Southeastern Alps Research Articles

An integrative taxonomic study reveals carychiid microsnails of the troglobitic genus Zospeum in the Eastern and Dinaric Alps (Gastropoda, Ellobioidea, Carychiinae)

The minute snails of the troglobitic genus Zospeum are known from the southeastern Alps through the Dinarides and from the Pyrenees to the Cantabrian Mountains. The majority of Zospeum has been described from the northernmost region of Southeast Europe, the geographical focus of our study. The taxonomic value of the few available morphological shell characters has been debated for nearly as long as the genus is known. Recent results of genetic studies questioned the established taxonomic system based on morphological characters in the 1970s, with one species (Z. isselianum) appearing to be polyphyletic. Here, we present a comprehensive revision of Zospeum from the Alpine and Dinaride regions, using an integrative approach including genetic methods, morphometry, X-ray micro computer tomography (micro-CT), and SEM. We reveal 25 species and describe 5 new to science. Genetic analysis separated the genus into five clades, strongly challenging the previously valid taxonomic system and revealing several species polyphyletic. The various methods used for morphological characterization often proved useful in separating species showing high incidence of cryptic speciation in the genus. Radular investigation, using SEM, uncovered new insights about the taxonomic value of the configuration of the radular ribbon within Zospeum as well as Zospeum’s dentitional affinity within the Ellobioidea.

Altitudinal Shift of Tetrao urogallus in an Alpine Natura 2000 Site: Implications for Habitat Restoration

Capercaillie (Tetrao urogallus L.), a territorial galliform species, is known to prefer mature conifer stands with canopy gaps and a vigorous understory of ericaceous species. Capercaillie is a useful umbrella species that has recently shown declining population trends and distribution changes in its southern geographic range. We aim to identify and assess the possible changes in summer capercaillie habitat selection between 2001 and 2011 in the Scanuppia Natura 2000 site (south-eastern Alps). The area is dominated by spruce (Picea abies (L.) Karsten) forests, followed by mixed forests, scrub, and open habitats. In both years, summer presence–absence of capercaillie was verified through the detection of droppings over 10 m radius circular plots located along contour lines (1500–1800 m). A set of environmental and habitat features was also surveyed. While overall population numbers remain unchanged over the surveyed period, results have shown an altitudinal shift in capercaillie distribution. Habitat variables had a stronger effect on the presence of capercaillie in 2001 than in 2011. Land cover and climate change are likely among the drivers of the shift in altitudinal distribution. This confirms the relevance of habitat restoration actions and to monitor changes in factors explaining capercaillie habitat selection.

On the interactions between airflow and ice melting in ice caves: A novel methodology based on computational fluid dynamics modeling

Motivated by progressive climate-change influence on ice degradation in caves, in this paper we present a novel methodology to investigate the link between air dynamics and ice melting. Specifically, we use surveys available for the Leupa ice cave (LIC), located in the Canin-Kanin group in the southeastern Alps and a general purpose computational fluid dynamics model (CFD). Detailed numerical simulations are evaluated on the basis of well-established approaches that consider domain, grid, boundary-conditions, turbulence closure models, buoyancy effects, porous media properties and verification with measured data. External atmospheric conditions are the main trigger for internal circulation but morphology and thermal characteristics of ice and bedrock induce a dynamical process of heat exchange ultimately responsible for ice melting. This process is generally poorly documented in real conditions. Using CFD analyses we show that both in summer and winter, warm and cold air currents within the cave are “disturbed” by several vortices and stagnation zones which locally modify the energy balance. To account for this we introduce a macroscopic physical model based on energy balance between ice surfaces and the inner ice cave airflow to determine the heat exchanged between ice and air. Using this model, a prediction of ice thickness decay over time is obtained. In the case of LIC a reduction of initial 4 cm per year is first obtained with projection of a much faster increase. The methodology is general and easily extendable to other sites, proving to be a powerful method to estimate ice evolution in caves induced by external and internal forcing.

Hiding deep underground - two new subterranean beetle genera for Slovenia

By offsetting the discipline of speleobiology with the discovery of the first subterranean beetle Leptodirus hochenwartii, Slovenia became the country with the longest tradition of speleobiological research. Subterranean beetles have been an undepletable study subject for almost two centuries, giving the impression that not much novelty is expected in beetle fauna. However, recent discoveries of two new beetle genera for Slovenia, one of them even being a new genus for science, have put this view into a new perspective. With the development of caving techniques and growing interest for surveying deep vertical caves, also the intensity of speleobiological studies of these caves gradually increased. So, it was only in 2017, that the first specialized, hygropetric beetle, was found in Slovenia. In Southern part of the country, a sole female specimen from genus Croatodirus (fam. Leiodidae), probably belonging to a new species, was collected from a cave in Mt. Snežnik, at depth of 475 m. Second, in the same year, even more spectacular finding came from the Southern Calcareous Alps. During sampling of a cave on Mt. Raduha, a peculiar and highly troglomorphic Trechinae (fam. Carabidae) was found at depth 450 m, near the cave hygropetric. Thorough morphological examination of a single male collected revealed characters similar to the ones known in the Southern Dinaric Scotoplanetes - genus known to inhabit the cave hygropetric. However, when the newly discovered genus was put into Alpine Trechinae phylogenetic framework, its sister relation with a narrow-endemic genus Aphaenopidius was revealed. Such rare and occasional findings raise questions regarding the completeness of our knowledge on alpha taxonomy and the mechanisms underlying convergent evolution in the subterranean realm. Poster: Suppl. material 1

Trace and Rare Earth Elements chemistry of detrital garnets in the SE Alps and Outer Dinarides flysch basins: An important tool to better define the source areas of sandstones

Abstract Garnet is one of the most abundant heavy minerals present in the Cretaceous – Eocene flysch deposits of the Southeastern Alps and Outer Dinarides (Julian, Brkini and Istrian basins). About 300 detrital garnets from the Cretaceous-Eocene flysch deposits of the Southeastern Alps have been analysed by means of electron microprobe and LA-ICP-MS. In the Julian and Istrian basins, supplies are from amphibolite-facies rocks and mafic and ultramafic metamorphic rocks, while in the Brkini basin the latter are almost missing. Moreover, in the Julian and Istrian basins, supplies from skarns, very low-grade metabasites, or from ultra-high temperature metamorphosed calc-silicate granulites are present. Among these different groups, LA-ICP-MS analyses showed that trace element content can be very different in almandine-rich garnets from the different sources. In particular, the source that supplied the Julian Basin is significantly different from that of the Istrian Basin. From the Cretaceous to the Palaeocene the main supplies of Bi-type garnets derived from an area where feldspar-free garnet-bearing rocks were exposed. Successively, Bi-type garnets were supplied from an area where feldspar-garnet-bearing rocks were exposed. The presence of garnets from feldspar-free garnet-bearing rocks in the Brkini and Istrian basins can be ascribed to both recycling of material from the Julian Basin as well as direct input from the same areas that supplied the Julian Basin.

Diversification of Cerastium sylvaticum and C. subtriflorum on the margin of the south-eastern Alps

The south-eastern Alps and the southerly adjacent areas are considered an important refugium for plant species during the Pleistocene glaciations; consequently, they harbour many endemic taxa. One of them is Cerastium subtriflorum, which in this area occurs sympatrically with morphologically similar, but more widespread C. sylvaticum. Here, we used amplified fragment length polymorphisms as well as ITS and plastid DNA sequences to explore phylogenetic relationships between the two species as well as their relationships to other Cerastium taxa previously deemed closely related. Our data show that both species are genetically well-differentiated sister taxa, but their relationship to other taxa remains unclear; both species rather form an independent evolutionary lineage within European Cerastium. Cerastium sylvaticum exhibits low genetic differentiation among populations in the investigated area, suggesting a single Pleistocene refugium in that part of Europe. The much more pronounced genetic differentiation within C. subtriflorum is likely a result of multiple Pleistocene refugia or more recent vicariance among the three disjunct partial distribution areas. Phylogenetic sequence data suggest hybridisation between the two taxa, resulting in a discordant phylogenetic position between ITS and plastid trees of one population of C. subtriflorum. Flow cytometric and multivariate morphometric analyses show that C. subtriflorum and C. sylvaticum differ in their genome size as well as in multiple morphological traits. We provide a taxonomic treatment for both species including an identification key and species descriptions.

Phytosociological analysis of European larch forests in the Southeastern Alps

Abstract Using the (unweighted) average linkage clustering (UPGMA) method we classified 458 phytosociological relevés of Larix decidua forests in the Southeastern Alps into 25 clusters. Based on their analysis we described the following new subassociations: Rhodothamno-Laricetum deciduae geetosum rivalis, sorbetosum chamaemespili, piceetosum abietis, adoxetosum moschatellinae, cystopteridetosum fragilis, cyclaminetosum purpurascentis, dryadetosum octopetalae and sorbetosum ariae. The selected method proved adequate in identifying the differences between larch stands on potential subalpine spruce and beech sites, and larch forests on the upper forest line, as well as the differences between initial larch stages on the upper forest line and more stable development stages on better developed soils on promontories and ledges above the upper beech forest line. Larch forests occur mainly in the altitudinal belt between (1,500) 1,600 and 1,800 (1,900) m, on shady aspects and slopes that are steeper than 30°. They are some of the best preserved forest types in the Southeastern Alps, on smaller surface areas (Macesnje above the Beli Potok valley in the Julian Alps) even virgin forests, and their role as biotopes is exceptional.

Phylogeography, genetic structure and wing pattern variation of Erebia pronoe (Esper, 1780) (Lepidoptera: Nymphalidae) in Europe.

The distribution of genetic diversity within Erebia pronoe (Esper, 1780) populations in relation to biogeographic ranges is essential for understanding the processes of evolution, speciation and phylogeography in this species. A certain degree of genetic variability was expected because of the species' linkage solely to calcareous soils. These ideas were focused on the water ringlet E. pronoe, a European endemic montane butterfly distributed over a narrow area of mountains, with its occurrence dependent on nutrient plants. Therefore, the origin, occurrence, phylogeography and variability are described in defined mountain localities in Europe in the light of glaciation events that occurred during the Quaternary (Pleistocene) period. The species' phylogeography is based on a combination of two mitochondrial genes (COI, CR) and morphology (wing morphometry). The study comprised samples from the Western Carpathians, Pyrenees, Alps, South-Eastern Carpathians (Romania) and Southern Limestone Alps (Slovenia). Moreover, the species' remarkable phylogeographic structure was observed, including four morphologic lineages and divergent genetic lineages. These lineages cover the Carpathian Mountains as well as the Western European mountains (Spanish populations) with no apparent gene flow between most regions, even across distances of only hundreds of kilometres.

Sedimentary evidence of glacial lake outburst floods (GLOFs) during the last glacial maximum in the Venetian-Friulian plain (NE Italy)

The outwash rivers of the Venetian-Friulian plain promoted a high-rate aggradation during the Last Glacial Maximum (LGM), with large sedimentary bodies fed by major glaciers along the south-eastern side of the Alps. Glaciers were temperate-type, hold up by high precipitation rates and characterized by large amount of water trapped in subglacial lakes or funneled in speedy streams. The stratigraphic analysis of these sedimentary bodies showed sharp changes from coarse gravels to well-sorted sandy gravels few kilometers downstream. Large boulders, 1–2 m in size, are present in many sites, especially in the Tagliamento outwash plain, from the end-moraine system to about 13 km far to the south. Most of the boulders are located on the eastern area of the sandur and lie stratigraphically above a paleosol, radiocarbon dated to 31,114 ± 643 cal a BP, thus belonging to the LGM sandur of the Tagliamento glacier. In some locations these boulders are associated to large bars, showing a rough cross-bedding. Similar sedimentary structures are observed 2 km downstream of the LGM frontal moraines in the Astico outwash system, a 25-km-long transfluence tongue of the Adige-Brenta glacial complex. In this case the occurrence gravel dunes containing many boulders marks the evidence of a high-energy deposition. The occurrence of cross-bedded bars, embedding large boulders up to 2 m of diameter, in the piedmont plain of the south-eastern Alps is peculiar. Breaks of natural dams, such as the frontal moraines or the glacier itself, may have triggered glacial lake outburst floods (GLOFs) that determined the formation of such gravel bars with meter-size clasts.

Three mires in the south-eastern Alps (northern Italy)

ABSTRACTHigh-resolution vegetation maps, at 1:500 scale, were realized in three mires located in the Italian south-eastern Alps (Coltrondo West, 12,800 m2; Coltrondo South, 22,300 m2 and Palù di sotto, 50,600 m2). Vegetation maps were based on topography surveyed by GPS, performed on ground surveys and produced using ArcGIS 9.1. A total of 36 plant communities, whose distribution was reported on the maps, were individuated and classified according to the Braun-Blanquet method. The mires strongly differed from each other with regard to vegetation cover, with Coltrondo West having a prevalent bog-like vegetation and Coltrondo South a prevalently fen-like vegetation. At Palù di sotto, bog-like vegetation covered a surface fed by ground water. This pattern could be explained by the lowering of water table determined by intensive water extraction for human activities. The maps will be profitably used as reference for future monitoring of vegetation dynamics under changing climatic and landuse conditions.

Three mires in the south-eastern Alps (northern Italy)

High-resolution vegetation maps, at 1:500 scale, were realized in three mires located in the Italian south-eastern Alps (Coltrondo West, 12,800 m 2 ; Coltrondo South, 22,300 m 2 and Palu di sotto, 50,600 m 2 ). Vegetation maps were based on topography surveyed by GPS, performed on ground surveys and produced using ArcGIS 9.1. A total of 36 plant communities, whose distribution was reported on the maps, were individuated and classified according to the Braun-Blanquet method. The mires strongly differed from each other with regard to vegetation cover, with Coltrondo West having a prevalent bog-like vegetation and Coltrondo South a prevalently fen-like vegetation. At Palu di sotto, bog-like vegetation covered a surface fed by ground water. This pattern could be explained by the lowering of water table determined by intensive water extraction for human activities. The maps will be profitably used as reference for future monitoring of vegetation dynamics under changing climatic and landuse conditions.

Testing the Hydrological Coherence of High‐Resolution Gridded Precipitation and Temperature Data Sets

AbstractAssessing the accuracy of gridded climate data sets is highly relevant to climate change impact studies, since evaluation, bias correction, and statistical downscaling of climate models commonly use these products as reference. Among all impact studies those addressing hydrological fluxes are the most affected by errors and biases plaguing these data. This paper introduces a framework, coined Hydrological Coherence Test (HyCoT), for assessing the hydrological coherence of gridded data sets with hydrological observations. HyCoT provides a framework for excluding meteorological forcing data sets not complying with observations, as function of the particular goal at hand. The proposed methodology allows falsifying the hypothesis that a given data set is coherent with hydrological observations on the basis of the performance of hydrological modeling measured by a metric selected by the modeler. HyCoT is demonstrated in the Adige catchment (southeastern Alps, Italy) for streamflow analysis, using a distributed hydrological model. The comparison covers the period 1989–2008 and includes five gridded daily meteorological data sets: E‐OBS, MSWEP, MESAN, APGD, and ADIGE. The analysis highlights that APGD and ADIGE, the data sets with highest effective resolution, display similar spatiotemporal precipitation patterns and produce the largest hydrological efficiency indices. Lower performances are observed for E‐OBS, MESAN, and MSWEP, especially in small catchments. HyCoT reveals deficiencies in the representation of spatiotemporal patterns of gridded climate data sets, which cannot be corrected by simply rescaling the meteorological forcing fields, as often done in bias correction of climate model outputs. We recommend this framework to assess the hydrological coherence of gridded data sets to be used in large‐scale hydroclimatic studies.

Constituents of the Essential Oils of Heracleum austriacum subsp. siifolium, an Endemic Plant of the Southeastern ALPS

Constituents of the Essential Oils of Heracleum austriacum subsp. siifolium, an Endemic Plant of the Southeastern ALPS

3-D structure of the crust and uppermost mantle at the junction between the Southeastern Alps and External Dinarides from ambient noise tomography

3-D structure of the crust and uppermost mantle at the junction between the Southeastern Alps and External Dinarides from ambient noise tomography

Landscape metrics as functional traits in plants: perspectives from a glacier foreland.

Spatial patterns of vegetation arise from an interplay of functional traits, environmental characteristics and chance. The retreat of glaciers offers exposed substrates which are colonised by plants forming distinct patchy patterns. The aim of this study was to unravel whether patch-level landscape metrics of plants can be treated as functional traits. We sampled 46 plots, each 1 m × 1 m, distributed along a restricted range of terrain age and topsoil texture on the foreland of the Nardis glacier, located in the South-Eastern Alps, Italy. Nine quantitative functional traits were selected for 16 of the plant species present, and seven landscape metrics were measured to describe the spatial arrangement of the plant species’ patches on the study plots, at a resolution of 1 cm × 1 cm. We studied the relationships among plant communities, landscape metrics, terrain age and topsoil texture. RLQ-analysis was used to examine trait-spatial configuration relationships. To assess the effect of terrain age and topsoil texture variation on trait performance, we applied a partial-RLQ analysis approach. Finally, we used the fourth-corner statistic to quantify and test relationships between traits, landscape metrics and RLQ axes. Floristically-defined relevé clusters differed significantly with regard to several landscape metrics. Diversity in patch types and size increased and patch size decreased with increasing canopy height, leaf size and weight. Moreover, more compact patch shapes were correlated with an increased capacity for the conservation of nutrients in leaves. Neither plant species composition nor any of the landscape metrics were found to differ amongst the three classes of terrain age or topsoil texture. We conclude that patch-level landscape metrics of plants can be treated as species-specific functional traits. We recommend that existing databases of functional traits should incorporate these type of data.

Biomagnetic monitoring and element content of lichen transplants in a mixed land use area of NE Italy

The aim of this study was to verify whether it is possible to discriminate between the different pollution sources present in a mixed land use area of NE Italy on the basis of the magnetic properties and the element content of lichen transplants. Thalli of Pseudevernia furfuracea were collected in a pristine area of the South-Eastern Alps and exposed for 2months in 40 sites located at the knots of a 700m step grid covering ca. 40km2 of a mosaic of agricultural, forested, industrial and urban areas. In this way, the samples could be analyzed after a defined period of time, and compared to pre-exposure conditions. The post-exposure element content and the magnetic data substantially agreed, revealing a rather modest anthropogenic impact on the territory, mostly limited to an industrial park. Since the magnetic mineralogy was homogeneous throughout the entire set of samples, with magnetite-like minerals as the main magnetic carriers, it was not possible to discriminate between PM originating from the different pollution sources. The contribution given by the industrial park could be confirmed by the multivariate analysis of the element data set. Conversely, it was possible to assess the low environmental impact of the largest local industry, a cement plant, located outside the industrial park. Notwithstanding the relatively short time of the survey, P. furfuracea was proven to be an effective accumulator for biomagnetic monitoring studies, its magnetic properties being excellent proxies for heavy metal pollution even when the anthropogenic impact on the territory is low.

Additional information on the distribution and ecology of the recently described diatom species Geissleria gereckei

Abstract The main objective of this paper is to report new information about the distribution and ecology of a recently described diatom species, Geissleria gereckei. The opportunity for updating the information on the distribution and ecology of the species was provided by the finding of well-developed G. gereckei populations on the lithic material and bryophytes in the Raška and Mlava rivers (Serbia). For several years after the first description, G. gereckei has been known only from the type locality and from another spring in the Dolomiti Bellunesi National Park (the south-eastern Alps). After accurate LM and SEM observations, we provide evidence for the occurrence of the species also in the two above-mentioned rivers in Serbia, as well as in the south-western and south-eastern Alps. After an extensive literature search, it appears that the species is known with certainty only from these sites. Our observations and details from the literature suggest that the species is able to occupy a much broader ecological niche than the very-specific one observed at the time of discovery. The two main determinants for the species’ occurrence appear to be the carbonate nature of the catchments or aquifers, and the ability of the species to be competitive in habitats or microhabitats exposed to seasonal desiccation.

Late Bronze Age copper smelting in the southeastern Alps: how standardized was the smelting process? Evidence from Transacqua and Segonzano, Trentino, Italy

The smelting copper slags from the archaeological sites of Transacqua and Segonzano in Trentino (Italy) were fully analysed to study the extraction of copper from copper and iron sulphide minerals that were carried out in the southeastern Alps during the Late Bronze Age. A combined approach involving physical, chemical, mineralogical and petrographic analyses was applied on over 130 copper slags from Transacqua and Segonzano. Three different types of slags were distinguished from the mineralogical and chemical points of view, differing in the size and relative amount of the unreacted sulphides and matte, the size of metallic copper prills, the ratio between unreacted quartz and newly formed silicate phases and viscosity. By combining all the observations, it is suggested that the three types of slags are the product of a Cu-smelting process formed by three main operations: slagging, matting and refining, which were standardised in the southeast Alps between the fourteenth and the eleventh century BC.

A cross-border regional earthquake early warning system: PRESTo@CE3RN

Since 2002 the Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS) in Udine (Italy), the Agencija Republike Slovenije za Okolje (ARSO) in Ljubljana (Slovenia) and the Zentralanstalt fur Meteorologie und Geodynamik (ZAMG) in Vienna (Austria), are collecting, analyzing, archiving and exchanging seismic data in real time, initially in the framework of the EU Interreg IIIa Italia-Austria project “Trans-national seismological networks in the South-Eastern Alps”. As outcome of the successful cooperation, in the 2013 OGS, ARSO and ZAMG decided to officially merge their seismic monitoring efforts into the “Central and Eastern European Earthquake Research Network—CE3RN”. This work reports the results of a nine-month real-time test of the earthquake early warning (EEW) algorithm probabilistic and evolutionary early warning system carried out at the CE3RN. The study allowed identifying the actions to be implemented in order to let the CE3RN become in the next future an efficient cross-border EEW system.

Taxonomy and nomenclature of the polymorphic European high mountain species Androsace vitaliana (L.) Lapeyr. (Primulaceae).

Androsace vitaliana (syn. Vitaliana primuliflora; Primulaceae) has been subject to several taxonomic treatments, whose conclusions ranged from a single species with numerous infraspecific taxa to several species usually without infraspecific taxa. Here, following molecular investigation, several taxonomic changes are made. A single species with the following infraspecific taxa is recognized: subsp. vitaliana (Pyrenees), subsp. cinerea (south-western Alps), subsp. lepontina (Pennine Alps), subsp. sesleri (south-eastern Alps), subsp. praetutiana (Apennines) and subsp. assoana (Iberian Peninsula excluding the Pyrenees), the last of which is divided into the four allopatrically distributed varieties assoana, centriberica, flosjugorum and nevadensis. Contrary to some previous assertions, all taxa are allopatric and, especially for subspp. vitaliana, cinerea and lepontina, where clear diagnostic characters are lacking, they can best be determined by their geographic origin.