Rotzo Formation

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Rotzo Formation
Stratigraphic range: Pliensbachian
~192.30–185.99 Ma
[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
TypeGeological formation
Unit ofCalcari Grigi Group
Sub-unitsTovel Member[2]
UnderliesMassone Oolitic Limestone
Overlies
AreaTrento Platform
Thickness250 m
Lithology
PrimaryLithified gray silty marl, gray grainstone, bioturbated/intraclastic/ooidal gray wackestone, mud banks and sand deposits.[3]
OtherLight-grey to yellowish-grey packstone with oolites, bioclasts, algal lumps, pellets, dasycladacean algae, foraminifera, lituolids, and miliolids
Location
LocationVicenza Province: Trentino-Alto Adige, Southern Alps
Coordinates45°42′N 11°06′E / 45.7°N 11.1°E / 45.7; 11.1
Approximate paleocoordinates32°06′S 16°42′E / 32.1°S 16.7°E / -32.1; 16.7
RegionVeneto
CountryItaly
Type section
Named forRotzo
Rotzo Formation is located in Italy
Rotzo Formation
Rotzo Formation (Italy)

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]

Succession of the Formation in Vajo dell'Anguilla (Verona Province)

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]

An in-situ bed of Pachygervillia from the lower Rotzo Formation

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
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

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

Centropyxis[14]

  • C. sp.

Tonezza del Cimone

Isolated Tests/Shells

A testate amoebae, member of the family Centropyxidae inside Arcellinida.

Extant Centropyxis

Difflugia[14]

  • D. sp.

Tonezza del Cimone

Isolated Tests/Shells

A testate amoebae, member of the family Difflugiidae inside Arcellinida.

Extant Difflugia

Pontigulasia[14]

  • P. sp.

Tonezza del Cimone

Isolated Tests/Shells

A testate amoebae, member of the family Difflugiidae inside Arcellinida.

Extant Pontigulasia

Foranimifera

Genus Species Provenance Material Notes Images
Agerina[15]
  • A. martana
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Cornuspiridae family
Ammobaculites[15]
  • A. coprolithiformis
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the family Ammomarginulininae.
Amijiella[15]
  • A. amiji
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Hauraniidae family
Bosniella[15]
  • B. oenensis
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Biokovinidae family
Cymbriaella[16]
  • C. Iorigae
  • Monte di Campoluzzo
  • Alpe Alba
Isolated Tests/Shells A foraminifer of the Hauraniidae family
Duotaxis[15][17]
  • D. metula
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Duotaxidae family

Everticyclammina[18]

  • E. praevirguliana
  • Camporosa
  • Rotzo
  • Monte Cimoncello di Toraro
  • Monte di Campoluzz
Isolated Tests/Shells A foraminifer of the Everticyclamminidae family.
Frondicularia[19]
  • F. sp.
  • Bellori
  • Garzon di Scotto
  • Ponte dell`Anguillara
Isolated Tests/Shells A foraminifer of the family Nodosariinae.
Glomospira[15]
  • G. sp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the family Ammodiscidae.
Haurania[15]
  • H. amiji
  • H. deserta
  • H. ssp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
  • Bellori
  • Garzon di Scotto
  • Ponte dell`Anguillara
Isolated Tests/Shells A foraminifer of the family Hauraniinae.
Kristanita[20]
  • K. inflata
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Duotaxidae family
Lituosepta[15][21]
  • L. recoarensis
  • L. compressa
  • L. ssp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
  • Bellori
  • Ponte dell`Anguillara
Isolated Tests/Shells A foraminifer of the Mesoendothyridae family.
Meandrovoluta[15][22]
  • M. asiagoensis
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Monte Baldo
Isolated Tests/Shells A foraminifer of the Cornuspiridae family
Mayncina[19][15]
  • M. termieri
  • Garzon di Scotto
  • Bellori
  • Ponte dell`Anguillara
Isolated Tests/Shells A foraminifer of the Mayncinidae family
Orbitopsella[19][15]
  • O. primaeva
  • O. preacursor
  • O. dubari
  • O. circumvulvata
  • O. spp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Campomolon
  • Bellori
  • Ponte dell`Anguillara
  • Sega di Noriglio
  • Rotzo
  • Val d'Assa
  • Monte Gallo
Isolated Tests/Shells A foraminifer of the Mesoendothyridae family.
Ophtalmidium[15]
  • O. concentricum
  • O. sp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the family Ophthalmidiidae.
Paleomayncina[15]
  • P. termieri
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Planiseptinae family.
Pseudocyclammina[15]
  • P. liasica
  • P. spp.
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
Isolated Tests/Shells A foraminifer of the Pfenderinidae family.
Pseudopfenderina[15]
  • P. cf. butterlini
  • Altopiano di Asiago
  • Tonezza del Cimone
  • Altopiano di Folgaria
  • Recoaro
  • Gruppo del Pasubio
  • Monte Baldo
  • Monte Scandolara
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]
  • B. zignoi
  • Monte Alba
  • Roverè di Velo
  • Rovereto
Imprints A Demosponge, member of Chaetetidae.

Pseudoseptifer[25][26]

  • P. beneckei
  • P. waehneri
  • Lancia refuge
  • Alpe Alba
  • Col Santo
  • Roverè di Velo

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.

Modern relative, Aaptos tenta

Anthozoa

Genus Species Provenance Material Notes Images

Isastrea[27]

  • I. sp.
  • Rotzo

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]
  • M. trochoidiformis
  • Rotzo
  • Sega di Noriglio
Colonial Imprints A Scleractinian Coral, member of Montlivaltiidae.
Oppelismilia[19]
  • O. sp.
  • Rotzo
Imprints A Scleractinian Coral, member of Oppelismiliidae.
Pinacophyllum[27]
  • cf. P. sp.
  • Rotzo
Colonial Imprints A Scleractinian Coral, member of Stylophyllidae
Stylophyllopsis[27]
  • S. ex gr. rudis
  • Rotzo
Colonial Imprints A Scleractinian Coral, member of Stylophyllidae
Synastrea[27]
  • S. sp.
  • Rotzo
Colonial Imprints A Scleractinian Coral, member of Synastraeidae

Bryozoa

Genus Species Provenance Material Notes Images

Orbipora[30]

  • O. circumvulvata
  • Sega di Noriglio
Imprints

A Stenolaematan of the family Aisenvergiidae

Brachiopod

Genus Species Provenance Material Notes Images

Gibbirhynchia[31]

  • G. curviceps
  • Sospirolo
Isolated Shells

A Rhynchonellidan, member of Gibbirhynchiinae. Unusual genus in the Mediterranean region, more common on NW Europe

Hesperithyris[28]
  • H. renieri
  • Cornacalda
  • Roveredo
Isolated Shells A Rhynchonellidan, member of Zeilleriidae.

Linguithyris[31]

  • L. aspasia
  • Ballino
  • Sospirolo
Isolated Shells

A Terebratulidan, member of Nucleatidae. Typical Mediterranean region taxon in the Pliensbachian

Liospiriferina[28][31]

  • L. obtusa
  • L. torbolensis
  • Cortina d'Ampezzo
  • Sospirolo
  • Torbole
  • Roveredo
Isolated Shells

A spiriferidan, member of Spiriferinidae.

Liothyrina[29]
  • L. norigliensis
  • Rotzo
  • Sega di Noriglio
  • Cornacalda
Isolated Shells A Terebratulidan, member of Terebratellidae.
Lobothyris[28]
  • L. punctata
  • Cornacalda
  • Roveredo
Isolated Shells A Terebratulidan, member of Lobothyrididae.

Lychnothyris[32]

  • L. rotzoana
  • Sette Comuni
  • Erbezzo
  • Vajo dell'Anguilla
  • Cimoncello di Toraro
  • Campomolon
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]
  • M. mediterranea
  • Val d'Assa
Isolated Shells A Terebratulidan, member of Plectoconchidae.
Plectothyris[28]
  • P.? fimbrioides
  • Cornacalda
  • Roveredo
Isolated Shells A Terebratulidan, member of Loboidothyrididae.

Prionorhynchia[31]

  • P.? flabellum
  • Cortina d'Ampezzo
  • Sospirolo
Isolated Shells

A spiriferidan, member of Spiriferinidae.

Waldheimia[28]
  • W. hexagona
  • Roveredo
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]
  • A. kamarika
  • A. depressaeformis[29]
  • Serrada
  • Albaredo
  • Castel Lizzana
  • Rotzo
  • Cornacalda
Isolated Shells A clam, member of Astartidae.
Extant specimen of the genus
Avicula[30]
  • A. spinicosta
  • Noriglio
Isolated Shells A clam, member of Aviculidae.
Cardinia[29]
  • C. rotzoana
  • Rotzo
Isolated Shells A clam, member of Cardiniidae.
Ceromya[29]
  • C. tirolensis
  • Sega di Noriglio
  • Cornacalda
  • Rotzo
  • Serrada
Isolated Shells A piddock, member of Ceromyidae.

Cochlearites[34][35][36][19]

  • C. loppianus
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv
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]

Cochlearites
Cucullaea[28][29]
  • C. cf. hettangiensis
  • Rotzo
  • Roveredo
Isolated Shells A clam, member of Cucullaeidae.
Extant specimen of the genus
Cypricardinia[29][30]
  • C. incurvata
  • C. sp.
  • Noriglio
  • Cornacalda
  • Rotzo
  • Serrada
Isolated Shells A clam, member of Trapezidae.
Cyprina[29]
  • C. candataeformis
  • C. grandiformis
  • Rotzo
Isolated Shells A clam, member of Arcticidae.

Eomiodon[34][35][37]

  • E. serradensis
  • E. baroni
  • E. gardeti
  • E. vulgaris
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv

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]
  • G. messisbugi
  • Column at Main Post Office of Ferrara, Italy
Clavate, smooth borings

Borings over Opisoma shells

Example of Gastrochaenolites

Gervillia[30][29]

  • G. buchi
  • G. lamellosa
  • G. volanensis
  • G. mandriolana
  • G. spp.
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv
  • Noriglio
  • Cornacalda
  • Serrada

Isolated Shells

An Oyster, member of Bakevelliidae. Found on greater accumulations on lower shale-dominated levels

Specimen of the genus

Gervilleioperna[34][35][36]

  • G. ombonii
  • G. sp.
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv

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]

Gervillioperna
Gresslya[30][32]
  • G. elongata
  • Vajo dell'Anguilla
  • Cimoncello di Toraro
  • Campomolon
  • Noriglio
Isolated Shells A clam, member of Ceratomyidae.
Gryphaea[29]
  • G. mimaeformis
  • Rotzo
Isolated Shells A clam, member of Gryphaeidae.
Homomya[28]
  • H. cf. punctifera
  • Sega di Noriglio
Isolated Shells A clam, member of Pleuromyidae.
Lima[28]
  • L. norigliensis
  • L. choffati
  • L. gigantea
  • Cornacalda
  • Sega di Noriglio
Isolated Shells A clam, member of Limidae.
Extant specimen of the genus
Liostrea[28]
  • L. sublamellosa
  • L. sp.
  • Sega di Noriglio
Isolated Shells A oyster, member of the family Flemingostreidae.
Lithophaga[28]
  • L. tirolensis
  • Sega di Noriglio
Isolated Shells A mussel, member of the family Mytilidae.

Lithioperna[34][35][36][19]

  • L. scutata
  • L. spp.
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv
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]

Lithioperna

Lithiotis[27][34][35][36][19]

  • L. problematica
  • L. spp.
  • Altipiano d'Asagio
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv
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]

Lithiotis
Lucina[28]
  • L spp.
  • Val d'Assa
  • Cornacalda
Isolated Shells A clam, member of Lucinidae.
Modiolus[28][29]
  • M. tirolensis
  • M. cf. hillana
  • M. cuneataeformis
  • M. alataeformis
  • M. schaurothi
  • M. tirolensis
  • Rotzo
  • Val d'Assa
  • Val Ghelpa
Isolated Shells A mussel, member of the family Mytilidae.
Extant specimen of the genus

Mytilus[28][34][35][36]

  • M. mirabilis
  • M. bittneri
  • M. lepsii
  • M. transalpinus
  • M. cf. pernoides
  • M. spp.
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Val d'Assa
  • Sega di Noriglio
  • Cornacalda
  • Mandrielle
  • Monte Gaza
  • Ciago bei Verzano
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv
  • Monte Gaza
  • Verzano

Isolated Shells

A mussel, member of the family Mytilidae

Extant specimen of the genus

Opisoma[34][35][24]

  • O. excavatum
  • O. menchikoffi
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv

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]

Pachygervillia[39]

  • P. anguillaensis
  • P. taramellii
  • Vaio dell'Anguilla
  • Vajo del Paradiso
  • Val di Sella
  • Viote section

Isolated Shells

An oyster, member of Plicatostylidae.

Pachygervillia

Pachyrisma[29]

  • P. (Pachymegalodon) chamaeformis
  • P. vaceki
  • P. trigonalis
  • P. (Durga) crassa
  • P. (Durga) nicolisi
  • P. ssp.
  • Bellori
  • Between Pedescala and Castelletto
  • Between Ferrazza and Campodalbero
  • Nosellari
  • Chiesa
  • Carbonare
  • Osteria alla Stanga
  • Between Chiesa S.Martino and Zaffoni
  • Between Boccaldo and Pozza
  • Rovereto
  • Leno di Terragnolo
  • Cimoncello di Toraro
  • Campomolon
  • Folgaria
  • Cornacalda

Isolated Shells

A clam, member of Megalodontidae.

Pecten[28][29]
  • P. norigliensis
  • P. textoriformis
  • P. clathrataeformis
  • P. lens
  • P. cf. norigliensis
  • P. cf. spatulatus
  • Sega di Noriglio
  • Cornacalda
  • Rotzo
  • Mte. Erio
Isolated Shells A scallop, member of the family Pectinidae.
Extant specimen of the genus
Pholadomya[29][32]
  • P. athesiana
  • P. norigliensis
  • Vajo dell'Anguilla
  • Sega di Noriglio
  • Cimoncello di Toraro
  • Campomolon
  • Serrada
Isolated Shells A clam, member of Pholadomyidae.
Specimen of the genus
Pinna[28][29]
  • P. sepiaeformis
  • P. cuneataeformis
  • P. sp.
  • Rotzo
  • Serrada
  • Roveredo
Isolated Shells An oyster, member of Pinnidae.
Extant specimen of the genus
Placunopsis[28]
  • P. italica
  • P. ghelpensis
  • Val Ghelpa
Isolated Shells A scallop, member of the family Anomiidae.
Plicatula[29]
  • P. rotzoana
  • Rotzo
Isolated Shells An oyster, member of Plicatulidae.
Extant specimen of the genus
Pleuromya[30]
  • P. elegans
  • P. gibbosiformis
  • P. jurassiformis
  • P. cf. elongata
  • Sega di Noriglio
  • Cornacalda
  • Rotzo
  • Serrada
Isolated Shells A clam, member of Pleuromyidae.
Protodiceras[32]
  • P. pumilum
  • P. spp.
  • Vajo dell'Anguilla
  • Cimoncello di Toraro
  • Campomolon
Isolated Shells A clam, member of Megalodontidae.

Pseudopachymytilus[34][35][36]

  • P. mirabilis
  • P. spp.
  • Vaio del Paradiso
  • Bellori
  • Vaio dell'Anguilla
  • Campodalbero
  • Pasubio
  • Albaredo
  • Giazzera
  • Valgola
  • Valbona
  • Rotzo
  • Mezzaselv

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]
  • P. volanensis
  • Vajo dell'Anguilla
  • Cimoncello di Toraro
  • Campomolon
Isolated Shells An oyster, member of Pteriidae.
Extant specimen of the genus
Tellina[28]
  • T?. cornacaldensis
  • Cornacalda
Isolated Shells A clam, member of Tellinidae.
Extant specimen of the genus
Unicardium[29]
  • U. abbreviatiforme
  • U. zonariaeforme
  • Rotzo
Isolated Shells An oyster, member of Unicardiidae.

Ammonoidea

Genus Species Provenance Material Notes Images
Androgynoceras[40]
  • A. striatum
  • Vedana near Sospirolo
Shells An ammonite of the family Liparoceratidae.
Androgynoceras

Charmasseiceras[40]

  • C. sp.
  • Serrada, Folgaria

Shells

An ammonite of the family Schlotheimiidae.

Fuciniceras[40]

  • F. suejense
  • F. cornacaldense
  • F. portisi
  • Fontana di Naole
  • Cornacalda, Rovereto

Shells

An Ammonite of the Family Hildoceratidae

Fuciniceras
Harpophylloceras[40]
  • H. eximium
  • Vedana near Sospirolo
Shells An Ammonite of the family Juraphyllitidae.

Juraphyllites[40]

  • J. libertus
  • Contrada Ronchi
  • Vedana near Sospirolo

Shells

Type member of the family Juraphyllitidae.

Juraphyllites
Liparoceras[40]
  • L. (Becheiceras) bechei
  • Vedana near Sospirolo
Shells An ammonite of the family Liparoceratidae.
Liparoceras
Partschiceras[40]
  • P. tenuistriatum
  • P. cf. retroplicatum
  • Vedana near Sospirolo
Shells An Ammonite of the family Phylloceratidae.
Protogrammoceras[41]
  • P. gr. celebratum-italicum
  • P. celebratum
  • P. dilectum
  • Monte Baldo
  • Vedana near Sospirolo
Shells An Ammonite of the family Hildoceratidae.

Gastropoda

Genus Species Provenance Material Notes Images

Anticonulus[42]

  • A. acutus
  • Certosa di Vedana

Shells

A Top Snail of the family Trochidae.

Aptyxiella[28][29]

  • A. norigliensis
  • A. spp.
  • Bellori
  • Between Pedescala and Castelletto
  • Between Ferrazza and Campodalbero
  • Nosellari
  • Sega di Noriglio
  • Chiesa
  • Carbonare
  • Osteria alla Stanga
  • Between Chiesa S.Martino and Zaffoni
  • Between Boccaldo and Pozza
  • Rovereto
  • Leno di Terragnolo

Shells

An snail of the family Nerinellidae.

Ataphrus[42]

  • A. (Ataphrus) latilabrus
  • A. (Ataphrus) cordevolensis
  • Certosa di Vedana

Shells

An snail of the family Ataphridae.

Austriacopsis[42]

  • A. austriaca
  • Certosa di Vedana

Shells

A keyhole limpet of the family Fissurellidae.

Ceritella[29]
  • C. rotzoana
  • Rotzo
Shells An snail of the family Cerithiidae.
Cerithium[29]
  • C. rotzoanum
  • Rotzo
Shells An snail of the family Cerithiidae.
Extant specimen of the genus
Cylindrites[29]
  • C. bullatiformis
  • Rotzo
Shells A barrel bubble snail of the family Acteonidae.

Discohelix[42]

  • D. excavata
  • Certosa di Vedana

Shells

An snail of the family Discohelicidae.

Specimen of the genus

Eucyclidae[42]

Indeterminate

  • Certosa di Vedana

Shells

Incertade Sedis

Eucyclus[42]

  • Certosa di Vedana

Shells

An snail of the family Eucyclidae.

Extant specimen of the genus

Emarginula[42]

  • Certosa di Vedana
  • Val d'Arsa

Shells

A keyhole limpet of the family Fissurellidae.

Extant specimen of the genus

Globularia[43]

  • G. sp.
  • Tonezza del Cimone

Shells

An snail of the family Ampullinidae.

Extant specimen of the genus

Guidonia[42]

  • G. pseudorotula
  • Certosa di Vedana

Shells

An snail of the family Trochonematidae.

Natica[30]
  • N. tridentina
  • N. spp.
  • Albaredo bei Roveredo
  • Noriglio
Shells A moon snail of the family Naticidae.
Extant specimen of the genus
Nerinea[29]
  • N. desvoidyiformis
  • N. norigliensis
  • Rotzo
  • Sega di Noriglio
Shells An snail of the family Nerineidae.

Neritopsis[29][42]

  • N. fabianii
  • N. minulaeformis
  • N. spp.
  • Rotzo
  • Certosa di Vedana
  • Bellori

Shells

An snail of the family Neritopsidae.

Extant specimen of the genus
Patella[30]
  • P. conoidea
  • P. costata
  • P. (Scurria?) tirolensis
  • Noriglio
  • Cornacalda
  • Val d'Arsa
Shells A limpet of the family Patellidae.
Extant specimen of the genus

Plectotrochus[42]

  • P. sp.
  • Certosa di Vedana

Shells

An snail of the family Trochidae.

Pleurotomaria[29]
  • P. obesaeformis
  • Rotzo
Shells An snail of the family Pleurotomariidae.
Specimen of the genus

Proacirsa[42]

  • Certosa di Vedana

Shells

An snail of the family Gordenellidae.

Pseudonerinea[43]

  • P. terebra
  • Tonezza del Cimone

Shells

An snail of the family Pseudonerineidae.

Pseudorhytidopilus[42]

  • P. detonii
  • Certosa di Vedana

Shells

A limpet of the family Acmaeidae.

Rissoina[29]
  • R. acutaeformis'
  • Rotzo
Shells An snail of the family Rissoinidae.
Extant specimen of the genus

Tretospira[29][43]

  • T. tridentina
  • T. morrisiiformis
  • Rotzo
  • Tonezza del Cimone

Shells

A periwinkle of the family Purpurinidae.

Trochus[30]
  • T. sinister
  • Noriglio
Shells A top snail of the family Trochidae.
Extant specimen of the genus
Turritella[29][43]
  • T. rotzoana
  • T. terebra
  • Rotzo
  • Sega di Noriglio
  • Val d'Assa
Shells An snail of the family Turritellidae.
Extant specimen of the genus

Echinodermata

Genus Species Provenance Material Notes Images
Asteriacites[44]
  • A. lumbricalis
  • A. isp.
  • Coste dell'Anglone dinosaur ichnosite
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]
Asteriacites specimen
Hypodiadema[30]
  • H. sp.
  • Noriglio
Sclerites A Pseudodiadematidae Euechinoidean

Polydiadema[45]

  • P. depressum
  • Monte Roite

Two specimens (MCV.20/02 and MCV.20/03)

An Emiratiidae Phymosomatoidan.[45]

Pseudodiadema[28]
  • P. roveredanum
  • P. cobellii
  • P. veronense
  • P. spp.
  • Monte Pombo
  • Sega di Noriglio
  • Albaredo bei Roveredo.
Multiple specimens A Pseudodiadematidae Euechinoidean

Arthropoda

Genus Species Provenance Material Notes Images
Cypris[30][28]
  • C. rotzoana
  • Rotzo
  • Sega di Noriglio
Valves An Ostracodan of the family Cyprididae

Eryma[46]

  • E. (Phlyctisoma) cf.sinemurianum
  • Campomolon, Valbona

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.

Example of Eryma specimen

Klieana[47]

  • K. sp.
  • Tonezza del Cimone

Valves

An Ostracodan of the family Cytherideidae. The earliest record of the genus.[47]

Limnocythere[47]

  • L. sp.
  • Tonezza del Cimone

Valves

An Ostracodan of the family Limnocytherinae. High probability to be a new species of Limnocythere.[47]

Ophiomorpha[46][48]

  • O. irregulaire
  • cf. O. nodosa
  • O. isp. A
  • O.? isp. B
  • Campomolon, Valbona

Burrowing and track Ichnofossils

Burrows of Decapodans

Example of Ophiomorpha trace fossil

Phraterfabanella[47]

  • P. tridentinensis
  • Tonezza del Cimone

Valves

An Ostracodan of the family Cytherideidae. The assemblage is dominated (>95%) by this taxon.[47]

Annelida

Genus Species Provenance Material Notes Images

Schistomeringos[49]

  • S. expectatus
  • Between Ferrazza and Campodalbero
  • Between Nosellari and Dazio
  • Between Virti and Osteria alla Stanga
  • Between Chiesa S. Martino and Zaffoni

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

Extant specimen of the same genus
Serpula[30]
  • S. spp.
  • Noriglio
  • Bellori
  • Castelletto
  • Campodalbero
  • Nosellari
  • Chiesa
  • Carbonare
  • Rovereto
Isolated or accumulated tubes A sessile Annelid of the family Serpulidae.
Example of modern Serpulid Tube

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

Chomatichnus[48]

  • C. wegberensis
  • Campomolon, Valbona

Vertical burrows with preserved entrances

Chondrites[46][48]

  • C. isp.
  • Campomolon, Valbona

Burrowing and track Ichnofossils

Example of Chondrites trace fossil

Glossifungites[48]

  • G. isp.
  • Campomolon, Valbona

Infilled abandoned burrows by coarse-grained skeletal debris

Skolithos[48]

  • S. isp.
  • Campomolon, Valbona

Infilled abandoned burrows by coarse-grained skeletal debris

Representation of Skolithos along the possible makers
.

Thalassinoides[46][48]

  • T. suevicus
  • T.? isp. B
  • Campomolon, Valbona
  • Coste dell'Anglone tracksite
  • Bella Lasta tracksite
  • Stol dei Campiluzzi tracksite
  • Tonezza del Cimone
  • Vajo dell'Anguilla

Burrowing and track Ichnofossils

Example of Thalassinoides specimens
.

Vertebrata

Flora

Bibliography

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