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This paper is an introduction to a collection of nine studies that are intended to fill the gap in the literature associated with landform development and landscape changes related to natural forces and human activities in the Central European Mountains and their close forelands. The papers are grouped into four general categories that describe the influence of climate on glacial landforms and snow avalanches, the evolution of slopes in high mountains, the development of mid-mountain relief, and changes in fluvial systems in mountains and their forelands. This paper summarises the contributions of these studies to this special issue and attempts to outline possible avenues of future research on landforms and landscapes in mountainous areas. [ABSTRACT FROM AUTHOR]

This commentary responds to Tim Oakes' analysis of infrastructural power by examining the inherent fragility of mobility infrastructures and their political ramifications. It emphasizes the human element in creating and maintaining these infrastructures, highlighting the intricate interplay of political will, bureaucratic planning, technological know-how, and specialized skills needed for their implementation. The paper contends that the COVID-19 pandemic has starkly demonstrated the vulnerability of mobility infrastructures to rapid collapse. It further explores the concept of infra-politics, referring to subtle acts of resistance within these networks, which significantly disrupt their efficient operation. The Chinese concept of jianghu, representing a metaphorical space of alterity, is introduced to propose that infra-politics might evolve into alternative relational forms, challenging and potentially subverting the dominance of centralized networks. [ABSTRACT FROM AUTHOR]

Antarctic Treaty Consultative Parties are entitled to participate in consensus-based governance of the continent through the annual Antarctic Treaty Consultative Meetings. To acquire consultative status, an interested Party must demonstrate "substantial research activity," but no agreed mechanism exists to determine whether a Party has fulfilled this criterion. Parties have generally demonstrated substantial research activity with the construction of a research station, as suggested within the Treaty itself. However, this largely demonstrates logistical capacity, rather than research activity, and often results in major and persistent impacts on Antarctic terrestrial environments. Our study found that national investment in Antarctic infrastructure, estimated by the number of bed spaces at stations, was not a reliable indicator of scientific output. Therefore, we investigated metrics to evaluate research activity directly, and identified both the overall number of Antarctic papers and the proportion of national scientific output these represented as meaningful metrics. Such metrics could (1) demonstrate a nation's level of research activity in Antarctica or (2) help Consultative Parties assess the level of research activity undertaken by a Party seeking to acquire consultative status. Our data showed that, even without land-based Antarctic infrastructure, Canada, Denmark and Switzerland may have reasonable grounds to demonstrate "substantial research activity" on a level comparable with existing Consultative Parties. The use of these metrics may help dispel any perceived requirement for the establishment of a research station to reach consultative status, by putting a greater emphasis on generation of scientific research outputs rather than construction of Antarctic infrastructure. [ABSTRACT FROM AUTHOR]

This document is an editorial published in the journal Frontiers in Environmental Science. It discusses the challenges faced by water and environmental sustainability in watersheds due to climate change and human interference. The editorial emphasizes the need for interdisciplinary research to understand the dynamics of watershed hydrology, water quality, and ecology. It also highlights the importance of adaptive management approaches to address the complexity and uncertainty associated with environmental changes. The document concludes by presenting recent research papers that explore watershed environmental changes and sustainable management worldwide. [Extracted from the article]

Mediterranean coastal dunes have an undeniable value in terms of floristic diversity as a result of their well-adapted plant species, such as psammophytes and halophytes. Unfortunately, these ecosystems are often disturbed by anthropogenic activities, such as the use of bathing settlements and trampling, the construction of paths or roads, and grazing by livestock. In this paper, these environmental factors were considered to determine their relative influences on several Algerian coastal dune systems undergoing ecological disturbance, by measuring in these systems various ecological gradients. Using ecological indices, multivariate analysis of data, and the analysis of variance, we compared the composition of the flora of 7 study sites that were subjected to various scales and types of disturbances. A total of 83 plant species were identified, reflecting the floristic richness of the sites. They seemed to be unevenly distributed and considerably modified according to environmental and human impact descriptors. The composition, abundance, and distribution of plant diversity are positively correlated with the height and width of the dunes. Regrettably, the floristic diversity of coastal dunes is more and more degraded by disturbance pressures (particularly grazing). [ABSTRACT FROM AUTHOR]

This paper presents new results on a quali-quantitative analysis of the heterocysts of the Rivularia type as a key bioindicator informative on local eutrophic conditions. The Rivularia type is usually reported in palynological analyses due to the thick, multilayered envelope that ensures the preservation of heterocysts in sediments. Samples come from two continuous terrestrial cores (N-S3: 77 samples, C-S1: 20 samples) drilled in the area surrounding the Bronze Age site of the Terramara S. Rosa di Poviglio (Po Plain; N Italy) and spanning at least over the last 15 ka years. Concentrations and percentages of the Rivularia type, combined with pollen curves of wet environments, describe local variability and rapid changes in ecological conditions over the millennia of deposition. Given the abundance and diversity of heterocysts of the Rivularia type in the studied samples, this paper attempts to group these cells based on morphology (ellipsoidal or elongated) and the state of preservation of the sheaths (presence or absence). Actually, it is difficult to confirm a relationship between heterocyst morphologies and the presence of different cyanobacteria species. Increasingly accurate identification of heterocysts from biostratigraphical archives may improve the data available on these bioindicators for achieving more detailed decoding of wetland (and terrestrial) transformations. Since the Bronze Age and at the most recent levels, the Rivularia type may be a good indicator of the local presence of agriculture and livestock, which lead to trophic and water changes in the soil. [ABSTRACT FROM AUTHOR]

Detailed palaeogeographical studies of the accumulative fan in the Serteyka River valley in W Russia and underlying biogenic deposits were carried out. The base of a representative core of biogenic sediments in the distal zone is dated to 1291 BC, while its top to 1631 AD. In this paper, palynological, plant macrofossils, Chironomide and Cladocera, geochemical, geochronological and sedimentological analysis were performed. Four phases of biogenic deposition were distinguished by pollen and geochemical analyses. Two of them coincide with the climatic fluctuation during Medieval Climate Anomaly and Little Ice Age. During the formation of the fan, overbank deposits were accumulated also, indicating numerous and intense floods, which are in line with the trend observed for other sites in this region. The accumulative fan is formed by lower, middle and upper deluvia and agricultural diamicton in its top. All units have specific sedimentological and geochemical features as well as low admixture of plant macrofossils. The beginning of the formation of this relief form dates back to the second half of the 17th century AD, and the end of the accumulation falls on the second half of the 18th century AD. Our work suggests that natural conditions had an impact on the formation and development of studied accumulative fan, however, the decisive factor causing the intensification of the slope processes were related with deforestation resulted from strong human impact, which was marked in palynological and macrofossils analyses (e.g. increase in the contribution of plants macrofossils related to agriculture). [ABSTRACT FROM AUTHOR]

Land use and settlement dynamics of two rural areas defined by the contact karst spring is the subject of this paper. The research area consists of the spring catchment of Ljubija in the northeast part of Slovenia and Gradole, the most water-rich spring in Istria (northwest Croatia), have been surveyed in terms of environmental conditions, and social and historic land use aspects. We used Statistical data and Geographic Information System (GIS) methods. Via a multidisciplinary approach we discovered that: 1) environmentally, both areas are actively managed due to drinking water resources— Gradole has 9.8% and Ljubija 8.9% of protected area; 2) data regarding social features showed that human pressure has not negatively influenced the natural settings and water supply vulnerability—the area of the Ljubija spring catchment has lower population density compared to the area of the Gradole spring catchment (1.4 inhabitants/ km² compared to 38.7 inhabitants/km² ), but the Ljubija area has more pronounced growth in the number of households—I2020/1948 = 115 compared to I2020/1948 = 88.1 at the Gradole spring catchment; and 3) the limited regeneration abilities of the karst water bodies have been preserved by the prevailing share of forest—land use data showed 84.8% for Ljubija and 34.4% for Gradole. [ABSTRACT FROM AUTHOR]

Channel incision is an evident trend for river evolution in many European rivers and notably the Western Carpathians, whose former braided and multichannel wandering river system is transforming into a single‐thread channel, but it is often difficult to separate drivers and determine if incision is finished or is still ongoing. To overpass these research gaps, this paper presents an innovative approach to assess the multidecadal incision of the Belá River in the Western Carpathians since 1949 by LiDAR‐based analyses of floodplain surfaces above the river channel dated from historical aerial images. Detailed analyses of ongoing incision were also calculated based on DEM of differences (DoD) using Structure‐from‐Motion (SfM) photogrammetry‐derived topo‐bathymetric models. The study applied the BACI (Before‐After‐Control‐Impact) approach that compared pre‐state (Before), post‐state (After) and reach (Control) that is not affected by potential external effects with degraded (impacted) reach to be able to distinguish the driver effects. Floodplain channel surface analyses indicate the maximum incision up to 4 m and incision rate of 5.7 cm/year that occurred in the most degraded reach. Moreover, cross‐section profiles point to accelerated incision of 24.5 cm/year in the last 10 years (2011–2021) by the propagation of incision upstream. Overall, the net changes from the UAV survey pointed to 22 759 m3 of gravel sediments, constituting outwash from the 1.6 km long channel system (2015–2022) by incision, whereas analyses of historical channel surfaces estimated erosion of 573 303 m3 from impacted reaches between 1949 and 2020. Incision evidence is only observed in the downstream part below the control section due to local drivers (channel regulation, comprising embankment and gravel mining that activated a backward erosion of the system with knickpoint migration upstream). This analysis shows the benefits of combining different sources of data to separate long‐term and ongoing channel responses and the BACI‐approach to better target cause–effect relationships in space and time. [ABSTRACT FROM AUTHOR]

This paper interprets the first archaeobotanical data to emerge from the island of Ustica (north-western Sicily, Italy). The excavation of the Neolithic site of Piano dei Cardoni (4600-4200 cal BC) and the Middle Bronze Age site of Faraglioni Village (1500-1250 cal BC), has made it possible to analyse plant macro-remains and compare them with data on local vegetation obtained from both historical literary sources and recent field surveys. The onset of agro-pastoral practices in the mid-5th millennium BC brought about significant changes to the local pristine plant communities. Indeed, the presence of holm oaks and pine trees in that period was recently detected for the first time. The evolution of the local vegetation following the first human settlement in the Neolithic has some crucial parallels with what happened following the recolonisation of the mid-eighteenth century. The massive presence of olive trees during the Middle Bronze Age suggests the deliberate introduction of this crop species on the island and attests to olives' paramount importance for the local economy at that time. The disappearance of some woody species shows that human occupation has had a powerful impact on the island's forest resources, which partially recovered during the repeated long phases of land abandonment. [ABSTRACT FROM AUTHOR]

Aquatic ecosystems are under pressure due to human activity. In the summer of 2022, the Odra River (Central Europe) suffered a massive death of fish and mollusks. This paper aims to show selected water quality parameters before and during the ecological disaster and find which parameters may have been crucial to the development of this disaster. We used the Kruskal–Wallis test and Spearman's correlation to check the water parameters' spatial and temporal diversification. In addition, non-metric multidimensional scaling was performed. The water quality parameters of the Odra system were analyzed in sections: middle Odra, lower Odra, transitional waters, and Szczecin Lagoon. Human activity has led to the formation of a system with unusual characteristics, disturbing the river's natural continuum and related processes. The year 2022 in the middle Odra differed from the previous years in having a high water temperature (>24 °C), high ammonium concentrations (>4 mg/L), and relatively low nitrate concentrations (<6.5 mg/L). At the same time, salt pollution in the river was very high (maximum 1.4 g/L). In June and July 2022, we observed low chlorophyll a concentrations in the middle Odra (on average 2.3 µg/L and 4.4 µg/L, respectively), presumably due to salinity stress and high temperatures, suppressing freshwater phytoplankton taxa. This circumstance has created the appropriate conditions for developing euryhaline and thermophilic Prymnesium parvum. Because of decaying organisms, hypoxia occurred in the lower Odra (0.26 mg/L of dissolved oxygen in surface waters), and oxygen conditions worsened in the transitional waters (<4 mg/L). The zonal deaths of fish and mollusks result from multiple stressors induced by human activity. This disaster has proven that it is necessary to improve selected water quality parameters to reduce the risk of such disasters. The most urgent recommendations are to reduce the salt pollution of the upper section of the Odra, reduce nutrient inputs, and improve the condition of smaller rivers feeding the main course of the Odra. [ABSTRACT FROM AUTHOR]

Although several studies have examined the functional diversity of freshwater macroinvertebrates, the variety of methodologies combined with the absence of a synthetic review make our understanding of this field incomplete. Therefore, we reviewed the current methodology for assessing functional diversity in freshwater macroinvertebrate research. Our review showed that most papers quantified functional diversity using biological traits, among which feeding habits were the most common traits probably due to the assumed links between feeding and ecosystem functions. A large number of diversity measures have been applied for quantifying functional diversity of freshwater macroinvertebrate assemblages, among which Rao's quadratic entropy looks like the most frequent. In most papers, functional diversity was positively related to taxon richness, and functional redundancy was a key concept in explaining this correlation. Most studies detected strong influence of the environmental factors as well as human impact on functional diversity. Finally, our review revealed that functional diversity research is biased towards European running waters and is hindered by yet insufficient information on the autecology of macroinvertebrates. [ABSTRACT FROM AUTHOR]

Drones are currently used for various purposes. The ever-increasing number of professionally or amateurly used drones is causing an ever-increasing noise load in the area. Those sources of noise that occur historically in the environment (dor example railways) are currently perceived by people as less disturbing. On the contrary, new noise sources are perceived as significantly disturbing (various types of industrial noise) and people are not able to tolerate them. Drone is a completely new and so far not explored source of noise, which is characterized by a specific spectral composition of noise and often subjectively felt a high degree of interference. At present, there are no clear national or international methodologies for assessing the impact of drones on the population. For this reason, we have started research in this area in order to develop a methodology for assessing this specific noise source. We also consider it important that this period of drone growth in some countries is crucial for the accelerated implementation of methodological procedures for dealing with noise issues. The paper proposes a basic methodology for assessing the impact of drones on humans and performed noise measurements at different flight speeds for two types of drones. [ABSTRACT FROM AUTHOR]

Copyright of Journal of Forestry Society of Croatia / Sumarski List Hrvatskoga Sumarskoga Drustva is the property of Forestry Society of Croatia and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Anticipating future successional forest trends in the face of ongoing global change is an essential conservation target. Mountain forests are especially sensitive to environmental shifts, and their past responses to climatic and anthropogenic (external) drivers may provide a basis for improving predictions of future developments. This paper uses independent high-resolution palynological and paleoclimatic reconstructions to statistically analyze the long-term effects of external drivers on regional forest succession in the central Iberian Pyrenees during the last 500 years. The statistical methods used are Gaussian response analysis, cluster analysis, rate-of-change analysis, principal component analysis, and redundancy analysis. The dominant taxa of these forests (Quercus, Betula, Pinus) showed significant relationships with summer temperature, summer drought, and autumn precipitation. Immediate and delayed (by two or more decades) responses of these trees to climatic drivers were identified. Regional succession showed a closed path, starting at the end points around the attraction domain of pine-dominated forests. This trajectory was determined by a trend toward anthropogenic forest clearing (16th to 18th centuries) and a reverse trend of natural forest recovery (18th to 20th centuries). Forest clearing was due to burning, facilitated by drought, and was followed by the expansion of cropping and grazing lands. Forest recovery was fostered by reduced human pressure and rising temperatures. The statistical approach used in this work has unraveled ecological relationships that remained unnoticed in previous works and would be important for predicting future successional trends under changing climates. The reported response lags of individual taxa to climatic drivers may complicate the establishment of reliable ecological relationships and should be addressed in future studies. [ABSTRACT FROM AUTHOR]

Wetlands in mountains are highly dynamic and provide ecosystem services to human wellbeing. Understanding temporal and spatial wetland dynamics is crucial for successful management. This paper presents the reconstruction of a mire evolution at a high-altitude Andean valley in central-western Argentina, in subtropical South America (30°-36° S), during the Mid- and Late Holocene. The research is based on sedimentological and pollen analysis from a sedimentary section of 3.2 m thick exposed at the El Peñón valley. The record begins with an outwash environment after ca. 5700 cal. yrs BP associated with Pteridophytes dominance, followed by the development of a mire environment after ca. 3700 cal. yrs BP associated with Cyperaceae dominance. The environmental and vegetation changes are hypothesised to have occurred in response to a shift from cold to warmer conditions. Colder environments may have occurred again between 800 until < 600 cal. yrs BP, probably associated with the Little Ice Age. Tephra inputs are evidenced in the record from 1200 years BP onwards. However, the results do not show any conclusive evidence about the impact of volcanism in the dynamics of the wetland. High Amaranthaceae proportions would evidence human activities in the high-altitude valleys of the southern Andes, probably for the last 250 cal. yrs BP. This work permitted us to infer the evolution of the El Peñón wetland under multiple concurrent forcing factors from the Mid- Holocene onwards at different temporal scales, i.e. climate during the last 5700 yrs, and volcanism and anthropogenic impacts during the last millennium. [ABSTRACT FROM AUTHOR]

Whereas 6 decades ago little attention was accorded to the influence of human activity on affecting river channel adjustment, great progress has been made subsequently, with many contributions published in River Research and Applications. Many concepts have been involved, and this paper considers how they have arisen and developed during a sequence of complementary research stages. The first stage during the 1970s and 1980s, including research by Geoff Petts, involved "recognition of change" and saw the emergence of two separate research strands focused on different timescales: over shorter timescales river channel adjustments affected by the impacts of dams and reservoirs, channelization, land use changes, and urban effects; over longer timescales investigations of river metamorphosis. The second "realization" stage involved significant advances in understanding by considering interaction between these two timescales, more detailed investigations of changing processes, a more holistic catchment‐based approach, and incorporation of ecological changes. These advances led into the third stage, "application" of results, stimulated by analysis of the effects of hard and soft engineering, development of international drivers such as the Water Framework Directive, and concern for what is "natural." This paper evaluates this sequence of stages, the concepts that have emerged, the extent to which they are consistent and sustainable, and how they can provide the foundation for evaluation of channel adjustments. The effects of urbanization in Fountain Hills, Arizona, USA provide an illustration. Finally, the future requirement for adaptation of existing concepts and the possible development of new ones is briefly considered in the context of global environmental changes. [ABSTRACT FROM AUTHOR]

As a result of climate change/variation and its aggravation by human activities over the past several decades, the hydrological conditions in the middle Yellow River in China have dramatically changed, which has led to a sharp decrease of streamflow and the drying up of certain tributaries. This paper simulated and analysed the impact of sediment-trapping dams (STDs, a type of large-sized check dam used to prevent sediment from entering the Yellow River main stem) on hydrological processes, and the study area was located in the 3246 km2 Huangfuchuan River basin. Changes in the hydrological processes were analysed, and periods of natural and disturbed states were defined. Subsequently, the number and distribution of the STDs were determined based on data collected from statistical reports and identified from remote sensing images, and the topological relationships between the STDs and high-resolution river reaches were established. A hydrological model, the digital Yellow River integrated model, was used to simulate the STD impact on the hydrological processes, and the maximum STD impact was evaluated through a comparison between the simulation results with and without the STDs, which revealed that the interception effect of the STDs contributed to the decrease of the streamflow by approximately 39%. This paper also analysed the relationship between the spatial distribution of the STDs and rainfall in the Huangfuchuan River basin and revealed that future soil and water conservation measures should focus on areas with a higher average annual rainfall and higher number of rainstorm hours. © 2015 The Authors Hydrological Processes Published by John Wiley & Sons Ltd. [ABSTRACT FROM AUTHOR]

The nature and extent of past indigenous transformations in the Amazon basin is an actively debated topic, and one that has important implications for both conservation policy and the cultural heritage of its indigenous and traditional populations. The use of charcoal and phytoliths to measure past human impacts in non-lacustrine settings has become especially influential in this debate but has also generated disagreement among scholars regarding the possible limits of these proxies for detecting ancient land-use. To contribute empirical data to this issue, our paper presents the first attempt to study charcoal and phytolith signals from areas of modern indigenous land-use, in the Xingu Indigenous Territory, southern Amazonia. Our findings show that, while charcoal and early successional herb phytoliths are good indicators of land-use intensity, certain types of land-use leave subtler traces in the phytolith record that can hinder their detection. We demonstrate how using finer sampling resolution and comparing local proxy data on their own terms are necessary steps in order to identify trends in human land-use across time and space. [ABSTRACT FROM AUTHOR]

As a contribution to the World Environment Day 2017, the Accademia Nazionale dei Lincei promoted the meeting “Changes and Crises in the Mediterranean Sea” devoted to the effects of climate change and human impact on the Mediterranean ecosystems and biodiversity. Here is presented a selection of papers given at the meeting held in Rome, on October 17, 2017. Studies deal with structural changes in the marine communities, the impact of thermal stress, acidification, pollution and fishing activities on benthic communities, and on deep-sea biodiversity and ecosystems. Understanding human impact on the Mediterranean Sea is the first step to manage and protect marine environments in a sustainable way. [ABSTRACT FROM AUTHOR]

The unique aquatic Pontocaspian (PC) biota of the Black Sea Basin (BSB) is in decline. The lack of detailed knowledge on the status and trends of species, populations, and communities hampers a thorough risk assessment and precludes effective conservation. This paper reviews PC biodiversity trends in the BSB (Bulgaria, Romania, Moldova, Ukraine, and Russia) using endemic mollusks as a model group. We aim to assess changes in PC habitats, community structure, and species distribution over the past century and to identify direct anthropogenic threats. The presence/absence data of target mollusk species were assembled from literature, reports, and personal observations. Pontocaspian biodiversity trends in the northwestern BSB coastal regions were established by comparing 20th‐ and 21st‐century occurrences. The direct drivers of habitat and biodiversity change were identified and documented. We found that a pronounced decline of PC species and communities is driven by (a) damming of rivers, (b) habitat modifications that disturbed previous natural salinity gradients and settings in the studied area, (c) pollution and eutrophication, (d) invasive alien species, and (e) climate change. Four out of the 10 studied regions, namely, the Danube Delta–Razim Lake system, Dniester Liman, Dnieper–Bug estuary, and Taganrog Bay–Don Delta, contain favorable ecological conditions for PC communities and still host threatened endemic PC mollusk species. Distribution data are incomplete, but the scale of deterioration of PC species and communities is evident from the assembled data, as are major direct threats. Pontocaspian biodiversity in the BSB is profoundly affected by human activities. Standardized observation and collection data as well as precise definition of PC biota and habitats are necessary for targeted conservation actions. This study will help to set the research and policy agenda required to improve data collection to accommodate effective conservation of the unique PC biota. [ABSTRACT FROM AUTHOR]

The paper concerns the transformation of water resources induced by the construction and functioning of the Brest Fortress defence structure and presents the current water resources resulting from these changes. The study was conducted by analysing historical materials: maps, plans and written documents. Hydrographic changes were analysed for five study periods covering almost 200 years, from 1823, presenting the hydrographic network before the construction of fortifications, up to 2018, when most of these structures ceased or were repurposed. Hydrographic changes were analysed in detail for the area of the Terespol Fortification. The analysis revealed that almost 80% of the wetland area had disappeared after intensive drainage works, and several dozen originally small and isolated areas had been incorporated into a vast drainage network. One of the consequences of these activities was the creation of significantly transformed artificial catchments within the study area. [ABSTRACT FROM AUTHOR]

We hope that this selection of papers will stimulate interest and research into those wonderful ecosystems that are TMFs and their elevation gradients, and provide insights into the future of TMF ecosystems in a century of rapid climate change. Keywords: carbon dynamics; cloud forests; global change; leaf traits; soil microbiome; human impact; resilience; abiotic stress EN carbon dynamics cloud forests global change leaf traits soil microbiome human impact resilience abiotic stress 1 5 5 08/13/21 20210811 NES 210811 Tropical montane forests (TMFs) are found on most of Earth's continents along variable elevation ranges, whose potential upper limits are influenced by cloud condensation heights and minimum temperatures. They assess how carbon stocks vary along elevation gradients and determine the influence of climate, particularly precipitation seasonality, on the distribution of these stocks across different forest compartments. The sensitivity of tropical leaf litter decomposition to temperature: results from a large-scale leaf translocation experiment along an elevation gradient in Peruvian forests. [Extracted from the article]

The paper presents a simple qualitative model of environmental consequences of wildlife tourism. Qualitative models use just three values: Positive/Increasing, Zero/Constant and Negative/Decreasing. Such quantifiers of trends are the least information intensive. Qualitative models can be useful, since models of wildlife tourism include such variables as, for example, Biodiversity (BIO), Animals' habituation to tourists (HAB) or Plant composition change (PLA) that are sometimes difficult or costly to quantify. Hence, a significant fraction of available information about wildlife tourism and its consequences is not of numerical nature, for example, if HAB is increasing then BIO is decreasing. Such equationless relations are studied in this paper. The model has 10 variables and 20 equationless pairwise interrelations among them. The model is solved and 15 solutions, that is, scenarios are obtained. All qualitative states, including the first and second qualitative derivatives with respect to time, of all variables are specified for each scenario. [ABSTRACT FROM AUTHOR]

The development since the beginning of the 20th century of the pollen-analytical theory and method as a palaeoecological tool for describing landscape development is outlined with reference to southern Scandinavia. Numerical methods applied since the 1980s are discussed. The aim of this paper is to provide a new perspective on the landscape development and human impact during the Holocene by applying the Regional Estimates of VEgetation Abundance from Large Sites (REVEALS) model to the pollen records from the reference site Lake Färskesjön in SE Sweden. The model was applied both to a previously published record (core 1956, entire Holocene until ad 1600) and a newly collected dataset (core 2013, the last 3000 years). The comparison between the REVEALS estimates of vegetation cover and historical landscape maps indicate that traditional, uncorrected pollen percentages significantly underestimate the degree of landscape openness created by long-term farming and pasturing, but that the degree of underestimation varies over time, depending on the species composition of both the forest and the open-land communities. The REVEALS reconstructions are also a useful tool for the quantification of past land-use changes that may have affected the nutrient loading to the Baltic Sea. [ABSTRACT FROM AUTHOR]

Copyright of Annales UMCS, Geographia, Geologia, Mineralogia et Petrographia is the property of Maria Curie-Sklodowska University in Lublin and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

This paper presents a map describing the main geomorphological and sedimentological features, hydrodynamics, benthic habitat distributions and human impact on the coastal and marine areas of the Archipelago of La Maddalena (NE Sardinia, western Mediterranean). This cartography is based on an interdisciplinary sea-land approach, with the aim being to support sustainable and successful beach management in the face of a changing climate and environment, thereby contributing to the achievement of the Agenda 2030 Sustainable Development Goals (13, 14 and 15). In the Main Map (1:14,000 scale), the static and dynamic features of the beach systems and adjacent inner shelf are divided into thematic sections that include the geomorphological elements, hydrodynamics, sedimentological distributions, benthic habitat (mainly Posidonia oceanica meadow) and anthropogenic impacts. The map establishes a fundamental, multidisciplinary benchmark that is able to provide substantial scientific support to policymakers in relation to future vulnerability-assessment activities and the definition of land-management strategies. [ABSTRACT FROM AUTHOR]

The increase of geomorphological research during the last decades in the Gorce Mts. caused the need for state-of-art review papers. The Gorce Mountains were formed as an isolated massif with Mt Turbacz (1310 m a.s.l.) as the highest summit. River channels are remodeled by sudden and high-level floods with the critical impact of log jams. The main processes influencing hillslope relief were landsliding, run-off, and tree uprooting. The review suggests the following issues await for studies: a long-term landscape evolution, monitoring of morphogenetic processes, and origin of landslides with their contribution to denudation rates. Also, current biomorphodynamics (uprooting process) has not been sufficiently studied. [ABSTRACT FROM AUTHOR]

Copyright of Acta Geographica Lodziensia is the property of Lodz Scientific Society / Lodzkie Towarzystwo Naukowe and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Anthropocene, geology, Holocene, human impact, stratigraphy The "Anthropocene" is most useful as an informal concept Keywords: Anthropocene; geology; Holocene; human impact; stratigraphy EN Anthropocene geology Holocene human impact stratigraphy 453 454 2 05/09/23 20230501 NES 230501 The "Anthropocene" (Crutzen & Stoermer, [4]; Crutzen, [3]) concept has rapidly gained prominence in recent years in both public narratives around the climate and environmental crisis, and academic discourses across a range of disciplines - the latter being demonstrated by the multitude of papers published discussing various aspects of the proposed new geological epoch (e.g. Waters et al., [14]). [Extracted from the article]

The Convention for Wetlands was signed in 1971 as part of a global measure to mitigate the loss and degradation of the world's wetlands. Signatory nations nominate wetlands as internationally important and commit to maintaining their 'ecological character'. In many cases the character that has been maintained was that occurring at the time of nomination with scant attention to the variability and change that occurs over longer periods. Palaeoclimate and palaeoecological research now reveals a diverse array of conditions in wetlands in the past and attests that any recently identified condition may be transient. The research further reveals the considerable magnitude and antiquity of the impact of people on wetlands. Hence the site description used by wetland managers would benefit from the provision of a longerterm perspective of change. The changing state of wetlands provides a dilemma for wetland managers. In response, a workshop on understanding change in wetlands was held in Queenscliff, Australia, in November 2013 to draw together perspectives of change from neo- and palaeoecological sources to enable the formulation of new pathways of assessment to better accommodate the dynamic nature of wetlands. A synthesis of the information provided at the workshop is provided in this paper. [ABSTRACT FROM AUTHOR]

The paper presents the results of palynological and geoarchaeological investigation carried out on the Greek-Roman site of Pantanello – ancient Metapontum – in the Metaponto Plain (southern Italy). This area, archaeologically investigated since the '70s, is an example of the long-term interaction between human communities and the environment. A total of 29 pollen samples and 43 bulk samples for sedimentological and mineralogical analyses were collected from three 2-m-deep trenches excavated in the vicinity of the archaeological complex of Pantanello and the alluvial plain of the Basento River. Our multidisciplinary investigation permitted to elucidate the main natural and human-controlled sedimentary processes that took place in the last two millennia. Large part of sedimentation occurred in fluvial environments and led to the accumulation of fine and organic matter-rich deposits. This happened in alluvial to swampy environments at the margin of the Basento River plain. Since the Greek occupation of the area, human communities contributed to the sedimentation with different degree of intensity. In fact, human agency (herding and cultivation) tuned the intensity of soil erosion and slope processes, thus activating the colluvial mobilization of coarse sediments into the sedimentary sequence. Pollen analyses allowed exhaustive landscape reconstructions of the site, giving specific details on the land use and its transformations during the Greek and Roman phases. The increased human exploitation of the area altered the intensity of surface processes (erosion and sedimentation) and the evolution of plant cover promoted by natural dynamics. [ABSTRACT FROM AUTHOR]

Late Holocene environmental changes were examined in Dee Why Lagoon, New South Wales, based on the sedimentological, geochemical and geochronological analysis of six cores collected from the fluvial delta and lagoon basin. The lagoon formed about 7300–7200 cal yr BP, following the post-glacial marine transgression and establishment of a sand barrier. Infilling of the lagoon occurred at a rate of 0.09–0.15 mm/yr until about 3300–3200 cal yr BP, when the barrier closed, resulting in mostly freshwater conditions, as evidenced by a change from pyrite-rich units to sediment containing little sulfur and a lack of foraminifera. Sedimentation rates increased to 0.23 then 0.43 mm/yr until about 100 years ago. Post-European land clearance led to an increase in sedimentation rates to 1.0–1.3 mm/yr on the fluvial delta, which are lower than those from other wave-dominated estuaries in New South Wales as well as those estimated by previous studies in Dee Why Lagoon. Our study shows that the fluvial delta started forming much earlier than originally thought, based on results of radiometric dating, and confirmed using sedimentological and geochemical data, as well as a critical examination of historic aerial photographs. Human impact has resulted in an increase in heavy metal (Cu, Pb, Zn) and metalloid (As) concentrations in the recent sediment, most likely attributed to stormwater discharge. Pb and As concentrations are above the ANZECC high sediment quality guideline values at the site closest to the stormwater outlet, with As-based pesticides one of the possible sources. Using the mean enrichment quotient, which is based on normalised Cu, Pb and Zn concentrations over their normalised background concentrations, we show that the surface sediments in Dee Why Lagoon are severely enriched, reflecting the recent anthropogenic impact that has also led to an increase in sedimentation rates. [ABSTRACT FROM AUTHOR]

Even though legally protected, many areas worldwide are under a certain level of human pressure. Significant for humanity for many reasons, mountain regions are also threatened because of different anthropogenic activities, especially the ones with developed winter tourism. There are four main ski resorts in Serbia (Kopaonik, Zlatibor, Stara Planina and Brezovica) and the strongest environmental impact is registered on Kopaonik Mountain. In this paper, we tried to answer if winter tourism could be sustainable in protected areas, especially on Kopaonik Mountain, which is recognized as the largest ski resort in Serbia and a natural protected area of the highest state level--a National Park. The main threats to the environment in Kopaonik National Park are logging, building and construction of ski slopes, urbanization, artificial snow use, illegal and unplanned building. Negative consequences of winter tourism development are land degradation, deforestation, loss and fragmentation of natural habitats, ecosystem disturbances, erosion, soil loss and pollution, water and air pollution, noise and light pollution. Harmonizing tourism development with conservation activities within natural protected areas is one of the main priorities of sustainable use of natural values and resources. For the successful and sustainable development of an area, it is necessary to conduct multidisciplinary planning, based on the results from the relevant scientific disciplines. [ABSTRACT FROM AUTHOR]

The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the "archaeologically invisible" Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols. [ABSTRACT FROM AUTHOR]

Water is one of the indispensable elements of life, ensuring the living conditions of people, plants and animals at the same time, intervening in the most varied production activities, either as a source of dynamics, raw materials, working gear or transport environment, etc. Water pollution modifies the physico-chemical and biological conditions of an aquatic ecosystem, a phenomenon that can occur naturally or as a result of human activity. A particular feature of water from the rivers is the selfpurification capacity. In this paper attention is paid to flowing waters (rivers), namely, to Bega river. A current issue that attracts the attention of specialists in the field is linked to water pollution caused by agricultural or industrial activities. The present paper presents the quality of the Bega River, namely on the section next to the locality SânmihaiulRomân. Sampling was made 3 times a year, respectively, in January, June and September, in 3 consecutive years, namely, year 2016, year 2017 and year 2018. The analyses were carried out by the Quality Laboratory of the Banat Water Administration and the results obtained were interpreted and compared with the physico-chemical quality standards of the Order 161,from 2006, published in the Official Gazette of Romania which allows water to be framed in a quality class from I to IV. The water samples were taken in January, June, and September for the years 2016, 2017 respectively 2018. The main quality analyzed indicators in the study are: Total chromium, copper, zinc, arsenic, barrier, selenium, cobalt, cadmium, lead, mercury, nickel, total nitrogen, nitrites and nitrates As a result of the analyses it has been noticed that higher overdoses were recorded in nitrites which framed water in IIIrd class quality and cadmium only at the level of 2016. The rest of the indicators are in category I and second, still highlighting the impact of human activity on the quality of the Bega River. Measures should be taken to limit the excess use of fertilizers on farmland, with a view to reducing the amount of nitrites in the water. [ABSTRACT FROM AUTHOR]

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Abstract The environmental context of cultural transformation' - frames the central issue of this paper – how were Neolithic and Chalcolithic landscapes in the Aegean, Balkan and Carpathian (ABC) zones shaped and transformed by climatic and anthropogenic impacts? The difficulties in interpreting proxy records for the middle, transitional stage of the Holocene aridification sequence, falling between the early wet stage and the late arid stage, have been created by the conjoint influence of two kinds of impact – climatic and anthropogenic. An unhelpful influence in this debate stems from Willis and Bennett's (1994) hypothesis of minimal human impact on the pre-Bronze Age landscapes of South East Europe. In this paper, two questions are posed: (1) what were the effects of the claimed global changes in Holocene climate at the regional and local scale in the ABC zones?; and (2) can we recognise human impact in these proxy records prior to the Bronze Age of our study regions? Following a discussion of general long-term climatic trends and RCCs (episodes of rapid climatic change), I base a discussion of the so-called 8200BP 'event' and pre-Bronze Age human impacts on a suite of 24 well-dated proxy records – mostly pollen sequences. The principal findings are that there is little evidence for impact from the 8200BP 'event' in these records, while there is substantial evidence for pre-Bronze Age human impacts on the landscapes of the Aegean, Balkan and Carpathian regions. [ABSTRACT FROM AUTHOR]

The great ecological and economic value of the biocenoses of Marine Protected Area 'Capo Caccia-Isola Piana' (MPA) requires a constant monitoring. For this reason, a continuous study of the area producing overlapping maps useful to control in real time the evolution of the biocenoses is necessary. The integrated use of several methodologies, such as Side Scan Sonar, Remote Operating Vehicle and Drone, has allowed us to realize a very detailed map. This paper presents the marine benthic map of the MPA and compares the present situation with that recorded in 2008. [ABSTRACT FROM AUTHOR]

Although recurrent fire events with very short return periods have the most dangerous effects on landscape degradation, only a few papers have explored the landscape ecological factors that drive the probability of fire recurrence. In this paper we apply a habitat suitability model for analyzing the spatial relationship between a selected set of landscape factors (mainly land use types) and fire recurrence in Sardinia (Italy) in the years 2005-2010. Our results point out that fire occurrence in already burned areas is lower than expected in natural and semi-natural land cover types, like forest and shrublands. To the contrary, like in all regions where human activity is the main source of fire ignitions, the probability of fire recurrence is higher at low altitudes and close to roads and to urban and agricultural land cover types, thus showing marked preference for those landscape factors denoting higher anthropogenic ignition risk. [ABSTRACT FROM AUTHOR]