Rotzo Formation
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| Rotzo Formation | |
|---|---|
| Stratigraphic range: Pliensbachian ~[1] | |
Panorama of the Rotzo area with several of the Outcrops visible: Tonezza mountain at the left, Val d´Assa cliff in the center-front and Campolongo mountain in the right | |
| Type | Geological formation |
| Unit of | Calcari Grigi Group |
| Sub-units | Tovel Member[2] |
| Underlies | Massone Oolitic Limestone |
| Overlies | |
| Area | Trento Platform |
| Thickness | 250 m |
| Lithology | |
| Primary | Lithified gray silty marl, gray grainstone, bioturbated/intraclastic/ooidal gray wackestone, mud banks and sand deposits.[3] |
| Other | Light-grey to yellowish-grey packstone with oolites, bioclasts, algal lumps, pellets, dasycladacean algae, foraminifera, lituolids, and miliolids |
| Location | |
| Location | Vicenza Province: Trentino-Alto Adige, Southern Alps |
| Coordinates | 45°42′N 11°06′E / 45.7°N 11.1°E |
| Approximate paleocoordinates | 32°06′S 16°42′E / 32.1°S 16.7°E |
| Region | Veneto |
| Country | Italy |
| Type section | |
| Named for | Rotzo |
The Rotzo Formation (also known in older literature as the Noriglio Grey Limestone Formation) is a geological formation in Italy, dating to roughly between 192 and 185 million years ago and covering the Pliensbachian stage of the Jurassic Period in the Mesozoic Era.[4] Fossil prosauropod tracks have been reported from the formation.[5]

Has been traditionally classified as a Sinemurian-Pliensbachian Formation, but a large and detailed dataset of isotopic 13C and 87Sr/86Sr data, estimated the Rotzo Formation to span only over the Early Pliensbachian, bracketed between the Jamesoni-Davoei biozones, marked in the Loppio Oolitic Limestone-Rotzo Fm contact by a carbon isotope excursion onset similar to the Sinemu-Pliens boundary event, while the other sequences fit with the a warm phase that lasts until the Davoei biozone.[1] A more recent work reinforced this datation, constraining the lowermost levels to 192.30 Ma and the uppermost to 185.99 Ma.[6] The Rotzo Formation represented the Carbonate Platform, being located over the Trento Platform and surrounded by the Massone Oolite (marginal calcarenitic bodies), the Fanes Piccola Encrinite (condensed deposits and emerged lands), the Lombadian Basin Medolo Group and Belluno Basin Soverzene Formation (open marine), and finally towards the south, deep water deposits of the Adriatic Basin.[7] The Pliensbachian Podpeč Limestone of Slovenia, the Aganane Formation & the Calcaires du Bou Dahar of Morocco represent regional equivalents, both in deposition and faunal content.
This formation was deposited within a tropical lagoon environment, similar to modern Bahamas which was protected by oolitic shoals and bars from the open deep sea located to the east (Belluno Basin) and towards the west (Lombardia Basin). It is characterized by a rich paleontological content. It is notable mostly thanks to its great amount of big aberrant bivalves, among which is the genus Lithiotis, described in the second half of the nineteenth century. The unusual shape of Lithiotis and Cochlearites shells, extremely elongated and narrow, characterized by a spoon-like body space placed in a high position, rarely preserved, seems to suggest their adaptation to soft and muddy bottoms with a high sedimentation rate.[8] The Bellori outcrop displays about 20 m of limestones with intercalated clays and marls rich in organic matter and sometimes fossil wood (coal) and amber. The limestones are well stratified, with beds 10 cm to more than one metre thick, whereas the clayey levels range between 3 and 40 cm in thickness.[9][10]

The sedimentary cover of the Southern Alps has been recognized as a well-preserved section of the Mesozoic Tethys' southern continental margin, featuring a horst and graben structure linked to the rifting associated with the opening of the central North Atlantic that in the Late Triassic and Early Jurassic, created elevated blocks separated by troughs. While the western margin (Piedmont and Lombardy) quickly submerged in the Early Jurassic (As seen by the Moltrasio Formation), the eastern regions maintained shallow water sedimentation, including the Friuli and Trento Platforms, this last one latter evolving into a pelagic plateau, and separated from the Lombardian basin by the Garda escarpment fault system.[11]
The Early Jurassic Calcari Grigi Group represents the shallow-water sedimentation phase of the Trento Platform, revealing several sites over an area of about 1,500 km2. The continuity of dinosaur tracks from the Hettangian-Pliensbachian interval indicates a stable connection between the Southern Alps' carbonate tidal flats and nearby vegetated lands and freshwater sources, although the exact locations of these lands remain uncertain.[12] Detailed sedimentological studies of the Calcari Grigi Group, particularly the Rotzo Formation, describe it as a shallow subtidal platform with an inner lagoon bordered by oolitic shoals.[9]
The Coste dell'Anglone ichnosite for example, situated on the margin of this lagoon within a sandy barrier complex, was influenced by pioneer plants like Hirmeriellaceae in semi-arid conditions. Sedimentary structures indicate a shallow water tidal environment with heterolithic stratification pointing to steady flows at low current velocities. The presence of dinosaur tracks and supratidal markers suggests repeated subaerial exposure, contrasting with previous interpretations of the site as fully subtidal.[12][13]
These findings align with the lagoon-barrier island complex scenario, featuring a subtidal ramp gently inclined to the west and an intertidal-supratidal barrier island complex trending approximately N-S, now corresponding to the Mt. Brento-Biaina and Mt. Baldo chains.[7][12]
Amoebae
Color key
|
Notes Uncertain or tentative taxa are in small text; |
The presence of the families Centropyxidae and Difflugiidae testifies the presence of a mixed marine-terrestrial depositional system, lacking large bodies of water.[14]
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
Tonezza del Cimone |
Isolated Tests/Shells |
A testate amoebae, member of the family Centropyxidae inside Arcellinida. |
| |
|
Tonezza del Cimone |
Isolated Tests/Shells |
A testate amoebae, member of the family Difflugiidae inside Arcellinida. |
||
|
Tonezza del Cimone |
Isolated Tests/Shells |
A testate amoebae, member of the family Difflugiidae inside Arcellinida. |
||
Foranimifera
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Agerina[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Cornuspiridae family | |
| Ammobaculites[15] |
|
|
Isolated Tests/Shells | A foraminifer of the family Ammomarginulininae. | |
| Amijiella[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Hauraniidae family | |
| Bosniella[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Biokovinidae family | |
| Cymbriaella[16] |
|
|
Isolated Tests/Shells | A foraminifer of the Hauraniidae family | |
| Duotaxis[15][17] |
|
|
Isolated Tests/Shells | A foraminifer of the Duotaxidae family | |
|
|
Isolated Tests/Shells | A foraminifer of the Everticyclamminidae family. | ||
| Frondicularia[19] |
|
|
Isolated Tests/Shells | A foraminifer of the family Nodosariinae. | |
| Glomospira[15] |
|
|
Isolated Tests/Shells | A foraminifer of the family Ammodiscidae. | |
| Haurania[15] |
|
|
Isolated Tests/Shells | A foraminifer of the family Hauraniinae. | |
| Kristanita[20] |
|
|
Isolated Tests/Shells | A foraminifer of the Duotaxidae family | |
| Lituosepta[15][21] |
|
|
Isolated Tests/Shells | A foraminifer of the Mesoendothyridae family. | |
| Meandrovoluta[15][22] |
|
|
Isolated Tests/Shells | A foraminifer of the Cornuspiridae family | |
| Mayncina[19][15] |
|
|
Isolated Tests/Shells | A foraminifer of the Mayncinidae family | |
| Orbitopsella[19][15] |
|
|
Isolated Tests/Shells | A foraminifer of the Mesoendothyridae family. | |
| Ophtalmidium[15] |
|
|
Isolated Tests/Shells | A foraminifer of the family Ophthalmidiidae. | |
| Paleomayncina[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Planiseptinae family. | |
| Pseudocyclammina[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Pfenderinidae family. | |
| Pseudopfenderina[15] |
|
|
Isolated Tests/Shells | A foraminifer of the Pseudopfenderininae family. |
Invertebrates
Microfossils of the Rotzo Formation consist of benthic foraminifera, calcareous algae, Ostracoda and coprolites. Foraminifera are mainly benthic agglutinated species belonging to the superfamily Lituolacea (suborder Textulariina), while lamellar and porcellaneous-walled species are very rare.[23] The bivalve Opisoma excavatum is very common.[24]
Sponges
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Bauneia[25] |
|
|
Imprints | A Demosponge, member of Chaetetidae. | |
|
|
Colonial Imprints |
A Demosponge, member of Suberitidae. Monospecific assamblages with encrusting and symbiont forms are found abundantly on lagoonal facies, distributed in several stratigraphic horizons. |
||
Anthozoa
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
|
Colonial Imprints |
A Scleractinian Coral, member of Montlivaltiidae. This Coral is often found in the Early Jurassic Tethys range, from the Iberian peninsula to Morocco. |
||
| Montlivaltia[28][29] |
|
|
Colonial Imprints | A Scleractinian Coral, member of Montlivaltiidae. | |
| Oppelismilia[19] |
|
|
Imprints | A Scleractinian Coral, member of Oppelismiliidae. | |
| Pinacophyllum[27] |
|
|
Colonial Imprints | A Scleractinian Coral, member of Stylophyllidae | |
| Stylophyllopsis[27] |
|
|
Colonial Imprints | A Scleractinian Coral, member of Stylophyllidae | |
| Synastrea[27] |
|
|
Colonial Imprints | A Scleractinian Coral, member of Synastraeidae |
Bryozoa
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
|
Imprints |
A Stenolaematan of the family Aisenvergiidae |
Brachiopod
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
|
Isolated Shells |
A Rhynchonellidan, member of Gibbirhynchiinae. Unusual genus in the Mediterranean region, more common on NW Europe |
||
| Hesperithyris[28] |
|
|
Isolated Shells | A Rhynchonellidan, member of Zeilleriidae. | |
|
|
Isolated Shells |
A Terebratulidan, member of Nucleatidae. Typical Mediterranean region taxon in the Pliensbachian |
||
|
|
Isolated Shells |
A spiriferidan, member of Spiriferinidae. |
||
| Liothyrina[29] |
|
|
Isolated Shells | A Terebratulidan, member of Terebratellidae. | |
| Lobothyris[28] |
|
|
Isolated Shells | A Terebratulidan, member of Lobothyrididae. | |
|
|
Isolated Shells |
A Terebratulidan, member of Plectoconchidae. The main Branchiopod locally associated with the local Lithiotid facies, where they formed rare mass occurrences at discrete intervals. |
||
| Merophricus[28] |
|
|
Isolated Shells | A Terebratulidan, member of Plectoconchidae. | |
| Plectothyris[28] |
|
|
Isolated Shells | A Terebratulidan, member of Loboidothyrididae. | |
|
|
Isolated Shells |
A spiriferidan, member of Spiriferinidae. |
||
| Waldheimia[28] |
|
|
Isolated Shells | A Terebratulidan, member of Terebratellidae. | |
Bivalves
The Rotzo Formation is known mostly due to its massive bivalve associations of the genera Lithiotis, Cochlearites and Lithioperna that extended all along the Pliensbachian Trento Platform forming mass accumulations of specimens that formed Reef-Like structures.[33] This fauna appeared after the early Pliensbachian C-cycle perturbation, that triggered the diffusion of the Lithiotis Fauna, noted on the rapid widespread of this biota after the event layers.[33] All of the genera related with this fauna appeared on the lower Jurassic, and all but one became extinct before the Middle Jurassic.[19] This "Reefs" had a strong zonation, starting with the bivalves Gervilleioperna and Mytiloperna, restricted to intertidal and shallow-subtidal facies. Lithioperna is limited to lagoonal subtidal facies and even in some low-oxygen environments. Finally Lithiotis and Cochlearites are found in subtidal facies, constructing buildups.[19] This sections formed various kinds of ecosystems on the Trento platform, where it appeared in branched corals filled with (Spongiomorpha), Domal corals (Stromatoporida), tubular corals, Styllophyllidae corals, unidentified Cerioidea colonial corals, regular echinoid debris, sponges, and the solitary coral Opelismilia sp., with also aggregated snail shells.[19]
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Astarte[28] |
|
|
Isolated Shells | A clam, member of Astartidae. | |
| Avicula[30] |
|
|
Isolated Shells | A clam, member of Aviculidae. | |
| Cardinia[29] |
|
|
Isolated Shells | A clam, member of Cardiniidae. | |
| Ceromya[29] |
|
|
Isolated Shells | A piddock, member of Ceromyidae. | |
|
|
Isolated & Accumulated shells |
An oyster, member of Plicatostylidae. It is one of the Three main bivalves recovered on the Lithiotis Facies, with its accumulations generally overlying megalodontid coquinas.[35] |
||
| Cucullaea[28][29] |
|
|
Isolated Shells | A clam, member of Cucullaeidae. | |
| Cypricardinia[29][30] |
|
|
Isolated Shells | A clam, member of Trapezidae. | |
| Cyprina[29] |
|
|
Isolated Shells | A clam, member of Arcticidae. | |
|
|
Isolated Shells |
A clam, member of Neomiodontidae. The so-called Eomiodon horizon represents the lower Rotzo Formation, composed of organic-rich marlstones with abundant specimens of this genus, typical of stressed environment with low salinity.[34] This genus considered an opportunistic shallow infaunal suspension feeder, and the marker genus for brackish environments.[37] |
||
| Gastrochaenolites[38] |
|
|
Clavate, smooth borings |
Borings over Opisoma shells |
|
|
|
Isolated Shells |
An Oyster, member of Bakevelliidae. Found on greater accumulations on lower shale-dominated levels |
||
|
|
Isolated Shells |
An oyster, member of Plicatostylidae. On the Rotzo formation this genus become abundant along rootlets, indicative of a very shallow and restricted lagoon or marsh environment.[35] |
||
| Gresslya[30][32] |
|
|
Isolated Shells | A clam, member of Ceratomyidae. | |
| Gryphaea[29] |
|
|
Isolated Shells | A clam, member of Gryphaeidae. | |
| Homomya[28] |
|
|
Isolated Shells | A clam, member of Pleuromyidae. | |
| Lima[28] |
|
|
Isolated Shells | A clam, member of Limidae. | |
| Liostrea[28] |
|
|
Isolated Shells | A oyster, member of the family Flemingostreidae. | |
| Lithophaga[28] |
|
|
Isolated Shells | A mussel, member of the family Mytilidae. | |
|
|
Isolated & Accumulated shells |
An oyster, member of Plicatostylidae. A large bivalve, up to 70 cm length. This genus was found to be a bivalve with a byssate juvenile stage that developed different modes of life on the adulthood depending on the individual density and bottom firmness.[36] |
||
|
|
Isolated & Accumulated shells |
An oyster, member of Plicatostylidae. It is the major Bivalve identified on the formation, and the genus that gives the name to the "Lithiotis fauna".[35] Its accumulation have had different denominations on literature, such as banks, bioherms, biostromes, bivalve reefs or bivalve mounds.[35] |
||
| Lucina[28] |
|
|
Isolated Shells | A clam, member of Lucinidae. | |
| Modiolus[28][29] |
|
|
Isolated Shells | A mussel, member of the family Mytilidae. | |
|
|
Isolated Shells |
A mussel, member of the family Mytilidae |
||
|
|
Isolated Shells |
A clam, member of Astartidae. Is considered a genus that evolved from shallow burrowing ancestors, becoming a secondarily semi-infaunal edgewise recliner adapted to photosymbiosis.[24] |
||
|
|
Isolated Shells |
An oyster, member of Plicatostylidae. |
||
|
|
Isolated Shells |
A clam, member of Megalodontidae. |
||
| Pecten[28][29] |
|
|
Isolated Shells | A scallop, member of the family Pectinidae. | |
| Pholadomya[29][32] |
|
|
Isolated Shells | A clam, member of Pholadomyidae. | |
| Pinna[28][29] |
|
|
Isolated Shells | An oyster, member of Pinnidae. | |
| Placunopsis[28] |
|
|
Isolated Shells | A scallop, member of the family Anomiidae. | |
| Plicatula[29] |
|
|
Isolated Shells | An oyster, member of Plicatulidae. | |
| Pleuromya[30] |
|
|
Isolated Shells | A clam, member of Pleuromyidae. | |
| Protodiceras[32] |
|
|
Isolated Shells | A clam, member of Megalodontidae. | |
|
|
Isolated Shells |
A clam, incertae sedis inside Pterioida. On the Rotzo formation this byssate bivalve indicates a shallow subtidal or intertidal environment.[36] |
||
| Pteria[32] |
|
|
Isolated Shells | An oyster, member of Pteriidae. | |
| Tellina[28] |
|
|
Isolated Shells | A clam, member of Tellinidae. | |
| Unicardium[29] |
|
|
Isolated Shells | An oyster, member of Unicardiidae. | |
Ammonoidea
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Androgynoceras[40] |
|
|
Shells | An ammonite of the family Liparoceratidae. | |
|
|
Shells |
An ammonite of the family Schlotheimiidae. |
||
|
|
Shells |
An Ammonite of the Family Hildoceratidae |
| |
| Harpophylloceras[40] |
|
|
Shells | An Ammonite of the family Juraphyllitidae. | |
|
|
Shells |
Type member of the family Juraphyllitidae. |
||
| Liparoceras[40] |
|
|
Shells | An ammonite of the family Liparoceratidae. | |
| Partschiceras[40] |
|
|
Shells | An Ammonite of the family Phylloceratidae. | |
| Protogrammoceras[41] |
|
|
Shells | An Ammonite of the family Hildoceratidae. | |
Gastropoda
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
|
Shells |
A Top Snail of the family Trochidae. |
||
|
|
Shells |
An snail of the family Nerinellidae. |
||
|
|
Shells |
An snail of the family Ataphridae. |
||
|
|
Shells |
A keyhole limpet of the family Fissurellidae. |
||
| Ceritella[29] |
|
|
Shells | An snail of the family Cerithiidae. | |
| Cerithium[29] |
|
|
Shells | An snail of the family Cerithiidae. | |
| Cylindrites[29] |
|
|
Shells | A barrel bubble snail of the family Acteonidae. | |
|
|
Shells |
An snail of the family Discohelicidae. |
||
|
Indeterminate |
|
Shells |
Incertade Sedis |
||
|
|
Shells |
An snail of the family Eucyclidae. |
||
|
|
Shells |
A keyhole limpet of the family Fissurellidae. |
||
|
|
Shells |
An snail of the family Ampullinidae. |
||
|
|
Shells |
An snail of the family Trochonematidae. |
||
| Natica[30] |
|
|
Shells | A moon snail of the family Naticidae. | |
| Nerinea[29] |
|
|
Shells | An snail of the family Nerineidae. | |
|
|
Shells |
An snail of the family Neritopsidae. |
||
| Patella[30] |
|
|
Shells | A limpet of the family Patellidae. | |
|
|
Shells |
An snail of the family Trochidae. |
||
| Pleurotomaria[29] |
|
|
Shells | An snail of the family Pleurotomariidae. | |
|
|
Shells |
An snail of the family Gordenellidae. |
||
|
|
Shells |
An snail of the family Pseudonerineidae. |
||
|
|
Shells |
A limpet of the family Acmaeidae. |
||
| Rissoina[29] |
|
|
Shells | An snail of the family Rissoinidae. | |
|
|
Shells |
A periwinkle of the family Purpurinidae. |
||
| Trochus[30] |
|
|
Shells | A top snail of the family Trochidae. | |
| Turritella[29][43] |
|
|
Shells | An snail of the family Turritellidae. | |
Echinodermata
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Asteriacites[44] |
|
|
Star-shaped impressions | An ichnogenus that represents the resting trace resting activity of brittle stars (Ophiuroidea).[44] The recovered from the Rotzo formation are probably from specimens trapped on tidal changes.[44] | |
| Hypodiadema[30] |
|
|
Sclerites | A Pseudodiadematidae Euechinoidean | |
|
|
Two specimens (MCV.20/02 and MCV.20/03) |
|||
| Pseudodiadema[28] |
|
|
Multiple specimens | A Pseudodiadematidae Euechinoidean | |
Arthropoda
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
| Cypris[30][28] |
|
|
Valves | An Ostracodan of the family Cyprididae | |
|
|
Slightly deformed Exuvia |
An Erymid Decapodan Crustacean. With a total length between 9-10 cm is one of the largest specimens belonging to this species. |
||
|
|
Valves |
An Ostracodan of the family Cytherideidae. The earliest record of the genus.[47] |
||
|
|
Valves |
An Ostracodan of the family Limnocytherinae. High probability to be a new species of Limnocythere.[47] |
||
|
|
Burrowing and track Ichnofossils |
Burrows of Decapodans |
||
|
|
Valves |
An Ostracodan of the family Cytherideidae. The assemblage is dominated (>95%) by this taxon.[47] |
||
Annelida
| Genus | Species | Provenance | Material | Notes | Images |
|---|---|---|---|---|---|
|
|
Isolated scolecodonts |
A polychaete of the family Dorvilleidae. Unlike the modern counterparts that live in deeper environments, this species is found linked with shallow marine facies |
| |
| Serpula[30] |
|
|
Isolated or accumulated tubes | A sessile Annelid of the family Serpulidae. | |
Ichnofossils
On the local limestone deep burrowing is a very common type of biogenic activity, as is shown due to the presence of a large characteristic network of burrows which reach down to the lagoonal, marly-clayey assigned strata, suggesting intense bioturbation by large unknown organisms, perhaps giant decapod crustaceans (probably members of the family Erymidae), although, the burrows found are not closely related to the ones of Shrimps or other decapods, but resemble those of Stomatopoda and Malacostraca.[48]
| Genus | Species | Provenance | Material | Made By | Images |
|---|---|---|---|---|---|
|
|
Vertical burrows with preserved entrances |
|
||
|
|
Burrowing and track Ichnofossils |
|
||
|
|
Infilled abandoned burrows by coarse-grained skeletal debris |
|||
|
|
Infilled abandoned burrows by coarse-grained skeletal debris |
|
||
|
|
Burrowing and track Ichnofossils |
|
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