Search Results (134)

Current climatic conditions are drying peatland ecosystems, compromising carbon storage through increased decomposition and vegetation shifts. Large-scale monitoring is essential to quantify climate change impacts on vegetation and hydrology. PlanetScope high-resolution imagery (3 m pixel) over seven years (2017–2023) served as proof-of-concept for a central European peatland (Rzecin, Poland). The enhanced vegetation index (EVI) was selected based on ground validation (R = 0.9 vs. 0.8 for NDVI-normalised vegetation index). Phenological metrics (SOS—start of the season; EOS—end of the season; LOS—length of the season; POS—peak of the season; EVImax; amplitude; area) were derived via DATimeS from snow-free EVI time series. Trends were analysed using pixel-wise slopes, change-point detection (break ~2020–2021), paired correlations, subarea (P1–P4) behaviour, and PCA, alongside air temperature (Tair), precipitation, and water table depth (WTD). Results revealed LOS and peak EVI increased until 2020, a 2021 break, and a 2022–2023 recovery, signalling nonlinear vegetation reorganisation. Transitional mire floating mats (Sphagnum spp.–Carex spp.–Vaccinium oxycoccus) showed the longest seasons/highest greenness but weakest hydrometeorological links, implying rising internal dynamics. Phragmites mats, fern–sedge edges, and riparian willow differed in tolerance or sensitivity to WTD and precipitation oscillations. Tair dominated EVI seasonality across types, while WTD and precipitation controlled phenology and greenness in edges, showing better results with phase-aligned means. Vascular plants outpaced mosses in peak EVI and persistence, with patch-specific shifts. Full article

Naomaohu coal from the Santanghu Basin, Xinjiang, is characterized by anomalously high Na and Ca contents, which strongly affect its gasification behavior and slagging tendency. However, the genetic linkage between geological alkali enrichment and their transformation during thermal processes remains insufficiently constrained. In this study, an integrated investigation combining coal seam profile analysis, coal petrography, mineralogical characterization, and fixed-bed gasification experiments was conducted to elucidate the enrichment mechanisms and transformation pathways of alkali and alkaline earth metals (AAEMs). A total of forty six samples were collected along a vertical seam profile to determine the depositional control of alkali and alkaline earth metals (AAEMs), and seven representative samples were further subjected to pressurized fixed-bed gasification. Alkali migration and mineral phase evolution were systematically analyzed using XRD, XRF, and SEM-EDS. The results indicate that Na enrichment is mainly controlled by groundwater infiltration and weak paleoweathering, while Ca accumulation reflects deposition in humid, Ca-rich mire environments. During gasification, Na volatilizes and recondenses as Na-feldspars (NaAlSi₂O₆) and NaCl, whereas Ca decomposes into gehlenite (Ca₂Al₂SiO₇) and brownmillerite (Ca₂AlFeO₅). The formation of these low-melting Na–Al–Si phases and Ca–Fe–Al phases dominate the ash fusion and slagging behavior. This study establishes a coupled geological–thermal transformation model for AAEMs in high-Na coal, providing mechanistic insight into mineralogical inheritance and offering guidance for mitigating alkali-induced slagging during gasification. Full article

This research investigates ten sediment cores extracted from Holocene deposits in Labu, northern Temburong District, Brunei Darussalam, to provide an initial inventory of the encountered peat-forming environments. Proximate, ultimate, and geochemical analyses were performed, along with mineralogical characterisations and ¹⁴C radiocarbon dating, as well as preliminary palaeontological and palynological examinations of the peat and underlying substrate layers. Localised organic deposits, termed “peat pockets”, were identified, with the oldest found to have begun accumulating under topogenous-mire conditions during the Middle Holocene. This coincides with the Mid-Holocene sea-level rise, which is thought to have peaked at 6000–4500 years BP. However, our data suggest that sea level may have continued rising until approximately 2500 years BP, peaking between 2500 and 1700 years BP, followed by delta progradation in Temburong. These “peat pockets” gradually coalesced into larger topogenous mires associated with estuarine environments. Over time, they became less influenced by marine conditions and increasingly shaped by a freshwater regime, resembling an upper delta system, similar to the present-day landscape observed in Temburong. It is proposed that these mires transitioned from a topogenous to an ombrogenous phase approximately 250 to 320 years BP, as inferred through forward age extrapolation based on a constant accumulation rate. The findings support the hypothesis of inland coastline migration during the Middle Holocene, followed by retraction due to deltaic progradation in the Late Holocene. These fluctuations align with well-established sea-level changes driven by climatic variability. Full article

Wetlands play a significant role in the climate system due to their ability to store large amounts of carbon, while remaining highly sensitive to hydrometeorological variability. Droughts can profoundly alter these ecosystems, causing them to become significant sources of CO₂ and reducing CH₄ emissions. However, long-term observational evidence quantifying this response remains scarce. Here, we analyze a 12-year dataset (2013–2024) of CO₂ and CH₄ fluxes measured using the eddy-covariance method at a site in the Biebrza wetlands of northeastern Poland. The study period included both cool, wet years and hot, dry years characterized by extremely low water table levels. In the warmest and driest year, 2024, the mire acted as a substantial CO₂ source with a net emission of 1260 ± 400 g CO₂ m⁻² y⁻¹. Other drought-affected years, 2019 and 2023, also showed high net emissions of 1020 ± 230 and 840 ± 300 g CO₂ m⁻² y⁻¹, respectively. Conversely, the wettest year, 2013, exhibited a considerable net uptake of CO₂ of −990 ± 250 g CO₂ m⁻² y⁻¹. During dry years, CH₄ emissions declined markedly to values close to measurement uncertainty (1–3 g CH₄ m⁻² y⁻¹). When expressed as CO₂ equivalents, drought conditions consistently transformed the mire into a strong net greenhouse gas source. Full article

Exceptionally high chlorine contents (up to 1.57%) occur in the Middle Jurassic coal seams of the Sha’erhu area, Turpan–Hami Basin, Northwest China, making this coalfield one of the most Cl-enriched coal occurrences reported in China. However, the occurrence modes and enrichment pathways of chlorine in such coals remain insufficiently characterized. In this study, we integrated coal quality analyses, mineralogical characterization (XRD and SEM–EDS), geochemical measurements (XRF and ICP–MS), and an integrated Sequential Chemical Extraction Procedure–High-Temperature Combustion Hydrolysis approach to systematically elucidate the occurrence forms and enrichment processes of chlorine in the Sha’erhu coals. The results indicate that chlorine predominantly occurs in water-soluble form (78.3%–84.7% of total Cl), followed by a minor adsorbed fraction, whereas carbonate-bound and organic/silicate-bound Cl are negligible. The mineral assemblages and geochemical indicators jointly suggest that the coal seams were deposited in a semi-closed, strongly evaporative lacustrine–peat mire system, which subsequently experienced structurally controlled brine intrusion. Chlorine enrichment is attributed to the combined effects of primary evaporative concentration, externally sourced brines migrating through tectonic conduits, and diagenetic fluid activities. This study provides an important case for understanding the genesis of High-chlorine coals in continental basins. Full article

In this paper, we establish the existence and uniqueness of the minimum intrinsic risk equivariant (MIRE) estimator for univariate linear normal models. The estimator is derived under the action of the subgroup of the affine group that preserves the column space of the design matrix, within the framework of intrinsic statistical analysis based on the squared Rao distance as the loss function. This approach provides a parametrization-free assessment of risk and bias, differing substantially from the classical quadratic loss, particularly in small-sample settings. The MIRE is compared with the maximum likelihood estimator (MLE) in terms of intrinsic risk and bias, and a simple approximate version (a-MIRE) is also proposed. Numerical evaluations show that the a-MIRE performs closely to the MIRE while significantly reducing the intrinsic bias and risk of the MLE for small samples. The proposed intrinsic methods could extend to other invariant frameworks and connect with recent developments in robust estimation procedures. Full article

Hamatocaulis vernicosus is a pleurocarpous moss of conservation concern, listed in Annex II of the EU Habitats Directive due to its significant and ongoing decline across Europe. H. vernicosus is also listed as ‘Vulnerable’ on the Red List of Romanian Bryophytes. Despite its protected status, the species remains under-recorded in Romania, where many potentially suitable habitats have yet to be surveyed. The ecosystems, classified as Transition mire and quaking bog (NATURA 2000 code: 7140), are wet peatlands with oligo- to mesotrophic conditions and a pH of 5.0–7.5 H. vernicosus is recorded in 58 Romanian locations (10 confirmed by us, 5 new), spanning the Continental and Alpine bioregions. Models showed good performance (AUC 0.79–0.83; TSS 0.54–0.59), with distribution mainly shaped by mean annual temperature and temperature range, and secondarily by precipitation. The species favors cold, stable climates with high seasonal rainfall. Even though the number of localities reported for this species has increased in recent years, this does not indicate an improvement in its conservation status, but rather is an effect of recent recording efforts. To support targeted conservation planning, an ensemble species distribution model was developed in order to predict the suitable habitats of H. vernicosus across Romania. Both climate models project major range losses for the varnished hook-moss: ~30% by 2050 and ~40–60% by 2100, depending on the scenario. Losses are gradual under SSP245 but more abrupt under SSP585, with increased fragmentation, especially between the Eastern and Southern Carpathians. By integrating field observations with predictive climate change modeling, our study brings critical insights applicable to the conservation of H. vernicosus and the unique peatland ecosystems it relies on. Full article

Mires are fragile ecosystems in which plant communities are structured by complex interactions among hydrological regimes and groundwater properties. Although extensively studied in boreal and temperate regions, their environmental drivers in southern European mountains remain poorly understood. We investigated five complex mires in the Pyrenees, sampling 156 plots of vascular plants and bryophytes while measuring water table dynamics and groundwater chemistry over two years. Vegetation was classified into six main groups, including acid and alkaline fens, transition mires and Sphagnum hummocks. Ordination analyses (tb-PCA and RDA) revealed that mean water table depth, groundwater calcium and silicon content, and pH were the most important determinants of floristic composition. Bryophytes responded primarily to pH, whereas vascular plants were more influenced by water table variables, reflecting functional trait differences. Despite these environmental effects, spatial structure explained a comparable or greater proportion of variance, especially for vascular plants, underscoring the roles of local species pools, dispersal limitation, and site history in shaping community patterns. Establishing a reliable baseline is crucial for interpreting the distribution patterns of mire vegetation. Our results demonstrate that both environmental gradients and spatial processes are fundamental to understanding mire vegetation and highlight the importance of analyzing plant taxonomic groups separately. Full article

A handful of Sphagnum species and their ecosystems find their southernmost occurrence in the Pyrenees, and these small, relict units are endangered through anthropic activities and climatic change. A number of hydropower reservoirs covered former mire systems with water or let them ashore. These infrastructures will eventually become useless and abandoned, and the mires could possibly be restored, but there have been no known experiments in the Pyrenees in this field. The removal of the dam of a small reservoir in the Central Pyrenees in 2012 uncovered bare ground that was appropriate for testing mire restoration. In 2017, we started the restoration of two Habitats of Community Interest (HCIs), i.e., transition mires and quaking bogs (HCI 7140) and active raised bogs (HCI 7110*). To restore HCI 7140, we set a Carex rostrata population by planting cuttings and then small tufts of two Sphagnum species within the sedge sward. In parallel, we set small clumps of two other Sphagnum species intended to grow into hummocks (HCI 7110*). After seven growing seasons, HCI 7140 reached a good progression level, with a prosperous C. rostrata sward and progressive expansion of the Sphagnum populations. HCI 7110* turfs had varying performance, exhibiting moderate survivorship and positive expansion of the remaining turfs. The varying performance of the restored populations illustrates the possibilities of restoring mire communities in suboptimal environments. Interestingly, such restorative actions are appropriate for enhancing populations of species under threat, such as Sphagnum divinum. Full article

Suillus flavidus is an ectomycorrhizal fungus associated with moist, nutrient-poor habitats, particularly peat bogs and transitional mires, where it forms symbiotic relationships with two-needle pines, especially Pinus sylvestris. This study presents an updated assessment of its distribution in Poland, identifies key ecological factors influencing its occurrence—such as habitat type and phenology—and evaluates its conservation status in the context of sustainability goals. Analysis of available data shows that over two-thirds of the known sites in Poland are located in peatland ecosystems, with more than half occurring within protected areas. Although S. flavidus is distinctly hygrophilous, it appears to prefer moderately wet habitats, particularly swamp forests. Despite an increase in recorded localities over the past five decades, S. flavidus remains an endangered species due to the ongoing degradation of peatland habitats, which are increasingly threatened by land-use change, drainage, and climate-related shifts in hydrology. The species’ long-term survival depends on sustainable landscape management, the preservation of suitable host tree populations, and the inclusion of fungi in conservation and restoration strategies. Thus, S. flavidus should be considered both an indicator species and a relevant element in meeting sustainability goals. Full article

Peatlands store huge amounts of soil carbon and play an important role in the global carbon cycle. Drained peatlands stop accumulating carbon and become a source of carbon emissions. Rewetting is an effective method used to restore the ecological functions and carbon sequestration capacities of previously drained peatlands. The eutrophic Berkazan-Kamysh peatland, located in the forest–steppe zone of Bashkir Cis-Urals (the Republic of Bashkortostan), was drained in the 1970s, and since 2017, it has been undergoing rewetting. The aim of this work is to assess and quantify above- and belowground phytomass and its associated carbon pool, as well as to study the dynamics of the vegetation in the Berkazan-Kamysh peatland after rewetting. Vegetation mapping was performed and the areas of the main plant communities were calculated using the Random Forest method. It was found that, over the 7 years from the start of rewetting, the total area of hygro- and hydrophytic mire communities increased almost 3-fold (from 218 to 608 ha). During the same time, the area of meadow communities decreased by half (from 808.0 to 398.9 ha). The areas occupied by helophytic communities of tall graminoid plants (Phragmites australis and Typha angustifolia) have increased 10-fold and have begun to occupy more than 40% of the total area of the peatland. The aboveground phytomass of these types of plant communities can reach 1500–2000 g m⁻². Helophytization and other changes in vegetation composition led to a general increase in the above ground phytomass of the peatland of more than twofold. Full article

Although peatland restoration has been widely promoted as a strategy for reducing carbon emissions and restoring hydrological function, its effectiveness remains context-dependent and highly variable across regions and methods. This study presents a systematic review and meta-analysis of 52 peer-reviewed studies from 2014 to 2024, synthesizing the ecohydrological impacts of restoration across multiple spatial scales and implementation types. In tropical peatlands, restoration frequently reduced CO₂ emissions by more than 65,000 kg·ha⁻¹·yr⁻¹ and increased carbon sequestration up to 39,700 kg·ha⁻¹·yr⁻¹, with moderate CH₄ increases (~450 kg·ha⁻¹·yr⁻¹). In boreal sites, CO₂ reductions were generally below 25,000 kg·ha⁻¹·yr⁻¹, with long-term carbon accumulation reported in other studies, typically around 2–3 tCO₂·ha⁻¹·yr⁻¹. Higher values in our dataset likely reflect the limited number of boreal studies and the influence of short-term measurements. Across all regions, restoration was also associated with an average rise in WTD up to 10 cm. These averages were derived from studies conducted across diverse climatic zones, showing high standard deviations, indicating substantial inter-site heterogeneity. These differences emphasize the need for region-specific assessments rather than global generalizations, highlighting the importance of adaptive restoration strategies that balance carbon dynamics with hydrological resilience in the face of climate change. Full article

True slime mould assemblages respond acutely to microhabitat structure, which may constitute potential indicators of forest dynamics; however, large-scale syntheses integrating habitat scale and substrate specificity remain exceedingly scarce. By collating 3085 occurrence records into eight ecologically coherent habitats and ten substrate guilds, we quantified richness, entropy, turnover and indicator strength via rarefaction, Chao1/ACE, Shannon–Simpson indices, $\beta$-diversity partitioning, NMDS, PERMANOVA and ${\mathit{IndVal}}_g$ analysis. Broadleaved deciduous forests accounted for 37.9% of observations and hosted the most taxa, while lignicolous samples in both deciduous and bog–mire contexts dominated species counts; open grasslands were compositionally depauperate. Species replacement, not nestedness, structured assemblages (${\beta }_{\mathrm{SIM}}/{\beta }_{\mathrm{SOR}}\approx 0.82$), and habitat plus substrate explained two-thirds of variance. Indicator analysis isolated six habitat-diagnostic genera (notably Cribraria, Hemitrichia and Licea) and, at species resolution, highlighted Diderma niveum, Fuligo septica and Ceratiomyxa fruticulosa as high-fidelity bioindicators of montane grassland, bog–mire and broadleaved forest conditions, respectively. Taken together, our findings lay the groundwork for employing true slime moulds to identify habitat types and assess their ecological condition, while underscoring the conservation value of dead wood retention and structural heterogeneity. The benchmarked indicator set we provide enables rapid assessments and establishes a temporal baseline for tracking climate- and management-driven change in Central European Eumycetozoa diversity. Full article

Background/Objectives: To avoid becoming mired in prolonged deep dementia, some people seek to hasten death by advance instructions rejecting life-sustaining medical intervention (LSMI) at a point of cognitive decline they define in advance as unacceptable. When the time comes to implement such advance instructions and to allow the person in advanced dementia to die, many clinicians experience moral and ethical qualms. The decision makers face a clash between people’s legally recognized self-determination prerogative to control their post-competence medical fate and the decision makers’ conviction that humane treatment dictates sustaining the well-being, i.e., the physical “best interests,” of the patient who no longer recalls prior instructions grounded in concerns about personal dignity. The authors’ objective here is to provide guidance in resolving this anguishing dilemma confronting medical decision makers. Methods: The authors construct and analyze a case scenario involving a patient in a state of advanced dementia with a clear advance instruction rejecting LSMI at the current point of debilitation, but who is not ostensibly suffering, is experiencing a modicum of life satisfaction, and is making life-affirming utterances. The two lead authors present contrasting views on whether legal and moral factors impel the implementation of the advance directive rejecting treatment or rather dictate life-sustaining medical intervention. Results: At this early stage of jurisprudence involving persons in advanced dementia, there can be no definitive resolution of the difficult legal/moral clash confronting decision makers. Some sources would conclude that persons are legally entitled to define precipitous mental decline and complete dependence on others as intolerably undignified and inconsistent with their self-defined life narrative. Other sources would be guided by humane respect for the contemporary well-being of a non-suffering patient, especially one making life-affirming utterances. Conclusion: Through the lens of this illuminating case and contrasting analyses, readers should better understand how clinicians should weigh advance directives against shifting care preferences subsequently articulated by persons with advanced dementia. Full article

Upland mires in Italy, excluding the Alps, have a fragmentary distribution, and most of them persist in climatically optimal mountain refugia. Based on the literature data, we assessed that the state of knowledge of Italian upland mires distributed in the Apennines, Sicily, and Sardinia is outdated. We analyzed 54 publications, and 220 peatland sites were found. Only a few publications were published in the last ten years, and most of the peat bogs described in the past have not been resurveyed. The largest number of sites is concentrated in the Tuscan-Emilian Apennines (60), followed by Sicily (51 sites) and Calabria (42). The vegetation belongs to 38 phytosociological associations, 19 sub-associations and variants, and 54 communities of 6 different classes; the most represented class is Scheuchzerio palustris-Caricetea fuscae. The most widespread disturbances are uncontrolled grazing by domestic livestock and wild fauna, groundwater extraction, and road construction. New investigations are urgently needed to update the state of Italian upland mires knowledge, which is the basis for all conservation strategies prescribed by national, European, and international policies. Full article