Obraz przewodnika górskiego w literaturze romantycznej. Część I

The intensive development of tourism in the 19th century significantly contributed to the emergence of the guide’s profession. In earlier centuries, this feat was practiced by random people, often unqualified, but with time they became indispensable companions and patrons of tourists. Special qualities were required from mountain guides who, when introducing people to the mountains, had to show special qualities: responsibility, good knowledge of the topography of a given area, care, specific knowledge, as well as good physical condition. The job was professionalized the earliest in the Alps, but the process took place more or less at the same time in other European mountains, for example in the Karkonosze Mountains. It was much more difficult to hire an experienced guide in the Carpathians, where the leadership developed much later. Travel literature of the nineteenth century brought numerous accounts describing the relationship between the guide and the tourist as well as providing numerous realistic descriptions of the first to “hike in the mountains”. Due to the factual nature of this travel literature (diaries, memoirs, etc.), the pioneers of the leadership remained anonymous and found their place in the history of tourism and mountain climbing. This article omits the subject of Tatra guides, which will be the subject of a separate study.

Progress in Grassland Cover Conservation in Southern European Mountains by 2020: A Transboundary Assessment in the Iberian Peninsula with Satellite Observations (2002–2019)

Conservation and policy agendas, such as the European Biodiversity strategy, Aichi biodiversity (target 5) and Common Agriculture Policy (CAP), are overlooking the progress made in mountain grassland cover conservation by 2020, which has significant socio-ecological implications to Europe. However, because the existing data near 2020 is scarce, the shifting character of mountain grasslands remains poorly characterized, and even less is known about the conservation outcomes because of different governance regimes and map uncertainty. Our study used Landsat satellite imagery over a transboundary mountain region in the northwestern Iberian Peninsula (Peneda-Gerês) to shed light on these aspects. Supervised classifications with a multiple classifier ensemble approach (MCE) were performed, with post classification comparison of maps established and bias-corrected to identify the trajectory in grassland cover, including protected and unprotected governance regimes. By analysing class-allocation (Shannon entropy), creating 95% confidence intervals for the area estimates, and evaluating the class-allocation thematic accuracy relationship, we characterized uncertainty in the findings. The bias-corrected estimates suggest that the positive progress claimed internationally by 2020 was not achieved. Our null hypothesis to declare a positive progress (at least equality in the proportion of grassland cover of 2019 and 2002) was rejected (X2 = 1972.1, df = 1, p < 0.001). The majority of grassland cover remained stable (67.1 ± 10.1 relative to 2002), but loss (−32.8 ± 7.1% relative to 2002 grasslands cover) overcame gain areas (+11.4 ± 6.6%), indicating net loss as the prevailing pattern over the transboundary study area (−21.4%). This feature prevailed at all extents of analysis (lowlands, −22.9%; mountains, −17.9%; mountains protected, −14.4%; mountains unprotected, −19.7%). The results also evidenced that mountain protected governance regimes experienced a lower decline in grassland extent compared to unprotected. Shannon entropy values were also significantly lower in correctly classified validation sites (z = −5.69, p = 0.0001, n = 708) suggesting a relationship between the quality of pixel assignment and thematic accuracy. We therefore encourage a post-2020 conservation and policy action to safeguard mountain grasslands by enhancing the role of protected governance regimes. To reduce uncertainty, grassland gain mapping requires additional remote sensing research to find the most adequate spatial and temporal data resolution to retrieve this process.

East Meets West in the Western Carpathians: Contact Zone Between Alpine and Carpathian Caddisfly Lineages Evidenced by COI Barcodes

European mountains are important areas regarding biodiversity of the continent, and they also harbour diverse freshwater fauna, which is critically endangered in terms of the current species extinction. However, sufficient knowledge of this valuable part of European biota is no longer possible without molecular data. This study focuses on the genetic diversity and distribution patterns of the classical representative of the mountain freshwater fauna, caddisfly Rhyacophila tristis, in the Western Carpathians. Based on the COI mitochondrial marker, two genetic lineages (separate BINs) were identified. BIN_W was found in 16 localities in the western part of the study area, BIN_E in 44 eastern localities. The data obtained indicate that BIN_W occurs in a significantly narrower altitude range, BIN_E is more closely related to the Balkan populations than to co-occurring BIN_W, and that the contact zone of the lineages passes through the Western Carpathians. The study revealed phylogeographic and demographic differences between lineages, supporting hypothesis of their evolutionary independence and specific ecological preferences. The obtained genetic data shifted our knowledge on the populations of the studied caddisfly and suggested patterns that could be common to other freshwater species. This could help us to protect unique freshwater ecosystems and preserve European biodiversity.

Genetic variation in lowland and mountain populations of Tofieldia calyculata and their ability to survive within low levels of genetic diversity

Loss of genetic diversity is expected to be a common reason for decline of populations of many rare species. To what extent this is true for populations at the range periphery remains to be explored. Alpine species with peripheral lowland populations are ideal but poorly known model system to address this issue. We investigated genetic diversity and structure of populations of Tofieldia calyculata, species common in central European mountains but highly endangered in lowlands using 17 microsatellite loci. We showed that lowland populations have lower genetic diversity than mountain populations and they are not clearly differentiated from mountain populations. Species probably survived the last glaciation in refugia in margins of Alps and western Carpathians. Some lowland populations are probably relict as well and contain unique genetic information. Their low genetic diversity is likely the result the of reduction of population sizes, gene flow during the Holocene and selfing. However postglacial colonization is also a case of some lowland populations. Based on data from herbarium specimens from extinct lowland populations, we demonstrated that lowland populations had low genetic diversity also in the past and main part of the genetic diversity was lost due to extinction of whole populations. Within population genetic diversity has not changed since the last century suggesting that these populations are able to survive with low levels of genetic diversity under suitable habitat conditions. This idea is also supported by finding of large viable recent populations with very low genetic diversity. We conclude that lowland populations are unique and deserve adequate conservation.

A re-examination of the West European species of Boreonectes Angus, 2010, with particular reference to B. multilineatus (Falkenström, 1922) (Coleoptera, Dytiscidae)

The West European species of Boreonectes Angus, 2010 are reviewed. B. multilineatus (Falkenström, 1922) is shown to be widely distributed in the Pyrenees, where it is the only species known to occur. The chromosomes of all five west European species are found to have, in addition their different numbers of chromosomes, differences in the number and locations of secondary constrictions, and in some cases, the number of chromosomes with clear centromeric C-bands. The level of differences between the chromosomes of the species is in stark contrast with the very slight genetic (DNA) differences between them and this suggests that chromosome differentiation may have been a driver of speciation. Two of the species, B. griseostriatus (De Geer, 1774) and B. multilineatus, have distributions extending northwards as far as Arctic Scandinavia. It is pointed out that, while these northern areas now constitute the major portions of their ranges, they must be of fairly recent origins as most of the area would have been covered by ice sheets and therefore not habitable during the glacial maximum of the Last Glaciation. This contrasts with the situation in the area of the Central European mountains where fossil faunas, including Boreonectes, are known. B. griseostriatus, identifiable to species by its parameres, was present in the Woolly Rhinoceros site at Starunia in the Western Ukraine, and this fauna is discussed as well as an English fauna of similar age.

Alpine Tundra Contraction under Future Warming Scenarios in Europe

The alpine tundra is the highest elevation belt of high mountains. This zone is an important reservoir of freshwater and provides habitat to unique species. This study assesses projected changes in the areal extent of the alpine tundra climate zone in three warming levels in European mountains. The alpine tundra was delineated using the Köppen-Geiger climate classification. We used 11 regional climate model simulations from EURO-CORDEX disaggregated at a one-kilometre grid size representing the RCP4.5 and RCP8.5 scenarios in the 1.5, 2 and 3 °C warming levels. Mitigation represented by the 1.5 °C warming level reduces projected losses of the alpine tundra. However, even in this warming level the projected contraction is severe. In this case, the contraction in the Alps, Scandes and Pyrenees together is projected at between 44% and 48% of the present extent. The contraction is projected to climb in the 2 °C warming to above 57%, while the 3 °C warming would imply that the alpine tundra will be near to collapse in Europe with a contraction of 84% in the three regions, which host most of the alpine tundra in Europe. The projected changes have negative implications for a range of ecosystem services and biodiversity, such as habitat provision, water provision and regulation, erosion protection, water quality and recreational services.

Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development

&lt;p&gt;The Holocene climate shifts had a significant impact on the development of ombrotrophic peatland ecosystems located in various biogeographic zones. Disturbances of the plant communities at peatlands ecosystems took place also due to intensified human activities in the past several centuries, that include peat excavation, fires, as well as deposition of dust and pollutants on peatland surfaces. This merger of natural and human impacts has led to direct hydrological and biochemical disturbances that triggered changes in plant populations, e.g. often leading to the decline of some species, such as Sphagnum austinii in Great Britain.&lt;/p&gt;&lt;p&gt;The knowledge about the development of peatlands across mountain ranges in Europe is still poor. Determining the resilience of peatland vegetation to disturbance is an important and significant task to aid further protection and management of the entire range of ombrotrophic peatlands found in the European mountains, from destroyed or restored to pristine. We carried out high-resolution, multi-proxy studies including plant macrofossils, pollen, testate amoebae, geochemical analyses (XRF and stable carbon isotopes), micro- and macro-charcoal, supported by radiocarbon dating, on replicate peat cores from five well-preserved ombrotrophic peatlands across Europe where peat-forming process is active. The studied peatlands are located along an east west gradient in the Central and Western Europe: Eastern Carpathian Mts. (Calimani-Gurghiu-Harghita, Romania; Bieszczady, Poland), Harz Mts. and Schwarzwald Mts. (Germany), and Vosges Mts (France). In our palaeocological studies we aimed to: i) reconstruct long-term local (mainly Sphagnum populations) and regional (forest communities) vegetation changes at and around selected bogs; ii) reconstruct long-term palaeohydrological shifts; iii) assess mountain peatland ecosystems resilience to Holocene climate shifts and disturbance by fire events and human impact (deforestation, dust and pollution).&lt;/p&gt;&lt;p&gt;Based on our results, we found that: i) despite human activites (pollutants and dust deposition, drainage) some of the mountain peatlands remained in a pristine state, however some plant communities had changed; ii) plant communities composed mainly by Sphagnum species, could repeatedly self-regenerate via autogenic processes following a decline in stressors; iii) recent climate warming has stimulated the spreading of some species indicative of more dry habitats; vi) lack of macrocharcoal in the peat layers indicate that fires did not play a significant role in the development or evolution of local peatland communities. Results from our studies show that palaeoecological records play an important role for the determination of present peatland ecosystem stage and reference conditions for the restoration of damaged ombrotrophic peatlands in European mountains.&lt;/p&gt;&lt;p&gt;The research has received support National Science Centre (Poland) grant No UMO-2016/23/B/ST10/00762 (PI: Mariusz Ga&amp;#322;ka).&lt;/p&gt;