Artykuły naukowe (WNGiG)

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26 December 2004 tsunami deposits left in areas of various tsunami runup in coastal zone of Thailand
(TERRAPUB, 2012-10) Szczuciński, Witold; Rachlewicz, Grzegorz; Chaimanee, Niran; Saisuttichai, Darunee; Tepsuwan, Thawatchai; Lorenc, Stanisław
The tsunami deposits left by the 26 December 2004 tsunami in the coastal zone of Thailand were studied within two months of the event and before any significant postdepositional changes could occur. The sediment structure and texture (grain size), as well as its thickness and spatial distribution, were documented for the tsunami deposits in 12 shore-perpendicular transects from areas of various tsunami runup and wave heights. The tsunami deposits were as thick as 0.4 m and were located as far as 1.5 km inland. They were composed mostly of poorly sorted sand and often consisted of one to four normally graded, massive or laminated layers. The deposits generally became finer in the landward direction; however, landward thinning trend of the deposits is not clear, and the maximum accumulation often is not located close to the shoreline but rather is further inland. In comparable coastal environments with similar available sediment sources the tsunami size (represented as the tsunami runup height) is reflected in the resulting deposits. Larger tsunamis are associated with deposits that are thicker, have a maximum accumulation located farther inland, include a finer sediment fraction (likely from deeper offshore areas) and frequently are composed of normally graded layers.
Accelerating retreat and high-elevation thinning of glaciers in central Spitsbergen
(2016-06-24) Małecki, Jakub
Svalbard is a heavily glacier-covered archipelago in the Arctic. Dickson Land (DL), in the central part of the largest island, Spitsbergen, is relatively arid, and as a result, glaciers there are relatively small and restricted mostly to valleys and cirques. This study presents a comprehensive analysis of glacier changes in DL based on inventories compiled from topographic maps and digital elevation models for the Little Ice Age maximum (LIA), the 1960s, 1990 and 2009/11. Total glacier area decreased by ~38 % since the LIA maximum, and front retreat has increased over the study period. Recently, most of the local glaciers have been consistently thinning in all elevation bands, in contrast to larger Svalbard ice masses which remain closer to balance. The mean 1990–2009/11 geodetic mass balance of glaciers in DL is among the most negative from the Svalbard regional means known from the literature.
Adjustment coefficients for planimetric analysis of the granulometry of coarse-grained sediments
(Wydawnictwo Naukowe UAM, 2011) Pisarska-Jamroży, Małgorzata; Kossowski, Tomasz; Jamroży, Jerzy
The relationship between results from granulometric analyses of by sieving and by planimetry was investigated by numerical simulation of cubes filled with boulders, cobbles and pebbles. Cross-sections through the sediment were simulated and compared with photos of an actual outcrop wall. Volumes estimated on the basis of planimetric analysis using the cross-sections were compared with sieve analyses, thus allowing to determine adjustment coefficients. The coefficients for pebbles and cobbles have a small standard error, but are larger for boulders, which might be a consequence of too small areas formed by the cross-sections.
Allotment gardens and parks: Provision of ecosystem services with an emphasis on biodiversity
(2015) Speak, A.F.; Mizgajski, Andrzej; Borysiak, Janina
Urban areas, in particular, present unique challenges for the conservation of ecosystems. Allotment gardens (AGs) are an important greenspace feature of urban landscapes in Europe which have the potential to offer multiple social and bio-physical ecosystem services in addition to food production. This study is an attempt to assess and compare the ecosystem services provided by AGs in Manchester, UK, and Poznań, Poland as well as a comparison to city parks. The surveys included a detailed land cover characterisation and an assessment of cultivated and spontaneous plant species. There are differences in the land use characteristics in the two cities with a preference for vegetable growing and water recycling in Manchester, and a greater number of trees and a higher focus on recreation in Poznań. The consequences of these basic differences are discussed in terms of the ecosystem services that are provided by the two different AG types, and parks. In terms of ecology, there is higher species richness on AGs with a greater proportion of neophytes, which may potentially spread into cities. The species recorded in parks and AGs contained a lot of native characteristics of urban, ruderal plant communities.
Attitudes of Future Tourism Sector Employees Towards Organise Accessible Tourism
(David Publishing Company, 2017-01) Zajadacz, Alina
The aim of this paper is to show a theoretical approach to the evolution of concepts perceiving disability, taking into account the medical, social, and geographical models, as the basis for the development of principles concerning the organisation of accessible tourism for people with disabilities (PwD). The main research objective was to identify the current attitudes of future, potential employees in the tourism (tourism and recreation students at the time of the study) towards accessible tourism. The study was based on surveys performed in May 2013 at the Adam Mickiewicz University in Poznań (UAM, Poland) and the State University in Irkutsk (ИГУ, Russia), a total sample of 216 people. The main section of the survey contained four questions regarding issues such as: optimal ways to organise tourism products for people with a disability; attitudes towards spending leisure time together with people with a disability; and specific requirements concerning the introduction of various types of improvements in tourism products aimed at people with a disability. In both cases, the results revealed that future tourism employees hold attitudes which are prevailingly open and positive towards the needs of tourists with disabilities. However, the hypothesis that the main factor influencing a reluctance to enter into contact with PwD is a lack of experience in this area, resulting in insufficient knowledge of what conditions the behaviour of PwD was also confirmed. This is a highly significant conclusion which should consider if mandatory educational programmes in the field of tourism and recreation studies are to be improved.
Cartographic and remote-sensing data as a source of landscape ecological information on the Poznań metropolitan area
(2010) Kijowski, Andrzej; Kubiak, Jarosław; Ławniczak, Radzym; Mania, Wojciech
This paper characterises the system of organisation and access to spatial information in Poland based on the example of the Poznań metropolitan area. It describes the available cartographic resources, both topographic (general) and thematic. Particular attention was paid to remote sensing, being the source of the most current and nongeneralised information on geographic space. As a result of the implementation of the INSPIRE directive, activities aimed at integrating and sharing spatial data in a digital form were intensified. A practical outcome of the above is presented in the article published at Geoportal (www.geoportal.gov.pl). The final part of this paper shows the current applications and requirements concerning the use of spatial data in the modern management of a metropolitan area.
Chronology and distribution of Pleistocene woolly rhinoceros: A review of the archival data from Poland
(Bogucki Wydawnictwo Naukowe, 2024) Pawłowska, Kamilla; Dedła, Kajetan; Płonka, Katarzyna
This work provides a review of the state of knowledge of woolly hinoceroses in Poland. We compile research results from the 19th century to the present day and consider the collected data not only quantitatively, but above all qualitatively. Here we present a list of 215 sites from Poland where the remains of the woolly rhinoceros have been found. Studies of woolly rhinos from Poland usually employ small samples. Our compilation of data also reveals that there is currently no basis for drawing conclusions regarding the geographical distribution pattern of the species in Poland. Only a small number of works have focused on matching the places where remains occurred with the geological conditions of the area and their depositional history. Moreover, the results show that the resolution of the radiocarbon dates that are currently published is insufficient to allow conclusions about the chronology of woolly rhinoceroses in Poland to be drawn. No works to date have dealt with any aspect of palaeopopulation research. The woolly rhinoceros is not present in Palaeolithic art in Poland. A summary of our knowledge of this taxon is the starting point for our multi-aspect research into this topic.
Coexistence of Lobelia dortmanna and Cladium mariscus, an ecological and paleobotanical study
(2021) Milecka, Krystyna; Kowalewski, Grzegorz; Lewandowska, Agnieszka; Szczuciński, Witold; Goslar, Tomasz
Lobelia dortmanna L. (Lobeliaceae family) is an indicator species that is predominantly found in oligotrophic and acidic lakes. They are mainly distributed in northwestern Europe. Their occurrence in Poland is highly threatened by the increasing grade of human activity and environmental eutrophication; however, new sites of Lobelia were discovered in the last few decades, for example, in Lake Krzywce Wielkie situated in Bory Tucholskie National Park (BTNP), Poland. The existence of Lobelia in this lake was unexpected because Cladium mariscus was also found in the lake. Cladium has different ecological demands and is regarded as a species typical of calcareous habitats where calcium is found in abundance in the substrate. To explain the coexistence of both species in Krzywce Wielkie, pollen analysis of organic sediments was performed for four short cores collected from the littoral zone of the lake and for one long deep-water core. Additionally, macrofossil analysis was done for all the short cores. Pollen analysis revealed the existence of Cladium from the early Holocene period up to the present time. Pollen and seeds of Lobelia were found to be present since the beginning of the 20th century. Development of L. dortmanna and Myriophyllum alterniflorum populations and a decrease in the number of aquatic macrophytes in the eutrophic water indicate oligotrophication of water. This process started following the construction of drainage canal and the consequent water level decrease. This situation can be attributed to the abandonment of the agricultural areas adjoining the lake, which causes a decrease in the inflow of nutrients into the lake. Development of pine forest and establishment of BTNP enabled the protection and conservation of the surrounding catchment areas, thus restricting the potential eutrophication of the habitats.
Controls on coastal flooding in the southern Baltic Sea revealed from the late Holocene sedimentary records
(2022-06-11) Leszczyńska, Karolina; Stattegger, Karl; Moskalewicz, Damian; Jagodziński, Robert; Kokociński, Mikołaj; Niedzielski, Przemysław; Szczuciński, Witold
Climate change and related sea-level rise pose significant threats to lowland coasts. However, the role of key controlling factors responsible for the frequency and landward extent of extreme storm surges is not yet fully understood. Here, we present a high-resolution sedimentary record of extreme storm surge flooding from the non-tidal southern Baltic Sea, spanning two periods: 3.6–2.9 ka BP and 0.7 ka BP until present. Sediments from coastal wetland, including sandy event layers, were analyzed by sedimentological (grain size, loss-on-ignition, micromorphology), geochronological (14C), geochemical (XRF), mineralogical (heavy minerals) and micropaleontological (diatoms) methods. The results show that both periods were characterized by high-frequency of storm surge flooding, in order of 1.3–4.2 events per century. These periods correlate with phases of enhanced storminess in northwest Europe and took place during both rising and fluctuating sea levels. The study shows that the frequency and landward extent of coastal inundation, largely depended on the development of natural barriers (e.g. beach ridges and aeolian foredunes). Thus, in the context of the future coastal storm-surge hazard, the protection of existing coastal barriers and their morphology is essential.
Cryoconite – From minerals and organic matter to bioengineered sediments on glacier's surfaces
(Elsevier, 2022) Rozwalak, Piotr; Podkowa, Paweł; Buda, Jakub; Niedzielski, Przemysław; Kawecki, Szymon; Ambrosini, Roberto; Azzoni, Roberto S.; Baccolo, Giovanni; Ceballos, Jorge L.; Cook, Joseph; Di Mauro, Biagio; Ficetola, Gentile Francesco; Franzetti, Andrea; Ignatiuk, Dariusz; Klimaszyk, Piotr; Łokas, Edyta; Ono, Masato; Parnikoza, Ivan; Pietryka, Mirosława; Pittino, Francesca; Poniecka, Ewa; Porazinska, Dorota L.; Richter, Dorota; Schmidt, Steven K.; Sommers, Pacifica; Souza-Kasprzyk, Juliana; Stibal, Marek; Szczuciński, Witold; Uetake, Jun; Wejnerowski, Łukasz; Yde, Jacob C.; Takeuchi, Nozomu; Zawierucha, Krzysztof
Cryoconite is a mixture of mineral and organic material covering glacial ice, playing important roles in biogeochemical cycles and lowering the albedo of a glacier surface. Understanding the differences in structure of cryoconite across the globe can be important in recognizing past and future changes in supraglacial environments and ice-organisms-minerals interactions. Despite the worldwide distribution and over a century of studies, the basic characteristics of cryoconite, including its forms and geochemistry, remain poorly studied. The major purpose of our study is the presentation and description of morphological diversity, chemical and photoautotrophs composition, and organic matter content of cryoconite sampled from 33 polar and mountain glaciers around the globe. Observations revealed that cryoconite is represented by various morphologies including loose and granular forms. Granular cryoconite includes smooth, rounded, or irregularly shaped forms; with some having their surfaces covered by cyanobacteria filaments. The occurrence of granules increased with the organic matter content in cryoconite. Moreover, a major driver of cryoconite colouring was the concentration of organic matter and its interplay with minerals. The structure of cyanobacteria and algae communities in cryoconite differs between glaciers, but representatives of cyanobacteria families Pseudanabaenaceae and Phormidiaceae, and algae familiesMesotaeniaceae and Ulotrichaceae were the most common. The most of detected cyanobacterial taxa are known to produce polymeric substances (EPS) that may cement granules. Organic matter content in cryoconite varied between glaciers, ranging from 1% to 38%. The geochemistry of all the investigated samples reflected local sediment sources, except of highly concentrated Pb and Hg in cryoconite collected from Europeanglaciers near indus-rialized regions, corroborating cryoconite as element-specific collector and potential environmental indicator of anthropogenic activity. Our work supports a notion that cryoconite may be more than just simple sediment and instead exhibits complex structure with relevance for biodiversity and the functioning of glacial ecosystems.
DEVELOPMENT OF RURAL LANDSCAPE IN WIELKOPOLSKA IN REFERENCE TO METABOLISM OF AGROECOSYSTEMS
(2007) Mizgajski, Andrzej
The purpose of this paper is to show the main features of landscape development in a regional scale with reference to socio-economic conditions and the processes of energy and matter flow in agroecosystems. Four main phases of rural landscape development have been distinguished during which the dominant processes determining the functioning of agroecosystems changed. After the initial phase there was a period of spatial expansion of the rural landscape at the expense of natural forests; this phase was followed by the intensification of use through increased external feeding of agroecosystems in energy and matter, and currently the diversification of human influence on environmental systems is becoming increasingly noticeable. The social role of farmers is going to be of fundamental importance to the future of the rural landscape. It is necessary to stimulate their behaviour to make sure that they acquire knowledge, skills and motivation to protect natural environment and the landscape.
Drift-dependent changes in iceberg size-frequency distributions
(Nature Publishing Group, 2017-11) Kirkham, James D.; Rosser, Nick J.; Wainwright, John; Vann Jones, Emma C.; Dunning, Stuart A.; Lane, Victoria S.; Hawthorn, David E.; Strzelecki, Mateusz C.; Szczuciński, Witold
Although the size-frequency distributions of icebergs can provide insight into how they disintegrate, our understanding of this process is incomplete. Fundamentally, there is a discrepancy between iceberg power-law size-frequency distributions observed at glacial calving fronts and lognormal size-frequency distributions observed globally within open waters that remains unexplained. Here we use passive seismic monitoring to examine mechanisms of iceberg disintegration as a function of drift. Our results indicate that the shift in the size-frequency distribution of iceberg sizes observed is a product of fracture-driven iceberg disintegration and dimensional reductions through melting. We suggest that changes in the characteristic size-frequency scaling of icebergs can be explained by the emergence of a dominant set of driving processes of iceberg degradation towards the open ocean. Consequently, the size-frequency distribution required to model iceberg distributions accurately must vary according to distance from the calving front.
Early Permian solitary rugose corals from Kruseryggen (Treskelodden Fm., Hornsund area, southern Spitsbergen)
(Bogucki Wydawnictwo Naukowe, 2009) Chwieduk, Edward
A collection of solitary rugose corals collected from the Treskelodden Formation of the Kruseryggen Hill, Hornsund area, south Spitsbergen, consists of 30 specimens representing the Bothrophyllidae family with the genera Bothrophyllum, Caninophyllum, Hornsundia, and Timania (5 species), and an indeterminate family with the genus Svalbardphyllum (one species). These large, dissepimental forms, dating from the Early Sakmarian (Tastubian), indicate a warm-water environment. The lithology, the thickness of the succession, the reddish hue and the abrasion of the fossils indicate that the area of the inner Hornsund showed a relief that enabled considerable erosion of the elevated areas and redeposition of the fossils at remote locations. The changing morphology of this area during the Early Permian was probably influenced by synsedimentary block tectonics.
Easily-accessible digital palaeontological databases – a new perspective for the storage of palaeontological information
(Bogucki Wydawnictwo Naukowe, 2009) Wolniewicz, Paweł
Techniques that allow to render diverse types of palaeontological data as publicly available internet resources are described. In order to develop an easily accessible digital palaeontological database, three steps should be followed: (1) digitization of the studied specimens, (2) acquisition of morphometric data, and (3) contribution of the data to open and searchable geoinformatic (palaeontological) databases. Digital data should be submitted to internet databases that allow a user to fetch various types of information from dispersed sources (semantic web services).
Elevation and volume changes of seven Dickson Land glaciers, Svalbard, Pyramiden region, 1960-1990-2009
(2013-10) Małecki, Jakub
Melting Svalbard glaciers have been recognized as an early indicator of climate change. Large parts of Svalbard remain little investigated, including Dickson Land, in the quasi-continental interior of Svalbard. In this study, elevation and volume changes of seven glaciers located in the Pyramiden region are assessed by analysing contour lines from 1960 topographic maps and photogrammetrically derived 1990 and 2009 digital elevation models. Mass loss was documented for all seven glaciers. In the period 1960-1990 their average elevation change rate was -0.49 m a-1, while in the more recent period, 1990-2009, it was more negative at -0.78 m a-1, caused by a significant equilibrium line altitude shift with post-1990 rise in summer temperatures. Large variation in elevation change rates between individual glaciers was found and is attributed mainly to aspect and hypsometry. This highlights the importance of choosing a representative sample when investigating mass balance of whole regions. Evidence of a rapid increase in thinning rates in the upper parts of the studied glaciers, linked to decreasing albedo in former accumulation zones, was also found.
Engineering-geological and geotechnical investigations for risk assessment of the University Olympic Village in Izmir (Turkey)
(Bogucki Wydawnictwo Naukowe, 2010-03) Kincal, Cem; Koca, Mehmed Yalçin; Yilmaz, H. Recep; Akgün, Mustafa; Özyalm, Şenol; Eskişar, Tuğba; Akçiğ, Zafer; van Loon, A.J. (Tom)
The Metropolitan Municipality of Izmir (Turkey) designated a steeply inclined area for the construction of buildings to house the participants of the Izmir University Olympic Games. Before the construction activities could start, engineering geological and geotechnical investigations had to be carried out in order to establish which zones in the area were suitable for safe constructions. Seismic studies, borings and laboratory tests yielded the data, which were used for preparing five hazard maps in a GIS environment. The construction activities based on the results of this complex investigation appeared successful. The engineering geological investigations included geotechnical measurements on core samples obtained from the boreholes (core drilling) and laboratory testing. The rock-quality designation (RQD%) values of the rock units were determined and used in the rock-mass classification (rock-mass rating method) as an in-put parameter and in the calculation of the bearing capacity of the various rock units. Geophysical surveys were carried out to determine the seismic velocity of the rocks at the site. A short overview is provided of the main problems that had to be dealt with, and of the successive steps taken to solve the engineering-geological problems. Determination of these problems is necessary for adequate land-use planning and construction activities.
Evaluation of Methods for Estimating Lake Surface Water Temperature Using Landsat 8
(2022-08-08) Dyba, Krzysztof; Ermida, Sofia; Ptak, Mariusz; Piekarczyk, Jan; Sojka, Mariusz
Changes in lake water temperature, observed with the greatest intensity during the last two decades, may significantly affect the functioning of these unique ecosystems. Currently, in situ studies in Poland are conducted only for 38 lakes using the single-point method. The aim of this study was to develop a method for remote sensing monitoring of lake water temperature in a spatio-temporal context based on Landsat 8 imagery. For this purpose, using data obtained for 28 lakes from the period 2013–2020, linear regression (LM) and random forest (RF) models were developed to estimate surface water temperature. In addition, analysis of Landsat Level-2 Surface Temperature Science Product (LST-L2) data provided by United States Geological Survey (USGS) and the National Aeronautics and Space Administration (NASA) was performed. The remaining 10 lakes not previously used in the model development stage were used to validate model performance. The results showed that the most accurate estimation is possible using the RF method for which RMSE = 1.83 °C and R^2 = 0.89, while RMSE = 3.68 °C and R^2 = 0.8 for the LST-L2 method. We found that LST-L2 contains a systematic error in the coastal zone, which can be corrected and eventually improve the quality of estimation. The satellite-based method makes it possible to determine water temperature for all lakes in Poland at different times and to understand the influence of climatic factors affecting temperature at the regional scale. On the other hand, spatial presentation of thermics within individual lakes enables understanding the influence of local factors and morphometric conditions.
Evidence of probable paleotsunami deposits on Kho Khao Island, Phang Nga Province, Thailand
(Springer, 2012) Yawsangratt, Supawit; Szczuciński, Witold; Chaimanee, Niran; Chatprasert, Sirapapa; Majewski, Wojciech; Lorenc, Stanisław
The 2004 tsunami deposits and probable paleotsunami deposits were studied at the southern Kho Khao Island, on Andaman Sea coast of Thailand. The 2004 tsunami laid down about 8cm of fining upward medium sand and locally about 40cm of massive coarse sand with common mud clasts. The sediments were characterized by the presence of marine foraminiferal assemblage; however, already after 5years many of carbonate foraminiferal tests were partly or completely dissolved. The probable paleotsunami deposits form layer about 1m thick. It consists of massive very coarse sand with common big shells and mud clasts. Its composition suggests a marine origin and the presence of mud clasts, and similarity to the 2004 tsunami deposits suggests that the layer was left by paleotsunami, which took place probably during the late Holocene, even though two shells within the layer gave 14C ages of 40,000years or more.
Explanation of the influence of geomorphometric variables on the landform classification based on selected areas in Poland
(Nature Publishing Group, 2024-03-05) Dyba, Krzysztof
In recent years, automatic image classification methods have significantly progressed, notably black box algorithms such as machine learning and deep learning. Unfortunately, such efforts only focused on improving performance, rather than attempting to explain and interpret how classification models actually operate. This article compares three state-of-the-art algorithms incorporating random forests, gradient boosting and convolutional neural networks for geomorphological mapping. It also attempts to explain how the most effective classifier makes decisions by evaluating which of the geomorphometric variables are most important for automatic mapping and how they affect the classification results using one of the explainable artificial intelligence techniques, namely accumulated local effects (ALE). This method allows us to understand the relationship between predictors and the model’s outcome. For these purposes, eight sheets of the digital geomorphological map of Poland on the scale of 1:100,000 were used as the reference material. The classification results were validated using the holdout method and cross-validation for individual sheets representing different morphogenetic zones. The terrain elevation entropy, absolute elevation, aggregated median elevation and standard deviation of elevation had the greatest impact on the classification results among the 15 geomorphometric variables considered. The ALE analysis was conducted for the XGBoost classifier, which achieved the highest accuracy of 92.8%, ahead of Random Forests at 84% and LightGBM at 73.7% and U-Net at 59.8%. We conclude that automatic classification can support geomorphological mapping only if the geomorphological characteristics in the predicted area are similar to those in the training dataset. The ALE plots allow us to analyze the relationship between geomorphometric variables and landform membership, which helps clarify their role in the classification process.
Fires, vegetation, and human - The history of critical transitions during the last 1000 years in Northeastern Mongolia
(2022-09) Słowiński, Michał; Obremska, Milena; Avirmed, Dashtseren; Woszczyk, Michał; Adiya, Saruulzaya; Łuców, Dominika; Mroczkowska, Agnieszka; Hałaś, Agnieszka; Szczuciński, Witold; Kruk, Andrzej; Lamentowicz, Mariusz; Stańczak, Joanna; Rudaya, Natalia
Fires are natural phenomena that impact human behaviors, vegetation, and landscape functions. However, the long-term history of fire, especially in the permafrost marginal zone of Central Asia (Mongolia), is poorly understood. This paper presents the results of radiocarbon and short-lived radionuclides (210Pb and 137Cs) dating, pollen, geochemical, charcoal, and statistical analyses (Kohonen's artificial neural network) of sediment core obtained from Northern Mongolia (the Khentii Mountains region). Therefore, we present the first high-resolution fire history from Northern Mongolia covering the last 1000 years, based on a multiproxy analysis of peat archive data. The results revealed that most of the fires in the region were likely initiated by natural factors, which were probably related to heatwaves causing prolonged droughts. We have demonstrated the link between enhanced fires and “dzud”, a local climatic phenomenon. The number of livestock, which has been increasing for several decades, and the observed climatic changes are superimposed to cause “dzud”, a deadly combination of droughts and snowy winter, which affects fire intensity. We observed that the study area has a sensitive ecosystem that reacts quickly to climate change. In terms of changes in the vegetation, the reconstruction reflected climate variations during the last millennium, the degradation of permafrost and occurrence of fires. However, more sites with good chronologies are needed to thoroughly understand the spatial relationships between changing climate, permafrost degradation, and vegetation change, which ultimately affect the nomadic societies in the region of Central and Northern Mongolia.

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