloraja sp One complete articulated specimen Osteno Outcrop A chimaerid type member of the family Squalorajidae inside Squalorajoidei This genus belongs to a lineage of ray like chimaeras nbsp Actinopterygii edit Genus Species Material Location Notes Images Cosmolepis 33 Cosmolepis ornatus MSNM V617 complete specimen Osteno Outcrop A primitive actinopterygiian member of the order Palaeonisciformes A late surviving representative of the family nbsp Dapedium 33 Dapedium sp MSNM V630 caudal fin with associated scales Osteno Outcrop A primitive actinopterygiian type member of the family Dapediidae inside Holostei Probably a Coral Environment wanderer nbsp Furo 33 Furo Eugnathus sp MSNM V659 skull amp anterior truncal body Osteno Outcrop A primitive actinopterygiian type member of the family Furidae inside Ionoscopiformes An enlongated Gar alike taxon nbsp Pholidophorus 33 Pholidophorus cf bechei MSNM V621 complete specimen MSNM V556 isolated complete skull Multiple referred specimens Osteno Outcrop A primitive actinopterygiian type member of the family Pholidophoridae inside Teleostei Open water swimmer probably forming schools It is the main fish recovered on the formation nbsp Pholidolepis 33 Pholidolepis sp MSNM V409 complete specimen MSNM V594 isolated complete skull Multiple referred specimens Osteno Outcrop A primitive Actinopterygiian member of the family Pholidophoridae inside Teleostei Open water swimmer probably forming schools nbsp Peripeltopleurus 33 34 Peripeltopleurus sp MSNM V659 almost complete specimen lacking the tail Osteno Outcrop A primitive actinopterygiian member of the family Peltopleuridae inside Neopterygii Probably represents the only known Jurassic survivor of the order Peltopleuriformes nbsp Pteroniscus 33 Cf Pteroniscus sp MSNM V618 19 skull amp toracic section specimen Osteno Outcrop A primitive actinopterygiian member of the order Palaeonisciformes A complicated genus know from younger aged freshwater deposits whose modern status is rather dubious Sarcopterygii edit Genus Species Material Location Notes Images Undina 6 33 Undina Holophagus cf gulo MSNM V587 isolated scales Osteno Outcrop A Coelacanth member of the family Latimeriidae inside Coelacanthiformes Isolated 20 mm scales of coelacanths analogous to the genus Holophagus are quite frequent on the Osteno deposits suggesting a taxon up to 75 cm long nbsp Plants edit Genus Species Material Location Notes Images Brachyphyllum 6 35 Brachyphyllum sp A Brachyphyllum sp B Brachyphyllum sp C Fronds Osteno Outcrop 33 A coniferophytan member of the family Cheirolepidiaceae inside Pinopsida Equisitites 6 35 Equisitites bunburyanus Stems Osteno Outcrop 33 A Horsetail member of the family Equisetaceae inside Equisetales A freshwater related plant that grew as fast as modern bamboo on tropical settings Otozamites 6 35 Otozamites bunburyanus Otozamites sp Fronds Osteno Outcrop 33 A spermatopsidan member of the family Bennettitales inside Bennettitopsida Cycad like flora common on dry settings Pachypteris 6 35 Pachypteris cf rhomboidalis Fronds Osteno Outcrop 33 A tree fern member of the family Umkomasiaceae inside Peltaspermales Fronds of large tree ferns related to humid ecosystems Pagiophyllum 6 35 Pagiophyllum sp A Pagiophyllum sp B Fronds Osteno Outcrop 33 A coniferophytan member of the family Araucariaceae inside Pinopsida Williamsonia 6 35 Williamsonia sp Fronds Osteno Outcrop 33 A spermatopsidan member of the family Bennettitales inside Bennettitopsida Cycad like flora common on dry settings nbsp Zamites 6 35 Zamites sp Fronds Osteno Outcrop 33 A spermatopsidan member of the family Bennettitales inside Bennettitopsida Cycad like flora common on dry settings nbsp See also editList of fossiliferous stratigraphic units in Italy Calcare di Sogno Toarcian fossiliferous formation of Lombardy Saltrio Formation Sinemurian fossiliferous formation of Lombardy Rotzo Formation Pliensbachian fossiliferous formation of VenetoReferences edit Stoppani A 1857 Studi geologici e paleontologici sulla Lombardia 461 pp Tipografia Turati Milano a b Muttoni G Erba E Kent D V Bachtadse V 2005 Mesozoic Alpine facies deposition as a result of past latitudinal plate motion Nature 434 7029 59 63 Bibcode 2005Natur 434 59M doi 10 1038 nature03378 hdl 2434 30440 PMID 15744297 S2CID 4316860 a b Jadoul F Galli M T 2008 The Hettangian shallow water carbonates after the Triassic Jurassic biocalcification crisis The Albenza Formation in the western Southern Alps Rivista Italiana di Paleontologia e Stratigrafia 114 3 453 470 Retrieved 2 May 2023 Sarti M Bosellini A Winterer E L 1992 Basin Geometry and Architecture of a Tethyan Passive Margin Southern Alps Italy Implications for Rifting Mechanisms Chapter 13 African and Mediterranean Margins AAPG Special Volumes 115 5 241 258 Retrieved 2 May 2023 a b c d e f g h i j k l m Pinna G 1985 Exceptional preservation in the Jurassic of Osteno Philosophical Transactions of the Royal Society of London B Biological Sciences 311 1148 171 180 Bibcode 1985RSPTB 311 171P doi 10 1098 rstb 1985 0149 Retrieved 2 May 2023 a b c d e f g h i j k l m n o p q r s t u v w x y z Pinna G 2000 Die Fossillagerstatte im Sinemurium Lias von Osteno Italien Europaische Fossillagerstatten Springer Berlin Heidelberg 3 7 91 136 doi 10 1007 978 3 642 57198 5 13 ISBN 978 3 642 62975 4 Retrieved 2 May 2023 Bottjer D J Etter W Tang C M Hagadorn J W 2002 Exceptional fossil preservation a unique view on the evolution of marine life Columbia University Press p 421 ISBN 9780231102544 Retrieved 2 May 2023 Wilby P R Briggs D E 1997 Taxonomic trends in the resolution of detail preserved in fossil phosphatized soft tissues Geobios 30 8 493 502 Bibcode 1997Geobi 30 493W doi 10 1016 S0016 6995 97 80056 3 Retrieved 2 May 2023 a b Arduini P Pinna G Teruzzi G 1983 Eophasma jurassicum ngn sp a new fossil nematode of the Sinemurian of Osteno in Lombardy Atti della Societa italiana di scienze naturali e del museo civico di storia naturale di Milano 124 1 2 61 64 Poinar G O 2011 The Evolutionary History of Nematodes As revealed in stone amber and mummies Nematology Monographs and Perspectives 9 Brill Publishers ISBN 9789047428664 a b Arduini P Pinna G Teruzzi G 1982 Melanoraphia maculata ngn sp a new fossil polychaete of the Sinemurian of Osteno in Lombardy Atti della Societa italiana di scienze naturali e del museo civico di storia naturale di Milano 123 4 462 468 Retrieved 2 May 2023 a b c Pinna G 1967 Decouverte d une nouvelle faune a crustaces du Sinemurien inferieur dans la region du Lac Ceresio Lombardie Italie Atti Soc It Sci Nat Museo Milano 106 4 183 185 a b Garassino A Teruzzi G 1990 The genus Aeger Munster 1839 in the Sinemurian of Osteno in Lombardy Crustacea Decapoda Atti della societa italiana di scienze naturali e del museo civico di storia naturale di Milano 131 5 105 136 Retrieved 2 May 2023 a b c Pinna G 1969 Due nuovi esemplari di Coleia vialiii Pinna del Sinemuriano inferiore di Osteno in Lombardia Crustacea Decapoda Ann Mus St Nat Genova 77 12 626 632 Teruzzi G 1990 The genus Coleia Broderip 1835 Crustacea Decapoda in the Sinemurian of Osteno in Lombardy Atti della Societa italiana di Scienze naturali e del Museo Civico di Storia naturale di Milano 131 4 85 104 Retrieved 2 May 2023 a b c d e f g h i j k l Duffin C J 1998 Ostenoselache stenosoma ngn sp a new neoselachian shark from the Sinemurian Early Jurassic of Osteno Lombardy Italy PDF Societa Italiana di Scienze Naturali 9 7 1 27 Retrieved 2 May 2023 a b c d e Garassino A 1996 The family Erymidae Van Straelen 1924 and the superfamily Glypheoidea Zittel 1885 in the Sinemurian of Osteno in Lombardy AAI Soc It Sci RWT Museo Civ Stor Mu Milano Milano 135 11 333 373 Retrieved 2 May 2023 Devillez J Charbonnier S 2019 Review of the Early and Middle Jurassic erymid lobsters Crustacea Decapoda Revision des Erymides Crustacea Decapoda du Jurassique inferieur et moyen Bulletin de la Societe geologique de France 190 1 121 134 doi 10 1051 bsgf 2019005 S2CID 196643332 Retrieved 2 May 2023 a b c d e Devillez J Charbonnier S 2017 The genus Eryma Meyer 1840 Crustacea Decapoda Erymidae new synonyms systematic and stratigraphic implicationsLe genre Eryma Meyer 1840 Crustacea Decapoda Erymidae nouveaux synonymes implications systematique et stratigraphique Bulletin de la Societe geologique de France 188 3 1 15 Retrieved 2 May 2023 Another piece in the puzzle of mantis shrimp evolution fossils from the Early Jurassic Osteno Lagerstatte of Northern Italy Comptes Rendus Palevol 22 2 17 31 2023 Retrieved 2 May 2023 Audo Denis Charbonnier Sylvain 2022 12 28 Teruzzicheles popeyei an early Sinemurian polychelid lobster from the Osteno Lagerstatte Italy Neues Jahrbuch fur Geologie und Palaontologie Abhandlungen 306 3 187 194 doi 10 1127 njgpa 2022 1103 ISSN 0077 7749 S2CID 254820598 a b c Lamsdell J C Teruzzi G Pasini G Garassino A 2021 A new limulid Chelicerata Xiphosurida from the Lower Jurassic Sinemurian of Osteno NW Italy Neues Jahrbuch fur Geologie und Palaontologie Abhandlungen 300 1 1 10 doi 10 1127 njgpa 2021 0974 S2CID 234814276 Arduini P Pinna G Teruzzi G 1984 Ostenocaris nom nov pro Ostenia Atli Del A Societcl Iraliwzn di Sc Ienze Naturali e del Museo Civico di Storia Naturale di Milano Miiano 125 1 2 48 Arduini P Pinna G Teruzzi G 1982 Il giacimento sinemuriano di Osteno in Lombardia Palaeontology Essential of Historical Geology Mucchi Modena 134 2 495 522 Pinna G Arduini P Pesarini C Teruzzi G 1985 Some controversial aspects of the morphology and anatomy of Ostenocaris cypriformis Crustacea Thylacocephala Earth and Environmental Science Transactions of the Royal Society of Edinburgh 76 2 3 373 379 doi 10 1017 S0263593300010580 S2CID 85401617 Retrieved 2 May 2023 Pinna D 1972 Rinvenimento di un raro cefalopode coleoideo nel giacimento sinemuriano di Osteno in Lombardia Atti de la SocietaA Italiana di Scienze Naturali e del Museo Civico di Storia Naturale di Milano 113 1 141 149 a b c d Garassino A Donovan D T 2000 A new family of coleoids from the Lower Jurassic of Osteno Northern Italy Palaeontology 43 6 1019 1038 Bibcode 2000Palgy 43 1019G doi 10 1111 1475 4983 00160 S2CID 129455509 Retrieved 2 May 2023 a b c Jaselli L 2021 Reappraisal of the Lower Jurassic crinoid fauna of Lombardy Italy insights on regional museum collections Bollettino della Societa Paleontologica Italiana 60 2 112 Retrieved 19 October 2023 a b Arduini P Pinna G Teruzzi G 1981 Megaderaion sinemuriense n g n sp a new fossil enteropneust of the Sinemurian of Osteno in Lombardy Atti della Societa Italiana di Scienze Naturali e del Museo Civico di Storia Naturale in Milano 122 2 104 108 Retrieved 2 May 2023 a b c Duffin C J 1991 A myriacanthid holocephalan Chondrichthyes from the Sinemurian Lower Jurassic of Osteno Lombardy Italy Atti della Societa italiana di scienze naturali e del museo civico di storia naturale di Milano 132 23 293 308 Retrieved 3 May 2023 Duffin C J 1987 Palaeospinax pinnai n sp a new Palaeospinacid shark from the Sinemuvian Lower Jurassic of Osteno Lombardy Italy Atti della Societa italiana di scienze naturali e del museo civico di storia naturale di Milano 128 1 185 202 Duffin Christopher J Garassino Alessandro Pasini Giovanni 2023 Squaloraja Riley 1833 Holocephala Squalorajidae from the Lower Jurassic of Osteno Konservat Lagerstatte Como NW Italy Natural History Sciences 10 1 doi 10 4081 nhs 2023 642 ISSN 2385 0922 S2CID 258822179 a b c d e f g h i j k l m n o Duffin C J Patterson C 1993 I Pesci Fossili di Osteno una Nuova Finestra sulla Vita del Giurassico Inferiore Paleocronache 34 2 18 38 Retrieved 3 May 2023 Franceschi F Marrama G Carnevale G 2023 Reassessment of a putative peltopleurid fish from the Sinemurian Lower Jurassic of Osteno Como Italy preliminary results PDF PALEODAYS Abstract Book XXIII Edizione delle Giornate di Paleontologia 2023 23 1 51 51 a b c d e f g Bonci M C Vanucci G 1986 I vegetali sinemuriani di Osteno Lombardia Atti della Societa italiana di scienze naturali e del museo civico di storia naturale di Milano 127 2 107 127 Retrieved from https en wikipedia org w index php title Moltrasio Formation amp oldid 1219116579, wikipedia, wiki, book, books, library,

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