Northern Carpathians Research Articles

From 20 to 2? Landmark-based geometric morphometrics reveal negligible wing-shape divergence between 20 subspecies of the Apollo butterfly, Parnassius apollo (Lepidoptera, Papilionidae), in the Carpatho-Pannonian region

For effective conservation management of endangered taxa, it is important to define operational units for conservation. In the absence of detailed genetic analyses, morphology-based taxonomy is often used as a surrogate. The Apollo butterfly, Parnassius apollo, is one of the most endangered butterfly species in Europe (considered as a flagship species) with 26 subspecies rank taxa described from the Carpatho-Pannonian region (Central Europe), often based on old, one-by-one descriptions. We applied landmark-based geometric morphometrics on wing shape to determine the number of morphologically distinguishable groups in the region, based on 949 males and 477 females from 20 Carpatho-Pannonian putative subspecies (both extant and potentially extinct). We found a single division between the Eastern Carpathian populations (described as two subspecies: ssp. transsylvanicus and ssp. rosenius) and the rest of the populations (including our outgroup from the Swiss Alps). Since P. apollo was not observed in the Eastern Carpathians in the last two decades, and the currently known extant populations in the Carpatho-Pannonian region are all located in the Northern Carpathians, our results support a single conservation unit in the region. We suggest that (i) extensive monitoring is needed to reveal whether the unique Eastern Carpathian populations have really gone extinct and (ii) more taxonomical/phylogenetic studies on Central European P. apollo are needed for establishing the taxonomy of the species and efficient conservation strategies. We emphasize that modern integrative taxonomy is not only important for clarifying taxonomical issues, but also for providing basis for sound conservation management.

ANALYSIS OF MOVEMENT DATA FROM GPS-MONITORED LIVESTOCK GUARDIAN DOGS (LGDS) AT TWO SHEEPFOLDS IN THE NORTH-WESTERN MARAMURES LAND, ROMANIA USING THE KERNEL DENSITY ESTIMATION METHOD. IMPLICATIONS FOR OUTDOOR TOURISM

The Carpathians and other mountainous regions around the world are renowned for their specific landscapes shaped by pastoralism, a millennia-old traditional and sustainable economic system. In Romania, this traditional occupation has an established place within the Romanian culture. In an environment where large predators are present, the livestock owners and shepherds have traditionally relied, and still do, on livestock guardian dogs (LGDs) to protect the flock against carnivores or theft, therefore, the dogs are perceived as an integral component of the traditional pastoral system. However, from late April until the end of September, many outdoor recreational activities like hiking, mountain trail running, or biking overlap with the pastoral calendar, creating a potential for conflict between two, very different categories of landscape users, with recurring incidents happening over the years. In this study, a winter GPS monitoring campaign was proposed, between November 2023 and January 2024 that used GPS professional collars to track the movements of two livestock guardian dogs stationed at two sheepfolds located at their winter bases in the hills at the foot of Ignis Mountains (part of the Romanian northern Carpathians) from northwestern Maramureș Land, Romania. The campaign generated point-based spatiotemporal data processed and analyzed in M. Excel and QGIS using Kernel density estimation as the main method to generate metrics and identify potential clusters of LGD activity in their usual environment. The results highlight high observational clusters near the winter folds but also lower observational clusters in areas situated hundreds of meters distance around the main compound, in certain locations. Although temporally limited, the results have the potential to help the understanding of the animal's preferred zone of habitation and substantiate future win-win cohabitation solutions that minimize conflictual encounters between the shepherds and their guardian dogs on one side, as primary land users, and outdoor recreationists as other landscape users.

Additional data to the historical breeding of the Eurasian Woodcock in the Carpathian Basin

Abstract The Eurasian Woodcock is a regular breeder in the wooded areas of the Carpathian Basin. In the past, several literature reviews on the distribution and breeding biology of the species in the Carpathian Basin have been published, but these have ignored the annual reports on spring returns collected between 1894 and 1926 under the coordination of the Hungarian Ornithological Centre. These included 379 nesting records from the present area of Austria, Croatia, Hungary, Romania, Serbia, Slovakia, Slovenia, and Ukraine. The majority of the data came from the Carpathians, with a smaller number from forested areas in the lower mountains and hills. It was particularly rare in lowland areas, with most of the records coming from floodplain forests. The spatial distribution of the data is somewhat at odds with that described in recent summary works. From the Northern Carpathians and the Eastern Alps, however, these sources report fewer nestings, and most of the data come from Transylvania. The temporal distribution of the data is consistent with previously published results. In some cases nestings were found in late February and early March. The peak of nesting was in April, with only a small number of nestings reported in the second half of May. Breeding occurred significantly later in areas at higher altitudes. Nevertheless, it can be concluded that knowledge of the species’ nesting in the Carpathian Basin is still incomplete.

Mapping grasslands' preservation potential: A case study from the northern Carpathians

AbstractThe grasslands which are an important part of an ecosystem are endangered due to abandonment of traditional forms of land use. Preservation of biodiversity of semi‐natural grassland communities is of great importance, therefore it is important to identify threats and prepare a sustainable plan for their protection The goal of this study was to develop an approach to predict threatened grasslands hotspots, basing on multi‐factor machine learning analyses. The Gorce Mountains in the Polish Carpathians were chosen as a study area, as it is region partially protected by National Park, surrounded by villages with different socio‐economic conditions (agriculture or touristic oriented). The grasslands were identified and classified on Sentinel‐2 multispectral imagery. As lack of regular mowing of grasslands was found as main factor promoting forest succession. Therefore, in order to find endangered grasslands areas, support vector machines' algorithm was used to classify them in mowed and unmowed categories. Then the preservation potential of grasslands was modeled with the random forest method, based on the grasslands' mowing classification, digital terrain model, land‐use and population statistical data, and the historical forest extent. We found the grasslands above 750 m above sea level to be the most endangered. Also, the tourism activity and ongoing changes in employment structure from agriculture to services has had a negative influence on the grasslands preservation potential. On the other hand, the Gorce National Park's active grassland conservation by mowing and grazing was shown as a positive element in keeping with the high biodiversity of the area.

Responses of small mammals to habitat characteristics in Southern Carpathian forests

Compared to Northern Carpathians, the small mammal fauna of Southern Carpathian forests is poorly known, with no data on habitat use; our study seeks to fill this gap. To this end, we conducted a survey in the Southern Carpathians for five years, assessing habitat use by small mammals in forests along an elevational gradient. Trapping was done using live traps set in transects at elevations between 820 and 2040 m. For each transect we evaluated variables related to vegetation structure, habitat complexity, and geographical location. We considered abundance, species composition and species richness as response variables. The rodents Apodemus flavicollis and Myodes glareolus and the shrew Sorex araneus were common and dominant. Their abundance were positively correlated with tree cover, the best explanatory variable. Responses to other variables were mixed. The strong divergence in the relative habitat use by the three most abundant species may act as a mechanism that enables their coexistence as dominant species, exploiting the same wide range of habitat resources. Overall, habitat use in our study area was similar to that reported from Northern Carpathians, but we found also important differences probably caused by the differences in latitude and forest management practices.

Drivers of Timberline Dynamics in Rodna Montains, Northern Carpathians, Romania, over the Last 131 Years

Currently, there is little information regarding the recent spatiotemporal dynamics of upper timberline in the Carpathian Mountains. We reconstructed the temporal (1887–2018) and spatial dynamics of upper timberline in the Rodna Mountains (Eastern Carpathians) based on seven sets of maps and aerial photographs and explained its variability in relation to three main drivers: air temperature, land morphometry and anthropogenic pressure. The impact of natural drivers (temperature, morphometry) on timberline position was evaluated using a high-resolution digital elevation model, local and regional instrumental and modelled climate databases. The impact of anthropogenic factors on timberline position was documented from published sources such as local paleolimnological studies and historical documents. Results show that timberline rose on average with 113 ± 2 m on the northern slope of the Rodna Mts (currently reaching 1640 m above sea level (a.s.l.)) and with 182 ± 2 m on the southern slope (up to an elevation of 1539 m a.s.l.). Our results suggest that this pattern might be connected with the rising temperature over the recent decades. On the northern slope where land morphometry restricts anthropogenic activities, timberline reached the highest elevation. On the more accessible southern slope, anthropogenic land-use changes likely moderated timberline elevational rise under increasing temperatures.

Influence of geographical factors on thermal stress in northern Carpathians

While general features of mountain climate are well recognised, there is not many research regarded their bioclimatic differentiation. The aim of the present study is to answer the question how different geographical factors: elevation above sea level, physiographical type of area, climate continentality and location of area in relation to the main mountain ridge influence thermal stress in northern Carpathians. To analyse thermal stress in the region, daily meteorological data from 21 stations of national weather networks of Poland, Ukraine and Slovakia for the period 1986–2015 were used. Daily data of air temperature, relative humidity, total cloud cover and wind speed at 10 m above ground for 12 UTC were used because they represent midday hours which are mostly used for any human activity. The Universal Thermal Climate Index (UTCI) was applied as a measure of thermal stress. The results show that (1) cold stress significantly increases and heat stress decreases due to rise of altitude, (2) due to climate continentality and physiographical differences between western and eastern parts of northern Carpathians in their eastern edge, the cold stress is more evident than in western one, (3) at southward slopes of Carpathian, heat stress is significantly more frequent then at northward areas.

Thermal stress in the northern Carpathians and air circulation

Abstract In mountain areas, air circulation plays a major role in the forming of the climate. This paper examines how it influences thermal stress in the northern Carpathians. The Niedźwiedź’s classification of air circulation was applied. Thermal stress was assessed by Universal Thermal Climate Index (UTCI). Daily meteorological and circulation data for the period 1986–2015 were used for 20 stations in Poland, Slovakia and Ukraine. Air circulation was found to have a significant impact on thermal stress. The highest UTCI values are observed at Ca+Ka (centre of the high and anticyclonic wedge or ridge of high pressure) and the lowest values at N+NE and W+NW circulation; at the Southward stations, UTCI is higher than in the Northward ones; thermoneutral days are more frequent on the southward than on the northward slopes; during N+NE, E+SE and W+NW circulation and for heat stress days, the greatest thermal privilege of the southward slopes is observed at E+SE, S+SW, Ca+Ka and Cc+Bc (centre of low and through of low pressure) types of circulation.

Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland: The Żarska Cave (southern Poland) case study

The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides important data that complement the global record. The Żarska Cave is an exceptional site, which owing to its thick and undisturbed Holocene sediments with very rich paleobotanical and paleozoological materials has become the most complete example of the uppermost Upper Pleistocene and Holocene cave deposits in the Polish uplands. The aim of our study was to understand paleoenvironmental changes in southern Poland, from the late Glacial to the late Holocene, which has been targeted by use of a detailed geological analysis accompanied by analysis of a wide range of paleobotanical, paleozoological, and archeological assemblages. All the results obtained have permitted characterization of the paleoenvironmental changes occurring in the area of the Polish Jura during the last >15 ka years. A particularly well-represented sequence covers the Allerød interstadial, which revealed the presence of forests with associated shade-loving mollusks and rodents. The beginning of the Holocene was clearly identified with an increase of shaded forest habitats, which developed in a still relatively cold climate with continental features, and with the first appearance of mesophilous deciduous trees. During the middle Holocene, unusual evidence for maple forests is documented, which developed before the formation of beech forests, typical for the late Holocene. The obtained sequence has great significance not only for the Polish Jura region, but also has wider implications for southern Poland and the vast area of the northern Carpathian foreland.

Tracing the Relationship between Precipitation and River Water in the Northern Carpathians Base on the Evaluation of Water Isotope Data

The aim of this study is to investigate the stable isotope composition of precipitation and river water from the northeastern part of Romania. For this study, we collected monthly samples (for variable periods of time) of precipitation from six stations, and river water from three stations, between March 2012 and December 2017. The precipitation in the area is sourced mainly from the Atlantic Ocean, and secondarily from the Black Sea, local recycling being important especially in summer. We found that the seasonal δ18O in precipitation is in agreement with the seasonal temperature variability, as shown by the significant correlation coefficient between the two variables (r = 0.77), which indicates that the temperature has an important role in the δ18O variability in precipitation water in this region. The local meteoric water line in the northeastern part of Romania is defined by the equation δ2H = 7.80 × δ18O + 7.47, (r2 = 0.99, n = 121). The results presented in this study emphasize that the δ18O (and δ2H) and d-excess variability are strongly influenced by temperature, precipitation and the prevailing large-scale atmospheric circulation.

,,Na sałasie ni ma pani lekko“. Życie codzienne pasterzy wołoskich na szałasach na pograniczu polsko-słowackim w XXI wieku jako dziedzictwo kulturowe regionu Karpat (wybór zagadnień)

The purpose of this article is to present the preliminary results of the research on the shepherds' everyday life that I have been conducting since 2015 in the field of history, migration, and cultural heritage of the Vlach minority inhabiting the areas from Albania to the northern Carpathians. One of the research stages entails the studies of the daily life and rituals of the highlanders living in the huts on the Polish side of the Carpathians. The article describes the issues concerning the organization and the time-space symbolism of a modern hut, including their daily life and schedule of activities. The research was conducted in the selected huts of Spiš, Orava, Podhale, Żywiec region, and Silesian Beskids in Poland in 2015-2018. In all cases, I applied qualitative research, mostly structured and unstructured interviews with senior and young shepherds working in the huts, as well as covert and overt participant observations conducted during selected pastoral holidays and meetings in various spaces—in temples, during highlander's and Vlach conventions, in theme meetings, and in the huts. I supplement these techniques with the analysis of the visual sources that I made during the field research, received from the enthusiasts of this topic, or found on the Internet. The research has shown that modern pastoralism oscillates between two poles: the traditional, which has made it possible to retain many elements from the past (cultural heritage), and the modern, thanks to which shepherds introduce global solutions to their huts and traditions.

Polityczne meandry łemkowskich cerkwi

Zachowane do dziś łemkowskie cerkwie są jednymi z najbardziej charakterystycznych elementów krajobrazu kulturowego północnych Karpat oraz dowodem na wielonarodową i wielowyznaniową przeszłość Beskidów. Dramatyczna i skomplikowana historia oraz współczesna sytuacja tego regionu pokazuje bezpośredni wpływ wydarzeń politycznych na dzieje Łemków, ich kulturę duchową i materialną. Głównym celem artykułu jest pokazanie na przykładzie Łemkowszczyzny nadrzędnego wpływu uwarunkowań politycznych na strukturę wyznaniową. Przekształcenia i decyzje polityczne, zapadające bez udziału najbardziej zainteresowanych (w tym przypadku Łemków), skutecznie determinowały tak bardzo prywatną sferę życia jak wiara religijna. Miało to miejsce zarówno w XX w., jak i kilkaset lat wcześniej, jest tak również współcześnie.

The birth and development of the oil and gas industry in the Northern Carpathians (up until 1939)

Abstract The northern segments of the Carpathians, stretching between Limanowa (Poland) and Kosów (Ukraine), belonged to the most prolific hydrocarbon province in the world in the late nineteenth and early twentieth centuries. The earliest written accounts of natural occurrences of hydrocarbons in the Carpathians date back to the sixteenth century. In the eighteenth and early nineteenth centuries, Rzączyński, Kluk, Hacquest and Staszic provided accounts on methods of practical use related to oil. Staszic's geological map shows numerous oil seeps and different rock types containing hydrocarbons. The development of the oil industry was triggered by Łukasiewicz's discovery of an oil-distillation process and the construction of a kerosene lamp. Following this, the oil industry flourished in the Northern Carpathians. Oil production peaked at 2 Mt (million tons) of crude oil in 1910. In subsequent years, the level of oil production steadily decreased due to a turbulent economy. Exploration for oil, gas and ozokerite resulted in the development of modern micropalaeontology and geological mapping, with a prime example being the regional coverage of almost the entire Northern Carpathians provided by the Atlas Geologiczny Galicyi ( Geological Atlas of Galicia ), which consisted of 99 high-quality geological maps at a scale of 1:75 000. Geophysical surveying techniques were applied to subsurface mapping, and higher educational institutions were established in order to support exploration efforts.

How warm? How wet? Hydroclimate reconstruction of the past 7500 years in northern Carpathians, Romania

As natural and anthropogenic ecosystems are dependent on the local water availability, understanding past changes in hydroclimate represents a priority in research concerning past climate variability. Here, we used testate amoebae (TA) and chironomid analysis on a radiocarbon dated complex of small pond and peat bog sediment profiles from an ombrotrophic bog (Tăul Muced, northern Carpathians, Romania) to quantitatively determine major hydrological changes and July air temperature over the last 7500years.Wet mire surface conditions with a pH between 2.3 and 4.5 were inferred for the periods 4500–2700 and 1300–400calyrBP by the occurrence of Archerella flavum, Amphitrema wrightianum and Hyalosphenia papilio. Dry phases in mire surface conditions and a pH between 2.5 and 5 were inferred for 7550–4500, 2750–1300 and 0calyrBP–present by the dominance of Nebela militaris, Difflugia pulex and Phryganella acropodia. The quantitative reconstruction of mean July temperature based on the chironomid communities suggests low summer temperatures for the periods 6550–5600, 4500–3150 and 1550–600calyrBP, while periods of slightly higher summer temperatures were observed for 5600–4500, 3150–1550 and 100calyrBP–present. There is a generally good agreement between drier phases of the peat surface conditions with higher July temperature, suggesting that temperature may have been a controlling factor for water table fluctuation.Our quantitative reconstructions, among the first for central eastern Europe, show a relatively good agreement with other palaeohydrological studies from central eastern Europe, but contrast with others estimates from north-west Europe. Another important aspect of our study is that it provides valuable information on changes in local hydrology and the potential effect of the mean summer temperature over these changes.

Fire has been an important driver of forest dynamics in the Carpathian Mountains during the Holocene

Fire frequency and severity are key parameters in evaluating fire-mediated changes in ecosystems, but these metrics are rarely reconstructed at extensive temporal scales. Notably our understanding of the role of fire regime dynamics in the functioning and biodiversity of Central Eastern European temperate forests is limited because investigation of the effect of fire has been neglected. To fill this gap in knowledge, we applied a multi-proxy approach (macrocharcoal, charred remains, pollen, plant macrofossils) to two sedimentary sequences spanning stands of closed canopy Picea abies to the P. abies treeline located in the northern Carpathians, Romania. We found that climate exerts a broad-scale influence, whereas vegetation feedbacks strongly modulate this fire-climate relationship. Fire has been almost continuously present throughout the Holocene with a remarkably stable mean fire rotation (∼250yr) with fires of mostly low to mid severity and/or small to medium size. Humans have shifted the fire regime during the last 2800years to slightly longer fire return intervals (mean 300yr) and more biomass consumption per fire. We found that P. abies was favoured by low to moderate fire severity/area burned. The establishment of late-successional, shade tolerant Fagus sylvatica was facilitated by fire disturbances, but its expansion coincided with major gaps in fire events. This highlights the key role of fire in the expansion of F. sylvatica that seems only possible in a low/small to mixed severity/size fire regime with a sufficiently long fire return interval. High magnitude charcoal peaks negatively affected F. sylvatica. We found more diverse pollen assemblages, especially taxa linked to anthropogenic impact, at times of moderate fire disturbance corroborating the intermediate disturbance hypothesis. In terms of forest management, our results show that, contrary to current understanding, fire is a natural and important driver of vegetation change in this region. The anticipated increase in fire activity with the climate warming and/or augmented fuel accumulation may threaten the dominant forest ecosystems, given that these are adapted to low frequency and severity fires. We advise forestry to consider the effects of fire as part of climate-change conservation strategies. Diversifying the forest tree mixture with more fire-resistant native species is desirable in order to mitigate the effects of increased fire occurrence and severity.

Understanding unexpected reintroduction outcomes: Why aren't European bison colonizing suitable habitat in the Carpathians?

Reintroductions are an important tool for re-establishing or reinforcing populations of threatened species, and thus to restore ecosystems. However, predicting how reintroduced populations will spread is difficult, and past reintroductions often lacked a thorough assessment of habitat availability and connectivity. Using the case of reintroduced European bison (Bison bonasus L.) in the northern Carpathians, we show how habitat suitability models in combination with connectivity assessments based on circuit theory can remedy such shortcomings, and identify potential habitat patches and corridors between these. European bison were reintroduced in our study area in the 1960s, and against prior expectation, have not spread along the Carpathian ridge, but instead expanded their range towards human settlements. Our analyses provide an explanation for this pattern. Although we identified a network of suitable habitat patches along the Carpathian ridge, the functional connections between them were limited due to a number of major barriers to movement. To avoid future conflicts between European bison and people, and to achieve the long-term goal of a viable bison metapopulation in this region, conservation action should focus on establishing connectivity between habitat patches through the creation and legal protection of corridors and wildlife passages, which would benefit Carpathian wildlife in general. Our study emphasizes the importance of landscape-scale connectivity analyses to guide restoration efforts, and of adaptive management to ensure the success of reintroduction projects.

Palaeoecological assessment of prehistoric and historic human impact in the high elevation areas of the Northern Carpathians, Romania

This paper presents a high resolution, multi-proxy palaeoenvironmental reconstruction (pollen, dung fungal spores, micro and macro-charcoal, mineral magnetic properties and geochemistry) in three sedimentary sequences located at different elevations across the Northern Carpathians (Romania) over the Late Holocene (i.e. the last 4000 years). We aim to: i) determine what aspects of prehistoric and historic human activity (e.g. burning, clearing, grazing) have shaped the landscapes of today, and ii) use this information to facilitate their environmental management and conservation strategies to maintain the ecological and economic sustainability of extant habitats in the currently changing environment

Using testate amoebae to infer Holocene palaeohydrological history in the Northern Carpathians, Romania

We used radiocarbon dating, testate amoebae (TA) and pollen analysis of a peat profile extracted from an ombrotrophic bog (Taul Muced) located in the Rodna National Park, Romania, to identify major changes in the wet-dry ecological gradient over the last 8000 years. We performed a quantitative reconstruction of the local depth to water table (DWT) and pH variation using the transfer function developed on a Polish modern testate amoebae data set and compared our reconstruction with other palaeohydrological studies in this region. The pollen record was used to determine regional vegetation dynamics as well as the potential impact of humans on peatland dynamics

Vegetation, climate and fire: new insight from palaeoecological records from the Romania

Palaeoecological datasets (pollen, plant macrofossils, stomata, charred remains, charcoal, testate amoebae) are a surrogate for measurement of past biotic responses to environmental and disturbance scenarios occurring at different temporal scales (10 to 10 3 years). Here, I provide an overview of the results from the latest methodological approach in fossil records from the Romanian Carpathians spanning the last glacial to the present. This paper is structured around three main research subjects: I) Past vegetation dynamics with focus on the vegetation sensitivity to the climate and human impact in the lowlands of Transylvania (Lake Stiucii). Particularly emphasis is on the application of Regional Estimates of Vegetation Abundance at Large Sites (REVEALS model) to correct for biases in taxon-specific pollen productivities and dispersal for an accurate quantification of vegetation cover changes and human induced land cover changes; II) Patterns and drivers of biomass burning in Carpathian region; and III) Hydro-climatic shifts during the last 1000 yeast as revealed in peat bogs from the Northern Carpathians.

Last Millennium hydro-climate variability in Central–Eastern Europe (Northern Carpathians, Romania)

Proxy-based reconstructions of climate variability over the last millennium provide important insights for understanding current climate change within a long-term context. Past hydrological changes are particularly difficult to reconstruct, yet rainfall patterns and variability are among the most critical environmental variables. Ombrotrophic bogs, entirely dependent on water from precipitation and sensitive to changes in the balance between precipitation and evapotranspiration, are highly suitable for such hydro-climate reconstructions. We present a multi-proxy analysis (testate amoebae, plant macrofossils, stable carbon isotopes in Sphagnum, pollen, spores and macroscopic charcoal) from an ombrotrophic peat profile from the Rodna Mountains (northern Romania) to establish a quantitative record of hydro-climatic changes. We identify five main stages: wet surface mire conditions between AD 800 and 1150 and AD 1800 and 1950, and drying of the mire surface between AD 1300 and 1450, AD 1550 and 1750 and AD 1950 and 2012. Our multi-proxy reconstructions suggest that conditions during the Medieval Climate Anomaly (MCA) period (AD 900–1150) were considerably wetter than today, while during most of the ‘Little Ice Age’ (LIA; AD 1500–1850), they were dry. Mire surface conditions in the Rodna Mountains have dried markedly over the last 40 years mainly as a result of anthropogenic climate change approaching the driest conditions seen over the last 1000 years. There is a marked difference between current hydro-climatic conditions (dry mire) and those of the MCA (wet mire). This implies that for the study region, the MCA cannot provide analogous climatic conditions to the contemporary situation. Our reconstructions are in partial agreement with water table estimates elsewhere in central and eastern Europe but generally contrast with those from NW Europe, especially during LIA. We suggest that these distinctive regional differences result from fluctuations in large-scale atmospheric circulation, which determine the relative influences of continental and oceanic air masses.