| Calcari di Aurisina | |
| Type: | Geological formation |
| Age: | Santonian-Campanian ~ |
| Period: | Campanian |
| Prilithology: | Limestone |
| Namedfor: | Aurisina |
| Region: | Trieste |
| Coordinates: | 45.8°N 13.6°W |
| Paleocoordinates: | 23.5°N 16.2°W |
| Subunits: | Zolla member |
| Area: | Friuli-Venezia Giulia |
The Calcare di Aurisina (Also known as Aurisina Formation, “Formazione di Monrupino”, Trieste Karst Limestone formation, “Repen formation”, “Sežana formation” and “Lipiza formation”)[1] [2] [3] is a Mesozoic geologic formation in Italy and Slovenia. This limestones are found in the Trieste area and are of Late Cretaceous (Santonian-Campanian) age, being a local record of Carbonate platform limestones, historically quarried by cutting large blocks using steel wire, what has allowed more access to them, as numerous quarries allow excellent exposure.[4] Due to being cut into large blocks and slabs, that usually end stored near the quarries, detailed, three-dimensional study of the rock's composition and fossils can be easily done.[5] [6]
The Aurisina limestone has usually a light grey background, sometimes appearing hazelnut in color. It is known for its high purity, compactness, and uniformity. The quarries where it is extracted consist of thick, solid layers of stone. Different varieties of Aurisina marble are distinguished by shades of grey and the distribution, size, and orientation of the organic remains within the stone. Well-known varieties include Aurisina Fiorita, Aurisina Lumachella, Aurisina Chiara, and Roman Stone, among others.[7] [8]
Aurisina marble's chemical composition and physical properties make it ideal for use in architecture, both for structural and decorative purposes, as well as in statues and monuments. The stone is valued for its durability and aesthetic appeal in various applications.[9]
The Aurisina Limestone has been used since the Roman Republic. Evidence from ancient monuments in Aquileia, a Roman colony founded in 181 BC, suggests that quarrying began in the 1st century BC and continued until the 5th century AD. The stone was widely used in Aquileia for architectural elements, statues, and funerary monuments.[10] [11] The nearby city of Tergeste (modern Trieste) also made extensive use of Aurisina Limestone for public buildings and sculptures. Its use spread across northern Italy, with artifacts found as far as Pavia.
In the post-Roman period, Aurisina marble was notably used in the Mausoleum of Theodoric in Ravenna, built around 520 AD. However, its use declined during the medieval and Baroque periods. In Venice, it was replaced by Istrian stone, but in Trieste, it saw a revival in the 18th century as the city grew following the establishment of the free port by Emperor Charles VI. Notable examples of its use in Trieste include Palazzo Pitteri (1780), the Stock Exchange (1802), and the renovation of the Greek Orthodox Church of San Nicolò dei Greci (1819).[12]
Aurisina Limestone
After Trieste's annexation to Italy in 1918, Aurisina Limestone was used in large-scale projects like the Military Shrine of Redipuglia and Milan's Central Station, where 38,000 tons were utilized. During this period, the marble also reached international markets, being used in Egypt and the United States.
In the post-war era, Aurisina Limestone continued to be popular in foreign markets, with notable projects including the Atlanta subway in the U.S., Berlin airport, and La Défense in Paris. In 1989, it was used for Milan Metro's Line 3. More recently, it has featured in prestigious architectural projects, such as Milan's Citylife Shopping District designed by Zaha Hadid and Turin's Lavazza headquarters. Internationally, it is used in projects across Europe, Asia, Australia, and the U.S.[13]
The formation is characterized by lagoonal facies with episodes of higher energy and rare bivalve patch reefs, such as Chondrodonta and Rudists, which are found throughout the entire unit. The lower section, referred to as the "Zolla member" consists of bivalve-rich limestone, including rudists and Chondrodonta, as well as foraminiferal limestone, often interbedded with dolomitized dark wackestones. In the upper part of this member, pelagic limestone with Pythonella fossils is present.[14] [15] The main body of the Aurisina Limestone is characterized by peritidal carbonates, with some dark laminated facies, dominated by rudists, benthic foraminifera, cyanobacteria (Decastronema), and algae (Thaumatoporella).[16] [17] The Paleoenvironment of this unit is accepted to be a succession of emerged and shallow marine carbonate platform settings, including inner lagoons, high-energy shoals, tidal channels, and rudist accumulations[18] The complex dolomitization and silicification in the region may be linked to a Monsoon climate with alternating wet and dry periods. Comparable dolomitization occurs across the Adriatic Platform, particularly in the Middle-Lower Cenomanian.[19]
The Villaggio del Pescatore site revelated bauxite and coal levels in the surrounding sediment indicate a humid climate. This karst region directed most water underground, limiting surface streams. Fossils of Hadrosaurs were found in a 10-meter layer of laminated limestone within a karst depression, unlike other hadrosauroids typically preserved in fluvial or marine deposits.[20] The site also contains remains of small crocodyliforms, fish, and crustaceans, which suggest fluctuating anoxic conditions that preserved the fossils. This depression likely functioned as a cenote, attracting animals seeking water, where some may have drowned and remained preserved in low-oxygen conditions at the sinkhole's base.
| Genus | Species | Location | Material | Description | Images | |
|---|---|---|---|---|---|---|
| Biradiolites[21] [22] |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Bournonia |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Chondrodonta[25] [26] |
|
| Isolated Shells | Scallop of the family Chondrodontidae | ||
| Durania[27] |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Eoradiolites |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Gorjanovicia |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Hippurites |
|
| Isolated Shells | Rudist of the family Hippuritidae | ||
| Katzeria |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Medeella |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Neithea |
|
| Isolated Shells | Scallop of the family Neitheoidae | ||
| Paronaites |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Praeradiolites |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Rajka |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Radiolites |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Radiolitella |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Requienia |
|
| Isolated Shells | Rudist of the family Requieniidae | ||
| Sauvagesia |
|
| Isolated Shells | Rudist of the family Radiolitidae | ||
| Vaccinites |
|
| Isolated Shells | Rudist of the family Hippuritidae |
| Caridea[29] [30] | Indeterminate |
| Multiple specimens |
| Anguilliformes | Indeterminate | Polazzo | Single complete specimen | This would be the oldest anguilliform found in Italy | ||
| Cypriniformes? | Indeterminate | Polazzo | Several small complete and incomplete specimens | This determination still needs to be confirmed | ||
| Enchodus | Indeterminate |
| Several small complete and incomplete specimens | A member of Enchodontidae | ||
| Holocentridae | Indeterminate | Polazzo | Several small complete and incomplete specimens | Represented mostly by small-sized specimens | ||
| Parachanos | P. ssp. | Polazzo | Several isolated and articulated remains | A member of Chanidae. The attribution to this genus is dubious | ||
| Pycnodontiformes | Indeterminate | Polazzo | Multiple complete specimens and isolated teeth | Some specimens have been referred to the genus Coelodus | ||
| Rhynchodercetis | R. acutissimus | Polazzo | Multiple specimens, complete and incomplete | A member of Dercetidae. The most abundant genus at Polazzo | ||
| Sloveniantriacanthus[33] | S. saksi | Šepulje, east of Tomaj | PMS, VS-001, single specimen | A member of Cretatriacanthidae | ||
| Teleost indet. | Indeterminate |
| Multiple specimens, complete and incomplete, as well isolated teeth and scales |
| Acynodon[34] [35] |
|
| MCNST 57248, A partial skeleton in anatomical connection.Multiple referred specimens: MCNST 57032, MCSNT 57031, MCSNT 57245, MCSNT 21.S239, MCSNT 21.S239 | A small Durophagous crocodrylomorph | ||
| Crocodylia | Indeterminate |
| MCSNT 57033, possibly a rib; MCSNT 57035, mandibular symphysis; MCSNT 57036, anteroposteriorly long vertebra; MCSNT 57037, fragmented ventral osteodermal surface. Referred Multiple teeth |
| Pterosauria | Indeterminate | Villaggio del Pescatore | Specimen number 13450, an alar metacarpal. |
| Coelurosauria[37] | Indeterminate | Križ, southwest of Tomaj | N° BJ 1742 - feather | Referral not confirmed | ||
| Dromaeosauridae | Indeterminate | Kozina, Kras | ACKK-D-8/081, teeth | Resembles other European taxa | ||
| Hadrosauroidea | Indeterminate | Kozina, Kras | ACKK-D-8/20, 121, teeth | Dominant teeth at the locality | ||
| Iguanodontidae? | Indeterminate | Kozina, Kras | ACKK-D-8/25, 8/04, teeth | Resemble Iguanodontid Teeth, but can belong to a convergently evolved Rhabdodontid | ||
| Ornithopoda | Indeterminate | Kozina, Kras | ACKK-D-8/21-Z1, teeth | Different from Rhabdodon | ||
| Tethyshadros[38] | T.insularis | Villaggio del Pescatore | Two nearly complete skeletons, a pair of front legs, a left pubis, a cervical vertebra with a still articulated right cervical rib, a complete but highly deformed skull, a series of caudal vertebrae and isolated dorsal rib. | A small hadrosauromorph dinosaur | ||
| Theropoda indet.[39] | Indeterminate | Villaggio del Pescatore | SC 57030, "arctometatarsalian metatarsal"; Another specimen may represent an epiphysis of a long bone, perhaps of a femur. | |||
| Troodontidae | Indeterminate | Kozina, Kras | ACKK-D-8/088, teeth | Troodontid-alike |
Palynology of the Villaggio del Pescatore section has been studied, dominated by a few gymnosperms and several angiospermous pollen types.
| Araucarites | A.? sp. | Kazlje | Isolated Cones | Conifer cones related with Araucariaceae | ||
| Brachyphyllum | B. spp. | Polazzo | Isolated Branched Shoots | Conifer shots related with Araucariaceae or Hirmeriellaceae. | ||
| Cunninghamites | C. cf. elegans | Polazzo | Isolated Branched Shoots | Conifer shots related with Cupressaceae | ||
| Dicotyledoneae | Indeterminate | Polazzo | Isolated Leaves | |||
| Frenelopsis | F. ssp. |
| Isolated Branched Shoots | A Conifer, member of Hirmeriellaceae. The msot abundant foliar remain locally | ||
| Ginkgoales? | Indeterminate | Polazzo | Isolated Leaves | |||
| Magnoliaephyllum | M. sp. | Kazlje | Isolated Leaves | A Flowering Plant, suggested to belong to Magnoliaceae | ||
| Pagiophyllum | P. ssp. |
| Isolated Branched Shoots | Conifer shots related with Araucariaceae or Hirmeriellaceae. | ||
| Pinophyta[40] | Indeterminate | Villaggio del Pescatore | Isolated Branched Shoots | |||
| Sphenolepis | cf.S. spp. | Polazzo | Isolated Cones | Conifer cones related with Cupressaceae |