Dinarides Research Articles

Context‐dependent behaviour and connectivity of recolonizing brown bear populations identify transboundary conservation challenges in Central Europe

AbstractFollowing historical restrictions to isolated and patchy populations, large carnivores like the brown bear Ursus arctos are recolonizing areas of their historical range in Europe. This process is of particular interest in the Alps and the Dinaric Mountains in Central Europe, the largest mountain range in the continent and of transboundary conservation interest. To assist policies focused on the expansion of bears in this region, we conducted habitat selection analyses accounting for different behaviour between three populations (Trentino, pre‐Alps and Dinaric) where bears have adapted to different intensities of human persecution. We then identified the landscape connectivity between these fragmented populations that could provide viable habitat and stepping‐stone patches for recolonization. To handle individual and population differences in space‐use, we modelled habitat selection per population from an individual‐level and integrated results into a multi‐population model using scale‐integrated resource selection functions. We then calculated connectivity indices per patch and the contribution of various countries involved in bear management in the region to enhancing connectivity. Bears mostly selected forests across all populations while preferences for other variables differed among populations and across scales. Bears in the highly humanized habitats of the Trentino selected the most intricate topography, where they could more easily find refuge. Suitable but fragmented habitat patches were common all over the study area with the most suitable habitat in the pre‐Alpine and Dinaric populations. However, the Trentino and pre‐Alp included the patches of maximum/medium priority as stepping‐stones to connect these populations. Transboundary initiatives for the conservation of existing habitat and the facilitation of connectivity are required to promote current bear expansion and reduce conflicts with humans. Our framework provides insight into the adaptive behaviour of large carnivores in human‐dominated landscapes in a conservation context.

Two new mesophilous oriental hornbeam communities from the northern Dinaric Alps (Bosnia and Herzegovina)

Abstract The paper describes two new mesophilous communities of oriental hornbeam (Carpinus orientalis) coppice from the northern Dinaric Alps in Bosnia and Herzegovina (B&H). While oriental hornbeam is mainly considered to be a part of thermophilous forests and scrub, numerical analysis of 103 relevés of C. orientalis dominated coppice from B&H has shown that two new, rather mesophilous, communities thrive on calcareous bedrock of NW B&H. They represent secondary successional stages of mesotermic forest vegetation in this region. Association Epimedio alpini-Carpinetum orientalis ass. nova hoc loco is related to Illyrian oak-hornbeam forests of Erythronio-Carpinion betuli, while Asplenio scolopendrii-Carpinetum orientalis ass. nova hoc loco is linked to Balkan submediterranean ravine forests of Ostryo-Tilion. Although these two associations were recorded only in the NW B&H, their distribution is potentially larger, as their source communities are relatively common throughout the Dinaric Alps, so the information about their distribution, vertical structure, and syndynamic relations could be very useful in a national scale forest management and nature conservation.

Spatial distribution, niche ecology and conservation genetics of Degenia velebitica (Brassicaceae), a narrow endemic species of the north-western Dinaric Alps

The high-biodiversity phenomenon of the Balkan Peninsula is a result of the past and present topographic, climatic and geological conditions, as well as human impact. The Dinaric Alps, as a part of the Balkan Peninsula, harbour a high number of endemic species, some of them comprising a small number of populations, which are often endangered. We investigated spatial distribution, community composition, site ecology, genetic diversity and conservation of Degenia velebitica, a stenoendemic species of the north-western Dinaric Alps. Our results showed that D. velebitica is nowadays restricted to three localities with the area of occupancy of 48,560 m2, harbouring approximately 37,000 individuals. Degenia velebitica stands are differentiated into three well-characterized, floristically homogenous syntaxa, very distinct from the surrounding vegetation, suggesting their azonal occurrence and restriction to spatially highly fragmented microsites exposed to stormy winds. Spatial distances of populations, differences in D. velebitica community composition and site ecology are mirrored in genetic variation patterns of the populations, such as high-frequency down-weighted marker values in the north-western populations and high gene diversity in the south-eastern group of populations. The fact that we could not find a single D. velebitica individual at the locus classicus indicates the existence of the ever-growing fragmentation. The analyses of genetic structure using AFLP data recognized two main genetic groups of populations as evolutionary significant units that should be considered when planning protection measures. According to our IUCN Red List reassessment, D. velebitica should be treated as a critically endangered species that requires immediate conservation actions.

Phylogenetics and population structure of the steppe speciesHycleus polymorphus(Coleoptera: Meloidae: Mylabrini) reveal multiple refugia in Mediterranean mountain ranges

AbstractMany continental species distributed in the Eurasian steppe occur as relict populations in the mountains of Western Europe. Their biogeographical responses to Quaternary climate changes have been poorly studied; however, they could have responded as cold-adapted species. We investigated the biogeographic history of a steppe beetle, Hycleus polymorphus, using mitochondrial and nuclear DNA sequences (COI, CAD, ITS2), and species distribution modelling (SDM) under present and past bioclimatic envelopes. We first performed a phylogenetic assessment to define species boundaries within the H. polymorphus species group. Specimens previously treated as Hycleus humerosus on morphological grounds are assigned to H. polymorphus, and those identified as Hycleus zebraeus assigned to Hycleus atratus. ITS2 data analyses revealed a strong phylogeographical structure of H. polymorphus populations, with four haplogroups corresponding to the (i) Italian Alps, (ii) French Alps and Pyrenees, (iii) South Balkan and Pontic mountains, and (iv) North Dinaric Alps. Based on these analyses and the SDM, we propose that during a glacial period, following the spread of steppic habitat, H. polymorphus underwent a range expansion from Asia to South-West Europe. Within the Mediterranean area, during the last interglacial the climatic suitability for the species was limited to mountains that acted as refugia and prompted allopatric divergence into four main lineages.

Climate-growth relationships of Norway Spruce and silver fir in primary forests of the Croatian Dinaric mountains

The past century has witnessed a global trend of increasing green house gas emissions, causing a rise in temperatures, changing hydroclimatic patterns and increasing occurrence of climatic extremes. Despite their importance for environmental conservation, scientific research and forest management, primary montane forests of the Dinaric Mts remain insufficiently studied. In this study, we examined the relationship between climate and growth of Norway spruce (Picea abies (L.) H. Karst.) and silver fir (Abies alba Mill.) in the primary forests of Smrčeve doline, located in Northern Velebit National Park, Croatia. Using dendrochronological methods, the temporal relationships between tree ring width (TRW) and blue intensity (BI) were assessed over the 1901–2014 interval, in relation to instrumental climatic data, including temperature, precipitation and self‐calibrating Palmer Drought Severity Index (scPDSI). TRW and earlywood BI (EWBI) chronologies of both species exhibited a clear negative response to summer temperatures, while also showing a positive relationship with summer precipitation and moisture, implying that tree growth in the region is water-limited. Generally, correlation values of EWBI were stronger compared to the TRW chronologies. Although both species showed a degree of common growth response to climatic extremes, the strength of correlations with the most responsive climatic variables was temporally unstable and showed considerable variability in both tree ring parameters. The observed differential response of the two species to climate indicates that the anticipated increase in dry conditions due to climate change could potentially alter the future development and composition of these primary forests by shifting competitive pressures in favor of silver fir. Increasing drought stress around the Mediterranean could have major negative implications for these water-limited primary forests.

Iron Age farming in the Central European Alpine and Dinaric regions; crop occurrence and distribution

The main objective of this paper was to holistically describe the occurrence of most important crop taxa found in different archaeological Iron Age sites in two selected biogeographical regions of Central Europe; in the Alpine and the Dinaric mountains. This study also links the known results of research about the ecological-biogeographical conditions in the Central Europe during the Iron Age time with the papers that include archaeobotanical data of the selected European landscapes as well. It is evident that many factors played crucial roles in the domestication process of many different plant taxa. This study showed that both the Alpine and the Dinaric region of Europe show similar ecological conditions for successfully growing important legumes and cereal taxa. The percentage of found cereal taxa is higher in the Dinaric region as it is in the Alps. In most archaeological sites in the Dinaric mountains, there were no evidence of the productionof pulses at all. However, if comparing the whole repertoire of cultivated plant taxa in the Iron Age epoch in both studied regions, one can conclude that there is not much difference in the number of cultivated planted taxa in the Iron Age epoch.

Modification of clays subjected to different stages of lithogenesis under microbial activity

A comparative study of the influence of microorganisms on physical-chemical clays’ properties at different lithogenetic stages concerned the formation of contact strength between particles was carried out. Natural samples were taken for experiments: dolomite-clay marl from outcrop, the Jahorina mountains, the Dinaric Alps, Bosnia and Herzegovina; alluvial loam from spring, West side of the Onega Lake, Konchezero village, Karelia Republic, Russia; bentonite from the Biklyan deposit, Tatarstan Republic, Russia; phyllite from outcrop, Les Sybelles, Rhone Alps, France. The microbial community was added into moistened clays for 2-4 months. Before and after the experiments such analyses were conducted: X-ray powder diffractometry, determination of water content in clays, maximum hygroscopicity, dry bulk density, total organic carbon, macroscopic wetting contact angle, liquid and plastic limits; incremental loading oedometer test, ion chromatography of filtrate. The microbial activity enhanced the hydrophilicity of marl and phyllite. Multidirectional factors of toughness formation acted in clays subjected to stages between sedimentogenesis and late diagenesis, among which organic matter content dominated.

Baseline radioecological data for the soil and selected bioindicator organisms in the temperate forest of Plitvice Lakes National Park, Croatia.

The aim of this study was to provide baseline radioecological data for the temperate forest ecosystem in Plitvice Lakes National Park. Emphasis was placed on the determination of naturally occurring radionuclides since there is an acknowledged lack of data for these radionuclides in non-accident conditions in wildlife, even for bioindicator organisms. Activity concentrations of 238U, 226Ra, 210Pb, 232Th, 40K, 134Cs, and 137Cs were measured by gamma spectrometry in soil and bioindicators: earthworms, conifer needles, mosses, and lichens. From the measured activity concentrations, concentration ratios were calculated to quantify the transfer of these radionuclides from soil to bioindicators. Our results show that soil activity concentrations are biased toward results from other studies conducted within the Dinaric mountain region. However, in moss and lichen samples, we measured higher activity concentrations of 226Ra and lower activity concentrations of 40K and 137Cs in comparison to similar studies. Also, we estimated lower concentration ratios for all radionuclides from soil to these organisms, except for 210Pb, in comparison to generic values. The transfer of 238U was generally low for all of the bioindicator organisms. For conifer needles, a correlation was found between activity concentrations of 226Ra and 137Cs in soil and related concentration ratios. Correlation was also found between the activity concentration of 40K in soil and transfer of 40K and 137Cs to mosses and lichens. A comparison with literature data highlighted the lack of 226Ra related concentration ratios for conifer trees and especially for earthworms. Therefore, the results of this study could supplement the sparse data currently available on radionuclide background data in similar ecosystems and related soil-to-wildlife transfer of radionuclides. Dose rate assessments, performed by the ERICA Tool, estimated that 96% of the overall exposure of wildlife in the Park area is due to the background dose rates, while 0.06μGyh-1 on average can be attributed as an incremental dose rate from 134Cs and 137Cs.

<p><strong>The endemic and range restricted vascular plants of Croatia: diversity, distribution patterns and their conservation status</strong></p>

The Balkan Peninsula is recognized as an important centre of native and endemic plant species diversity as well as an important wildlife refuge area. However, although Croatia hosts more than half of plant species found on the Balkan Peninsula, the endemic taxa have never been evaluated or used to define conservation priorities. We analyzed the qualitative composition of the endemic and range restricted species, their spatial distribution, centres of endemism, and conservation status (non-IUCN). We generated an updated and annotated checklist of 349 endemic or range-restricted plant taxa (6.9% of the entire native flora), subdivided in 231 species, 103 subspecies and 15 hybrids and belonging to 149 genera and 43 families. Among the 231 species, 69 are considered endemic to Croatia and confined to a small area (< 4,500 km2), while 162 are considered range restricted species, which have larger ranges and/or are shared with neighbouring countries. The genera Centaurea and Hieracium have the highest number of endemic and range restricted taxa. Spatial analyses indicated two notable centres of species richness—the mountainous Dinaric Alps and the SE Adriatic coast, including the islands. Regions with a high richness of range-restricted taxa did not coincide with areas of high richness of endemic species. Taxa exhibited modest bimodality with respect to altitudinal distribution. In addition, the greatest diversity of taxa is concentrated in northwest of Croatia and could be related to differences in mean annual air temperatures and the duration of insolation. As regards their conservation status, 13 of the 349 taxa are endangered, and 62 are near threatened or vulnerable. Despite relatively strong legal protection of endemic and range restricted species, 37 taxa remain unprotected. Changes in conservation practice are therefore proposed.

Crustal Thickness Beneath the Dinarides and Surrounding Areas From Receiver Functions

AbstractKnowledge about the crustal thickness is one of the key elements in the reconstruction of the regional tectonic history. The Dinaric mountain belt is one of the most enigmatic segments of the Alpine‐Mediterranean collision zone, characterized by large variations in crustal thickness and not studied sufficiently. We present a new Moho depth map for the wider Dinarides region which was created using teleseismic earthquake recordings from 87 permanent and temporary seismic stations in the region. Teleseismic data were analyzed using the receiver function method to extract converted P to S waves.The resulting Moho topography fits well within a structural framework comprising a thicker crust under the Dinarides, which gradually becomes thinner toward the Pannonian and Adriatic domains. The profiles crossing the northwestern Dinarides are marked by a relatively sharp decrease in crustal thickness north of the main thrust front. This transition is followed by significant crustal thinning toward the Pannonian basin. The Mohorovičić discontinuity lies the deepest in the central and southern Dinarides, at depths of over 55 km. Here similarly to the northwestern segment we observe a jump in the crustal thickness when transitioning toward the Internal Dinarides, which hints at possible underthrusting (or subduction) of the Adria plate in this region. Moho depths in the transition zone toward the Pannonian basin and in the Pannonian basin proper vary between 25 and 35 km. In the Adriatic domain, we find crustal thickness ranging from 30 km to more than 45 km around the Central Adriatic islands.

Long term changes (1990-2016) in carabid beetle assemblages (Coleoptera: Carabidae) in protected forests on Dinaric Karst on Mountain Risnjak, Croatia

Carabids, as well-known bioindicators, have been used to study the long term changes that have occurred in their communities in the Dinaric Alps. This study involved eight sites in the protected forests of the Risnjak National Park in the years 2015 and 2016 of which three were previously studied in 1990 and 1991. A total of 9, 521 individual ground beetles belonging to 17 genera and 33 species were collected. Species diversity and community composition, including percentages of species grouped according to their habitat preferences, body size, wing morphology, preferred moisture and temperature were used to compare the sites sampled in 1990 and 1991 and resampled in 2015 and 2016. Even though this study was carried out in protected forests within the National Park with minimal anthropogenic pressure and the fact that available climatic data didn't show any significant change in climate over the last 25 years, there was a reduction in the abundance of specialist species and increase in the spread of generalist species. Furthermore, the lower abundance of a mountain specialist and endemic species, Pterostichus variolatus, and the lack of mountain specialists Molops alpestris, Pterostichus unctulatus and Trechus croaticus in the catches indicate the importance of further monitoring of these mountain forest ecosystems and for a well-timed and appropriate conservation approach.

Phytosociological analysis of basophilic Scots pine forests in the Southeastern Alps

Abstract Based on hierarchical classification of more than 300 phytosociological relevés of basophilic black and (or) Scots pine communities in the Southern, Eastern and Southeastern Alps we described a new association Rhodothamno chamaecisti-Pinetum sylvestris, into which we classify stands that have until now been discussed in the framework of subassociations Fraxino orni-Pinetum nigrae pinetosum sylvestris, laricetosum deciduae and (partly) caricetosum humilis, and are floristically slightly similar also to certain forms of the association Erico-Pinetum sylvestris. The stands of the new association are for now classified into Natura 2000 habitat type Southeastern-European Pinus sylvestris forests (91R0), within it we propose a special habitat subtype Southeastern-Alpine Scots pine forests, and into a new forest site type Southeastern-Alpine Scots pine forest. At the contact of the Julian and Dinaric Alps we described a new subassociation Genisto januensis-Pinetum sylvestris campanuletosum cespitosae, which comprises also a Natura 2000 species Primula carniolica.

The Boundaries of the Carpathian Basin – Frontiers and Regions

Abstract The Carpathian Basin (or Pannonian Basin) is the south-eastern part of Central Europe, its geopolitical place being defined by geography (it is placed between the Eastern Alps, the Dinaric Alps, and the Carpathian Mountains) and from historical point of view by the fact that its core region was ruled for many centuries by the Hungarian Kingdom and the Habsburg Monarchy, and the neighbouring states aimed to extend their territories in the basin reducing the central role of the basin from the margins. The changes of the spatial domination in the Carpathian Basin created several centre–periphery relations, which established, through a longue durée, specific social features in some border regions of the Carpathian Basin. This paper examines from the viewpoint of limology (border studies) three frontier regions of the basin, Spiš, Székely Land, and Banat, and investigates the historical process of the regional construction in order to ascertain what circumstances helped or blocked these periphery constructions.

Microsatellite based assignment reveals history of extirpated mountain ungulate

During the early 1900s, Northern chamois (Rupicapra rupicapra) populations in the northern Dinaric Mountains were extirpated. During the 1960s and 1970s there were several reintroductions of individuals from two Northern chamois subspecies (Alpine chamois, R. r. rupicapra and Balkan chamois, R. r. balcanica) from neighbouring areas in the attempt to re-establish the population. Accurate taxonomic classification, at subspecies level, of the autochthonous extirpated population was not known. To clarify which subspecies was present before reintroduction, we genotyped four male chamois skulls originating from Velebit Mountain, collected around 25 years before the population local extinction. DNA was successfully extracted from middle layer and outer sheath of horns. Assignment based on microsatellite loci, using both Bayesian clustering in STRUCTURE (with q values between 0.55 and 0.73) and DAPC (with individual membership probabilities of 0.99 and 1.00) indicated higher assessed likelihood for the Alpine subspecies.

Geographic variation of Pinus heldreichii Christ from the Western Balkans based on cone and seed morphology

Pinus heldreichii (Bosnian pine) is a Balkan-Apennine endemic and relict pine species that inhabits high mountains in the Mediterranean and sub-Mediterranean regions. Nineteen populations of P. heldreichii from the Western Balkans encompassing 187 individual trees were examined to evaluate morphological variation, a rarely studied aspect of the species. Univariate and multivariate statistics were applied in order to assess the variation of morphological traits of cones and seeds, evaluate the relationships among the sampled populations and verify geographic differentiation in the Dinaric Alps versus Scardo-Pindic mountains. The observations of P. heldreichii covering the populations from the western margins and the centre of the species distribution range indicated a morphological variation among populations and their geographic structure. In general, the southern populations (Scardo-Pindic group) had lower values for the most of morphological traits than the northern ones (Dinaric group). The observed geographic differences between these populations exhibit a north-western to south-eastern gradient, with a few inconsistencies. The southernmost sampled population, Tomorr in Albania, showed remarkable morphological divergence from the other studied populations and appeared to be a distinct morphological group. The pattern of morphological variation in Bosnian pine most likely resulted from multiple effects of long-term isolation and fragmentation in high mountain systems, adaptation to extreme environments and human disturbances.

CHALLENGES FOR BIODIVERSITY PROTECTION STEMMING FROM BORDER WALLS IN SLOVENIA AND KOREA

The proliferation of border walls around the world, including in European Union territory, is a fact. Their construction can have harmful and irreparable consequences for biodiversity and ecosystems. This paper analyses the construction of the border fence between Slovenia and Croatia, paying special attention to the violations of European and international law and to the harm caused to the biodiversity of the Dinaric Alps region. It will also look at the singular case of the demilitarized zone between North and South Korea, which, because it has been free of human interference for more than sixty years, has enabled wildlife to thrive and the establishment of a unique ecosystem in the world. The challenge for international law is thus twofold: to ensure the conservation and protection of biodiversity without compromising the peace process or a hypothetical reunification.

Lower Jurassic benthic foraminiferal assemblages from shallow-marine platform carbonates of Mallorca (Spain): stratigraphic implications

The stratigraphic distribution of larger benthic foraminifera and other microfossils, as analysed in thin-sections, has been investigated in three stratigraphic sections from the island of Mallorca (Son Maina, S’Heretat and Cuevas de Arta). These stratigraphic sections represent deposition in a Lower Jurassic shallow-water carbonate platform succession (Es Barraca Member, Soller Formation) of the Llevant Mountains. The microfossil assemblages contain abundant benthic foraminifera and calcareous algae, including the typical Liassic dasycladalean alga Palaeodasycladus mediterraneus (Pia) and the microproblematica Thaumatoporella parvovesiculifera (Raineri), which provide good age constraint of the succession. Three consecutive biozones have been recognized based on the stratigraphic distribution of foraminifera, including the evolutionary bioseries Mesoendothyra—Lituosepta—Orbitopsella spp., which are documented for the first time in the Balearic Basin: Biozone A (interval Zone) is characterized by the occurrence of small Siphovalvulina spp., Mesoendothyra sp. and rare Lituosepta ancestors. Biozone B (lineage Zone), whose lower boundary is defined by the first occurrence of Lituosepta recoarensis Cati and its top by the first appearance of Orbitopsella aff. primaeva (Henson). The uppermost part of biozone B shows an interval with transitional morphotypes between Lituosepta and Orbitopsella, indicating that the change between biozones B and C1 is gradual (B/C1 transition). This interval is characterized by the presence of very primitive forms of Orbitopsella. Finally, Biozone C1 (lineage Zone) is defined by the first occurrence of Orbitopsella aff. primaeva together with L. recoarensis. The upper boundary of the Biozone C1, which is defined by the first occurrence of O. praecursor s.l., is not recorded in the studied sections of the Es Barraca Member. This biostratigraphic zonation is consistent with a Sinemurian age for the Es Barraca Member with its top most likely not extending into the Pliensbachian. The proposed biostratigraphic scheme is comparable with those established for other western Tethyan margins such as the High Atlas of Morocco, the Southern Italian Alps or the Dinaric Alps of Slovenia and Croatia. The reconstruction of a depositional transect across the studied sections shows the progressive loss of the upper biozones towards the northeast, demonstrating the existence of significant hiatuses in some sections of the Llevant Mountains domain. These hiatuses point to an intra-lower Pliensbachian (Carixian) early stage of platform fragmentation, with areas affected by erosion or non-deposition, and areas with marine marly limestone sedimentation followed by deltaic siliciclastic progradation on the north-western part of Mallorca.

Phylogeography and taxonomic reassessment of Arabidopsis halleri – a montane species from Central Europe

Evolutionary histories of plants from the mid-elevation (montane) zone of European mountain ranges have only rarely been documented, standing in contrast to those of well-researched inhabitants of (sub-)alpine and foothill zones. To fill this gap, we have reconstructed the phylogeography of Arabidopsis halleri, a species preferring coniferous woodlands and corresponding secondary habitats in the montane zone of the Alps, Carpathians, Hercynian massif and Dinaric Alps. Based on range-wide sampling and finer-scale analyses of multiple multilocus DNA markers, we have addressed phylogeographic patterns among the Carpathian populations and inferred their relationships to A. halleri from neighbouring mountain ranges. We also present a taxonomic re-evaluation of the species in Europe, based on the revealed genetic structure complemented by morphological data. Besides two distinct Alpine groups, we identified a major phylogeographic split between the Western and South-Eastern Carpathians. Interestingly, Western and South-Eastern Carpathian populations were genetically closer to populations from neighbouring mountain ranges (the Hercynian massif and the Dinaric Alps for the Western and South-Eastern Carpathians, respectively) than they were to each other, likely reflecting long-term isolation in different parts of the Carpathians or different (re)colonization pathways during the Holocene. In spite of the considerable environmentally correlated variation, the five major European genetic groups exhibited distinctive morphological characters, and we therefore propose treating them as separate subspecies: A. halleri subsp. halleri (Western Europe, Hercynian massif), A. halleri subsp. tatrica (Western Carpathians), A. halleri subsp. ovirensis (Eastern Alps), A. halleri subsp. occidentalis (Western Alps) and A. halleri subsp. dacica (Eastern and Southern Carpathians and Dinaric Alps).

Using video surveillance to monitor feeding behaviour and kleptoparasitism at Eurasian lynx kill sites

Recent technological developments in non-invasive methods facilitate study of the behaviour of elusive predators. We used two types of automatic digital video surveillance systems in combination with GPS telemetry to record feeding behaviour of wild Eurasian lynx (Lynx lynx), intraspecific prey sharing and scavenger activity at ungulate kill sites in the Dinaric Mountains. This approach proved an effective and mostly non-invasive way to obtain detailed data on the consumption of prey by lynx and kleptoparasites, especially when the advanced video system was used. Lynx spent a considerable amount of time in the vicinity of the kill site, but usually visited the carcass for feeding only once per night with a mean visit time of 35 min and most of the feeding occurred during the first half of the night. Lynx covered 83 % of prey remains, which seemed to be effective against avian scavengers that only found 17 % of the carcasses. We recorded six vertebrate species scavenging on lynx kills, with red fox (Vulpes vulpes) and brown bear (Ursus arctos) being the most frequent kleptoparasites. Based on our results, we provide recommendations for future research using this method, as well as outlining the pros and cons of advanced vs. simple video systems.

Dating of alluvial sediments from borehole at the lower course of the Sava river and indications of the connection between their genesis and climate changes in the Pleistocene

This paper analyses the way in which Pleistocene climate change and glaciations in Dinaric Mountains was reflected in the deposition of alluvial sediments in the Sava river Valley, using a case study of Belgrade Groundwater Source (BGS), the largest and most downstream alluvial water supply source along the Sava river. A stratigraphic analysis of the Quaternary sediments from two boreholes on this site, based on sediment dating, lithological members identification, grain size distribution analysis was performed. Comparison with the results of dating of the moraines and glacial outwash, the remnants of glaciations in Dinaric mountains of Montenegro, by Hughes et al. and Adamson et al. showed a good match, as the dating of the last four sedimentation cycles yielded the 13.2 ka (start of MIS1), 80.9 ka (MIS 5a), 137.5 (end of MIS6 or start of MIS5) and 193.4 ka (MIS 7) ages, corresponding to MIS1, MIS 5a, end of MIS6 and start of MIS5, and MIS7 stages for glacial outwash, and to MIS2, MIS5b and MIS5d, end of MIS6 and start of MIS5, and MIS8 stages for the moraines. The ages of older cycles were presented as a hypothesis based on aforementioned succession of ages.