Geoconservation Research
2021, Volume 4 / Issue 2 / pages(299-309)
European UNESCO Geoparks: Review Article
1 Idrija UNESCO Global Geopark (Idrija Tourism Board), Mestni trg 2, 5280 Idrija, Slovenia
2 Slovenian Museum of Natural History, Prešernova cesta 20, 1000 Ljubljana, Slovenia
Mojca Gorjup Kavčič Idrija UNESCO Global Geopark (Idrija Tourism Board), Mestni trg
2, 5280 Idrija, Slovenia
ORCID: 0000-0003-4619-7163
Email:mojca.gorjup-kavcic@ geopark-idrija.si
Abstract
Geoheritage interpretation.
Article information | |
Received: 2020-11-12 Accepted: 2021-06-22 DOI: 10.30486/GCR.2021.1914835.1064 How to cite: Gorjup Kavčič M & Križnar M (2021). The ammonite Tirolites idrianus: A paleontological icon of the Idrija UNESCO Global Geopark (Slovenia). Geoconservation Research. 4(2): 299-309. doi: 10.30486/gcr.2021.1914835.1064 Geoconservation Research e-ISSN: 2588-7343 p-ISSN: 2645-4661 © Author(s) 2021, this article is published with open access at http://gcr.khuisf.ac.ir |
The town of Idrija (Slovenia) is best known for its mercury mine. It was an important economic center from the discovery of its mercury deposit in 1490 to the closure of the mine in the 1990s, and the driving force behind both local and glob- al development. The mercury of Idrija was ex- ported to South America in the 16th century to be used as an amalgamation reagent to procure gold and silver. The mine was also the primary reason why Idrija was home to several Europe- an naturalists, such as Giovanni Antonio Scopo- li, Balthasar Hacquet, Johann Jacob Ferber, and others. They were interested both in the mercury deposit as well as the natural world of the Idrija region. They discovered and documented numer- ous fossils, plant and animal species, and created the first geological maps of the area, setting the foundations of modern natural sciences in Slove- nia. It should be noted that most of modern-day Slovenia were part of the region of Carniola in the Habsburg Monarchy, which meant that these early natural scientists had a wide network of correspondents.
The heritage of mercury in Almadén and Idrija has been inscribed in the UNESCO World Heritage List, but it is equally important to consider the her- itage of some of the naturalists who researched in Idrija. We focus on an ammonite discovered in the Idrija region in 1863 by the Austrian paleontolo- gist Franz Ritter von Hauer, who documented the species and named it Tirolites idrianus after Idrija. Because of its name and the fact that it represents the index fossil for the period between 252.3 and
247.2 million years ago, it has been included in the exhibition titled “Written in the Rocks” at the Idrija Geopark Visitor Centre.
The exhibition shows the role of Idrija in the development of natural science and explains the origins of the Tirolites idrianus fossil, which has also inspired works of art (as a lace motif, for instance) and the design of various geoprod- ucts.
Tirolites idrianus (Hauer, 1865) and its Paleon- tological Background
The Idrija UNESCO Global Geopark is charac- terized by a rich natural and cultural heritage that makes the area one of the most interesting parts of Slovenia. Its unique location at the crossroads of the Julian and Dinaric Alps explains its extreme- ly varied and divergent terrain, with deep ravines, vast plateaus, and high peaks. The most important natural resource in the Idrija Geopark is the Idrija mercury deposit along with Anthony’s Main Road, part of the closed-down Idrija mercury mine. To- day it is a tourist attraction, allowing visitors to learn about different types of cinnabar ore, native mercury, and mining methods, both traditional and modern (Čar 2010; Peljhan et al. 2011).
The geological structure of the area is extremely varied, with fossils dating back as far as 360 to 45 Ma. Erosion has revealed numerous natural phe- nomena formed by vast tectonic shifts, the most obvious being the Idrija Fault, along which a deep valley has formed (Čar 2010; Peljhan et al. 2011; Gorjup Kavčič 2012).
Throughout history, these phenomena spiked the interest of numerous scientists who traveled to Id- rija in connection with the mercury mine and used their knowledge to set the foundations of natural sciences in Slovenia. They discovered and docu- mented new plant and animal fossil species. Some fossils were first discovered and documented in Idrija or its surroundings, and were also named after the town, including the megalodontid mol- lusk Triadomegalodon idrianus Vegh-Neubrandt (Cigale et al. 1976) and the ammonite Tirolites idrianus (Hauer 1865) (Fig. 1), which is the focus of this article.
Tirolities idrianus inhabited warm and shallow waters of the Neotethys Ocean (Fig. 2) in the Ear- ly Triassic (252.3–247.2 Ma), when Neotethys formed an extensive gulf into the eastern shores of Pangea, causing the supercontinent to start break- ing apart. The Early Triassic was characterized
Figure 1. Original illustration of Tirolites idrianus
(from Hauer 1865).
by intense development of carbonate and evapo- rite-carbonate platforms (continental shelves) ex- tending between latitudes 40–54° North and 40– 50° South, along the eastern and western coasts of Pangea and the microcontinent Cimmeria (Žalo- har 2010). Besides Tirolites idrianus, other spe- cies from the Early Triassic commonly found in the Idrija Geopark include the bivalve Pseudomo- notis (Eumorphotis) lipoldi and the ammonites Ti- rolites cassianus and Tirolites mercurii (Table 1).
In later parts of the Triassic, vast carbonate plat- forms were formed mostly at the edges of the Neotethys and Paleotethys Oceans, and the Cim- merian plate (Golonka 2007; Žalohar 2010). Algal
and coral reef limestones were formed, as well as shallow water platform limestones and dolomites; these are also present in the Idrija region, where the aforementioned Middle Triassic rocks contain fossils of the ammonites Trachyceras idrianum and Joannites deschmani, the bivalve Posidonia idriana, and the brachiopod Lingula lipoldi. The Late Triassic of the Idrija Geopark also contains a varied array of bivalves, including Myophoria kefersteini, Pachycardia rugosa, and Triadomeg- alodon idrianus (Table 1).
The ammonite Tirolites idrianus from the Idri-
Figure 2. A reconstruction of the palaeoenvironment with Ti- rolites idrianus during the Early Triassic period; Legend: 1 – ammonites Tirolites idrianus, 2 – crinoids (Holocrinidae), 3 – bivalvia Costatoria costata, 4 – fish bone remains, 5 – ichnofossil Rhizocorallium sp. (Depiction: Matija Križnar, 2011)
Table 1. A selected list of Triassic marine fossils from the vicinity of the Idrija Geopark. Data from Hau- er 1865; Mojsisovics 1882; and Pleničar et al. 2009.
Epoch | Fossil | |||||
Bivalvia | Gastropoda | Ammonites | Corals | Brachiopoda | Ichnofossil | |
Upper Triassic | Myophoria kefersteini | Trachyceras aon | Volzeia badiotica | |||
Pachycardia rugosa | Protrachyceras rutorarum | |||||
Hoernesia bipartita (=Gervillia bipartita) | ||||||
Neomegalodon triqueter | ||||||
Triadomegalodon idrianus | ||||||
Middle Triassic | Daonella lommeli | Protrachyceras archelaus | cf. Discina sp. | |||
Daonella (Arzelella) cf. tripartita | Trachyceras idrianum | Lingula lipoldi | ||||
Posidonia wengensis | Trachyceras julium | |||||
Posidonomya idriana | Joannites deschmani | |||||
Arcestes (Proarces- tes) esinensis | ||||||
Arpadites arpadis | ||||||
Reitziites reitzi | ||||||
Megaphyllites oenipontanus | ||||||
Lower Triassic | Costatoria costata | Werfenella rectecostata | Tirolites idrianus | Rhizo- corallium jenense | ||
Claraia claraia | Natiria costata | Tirolites carniol- icus | ||||
Pseudomonotis (Claraia) aurita | Tirolites cassianus | |||||
Pseudomonotis (Eumorphotis) lipoldi | Tirolites mercurii | |||||
Anodontophora (Mya- cites) fassaensis | Dinarites mu- chianus | |||||
Dinarites cf. dalmatinus | ||||||
ja region was first documented by Hauer (1865) (Fig. 1), who named it Ceratites idrianus. As its type locality, he listed the settlement of Zagodov Vrh (Fig. 3) to the southeast of Idrija (Hauer 1865; Mojsisovics 1882). The status of Zagodov Vrh as
a type locality can be inferred based on a docu- mented and illustrated case of a Tirolites idrianus discovered at this location (Hauer 1865). Howev- er, the exact location and collection of this holo- type are unknown.
As other locations in the Idrija region where Tirolites idrianus is present, Hauer (1865) lists a ravine south of Lazec above the Idrijca Riv- er Valley and the settlement of Izgorje near Žiri (Fig. 3). After extensive studies and comparisons of numerous specimens, Mojsisovics (1882) di-
vided the genus Ceratites into three new genera, Ceratites, Dinarites, and Tirolites. He renamed the idrianus species as Tirolites idrianus and classified the specimens with a wider cross-sec- tion as a new species, Tirolites mercuri (Cigale 1977).
Figure 3. A simplified geological map of the Idrija UNESCO Global Geopark with the main locations of Tirolites idrianus (the geological map was adapted from Buser & Draksler 1993).
Tirolites idrianus is characterized by conspicuous ribs and by 2–5 (usually 3–4) spines and/or nodes on the last whorl (Posenato 1992) (Fig. 4). The shell of Tirolites idrianus is less involute com- pared to Tirolites carniolicus. It has a narrower cross-section and a faster growth process of the whorls that differentiates the species Tirolites id- rianus from Tirolites mercurii (Mojsisovics 1882;
Cigale 1977). Posenato (1992) reviewed Tirolites from the Dolomites (Italy), Bakony (Hungary), and Dalmatia (Croatia). He categorized Tirolites idrianus as one of the younger species from the Early Triassic, along with Tirolites carniolicus (Posenato 1992), which is characterized by a larger shell with fewer spines/nodes on the final whorl.
Figure 4. Ammonite fossil of the species Tirolites idrianus from Vrsnik, Bojan Režun’s private collection, Idrija. (Photo: Jani Peternelj, CUDHg Archive, 2012)
Tirolites is one of the most important ammonite remnants from the upper parts of the Early Tri- assic layers in Slovenia. Numerous species have been identified, such as Tirolites cassianus, Ti- rolites spinosus, Tirolites carniolicus, Tirolites haueri, and Tirolites stachei (Pavšič 2003). In the Idrija Geopark, several specimens of Tirolites id- rianus have been found in the area of Vrsnik (Fig. 3), including the ammonite in Figure 4, part of the private collection. Aside from the Vrsnik site, Ti- rolites idrianus fossils have also been discovered on the Ledine Plateau (Fig. 5) and in Zagodov Vrh, southeast of Idrija (Fig. 1).
In Slovenia, based on the legislation on the desig- nation and protection of valuable natural features (The Official Gazette of the Republic of Slovenia 111/04, 70/06, 58/09, 93/10, 23/15, and 7/19),
cephalopod fossils are treated as valuable natural features if more than half of their shell or half of their cast is preserved.
The Idrija Geopark currently has no ammonite fossil site with a natural value status. The ammo- nite finds in the Idrija Geopark are kept in private collections, so there is no clear overview of the actual number of finds. In addition, many ammo-
Figure 5. An ammonite fossil of the species Tirolites idri- anus from the Ledine fossil site. Private collection of Go- ran Velikonja, Idrija. (Photo: Matija Križnar 2009)
nite fossils are not classified by experts, which possibly leads to them being misclassified as am- monites of other species, e. g. Tirolites cassianus.
European scientists, who moved to Idrija because of the mercury mine, focused their research not only on their work in the mining activities but also on the area of Idrija in general. In this peri- od, the first geological maps of the region were made, numerous fossils were discovered, and the local fauna and flora were documented. It is known that Johannes Antonius Scopoli, who worked for the mine as a doctor between 1754 and 1769, corresponded with Carl Linnaeus (So- ban 2004), the father of modern taxonomy. To- gether, they classified numerous plant and ani- mal species. In the 18th century, Idrija was thus a
town where the foundations of Slovenian natural sciences were set.
After the closing of the mine in 1995, Idrija lost its global importance as a source of mercury. Howev- er, from an economic point of view, the town did not suffer because of the rise of two large technol- ogy companies. Today, the heritage of the mercury mine is maintained by the Centre for the Conser- vation of the Mercury Heritage of Idrija (CUD- Hg Idrija), while the conservation, interpretation and promotion of the natural heritage of the whole Idrija region fall to the Idrija UNESCO Global Geopark, which organizes a wide range of activi- ties to present the natural and cultural heritage of Idrija to visitors. In 2019, the Idrija Geopark es- tablished a Visitor Centre, where many geological treasures of Idrija are on display, including Tiro- lites idrianus (Fig. 6).
Figure 6. The Tirolites idrianus ammonite featured in the exhibit titled “Written in the rocks” in the Idrija Geopark Visitor Center. (Photo: Bojan Tavčar 2020)
Tirolites idrianus may not be as spectacular as other ammonite fossils, but it had a key role in the development of the natural sciences in Slo- venia. Further, it is the index fossil for the Tiro- lites-Columbites Assemblage Zone of the Oleneki- an (early Spathian) in the Early Triassic, a zone that is recognized worldwide, from Europe to Asia (Russia, China, Japan, Vietnam).
The index fossils are characterized by the fact that they lived in a relatively short time in a geologi- cal period, but they inhabited a rather large living environment. Based on their findings in a specific rock, we can accurately determine the age of the rock.
Slovenian legislation, namely the Nature Conser- vation Act, does not mandate reporting finds to the Institute of the Republic of Slovenia for Nature Conservation nor does it address the possibility
of reclamation, adequate conservation, and pro- tection of small-scale Tirolites idrianus fossil sites in Idrija. For this reason, the fossil sites are not documented on any tourist map and are not widely known, so neither independent nor guided tours of the Tirolites idrianus sites are currently possible in the Idrija Geopark. The Tirolites idrianus ammo- nite and its story are described in the new exhibit titled “Written in the rocks” at the Idrija Geopark Visitor Centre. The exhibit also features a replica of the ammonite fossil find from Ledine (Fig. 5). Tirolites idrianus is also frequently the focus of various educational activities and workshops we organize for schools or other educational institu- tions. Through a short presentation, the students learn what fossils are and how they are formed. They also learn about the characteristics of am- monites and the role Tirolites idrianus played in the history of Idrija. At the end of the workshop, the students craft their souvenirs (e.g., refrigerator magnets, brooch pins, pendants, earrings) in the
shape of the ammonite (Fig. 7). The models used are replicas of actual fossil finds from Idrija area. Such replicas of the Tirolites idrianus ammonite fossils could perhaps be sold as a geoproduct at the Idrija Geopark Visitor Centre or serve as a basis for the development of geoproducts for the
collective “Idrija – selected” trademark (“Idrija – izbrano” in Slovenian), which was established in 2018. The trademark includes products based on innovative techniques, quality, tradition, and local heritage.
Figure 7. A workshop for crafting plaster cast replicas of the Tirolites idrianus ammonite. (Photo: Mojca Gorjup Kavčič 2020)
The Idrija Lace School, the role of which is to con- serve the lace-making tradition of Idrija, has includ- ed the ammonite motif in its lace-making curricu- lum. The ammonite-shaped pattern is copyright of the Idrija Lace School and is available to all stu- dents who wish to make an ammonite-shaped lace in the course of their studies (Fig. 8).
greater problem is posed by private collectors who independently carry out fossil hunts to find specimens for their private collections and do not (and are not obligated to) report their dis- coveries to the relevant research institutions. In certain cases, rumors of a fossil site spread in the fossil collector community, which leads to the fossil site being depleted. In terms of leg- islation, these issues are still very loosely reg- ulated in Slovenia, which is why it is necessary to amend the Nature Conservation Act to cover such cases as well.
Figure 8. Idrija lace in the shape of an Ammonite. Lacemaker: Ana Fajdiga, Idrija Lace School, Unit of Vipava. Mentor: Katarina Mlakar. (Photo: Bojan Tavčar 2019)
Another problem is the scientific classification of the fossil finds. As already mentioned, it is possi- ble to discriminate between Tirolites idrianus and Tirolites mercuri, but it is unclear whether amateur collectors regularly discriminate between these two species.
So far, there has been no systematic overview and exact documentation of the discovered specimens. The Idrija Geopark is of course in favor of a sys- tematic solution to this issue, but this has not yet been done. The idea is to organize a workshop with all the private collectors to create a registry of private collections and document their miner- als and fossils. The success of such a workshop is of course questionable as many collectors do not wish to present their finds to the public, particu- larly those who have had previous negative expe- riences.
In the 18th century, Idrija was a town where the foundations of Slovenian natural sciences were set. Today, it plays a different role, with new po- tential. Mining ended in the 1990s, and since then,
its institutions have turned to the protection, inter- pretation, and promotion of its heritage. The her- itage of the Idrija mercury mine was inscribed on the UNESCO World Heritage List in 2012, along with the mercury mine in Almadén, Spain. The region of the Municipality of Idrija, with its nat- ural and cultural heritage and its manner of repre- senting and connecting diverse rural stakeholders, was granted the status of a European and global geopark in 2013 and was declared a UNESCO Global Geopark in 2015. All these titles confirm that the region of Idrija is unique in a global sense. The importance of the Tirolites idrianus ammonite in the Idrija Geopark lies in the fact that the find serves as a basis to educate visitors on the role of Idrija in the development of natural sciences in Slovenia, as well as the importance of the mercury mine for the development of the world in general. This creates excellent conditions for the develop- ment of geotourism and geoproducts, both artisan products and experiences, which are particularly popular today. Some of these ideas have already been realized in the Idrija Geopark Visitor Centre and through different workshops, but some ambi- tious plans remain for the future.
The authors declare that there is no conflict of in- terest in their work.
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