@article{2-s2.0-105053588248,

title = {Strong amitraz resistance in Varroa destructor is associated with a sustained GST-dominant detoxification profile},

author = { A.W. Nicewicz and Ł. Nicewicz and V. Gepfert and P. Pawłowska and T. Stański and M. Stańska and M. Nakonieczny},

url = {https://doi.org/10.1016/j.vetpar.2026.110945},

doi = {10.1016/j.vetpar.2026.110945},

issn = {03044017},

year  = {2027},

date = {2027-01-01},

journal = {Veterinary Parasitology},

volume = {349},

abstract = {Varroa destructor is a major ectoparasite of honey bees, and the development of amitraz resistance threatens the long-term efficacy of one of the most widely used acaricides in apiculture. This study assessed amitraz susceptibility in Varroa populations from three Polish apiaries and examined whether differences in susceptibility were associated with population-specific detoxification enzyme responses. Amitraz toxicity was evaluated using vial bioassays and probit dose–response modelling, while glutathione S-transferase (GST) and nonspecific esterase activities were measured in surviving mites. The studied populations differed markedly in amitraz susceptibility. Population A1 showed an LC₅₀ of 0.0043 ppm, whereas A2 had an LC₅₀ of 0.0627 ppm and a conservative RR₅₀ lower bound of > 12.54, indicating strong amitraz resistance. In the reference population, mortality was 100% at all tested amitraz concentrations; therefore, the LC₅₀ was reported as < 0.005 ppm. Multivariate analyses revealed distinct population-specific detoxification profiles. A1 exhibited a pronounced esterase-dominant response at the lowest amitraz concentration, whereas the strongly resistant A2 population showed sustained GST-dominant activity across increasing amitraz concentrations at which mites survived. Further analysis demonstrated that enzymatic responses depended on both population origin and amitraz exposure. These findings suggest that amitraz resistance may be associated not with a generalized increase in detoxification capacity, but with the activation and persistence of specific enzymatic pathways, particularly GST-mediated detoxification. Because live honey bees are traded internationally, the occurrence of strongly resistant Varroa populations in exporting countries may have consequences beyond local beekeeping and highlights the need for coordinated resistance surveillance within international bee-trade networks.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105049441584,

title = {Deeper view on Patchiella reaumuri (Kaltenbach, 1843) (Hemiptera: Aphididae: Pemphiginae): General morphology and sensilla diversity},

author = { N. Kaszyca-Taszakowska and M. Kanturski},

url = {https://doi.org/10.1016/j.micron.2026.104115},

doi = {10.1016/j.micron.2026.104115},

issn = {09684328},

year  = {2027},

date = {2027-01-01},

journal = {Micron},

volume = {208},

publisher = {Elsevier Ltd},

abstract = {Scanning electron microscopy (SEM) methods were used for the first time to elucidate the external morphology of Patchiella reaumuri reaumuri (Kaltenbach; 1843) (Hemiptera: Aphididae: Pemphiginae). We examined and compared the external morphology of stem mothers and alate viviparous females from the parthenogenetic generation. Analysis identified diverse sensilla types, including coleoconic, campaniform, placoid, and trichoid sensilla, occurring on the antennae, mouthparts, and legs. Beyond the sensilla previously documented in the literature, we identified for the first time in aphids chaetic-type sensilla on the legs of alate viviparous females. In addition, species identity was confirmed by DNA barcoding based on the mitochondrial cytochrome c oxidase subunit I (COI) gene, and the obtained sequence was deposited in GenBank under accession number PP535559.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105050545731,

title = {Field and simulated Ground Penetrating Radar (GPR) Data for improved snow structure analysis on Arctic glacier},

author = { M. Grabiec and M. Laska and D. Ignatiuk},

url = {https://doi.org/10.1016/j.coldregions.2026.105118},

doi = {10.1016/j.coldregions.2026.105118},

issn = {0165232X},

year  = {2027},

date = {2027-01-01},

journal = {Cold Regions Science and Technology},

volume = {253},

publisher = {Elsevier B.V.},

abstract = {Geophysical surveys, including Ground Penetrating Radar (GPR), provide essential insights into the probed subsurface formations, including snow cover. However, interpreting snow structure within GPR data remains challenging. To address this, the study establishes a direct link between GPR signal characteristics and snowpack structure using field GPR soundings and snowpit analyses from Hansbreen (glacier located in the South Svalbard) across five spring seasons (2008; 2011; 2016; 2018; and 2019). Based on measured snow layer densities, a forward wave propagation model was developed using gprMax software. Amplitude variations of field and simulated signals were converted to absolute extreme values (AEVs), normalized, and compared using quantitative similarity metrics. In the upper sections of each paired dataset, 3 to 11 corresponding signal peaks (local AEV maxima) were recognized. Identified AEV peaks correspond to structural boundaries with significant relative permittivity contrasts. Among these, ice layers play a key role in linking snow stratigraphy with the in situ GPR profile, accounting for over 50% of the matched AEV peaks. Similarity measures confirm a significant relationship between simulated and field GPR signals (with the highest agreement in 2008), thereby validating that snowpack stratigraphy is effectively captured in radar imagery. Sites in the glacier accumulation zone exhibit stronger agreement than those in the ablation area due to a higher frequency of signal peaks. Simulated signals exhibited high AEV variability in the upper temporal section and low AEVs in the lower section, reflecting a heterogeneous snowpack overlying more homogenous ice or firn substrate. Comparing field GPR soundings with simulated signals provides a solid basis for relating snow stratigraphy directly to GPR data.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105052726182,

title = {The impact of the NZFO content on the synergy effect in NZFO/f-MWCNTs nanocomposites synthesized via ex-situ method},

author = { A. Bajorek and B. Szostak and M. Dulski and J.M. Greneche and S. Lewińska and B. Liszka and M. Pawlyta and A. Ślawska-Waniewska},

url = {https://doi.org/10.1016/j.mseb.2026.119899},

doi = {10.1016/j.mseb.2026.119899},

issn = {09215107},

year  = {2027},

date = {2027-01-01},

journal = {Materials Science and Engineering B},

volume = {335},

publisher = {Elsevier Ltd},

abstract = {We present a comprehensive study of the synergistic effects in as-received NZFO/f-MWCNT nanocomposites synthesized via an ex-situ method with varying contents (2; 5; 25; and 50 wt%) of Ni0.5Zn0.5Fe2O4(NZFO) nanoparticles dispersed within a matrix of functionalized multi-walled carbon nanotubes (f-MWCNTs). The structural and microstructural characteristics governing the efficiency of the synthesis process were investigated using complementary techniques, including X-ray diffraction (XRD) and Raman spectroscopy. The results reveal that the NZFO crystallite size remains nearly constant across the investigated composition range, while the structural integrity of the carbon matrix is preserved. The redistribution of cations between the A-tetrahedral and B-octahedral sites was quantified by the cation inversion parameter (δ). Magnetic characterization indicates the presence of a cluster-glass state in the NZFO nanoparticles. A core-shell-like magnetic structure, consisting of a magnetically ordered core surrounded by a disordered magnetic dead layer (MDL), is identified. The magnetic behaviour is discussed within the framework of the Yafet–Kittel model, taking into account the evolution of the cation inversion parameter. Comparative analysis of photoemission spectra highlights the contributions of magnetic trivalent iron at A and B sites and Fe-based residual species originating from the carbon matrix, irrespective of the NZFO content in the composites. These findings provide insight into the interplay between the ferrite phase and the carbon nanotube matrix, elucidating the origins of the observed synergic effects in NZFO/f-MWCNT nanocomposites.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105048802116,

title = {Population density-dependent changes in oviposition behaviour and offspring quality in the seed beetle Callosobruchus maculatus},

author = { M. Krzyżowski and B. Baran and J. Francikowski},

url = {https://doi.org/10.1016/j.jspr.2026.103222},

doi = {10.1016/j.jspr.2026.103222},

issn = {0022474X},

year  = {2027},

date = {2027-01-01},

journal = {Journal of Stored Products Research},

volume = {120},

publisher = {Elsevier Ltd},

abstract = {Founder density can influence both reproductive output and offspring quality in stored-product insects, yet the behavioural mechanisms underlying these effects remain poorly understood. We examined the effects of founder female density (1; 2; 5; and 10 females per container) on fecundity, egg distribution, offspring performance, and sex ratio in the seed beetle Callosobruchus maculatus developing on mung bean (Vigna radiata). Increasing founder density significantly reduced per-capita fecundity and offspring production. Eggs per female declined from 189.3 ± 49.4 at the lowest density to 49.8 ± 2.7 at the highest density, while offspring production per female showed a similar decrease. In contrast, the mean number of eggs per occupied seed increased with density, indicating greater egg aggregation. Egg distribution patterns differed markedly among sets (χ2 = 1346.2; p < 0.001), demonstrating a strong density-dependent shift in oviposition behaviour. Higher founder densities also produced lighter offspring and altered development time, consistent with increased larval competition within seeds. Although offspring number and female body mass were positively correlated at the container level, this relationship disappeared after controlling for founder density, suggesting that both traits were influenced by a common density-dependent process rather than a direct quantity-quality trade-off. Offspring sex ratio remained unaffected by founder density. Our results demonstrate that high founder density influenced not only reproductive output in a negative correlation but also patterns of host exploitation and offspring quality. Density-dependent changes in egg distribution appear to represent an important mechanism linking adult density to offspring performance in this economically important stored-product pest.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105054136835,

title = {MAKR6 integrates TMK and CAMEL/CANAR signalling for auxin canalization in Arabidopsis},

author = { Z. Ge and L. Koczka and E. Mazur and G. Molnár and D. Vladimirtsev and N. Kassem and S.A. Ikene and L. Fiedler and J. Friml},

url = {https://doi.org/10.1038/s41477-026-02435-0},

doi = {10.1038/s41477-026-02435-0},

issn = {20550278},

year  = {2026},

date = {2026-01-01},

journal = {Nature Plants},

abstract = {Adaptive plant development is orchestrated, among other means, by directional, intercellular transport of the phytohormone auxin. Self-organizing phenomena such as flexible vasculature formation depend on auxin canalization, which manifests as the gradual formation of auxin-transporting channels through feedback between auxin signalling and transport. Here we identify MAKR6 as a component of this feedback. MAKR6 transcripts accumulate in vascular cells and are tightly regulated by auxin via the Aux/IAA–ARF–WRKY23 transcriptional cascade. MAKR6 is required for auxin canalization-dependent processes, including leaf venation, vascular regeneration and de novo channel formation from local auxin sources. Mechanistically, MAKR6 interacts with the PIN1 auxin transporter and modulates its trafficking and polarization. MAKR6 also associates with and integrates TMK1/4 and CAMEL–CANAR, two key receptor-like kinase complexes involved in canalization. Together, our study establishes MAKR6 as a multifaceted regulator that couples transcriptional auxin signalling to PIN1 repolarization and coordinates multiple RLK-mediated pathways into a concerted process. This provides mechanistic insight into auxin canalization and exemplifies a framework for exploring similar regulatory nodes in other developmental contexts.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053682054,

title = {Unexpected Localization of AGP Epitopes in the Plastids of Aldrovanda vesiculosa: New Questions About the Distribution of These Epitopes in Angiosperms},

author = { B.J. Płachno and M. Kapusta and M. Feldo and P. Stolarczyk and P. Świątek and A. Leszczuk},

url = {https://doi.org/10.3390/ijms27198452},

doi = {10.3390/ijms27198452},

issn = {16616596},

year  = {2026},

date = {2026-01-01},

journal = {International Journal of Molecular Sciences},

volume = {27},

number = {19},

abstract = {Arabinogalactan proteins (AGPs) are the glycoproteins that are characteristic of plant cells (except for some algae) and are essential for cell function (cell–cell communication; cell adhesion; cell expansion; cell-wall organization; and signaling) but also for the development of roots, shoots, leaves, flowers, and reproductive structures. They occur inside and on the surface of plant cells, but mainly at the interface between the plasma membrane and the cell wall. Reports on the occurrence of arabinogalactan proteins in plastids are very rare and unclear. Our goal was to determine whether AGP-reactive carbohydrate epitopes are associated with plastids and starch in turion cells of Aldrovanda vesiculosa L. To do this, the localization of the AGP-reactive carbohydrate epitopes was assessed using immunolabeling and confocal and electron microscopy. Abundant signals for the antibodies LM2 and JIM8 against the AGP epitopes were detected in plastids. The LM2 signals were particularly frequent in starch grains. Also, electron microscopy confirmed the presence of AGP-reactive carbohydrate epitopes in plastids. These findings provide further evidence for the unusual intracellular localization of AGP-reactive carbohydrate epitopes in plastids and highlight starch grains as a target for future studies aimed at determining the molecular identity and biological significance of these epitopes.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105054088445,

title = {Single-Crystal X-Ray Diffraction and Raman Spectroscopic Studies of Miyahisaite Sr₂Ba₃(PO₄)₃F from the Graulai Quarry, Germany},

author = { R. Juroszek and B. Krüger and K.N. Truong and H. Krüger and C. Schäfer},

url = {https://doi.org/10.2113/lithosphere_2026_124},

doi = {10.2113/lithosphere_2026_124},

issn = {19418264},

year  = {2026},

date = {2026-01-01},

journal = {Lithosphere},

volume = {2026},

number = {4},

pages = {1-14},

abstract = {Miyahisaite, ideally Sr_2Ba_3(PO_4)_3F, a member of the apatite supergroup, was identified in pegmatite-like veins hosted by melilite–nephelinite volcanic rocks at the Graulai quarry, Hillesheim, West Eifel, Germany. This represents the second occurrence of this rare mineral, previously known only from the hydrothermally altered chert at the Shimoharai mine, Japan. At Graulai, miyahisaite occurs as colorless anhedral crystals, up to 300–400 μm in size, within a complex late-stage mineral assemblage that includes leucite, nepheline, diopside, fluorapatite, götzenite, delhayelite, lamprophyllite-group minerals, magnetite, fresnoite, oxyphlogopite, and perovskite. Electron-microprobe analyzes yielded the empirical formula (Sr_0.97Ca_0.87Ba_0.12Na_0.04)_Σ2.00(Ba_3.00)(P_2.87S_0.06V_0.04Al_0.04)_Σ3.01(F_1.00Cl_0.03)_Σ1.03 confirming a Sr- and Ba-dominant fluorophosphate member of the hedyphane group. Previously unavailable, single-crystal X-ray diffraction data show that miyahisaite has an apatite-type structure and crystallizes in the hexagonal P6_3/m, with unit-cell parameters a = 9.8876(5) Å},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053970681,

title = {Additional contribution to the genus Psallops Usinger (Hemiptera: Heteroptera: Miridae: Psallopinae), with descriptions of three new species},

author = { A. Taszakowski and W. Kowolik and A. Poźniak and J. Kim},

url = {https://doi.org/10.11646/zootaxa.5878.3.7},

doi = {10.11646/zootaxa.5878.3.7},

issn = {11755326},

year  = {2026},

date = {2026-01-01},

journal = {Zootaxa},

volume = {5878},

number = {3},

pages = {429-441},

abstract = {Three new species of the genus Psallops (Hemiptera: Miridae: Psallopinae) are described from different regions: P. carolinus sp. nov. from Madagascar, P. matarankensis sp. nov. from Australia, and P. ulu sp. nov. from Brunei. Diagnostic characters and illustrations of the male (P. matarankensis sp. nov. and P. ulu sp. nov.) and female (P. carolinus sp. nov.) genitalia are provided. The female genitalia of Psallops are described for the first time. Detailed morphological examination using scanning electron microscopy revealed additional states of several characters recently recognized as taxonomically informative within Psallops. These findings broaden the currently known morphological limits of the genus and further support the taxonomic importance of these characters for future studies on the internal classification of Psallops.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053964477,

title = {Taxonomic Contributions to Xenocylapidius Gorczyca, 1997 (Hemiptera: Miridae: Cylapinae) from New Caledonia, with Descriptions of Two New Species},

author = { A. Taszakowski and G. Gierlasiński and D. Palinker and K.I.M. Junggon},

url = {https://doi.org/10.3161/00034541ANZ2026.76.28.28},

doi = {10.3161/00034541ANZ2026.76.28.28},

issn = {00034541},

year  = {2026},

date = {2026-01-01},

journal = {Annales Zoologici},

volume = {76},

number = {28},

pages = {1-13},

abstract = {Xenocylapidius Gorczyca, 1997 is a genus of Cylapinae comprising five species occurring in Australia and three known from New Caledonia. In this paper, we describe two additional species of this genus, X. rutkowskiisp. nov. and X. wanatisp. nov., from New Caledonia. The male of X. gressitti is described for the first time, and new locality records for X. tamasi are presented. Habitus images, scanning electron micrographs of the selected structures, as well as female genitalia of the new taxa are provided.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105054173281,

title = {Sustainable carbon based metal-free catalysts for the green synthesis of next generation 1,3-dioxolane adjuvants: AI assisted data exploration and structure mechanism relationships},

author = { M. Kapkowski and T. Zelenka and G. Zelenková and V. Slovák and K. Prusik and G. Dercz and M. Ludynia and K. Kocot and K. Balin and U. Zhdan and M. Doležal and M. Almáši and J. Polanski},

url = {https://doi.org/10.1016/j.jece.2026.125522},

doi = {10.1016/j.jece.2026.125522},

issn = {22132929},

year  = {2026},

date = {2026-01-01},

journal = {Journal of Environmental Chemical Engineering},

volume = {14},

number = {6},

abstract = {Surface functionalized porous carbons provide a versatile platform for metal-free acid catalysis. Here, oxidized (Coxo) and nitrated (Cnitro) hierarchically porous carbon monoliths were prepared from the same resorcinol-formaldehyde-derived carbon scaffold (CMM) and evaluated as catalysts for the solvent-free synthesis of 1,3-dioxolanes. The use of a common parent scaffold enabled a direct comparison of both surface modifications under identical reaction conditions, while retaining the materials as macroscopic monolithic pieces during catalytic testing. AI-assisted and manually verified literature screening, combined with principal component analysis and self-organizing maps, identified four major catalyst classes for glycerol acetalization and provided a benchmark for the developed materials. Comprehensive physicochemical characterization confirmed the formation of distinct oxygen- and nitrogen containing surface functionalities and the retention of hierarchical porosity. Surface modification decreased the BET area from 689 m2 g−1 for CMM to 213 and 332 m2 g−1 for Coxo and Cnitro, respectively, whereas Coxo exhibited a higher total acidity than Cnitro (2.380 vs. 1.845 mmol g−1). Under solvent-free conditions at 55 °C for 1 h, Coxo and Cnitro catalyzed nine polyol-ketone reactions with conversions of 53.8–91.5% and 50.0–86.2%, respectively, and selectivities toward the corresponding cyclic ketals of 91.7–100%. In comparison, the parent CMM afforded only 0–4.2% conversion. The highest conversion was achieved in the reaction of glycerol with acetone using Coxo (91.5%) and Cnitro (86.2%). Selected acetone-derived 1,3-dioxolanes were subsequently evaluated as foliar-fertilization adjuvants in maize and demonstrate the potential of the synthesized 1,3-dioxolanes in foliar nutrient delivery.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105052927406,

title = {CRISPR/Cas9-mediated FeS-ELF3 inactivation overcomes heteromorphic self-incompatibility in common buckwheat},

author = { A. Piński and M. Zaranek and J. Lusinska and P. Kopeć and A. Płazek and M. Zhou and A. Betekhtin},

url = {https://doi.org/10.3389/fpls.2026.1919002},

doi = {10.3389/fpls.2026.1919002},

issn = {1664462X},

year  = {2026},

date = {2026-01-01},

journal = {Frontiers in Plant Science},

volume = {17},

abstract = {Common buckwheat (Fagopyrum esculentum) is a climate-resilient pseudocereal; however, its global adoption is constrained by the heteromorphic self-incompatibility associated with distyly. While the S-locus early flowering 3 (FeS-ELF3) gene has been identified as a key regulator of self-compatibility, a stable genetic transformation of F. esculentum has not yet been developed. In this study, we established an Agrobacterium-mediated transformation protocol for F. esculentum by adapting an F. tataricum procedure, incorporating a heat-shock treatment at 43 °C for 5 min. This achieved a transgenic frequency of 27.27% among regenerated plants (6/22) and an absolute editing efficiency of 4.55% (1/22) in the agronomically relevant ‘Panda’ cultivar. Targeted knockout of FeS-ELF3 via CRISPR/Cas9 yielded a self-compatible line with long-homostylous flowers. Plants derived from this single edited founder event exhibited architectural shifts - specifically reduced height and shorter inflorescences – without an apparent reduction in seed yield under greenhouse conditions. Because these observations stem from a single edited line, further evaluation of independent mutant lines or complementation assays is required to definitively distinguish FeS-ELF3-specific pleiotropic effects. Nevertheless, this study provides a proof-of-concept for overcoming self-incompatibility and establishes a genomic framework for the rapid improvement of Fagopyrum esculentum.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053381692,

title = {Pangenome-guided breeding restores high-altitude adaptation and improves yield in Tartary buckwheat},

author = { K. Zhang and Y. He and H. Lin and J. He and Z. Wang and W. Li and Y. Chen and J. Li and Y. Shi and X. Huang and M. Ding and P. Yang and Z. Chen and A. Chitikineni and Ji. Li and J. Gao and B. Feng and Zh. Zhang and M. Hao and R.R. Mir and D. Liu and S. Woo and D. Janovská and M. Quinet and A.R. Fernie and W. Liao and X. Feng and D.P. Gauchan and N. Dhami and I. Kreft and A. Piński and A. Betekhtin and M. Spannagl and X. Liu and R.K. Varshney and J. Liu and M. Zhou},

url = {https://doi.org/10.1016/j.cell.2026.09.049},

doi = {10.1016/j.cell.2026.09.049},

issn = {00928674},

year  = {2026},

date = {2026-01-01},

journal = {Cell},

volume = {189},

number = {21},

pages = {6898-6898},

abstract = {(Cell 189; 5214–5231.e1–e12; August 20; 2026) After the article was published online, the authors noticed a minor labeling error in Figure 4M. During figure assembly, a “0” was inadvertently omitted from the labels of the competitive probes. Specifically, for both EMSA experiments in Figure 4M, the final competitor condition should be labeled as 100×, rather than 10×. This is solely a labeling error introduced during figure assembly and does not affect the underlying experimental data, results, or conclusions of the paper. The authors sincerely apologize for any confusion this may have caused. (Figure presented) (Figure presented)},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105054135531,

title = {Delayed deepening: Bathymetric patterns of post-Paleozoic stalked crinoids in the Panthalassan realm},

author = { M.A. Salamon and T. Brachaniec and G.S. Bressan and J. Ciesielczuk and C. Esquivel-Macías and K. Gaidzik and T. Kapitany and A.A. Klompmaker and M. Krajewski and D.G. Lazo and T. Oji and B. Poatskievick-Pierezan and B.J. Płachno and  and A. Wilk and K. Humański and P. Gorzelak},

url = {https://doi.org/10.1130/G54806.1},

doi = {10.1130/G54806.1},

issn = {00917613},

year  = {2026},

date = {2026-01-01},

journal = {Geology},

volume = {XX},

number = {XX},

abstract = {Stalked crinoids were widespread in shallow-marine ecosystems throughout much of the Paleozoic and Mesozoic but are confined to deep-sea environments today. In the Tethyan realm, this bathymetric restriction is inferred to have begun in the Cretaceous and was largely completed by the Eocene. This pattern started during the Mesozoic Marine Revolution when predators and predation became more prevalent. Whether this pattern was globally synchronous remains uncertain. We compiled Jurassic–Neogene occurrences of stalked crinoids from the Panthalassan realm to evaluate long-term bathymetric trends. Throughout the Jurassic, Cretaceous, and Paleogene, deep-water occurrences constitute a consistently minor component of the stalked crinoid record (3–13%), with the Cretaceous interval yielding the lowest relative proportion. An increase in the relative proportion of deep-water occurrences to 57% is observed only in the Neogene. These results indicate that the transition toward deep-sea restriction was temporally decoupled from ecological escalation in the late Mesozoic and was not globally synchronous. In the Panthalassan realm, shallow-marine persistence extended well beyond the interval of Tethyan depth restriction, underscoring the importance of basin-scale perspectives in interpreting the Meso-Cenozoic marine restructuring. Together, these findings challenge the assumption of a globally synchronized Mesozoic Marine Revolution–driven bathymetric shift and recast deep-sea restriction as a spatially asynchronous, long-term macroecological transition.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053779507,

title = {Explainable machine learning for flood susceptibility mapping in Kyrgyzstan’s major urban areas},

author = { N.T.T. Linh and C. Singha and V.K. Rana and E. Duulatov and E.B. Łupikasza and Q.B. Pham},

url = {https://doi.org/10.1038/s41598-026-58498-8},

doi = {10.1038/s41598-026-58498-8},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

abstract = {This study constructs ML models for flood susceptibility modeling in Kyrgyzstan’s three primary urban hubs: Jalal-Abad, Osh, and Tokmok. By developing a robust and explainable modeling approach, this study provides valuable insights into flood susceptibility assessment in these flood-prone metropolitan areas. A detailed flood inventory dataset was created using Sentinel-1 satellite imagery to delineate flood and non-flood areas and to integrate values for flood-contributing factors. Machine Learning (ML) algorithms: Random Forest (RF), eXtreme Gradient Boosting (XGB), and AdaBoost were deployed to generate flood susceptibility maps. Subsequently, model performance was rigorously evaluated using various statistical metrics, including accuracy, kappa coefficient, sensitivity, specificity, positive predictive value (PPV), negative predictive value (NPV), and the Area Under the Receiver Operating Characteristic Curve (AUC-ROC). All three models gave success and prediction rate curve values above 84%. The averages of the very high susceptibility class for the cities of Jalal-Abad, Osh, and Tokmok were 8.44%, 12.01%, and 37.8%, respectively. Additionally, SHAP (SHapley Additive exPlanations) analysis was employed to interpret and explain the importance of flood-contributing factors in the predictive models, enhancing model interpretability and providing insights into flood susceptibility mechanisms.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105054076326,

title = {Stage-specific developmental toxicity of C60 and C70 fullerene derivatives in Drosophila melanogaster: impact on oxidative balance, cell cycle, and metamorphosis success},

author = { K. Małota and A.Z. Urbisz and M. Serda and K. Kosiorowski and M.M. Rost-Roszkowska},

url = {https://doi.org/10.1039/d6en00776g},

doi = {10.1039/d6en00776g},

issn = {20518153},

year  = {2026},

date = {2026-01-01},

journal = {Environmental Science Nano},

abstract = {With the increasing production and use of carbon-based nanomaterials, understanding their potential biological effects on non-target organisms has become increasingly important. In this study, we investigated the sublethal effects of two water-soluble fullerene derivatives, C60-PEI and C70-PEI on the post-embryonic development of Drosophila melanogaster larvae. Thus, three successive larval stages (L1; L2; L3) were cultured in medium containing 1 mg mL−1 of fullerene C60 or C70. To link subcellular endpoints to whole-larval developmental effects, we compared midgut ultrastructure, oxidative stress, cell cycle phase distribution, and DNA damage, alongside metamorphosis success. Both fullerene derivatives reduced metamorphosis success relative to the control (90.1%; SE 4.9), by 23.3 (SE 6.9) and 37.9 (SE 6.9) percentage points for C60-PEI and C70-PEI, respectively (both Bonferroni-adjusted p ≤ 0.006); the two derivatives did not differ significantly from each other (p = 0.13). Flow cytometry suggested oxidative imbalance as a contributing mechanism, while TEM confirmed cellular uptake. Although no widespread cell death was observed, the C70-PEI group showed isolated autophagosomes at the L2 and L3 stages, suggesting a protective autophagic response. Importantly, these effects occurred without photoactivation, representing a conservative estimate of biological activity, as light exposure typically amplifies fullerene-induced ROS generation. Because impaired metamorphosis emerged at an exposure that left midgut ultrastructure largely intact, morphological endpoints alone are an insufficient basis for judging the safety of functionalized fullerenes, and developmental endpoints in insects should be included in their risk assessment.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105044947003,

title = {Multistage metasomatism during experimental reaction of axinite-(Fe) with F-, Cl-, OH-, Si-bearing fluids at 600 °C, 200 MPa and 800 °C, 500 MPa},

author = { W. Gmochowska and D.E. Harlov and E. Słaby and D. Chew and R. Juroszek and V. Peverelli and G.A. Kozub-Budzyń},

url = {https://doi.org/10.1007/s00710-026-00999-5},

doi = {10.1007/s00710-026-00999-5},

issn = {09300708},

year  = {2026},

date = {2026-01-01},

journal = {Mineralogy and Petrology},

abstract = {Many studies have shown that geological processes, such as metamorphism and metasomatism, consist of multiple superimposed events developing over various timescales, with each stage overprinting the previous one and thus complicating reconstruction of the complete history. Here, we report the use of a natural calcium aluminum borosilicate mineral axinite-(Fe) [(Ca2Fe2+Al2BSi4O15(OH)]; which occurs in skarn deposits; as a starting material in a series of experiments representing various metasomatic processes. The fluids used include NaF+H2O; NaCl+H2O; KCl+H2O; CaCl2+H2O; 2 M NaOH; 2 M KOH; Ca(OH)2+H2O; and Na2Si2O5+H2O; which are representative of common crustal fluids. The experiments were conducted at 600 °C; 200 MPa and at 800 °C; 500 MPa. The dominant experimental product was grandite garnet and; to a minor extent; wollastonite; titanite; and fluorite. Grandite garnet compositions vary significantly with respect to the fluid composition and the P-T conditions used; showing a wide range of grossular to andradite solid solutions. Under both P-T conditions; andradite-grossular zoning develops in experiments with metal-hydroxide–bearing fluids; whereas andradite-rich grandite garnet crystallizes in experiments utilizing Na2Si2O5+H2O. Despite varying physicochemical conditions; no differences are observed in the REE-chondrite normalized patterns from the product grandite garnet in each of the experiments. Wollastonite contains bustamite and ferrobustamite components whose composition is strongly controlled by the coexisting grandite garnet. These experiments provide important insights into understanding how first order skarn mineral assemblages may be altered during subsequent fluid-rock interaction under a variety of P-T conditions; highlighting how variations in the grandite garnet composition respond to variations in fluid composition.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105049286295,

title = {Development of the nasal capsule in Emydura subglobosa (Testudines: Pleurodira) with a comparison to other turtles},

author = { Ka. Ito and P. Kaczmarek and T. Nojiri and M.V. Fernandez Blanco and R. Kodera and I. Werneburg},

url = {https://doi.org/10.1002/ar.70326},

doi = {10.1002/ar.70326},

issn = {19328486},

year  = {2026},

date = {2026-01-01},

journal = {Anatomical Record},

abstract = {Extant turtles occupy freshwater, marine, and terrestrial habitats, and their nasal region provides important evidence for the evolution of respiration- and sensory-related cranial morphology. However, developmental data on the turtle nasal capsule remain limited, particularly in Pleurodira. Here, we describe nasal capsule development in the pleurodiran turtle Emydura subglobosa based on histological cross-sections of five distinct developmental stages and three-dimensional reconstructions. The nasal capsule underwent marked reorganization between Emyd. subglobosa developmental stages 4− and 5− (ES 4− and ES 5−), during which its basic architecture became established. Several features are notable. First, the nasal entrance shows distinctive pleurodiran specializations, including a processus supranarinus communis formed by medial fusion of the paired processus supranarini and a dorsally projecting processus rostralis medialis formed from the paired processus infranarini. In addition, Emyd. subglobosa possesses a fenestra rostralis at the nasal entrance, a feature not identified in other turtles examined to date. Second, the floor of the nasal capsule exhibits the expanded solum nasi complex characteristic of turtles, including the lamina transversalis anterior, pars paraseptalis, and pila supraglandularis, together with a canalis praepalatinus and a posteriorly facing fenestra basalis. Third, the pars ectochoanalis differs between the two major turtle clades: in pleurodires, it extends only slightly caudally, whereas in cryptodires it typically extends farther caudally and forms the ventral margin of the ductus nasopharyngeus. These findings provide a developmental framework for interpreting pleurodiran nasal morphology and a broader comparative framework for understanding turtle nasal evolution.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053335016,

title = {Machine learning assessment of industrial corrosion and public health risks in data limited aquifers of Northeastern Algeria},

author = { M.H. Eid and O. Saeed and P. Szücs and V. Mikita and A.A. Tamma and S. Elsayed and M.S.A. El-Baki and M.R. Abukhadra‬ and M.N. Bin-Jumah and A.A. Allam and M.S. Kamel and D. Dąbrowska and M. Gad},

url = {https://doi.org/10.1038/s41598-026-70426-4},

doi = {10.1038/s41598-026-70426-4},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

abstract = {Industrializing arid regions face a dual challenge: ensuring water suitability for emerging industries while protecting public health amidst chronic data scarcity. This study confronts this issue in northeastern Algeria by developing and validating an interpretable machine learning (ML) framework to predict industrial water quality and associated health risks from limited groundwater data. Based on 45 samples collected from the Debila and El-Oued regions of the Souf Valley, Artificial Neural Network (ANN), Random Forest (RF), and Decision Tree (DT) models were trained to predict seven corrosion and scaling potential (CSP) indices, namely the Langelier Saturation Index (LSI), Ryznar Stability Index (RSI), Aggressive Index (AI), Puckorius Scaling Index (PSI), Larson-Skold Index (LS), Chloride-Sulphate Mass Ratio (CSMR), and Revelle Index (RI), alongside the Canadian Council of Ministers of the Environment Water Quality Index (CCME-WQI). Physicochemical analysis revealed pervasive water quality deterioration, with 60% of samples exhibiting corrosive tendencies (LSI < 0) and 85% showing high corrosion risk (RSI > 6.8). All sites were uniformly classified as “Poor” by the CCME-WQI, and Monte Carlo simulations (10;000 iterations) confirmed significant non-carcinogenic health risks from nitrate for children (mean Hazard Index > 1.0). The ANN and RF models demonstrated robust predictive power, achieving R² values above 0.90 for six of the eight predicted indices. SHAP (SHapley Additive exPlanations) analysis identified the dominant hydrochemical drivers for each index, providing a transparent and actionable basis for targeted monitoring. This study presents a novel, validated, and transferable ML-based decision support tool that simultaneously integrates industrial process risks with public health assessment, offering a replicable water management paradigm for data-limited, industrializing regions worldwide.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053270030,

title = {Molecular Links Between Heat Stress and DNA Damage Response in Plants},

author = {  and M.E. Szurman-Zubrzycka},

url = {https://doi.org/10.1111/pce.70902},

doi = {10.1111/pce.70902},

issn = {01407791},

year  = {2026},

date = {2026-01-01},

journal = {Plant Cell and Environment},

abstract = {Climate change poses a major threat to agricultural productivity and, consequently, to global food security. Among the consequences of climate change, heat stress (HS) has emerged as a critical factor limiting crop performance. This has stimulated extensive research over the past decade to elucidate the molecular and physiological mechanisms underlying plant responses to HS. Recent findings indicate that the DNA damage response (DDR) pathway, associated with the maintenance of genome integrity, also plays an important role in plant thermotolerance. This review summarizes recent advances linking DDR components to plant HS responses. We discuss the involvement of the canonical DDR pathway, with particular emphasis on the role of SUPPRESSOR OF GAMMA RESPONSE 1 (SOG1) and its downstream targets in HS responses. In addition, we highlight emerging SOG1-independent modules, including the HOS1–RECQ2 pathway, as well as the recent insights into the plant DREAM complex, which further strengthens the connection between DDR and HS responses. Together, these findings position DDR as a key regulatory node coordinating genome stability, stress signalling and growth modulation under HS conditions. A deeper understanding of this connection may provide new opportunities for developing heat-tolerant crops and improving agricultural resilience in the context of global climate change.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053294612,

title = {Dynamics of Paraglacial Beach Development in Front of Rapidly Retreating Marine-Terminating Glacier – Hansbreen, Svalbard},

author = { O. Kostrzewa and K. Senderak and M. Ciepły and O. Glowacki and M.C. Strzelecki},

url = {https://doi.org/10.1002/esp.70432},

doi = {10.1002/esp.70432},

issn = {01979337},

year  = {2026},

date = {2026-01-01},

journal = {Earth Surface Processes and Landforms},

volume = {51},

number = {10},

abstract = {This study investigates the formation and controlling mechanisms of shorelines in the forefield marine-terminating glacier in Svalbard (Hansbreen; SW Spitsbergen), utilising multi-temporal remote sensing, sedimentological analysis and ground-penetrating radar (GPR). Since the end of the Little Ice Age (LIA), glacier retreat has exposed nearly 10 km of new coastline, with a marked acceleration with intensified deglaciation. Digital Shoreline Analysis System (DSAS) results reveal widespread coastal erosion characterised by high spatial variability. This variability is more strongly associated with contrasting wave-exposure conditions within the fjord than with distance to the present glacier front, which explains little of the observed shoreline change. Sea ice acts as a seasonal regulator—limiting the duration of wave activity rather than directly exerting thermodynamic or mechanical magnitude. Furthermore, sedimentological and geophysical data show a clear transition from heterogeneous glacigenic environments near the terminus to progressively reworked, wave-dominated systems. Grain-size distributions and internal stratigraphic architectures revealed by GPR surveys reflect greater sorting efficiency and morphological organisation as distance from active sediment sources increases. Ultimately, Hansbreen forefield represents a strongly process-structured paraglacial system, where coastal evolution is governed by the spatial distribution of wave energy and exposure history rather than direct glacial forcing or fluctuations in sediment supply.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053365575,

title = {Mobility and environmental availability of metal(loid)s at a historically recultivated Cu/Pb smelter site in Polichno, Holy Cross Mountains, Poland},

author = { K. Kupczak and R. Warchulski and V. Ettler and M. Mihaljevič},

url = {https://doi.org/10.1038/s41598-026-61748-4},

doi = {10.1038/s41598-026-61748-4},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

abstract = {This study investigates the long-term effects of partial recultivation on metal(loid) contamination and environmental risks at the historical (14-17th century) Cu–Pb smelting site at Polichno (Holy Cross Mountains; Poland). More than 50 years ago, the site underwent partial recultivation involving slag removal; however, residual slag fragments remain dispersed throughout the soil profile. The slag contains high mean concentrations of metal(loid)s, including 111,000 mg·kg− 1 Pb, 56,300 mg·kg− 1 Ba, 8370 mg·kg− 1 Zn, 465 mg·kg− 1 Cu, 110 mg·kg− 1 As, mainly hosted in sulfides, arsenides, sulfates, and a glassy matrix. Maximum soil concentrations reached 7010 mg∙kg− 1 Pb, 4180 mg∙kg− 1 Ba, 1500 mg∙kg− 1 Zn, 658 mg∙kg− 1 Cu, 45.4 mg∙kg− 1 As, with the highest levels in ash- and wood-containing horizons. Average pore water concentrations were 115 µg∙l− 1 Pb, 166 µg∙l− 1 Ba, 161 µg∙l− 1 Zn, 58.9 µg∙l− 1 Cu, and 1.9 µg∙l− 1 As. Batch leaching tests using deionized water classified the slag as non-hazardous waste rather than inert waste, as Pb release exceeded the regulatory threshold for inert waste. pH-static tests showed peak mobilization at pH 2 (Ba 39;000 mg·kg− 1; Pb 4860 mg·kg− 1; Zn 3870 mg·kg− 1; As 21.7 mg·kg− 1), with minima at neutral pH. The formation of secondary phases during leaching indicates immobilization processes that limit metal(loid) mobility.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053379040,

title = {On the possibility of deep seabed permafrost to occupy Ca. 7 million km2 in the Arctic Ocean},

author = { W. Dobiński and K. Saito},

url = {https://doi.org/10.1038/s41598-026-68112-6},

doi = {10.1038/s41598-026-68112-6},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

abstract = {Arctic Ocean (AO) shelf permafrost is the most popular and best-known type of subsea permafrost. Genetically, it is analogous to the ordinary subaerial permafrost. Today, the following types of subsea permafrost are also known: i) ice-bearing sediment layers formed from porewater freshening of terrestrial origins, ii) thermokarst lake taliks refreezing under cryotic seabed conditions, iii) bottom-fast ice preserving permafrost due to efficient heat conduction from atmosphere-ice-sediment coupling in winter, and iv) similar permafrost aggradation processes occurring beneath small islands and spits evolving with sediment dynamics. Here, we propose another type of marine permafrost: a deep seabed permafrost (DSP) underlying AO bottom sediments in a cryotic but not frozen state because of salty, supercooled seawater. Primary calculations indicate that the area of DSP deeper than 150 m may reach about 7.0 million km2, with the contacting seawater temperature ranging from − 2.5 °C to 0 °C. The formation and persistence of DSP or, almost equivalently, the negative-temperature regime of the AO seawater at the deeper layers may have begun at the Pliocene–Pleistocene border, ca. 3.5–2.4 Ma ago.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105025422071,

title = {Mechanisms of silver capture, reduction, and release in propyl carboxylic acid-functionalized SBA-15},

author = { M. Dulski and A. Strach and R. Zaleski and M. Gorgol and E. Matyja and M. Laskowska and A. Nowak and K. Pawlik and P. Rawicka and V. Grebņevs and Ł. Laskowski},

url = {https://doi.org/10.1016/j.seppur.2025.136542},

doi = {10.1016/j.seppur.2025.136542},

issn = {13835866},

year  = {2026},

date = {2026-01-01},

journal = {Separation and Purification Technology},

volume = {386},

abstract = {The growing contamination of aquatic systems by silver pollutants necessitates the development of advanced, sustainable remediation strategies. This study investigates Ag+ sequestration using propyl-carboxyl-functionalized SBA-15 (1.25–20 % COOH), focusing on how the density of functional groups governs structure, adsorption, and reduction. PALS and TEM revealed that low functionalization (1.25–5 %) enhances microporosity, whereas higher COOH contents (10 % and 20 %) expand mesopores. UV–Vis and FL-AAS confirmed that adsorption capacity depends on both surface chemistry and pore accessibility. Kinetic modeling indicated multistage sorption in highly functionalized samples, involving diffusion and surface adsorption. XPS results showed partial Ag+ reduction, with metallic fractions of ∼8.5 %, 64.4 %, and 73.7 % for the 2.5 %, 10 %, and 5 % COOH samples, respectively. LAXRD showed preserved mesostructural ordering, slightly weakened at lower COOH density, while TEM confirmed in-pore nucleation of reduced Ag0 nanoparticles. Despite having fewer -COOH sites, the 2.5 % COOH material exhibited comparable sorption to higher density carboxyl-functionalized SBA-15 as a result of the presence of larger mesopores and accessible silanols that enhanced Ag+ binding. Raman spectra revealed both unidentate/bidentate carboxylate coordination and silanol interactions. Desorption studies distinguished single-step surface release (10 % COOH) from dual-stage surface/pore release at lower functionalization. Overall, the results highlight the cooperative role of pore geometry and functionalization in controlling Ag+ adsorption, reduction, and release, positioning COOH-modified SBA-15 as an efficient, eco-friendly adsorbent.},

note = {3},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105049621882,

title = {Otoliths of cyprinids from Miocene sediments of the Kleszczów Gra ben (central Poland)},

author = { T. Brachaniec and M. Bugajski and O.M. Kovalchuk},

url = {https://doi.org/10.7306/2026.47},

doi = {10.7306/2026.47},

issn = {00332151},

year  = {2026},

date = {2026-01-01},

journal = {Przeglad Geologiczny},

volume = {74},

number = {7},

pages = {562-566},

abstract = {We report cyprinid (Cyprinidae) otoliths from the Middle Miocene lacustrine deposits of the Kleszczów Graben (Szczerców open-cast mine; central Poland). The specimens were recovered from dark gyttjas and lacustrine chalks within the Bełchatów lignite-bearing succession. They document freshwater fish communities inhabiting an extensive lake–marsh system that developed in central Poland during the Middle Miocene. The otoliths are well preserved and occur together with diverse vertebrate and invertebrate re mains, indicating favourable depositional and taphonomic conditions. Because freshwater cyprinids evolve rapidly and isolated lapilli may show convergent morphologies, the taxonomic assignments are treated cautiously and expressed mainly as open identifications. In contrast to the numerous marine otolith assemblages known from the Polish Miocene, freshwater otolith records remain scarce. The new material therefore provides valuable data on Neogene freshwater fish faunas of Central Europe and underscores the palaeontological potential of the lacustrine deposits of the Kleszczów Graben.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105042282049,

title = {Remains of anurans from the Miocene of central Poland},

author = { M.A. Salamon and M. Bugajski and T. Brachaniec and B. Czader},

url = {https://doi.org/10.7306/2026.32},

doi = {10.7306/2026.32},

issn = {00332151},

year  = {2026},

date = {2026-01-01},

journal = {Przeglad Geologiczny},

volume = {74},

number = {4},

pages = {375-380},

abstract = {The newly recovered anuran remains from Miocene deposits of the Bełchatów Lignite Mine (Kleszczów Graben; central Poland) provide the first confirmed record of amphibians from this sedimentary basin and constitute only the second Miocene occurrence of frogs in Poland, following the classic material from Nowa Wieś Królewska. A total of 33 isolated skeletal ele-ments, including vertebrae, a humerus, a probable jaw fragment, and ornamented cranial pieces, were retrieved from lacustrine gyttja and carbonate muds of the Szczerców pit. Despite the fragmentary preservation, their morphological attributes point to extinct repre-sentatives of Latonia, as well as spadefoot toads of the family Pelobatidae (Pelobates). More precise taxonomic identification, how-ever, requires a broader comparative framework and the acquisition of additional specimens. The assemblage adds important data to the sparse Neogene anuran record of Poland. The co-occurrence of fish, reptiles (including Diplocynodon), mammals (Chiroptera; Plesiosorex and other insectivores), and diverse molluscs underscores the mosaic character of the local ecosystems and supports reconstructions of a humid, dynamic lacustrine-wetland environment. These findings expand our understanding of anuran evolution-ary history, taphonomy and palaeobiogeography in central Europe, and they stress the need for further integrative studies aimed at refining species-level identifications and clarifying the ecological structure of Miocene vertebrate communities of the Kleszczów Graben.},

note = {1},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105041627416,

title = {Who is your Neighbour? Energy Consumption Relations in Suburban and Urban Areas. Evidence From Central Europe},

author = { P. Verma and J. Chodkowska-Miszczuk and Ag. Lewandowska and D. Perrotti},

url = {https://doi.org/10.1007/s10666-026-10141-6},

doi = {10.1007/s10666-026-10141-6},

issn = {14202026},

year  = {2026},

date = {2026-01-01},

journal = {Environmental Modeling and Assessment},

abstract = {Urban energy consumption shows a spatial association. This paper aims to investigate the spatial patterns of electricity consumption in Poland and determine its environmental, economic, demographic and infrastructural predictors. Spatial autocorrelation, Local Indicators of Spatial Association (LISA) and spatially lagged regression model were applied to selected predictors. Analysis was performed at the poviat (municipalities) scale for the year 2022. Per capita electricity (PCE) consumption showed a significant spatial autocorrelation and spatial distribution among the districts of Poland. Local clusters of similar consumption patterns were identified. Urbanisation rate and particulate matter showed negative total spatial impacts, while per capita municipal waste and petrol cars showed positive total impacts on PCE in a Spatial Autoregressive Combined (SAC) model. Creating strategies for cities with similar energy consumption can lead to local and regional renewable and sustainable energy transition. Exploration of these clusters is important for an organic understanding of spatial planning.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105046339097,

title = {Public Sports Facilities in the Era of Climate Change: Decarbonisation and Sustainable Transition in Toruń, Poland},

author = { A. Michalska and J. Chodkowska-Miszczuk},

url = {https://doi.org/10.21697/seb.5892},

doi = {10.21697/seb.5892},

issn = {17331218},

year  = {2026},

date = {2026-01-01},

journal = {Studia Ecologiae Et Bioethicae},

volume = {24},

number = {3},

pages = {129-144},

abstract = {This study examines how public sports facilities can support urban sustainable transition in the context of climate change, with particular attention to decarbonisation, climate mitigation, and social resilience. The analysis focuses on sports infrastructure managed by the Municipal Sports and Recreation Centre in Toruń, Poland, and combines two analytical perspectives: infrastructural and social. The first addresses technical modernisation, energy efficiency, renewable energy integration, and water management, while the second considers the role of sports facilities as multifunctional public spaces supporting social integration, environmental awareness, and urban well-being. The findings reveal substantial differences in the environmental performance of individual facilities, with aquatic facilities achieving the highest scores due to their technical specificity, stronger investment capacity, and greater functional complexity. The study identifies the urgent need for a coherent modernisation strategy for public sports infrastructure, particularly in relation to renewable energy systems, rainwater retention, and long-term cross-sector cooperation between local government, research institutions, and private actors. The article argues that public sports facilities should be understood not only as sites of recreation, but also as strategic components of climate-responsive and socially sustainable urban development.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105053343279,

title = {Uncovering a medieval tsunami: Multidisciplinary evidence for a ∼1300 CE tsunamigenic earthquake and coseismic subsidence in the Guerrero seismic gap, Mexico},

author = { M.T. Ramírez-Herrera and O. Coca and J. Černý and N. Corona and K. Gaidzik and D. Sugawara and A. Goguitchaichvili and A.C. Ruiz-Fernández},

url = {https://doi.org/10.1016/j.quaint.2026.110496},

doi = {10.1016/j.quaint.2026.110496},

issn = {10406182},

year  = {2026},

date = {2026-01-01},

journal = {Quaternary International},

volume = {786},

abstract = {Reconstructing long-term seismic behavior using geological records along subduction zones, where the largest tsunamigenic earthquakes occur, is key in understanding earthquake and tsunami hazard. To assess whether the Guerrero seismic gap, a segment of the Mexican Subduction Zone, can generate great megathrust earthquakes, we present original geomorphological, sediment characteristics, geochemical, microfossil, magnetic properties, and radiocarbon data, documenting a tsunamigenic earthquake at approximately 1300 CE from Boca de Mitla, Guerrero. The sand deposit displays basal erosional contact, rip-up clasts, flame-like basal structures, marine geochemical signal, and brackish-marine diatoms. Diatom assemblages show evidence of coseismic subsidence of ∼21 cm. Radiocarbon constrain the event at ∼1300 CE, accordant with a prehistoric tsunami previously identified approximately 30 km WNW of Boca de Mitla. The reconstructed long-term seismic prehistory shows that the Guerrero seismic gap can produce large tsunamigenic earthquakes (Mw > 8). The new evidence enhances our understanding of the region's seismic behavior by integrating the paleoseismic and paleotsunami evidence in the assessment of earthquake and tsunami hazard along the Mexican subduction zone, and underscores the importance of geomorphological, geological and geochronological research in this and other active convergent margins globally.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105052880602,

title = {Snow cover variability in the Western Beskids (Poland) during the 1951–2023 winter seasons},

author = { A. Drabek and A. Biesmer and D. Absalon},

url = {https://doi.org/10.1038/s41598-026-69770-2},

doi = {10.1038/s41598-026-69770-2},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

abstract = {The impact of long-term snow cover variability on winter tourism in the mountainous areas of Poland is an increasingly important research topic, particularly in light of the anticipated effects of climate change. Available studies are often of regional scope, limited to higher elevations, while lower mountain ranges such as the Western Beskids remain insufficiently studied. This study aims to examine trends, determine the rate of change, and identify abrupt changes for selected snow cover variables: snow cover duration [SCD], total number of days with snow cover equal to or greater than 30 cm [SCD ≥ 30], and potential snow cover duration [PSCD]. We show that during the study period, the seasonal duration of snow cover decreased at approximately half of the studied locations, while no significant trends were observed for skiing-specific indicators. The most pronounced downward trends occurred in January and March. At the same time, step change detection revealed abrupt changes in time series, mostly in the 1980s. Our results demonstrate that snow cover variability can be effectively assessed in lower mountainous regions and in climatically complex temperate zones, provided that sufficiently long time series are available. They also confirm that the declining trends in snow cover observed elsewhere are likewise present in the Western Beskids.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105044986181,

title = {Influence of tree species on glomalin-related soil protein and organic carbon fractions in reclaimed post-coal-mining sites},

author = { A.M. Misebo and W.M. Bierza and M. Pietrzykowski},

url = {https://doi.org/10.1016/j.geoderma.2026.117949},

doi = {10.1016/j.geoderma.2026.117949},

issn = {00167061},

year  = {2026},

date = {2026-01-01},

journal = {Geoderma},

volume = {472},

publisher = {Elsevier B.V.},

abstract = {The choice of tree species for restoring postmining landscapes critically determines soil development, yet its specific effects on the dynamics of soil organic carbon (SOC), soil nitrogen, and glomalin-related soil protein (GRSP) fractions remain inadequately quantified. We investigated the influence of five tree species (Scots pine; black alder; black locust; pedunculate oak; and European larch) on the distribution of carbon and nitrogen among three physical SOC fractions—free light fraction (FLF), occluded light fraction (OLF), and mineral-associated fraction (MAF)—and on GRSP concentrations in a reclaimed post-coal-mining site. The trees investigated were 24–28-year-old stands, and soil samples were collected at depths of 0–10 cm and 10–30 cm. Our findings demonstrate that the choice of tree species significantly altered the pathways of SOC and nitrogen accumulation and stabilization. Recalcitrant litter under Scots pine promoted slow-cycling carbon, sequestered primarily in the FLF pool, whereas nitrogen-fixing species (black alder and black locust) and pedunculate oak enhanced the accumulation of stable carbon and nitrogen in physically protected (OLF) and mineral-associated (MAF) fractions. GRSP concentration was the highest under black alder, with average values of 6.52 mg g⁻1 at 0–10 cm and 4.43 mg g⁻1 at 10–30 cm. Moreover, GRSP fractions were strongly positively correlated with OLF carbon and MAF nitrogen fractions, indicating that GRSP plays a pivotal mechanistic role in the formation of stable aggregates and organo-mineral complexes during pedogenesis. These results highlight how different tree species influence the dynamics of labile and stable soil organic matter pools differently. Our findings suggest that nitrogen-fixing broadleaf species (black alder and black locust) and the ectomycorrhizal species pedunculate oak should be prioritized during postmining land restoration to optimize GRSP enrichment and the sequestration of stable SOC and nitrogen.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105051198181,

title = {Disaster history of the Prambanan temple complex (Java, Indonesia) – an archaeoseismological study},

author = { M. Kázmér and R.N.F.A. Nahar and K. Gaidzik},

url = {https://doi.org/10.1016/j.quaint.2026.110468},

doi = {10.1016/j.quaint.2026.110468},

issn = {10406182},

year  = {2026},

date = {2026-01-01},

journal = {Quaternary International},

volume = {784},

publisher = {Elsevier Ltd},

abstract = {Yogyakarta (Java; Indonesia) has long been considered a seismic gap in the Sunda Arc. Then a 6.5 magnitude earthquake struck the region on 26 May 2006. A large number of casualties and property losses raised the question of whether there were preceding earthquakes. The adjacent Hindu temple complex Prambanan holds the longest record of 1200 years of disaster history. We reviewed historical data from construction through abandonment, burial, first collapse, restoration, and second collapse, to modern reconstruction. The damage caused by the AD 1584 and 2006 collapses allowed to identify recurring seismic events. Archaeoseismology yielded intensity IX for the 2006 event and intensity IX + for 1584. Geometry of shifted and collapsed masonry shows that the direction of the highest, σ1 stress (30°-210°) is parallel to the strike of the causative fault. Small but persistent deformation of heritage buildings caused by earthquakes is a good indicator of past earthquake parameters. This is the first study to use archaeoseismology to parameterize past earthquakes in the Southeast Asian archipelago.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105052560518,

title = {Satellite-Based Assessment of Chlorophyll-a Variability, Seasonal Trends, and Eutrophication Risk for Water Sustainability in a Strategic Desert Reservoir},

author = { S.N. Alowfi and I.M. Hamdi and J. Selín and A.A. Aldohan and M. Zeleňáková and D. Dąbrowska and Y.M. Youssef},

url = {https://doi.org/10.3390/w18182256},

doi = {10.3390/w18182256},

issn = {20734441},

year  = {2026},

date = {2026-01-01},

journal = {Water Switzerland},

volume = {18},

number = {18},

publisher = {Multidisciplinary Digital Publishing Institute (MDPI)},

abstract = {Lake Nasser represents Egypt’s principal strategic freshwater reservoir; however, its long-term phytoplankton dynamics at the basin scale remain insufficiently characterized. This study presents a detailed spatiotemporal investigation of chlorophyll-a (Chl-a) variability across the reservoir during the 2002–2020 period using exclusively MODIS-Aqua Level-3 satellite observations. As no concurrent in situ measurements were available for validation, the reported values are treated as satellite-derived Chl-a estimates rather than direct observations of phytoplankton biomass. A non-parametric statistical approach, incorporating the Mann–Kendall test, Theil–Sen slope estimator, coefficient of variation (CV), and relative anomaly analysis, was used to characterize pixel-level climatology and temporal trends. The findings demonstrate that the reservoir exhibits pronounced spatial heterogeneity and a well-defined bimodal seasonal pattern associated with the annual Blue Nile flood pulse during August–October and winter convective mixing processes between November and February. Although annual-scale analysis did not indicate a statistically significant monotonic trend, seasonal investigations revealed strongly contrasting temporal responses throughout the year. At the pixel level, significant increases dominated ten of the twelve calendar months, from September through June, with median slopes among significant pixels of +0.36 to +1.47 mg m−3 yr−1. July and August reversed this pattern, combining significant declines along the northern and central main channel with the steepest increases in the record at the extreme southern inflow. The directional contrast was unaffected by control of the false discovery rate within each calendar month (q = 0.05), which retained 66% of the significant pixels. Summer conditions were additionally marked by substantial temporal variability (CV > 60%) and pronounced positive anomalies, reaching +274.51% during August. Notably, these anomalies were spatially concentrated within the central and southern sectors of the reservoir, rather than within the conventionally productive northern region. This spatial redistribution, together with the broad enrichment tendency indicated by the pixel-level trends, points to an intensification of the summer maximum within the southern inflow zone and to a possible emergence of localized eutrophication risk, a hypothesis that requires confirmation through concurrent nutrient, transparency, and dissolved-oxygen observations. Overall, the study provides valuable geospatial insights for the environmental management of Lake Nasser, emphasizing the importance of implementing targeted early-warning systems for harmful algal bloom monitoring. The results also demonstrate the critical role of satellite-based Earth observation technologies in supporting adaptive water resource management under evolving climatic and hydrological conditions.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105052159277,

title = {To acetylate or deacetylate? WIND1 directs opposing H3K27 modifications in plant somatic cell reprogramming},

author = { J. Falińska and K. Nowak and B. Wójcikowska},

url = {https://doi.org/10.1007/s11103-026-01765-z},

doi = {10.1007/s11103-026-01765-z},

issn = {01674412},

year  = {2026},

date = {2026-01-01},

journal = {Plant Molecular Biology},

volume = {116},

number = {5},

publisher = {Springer Science and Business Media B.V.},

abstract = {Understanding the mechanisms that trigger the embryogenic program in plant somatic cells remains a major focus of modern molecular biology, because this process is widely used for clonal propagation, cryopreservation, and genetic transformation. Recently, Iwase et al. demonstrated that the transcription factor WOUND INDUCED DEDIFFERENTIATION 1 (WIND1) can simultaneously promote histone H3 acetylation at lysine 27 and induce expression of genes associated with the embryogenic response, while also activating deacetylation of this histone and repressing genes associated with differentiation.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105033602049,

title = {An interlaboratory study of biochar reflectance measurements: Methodological implications},

author = { A. Drobniak and M. Mastalerz and Be. Liu and G.P. Lis and K. Lis and A. Rudra and H.I. Petersen and J.C. Hower and C.F. Eble and K. Widziewicz-Rzońca},

url = {https://doi.org/10.1016/j.coal.2026.104989},

doi = {10.1016/j.coal.2026.104989},

issn = {01665162},

year  = {2026},

date = {2026-01-01},

journal = {International Journal of Coal Geology},

volume = {318},

publisher = {Elsevier B.V.},

abstract = {Reflectance has been recognized as a key indicator of biochar permanence, yet no internationally standardized biochar-specific methodology exists for its measurement. To evaluate the currently used practices, a round-robin study involving nine experienced petrographers across multiple international laboratories was performed to assess the reproducibility of reflectance values and the influence of biochar particle size on analytical outcomes. Despite shared petrographic expertise, the results revealed noticeable, though anticipated, variability among analysts, primarily stemming from system calibration and subjective differences in selecting measurement spots. Among the three biochars studied (hardwood; kolmar wood; and rice hull), this factor was particularly pronounced in the highly heterogeneous rice hull biochar. Average reflectance values for analyzed hardwood biochars were consistently high, ranging from 4.25% to 5.39% across petrographers and three particle sizes (20; 60; and 230 mesh). In contrast, kolmar wood biochar showed lower and more uniform values of 1.29–1.91%, while rice hull biochar exhibited the lowest reflectance, between 1.05 and 1.52%. Discrepancies in reflectance reached up to ∼1.0% for high-reflectance biochars and 0.4–0.5% for the kolmar and rice hull samples—acceptable for permanence assessment but highlighting the need for standardized measurement protocols. Statistical validation confirmed that most petrographers produced results within accepted limits (h ± 2.23; k < 2.09), demonstrating reliable consistency and reproducibility. Particle size influenced reproducibility, with coarser fractions (20- and 60-mesh) yielding more consistent results than finely ground samples (230-mesh), which introduced greater subjectivity in spot selection. Additionally, no statistically significant differences were detected between manual grid-based and automated frame-based measurement setups, indicating that both approaches provide comparable analytical outcomes. This study highlights the considerable capability of reflected light microscopy (RLM) as a rapid and quantitative approach for assessing biochar permanence. At the same time, it emphasizes the need to consider biochar heterogeneity, calibration range, and the importance of explicit spot-selection criteria in developing biochar-specific protocols. Based on the results obtained, the method proved reliable and reproducible, reinforcing its suitability as a standardized technique for biochar characterization.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105044365010,

title = {Balancing pastoral heritage and tourism – A DRSIR perspective on landscape transformation in European mountains},

author = { M. Sobala and A. Żemła-Siesicka},

url = {https://doi.org/10.1016/j.landusepol.2026.108202},

doi = {10.1016/j.landusepol.2026.108202},

issn = {02648377},

year  = {2026},

date = {2026-01-01},

journal = {Land Use Policy},

volume = {170},

publisher = {Elsevier Ltd},

abstract = {European mountain areas have been historically shaped by traditional pastoral practices, creating culturally, ecologically, and visually valuable traditional landscapes. Over the past decades, these landscapes have faced profound transformations due to the decline of pastoralism and the rapid development of tourism. This paper applies a modified DPSIR framework, referred to as the DRSIR model, to present driving forces, local reactions, landscape state changes, impacts, and responses related to transformations of pastoral landscape in European mountain regions. The aim of this paper is to present a conceptual synthesis of these transformations based on a literature review and structured using the DRSIR framework. The conceptual synthesis enabled the identification of three landscape transformation models: Co-presence, Sequence, and Abandonment. These models reflect varying degrees of interaction between pastoralism and tourism. Co-presence allows for sustainable coexistence or cooperation between traditional pastoralism and tourism which allows the preservation of traditional landscape features. Sequence models illustrate transitions where one function succeeds or suppresses the other, and abandonment reflects the decline of pastoral practices and tourism, often leading to afforestation and loss of landscape and cultural values. The essay highlights landscape consequences of these trajectories. Management responses, guided by legal protection, agri-environmental policies, and sustainable tourism initiatives, can either prevent abandonment or mitigate negative impacts, shaping future landscape scenarios. The DRSIR framework provides a comprehensive lens for understanding these dynamics, supporting spatial planning and landscape management by enabling the identification of dominant relationships between tourism and pastoralism in different mountain regions. Maintaining the evolutionary continuity of traditional landscapes while integrating pastoralism and tourism functions emerges as a key strategy for preserving European mountain landscapes.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105045301064,

title = {Genomic and functional characterization of Rhizobium metallidurans NS41, a heavy-metal-resistant, non-legume-associated endophyte that reduces oxidative stress in metal-exposed maize},

author = { I. Bodnaruk and M. Rudnicka and Z. Piotrowska-Seget},

url = {https://doi.org/10.1007/s00438-026-02482-4},

doi = {10.1007/s00438-026-02482-4},

issn = {16174615},

year  = {2026},

date = {2026-01-01},

journal = {Molecular Genetics and Genomics},

volume = {301},

number = {1},

publisher = {Springer Science and Business Media Deutschland GmbH},

abstract = {Heavy metal (HM) contamination threatens plant health and poses significant challenges to agriculture and ecosystem functioning. Plant-associated microorganisms from HM-contaminated environments play a vital role in enhancing host stress tolerance and are promising candidates for sustainable, microbe-based strategies to support plant fitness. Non-legume-associated rhizobia, however, remain poorly described in this context. In this study, we characterized Rhizobium metallidurans strain NS41, an endophyte of goldenrod (Solidago canadensis) growing at a highly metal-contaminated site. To our knowledge, this is the first report of this species associated with a non-leguminous host, thereby expanding current knowledge about R. metallidurans. Genome analysis revealed determinants of HM resistance, oxidative and osmotic stress mitigation, and metabolism of plant-derived compounds, but no canonical nodulation genes, indicating a facultative endophytic, rather than nodulation-dependent, lifestyle adapted to metalliferous environments. In vitro, NS41 demonstrated tolerance to high Zn, Cd, and As(III) concentrations (MIC 20 mM; 2.5 mM; 5 mM; respectively), produced indole-3-acetic acid and ammonia, and solubilized phosphates. In a maize pot experiment in HM-contaminated soil, seed inoculation with NS41 resulted in lower hydrogen peroxide and anthocyanin levels and higher chlorophyll content, without significantly altering biomass or Cd accumulation. This identifies NS41 as a stress-mitigating endophyte rather than a strong direct growth promoter under the tested conditions. Together, these genomic features and stress-mitigating phenotype support further investigation of NS41 as a plant-protective bioinoculant for improving plant performance on HM-contaminated soils.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105048181160,

title = {Value of ponds in bomb craters formed during World War II in maintaining biodiversity},

author = { M. Krodkiewska and A. Cieplok and A. Spyra and A. Koczorowska and J.M. Waga and M. Fajer and B. Szypuła and T. Molenda},

url = {https://doi.org/10.1080/24750263.2026.2716439},

doi = {10.1080/24750263.2026.2716439},

issn = {24750263},

year  = {2026},

date = {2026-01-01},

journal = {European Zoological Journal},

volume = {93},

number = {1},

pages = {936-948},

publisher = {Taylor and Francis Ltd.},

abstract = {With the ongoing loss of aquatic habitats worldwide, small water bodies are becoming increasingly important as substitute habitats for aquatic biota. In this study, we evaluated the diversity of benthic fauna in ponds formed in craters created by bombings during World War II in Poland (Central Europe), as water bodies originating under such circumstances are rarely studied. Macroinvertebrate samples were collected from 62 ponds, and data on macrophyte distribution, water parameters, and the water bodies surface area were recorded. Despite the small size, the ponds were characterized by a high diversity of benthic fauna. In total, invertebrates representing 61 lower taxa (species; genera; and families) were collected. Among the environmental variables examined, only water oxygenation, conductivity, phosphate content, macrophyte coverage, and sunlight exposure affected the structure of the benthic fauna. No correlation was observed between pond size and diversity indices, although a relationship was found between surface area and macroinvertebrate density. The Kruskal–Wallis ANOVA indicated significant differences between ponds with different macrophyte distributions and diversity indices. The Mann–Whitney U test revealed significant differences in faunal diversity between shaded and sunlit ponds. This study demonstrated that individual ponds had a significant influence on regional diversity (γ diversity), emphasizing the importance of pond networks in maintaining biodiversity at the landscape level. Despite the ecological role of bomb crater ponds, they are often omitted from studies on small ponds. Further research is, therefore, essential, especially since small aquatic environments are particularly sensitive to disturbances and may disappear within a short period.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105050757345,

title = {Somatic embryogenesis and organogenesis in Narcissus poeticus var. recurvus (Haw.) Baker—relationship to alkaloid content},

author = { A. Błażejczak and A. Milewska-Hendel and R. Spina and D. Laurain-Mattar and F. Dupire and A. Ptak},

url = {https://doi.org/10.1007/s11240-026-03597-7},

doi = {10.1007/s11240-026-03597-7},

issn = {01676857},

year  = {2026},

date = {2026-01-01},

journal = {Plant Cell Tissue and Organ Culture},

volume = {167},

number = {1},

publisher = {Springer Science and Business Media B.V.},

abstract = {Amaryllidaceae plants are known for their ornamental value and the production of alkaloids with pharmacological properties. The aim of the research was to obtain, for the first time, in vitro cultures of Narcissus poeticus var. recurvus using the process of somatic embryogenesis and adventitious organogenesis from leaf and flower stem explants and to check their biosynthetic capacity. The medium supplemented with 25 µM 4-amino-3,5,6-trichloropicolinic acid (picloram) and 5 µM benzyladenine (BA) stimulated the induction of embryogenic callus and the subsequent formation of somatic embryos from this callus. Scanning electron microscopy and histological analyses confirmed the presence of somatic embryos. Somatic embryos converted into plants on a medium with 0.5 µM α-naphthaleneacetic acid (NAA) and 5 µM BA. The highest number of bulbs was formed on stem explants cultured on a medium containing 5 µM NAA and 5 µM BA or 5 µM 2,4-dichlorophenoxyacetic acid (2;4-D) and 5 µM BA while 25 µM NAA and 0.5 µM BA stimulated root formation. The chromatography–mass spectrometry analysis revealed the presence of galanthamine, 1,2-didehydrocrinan-3-ol, anhydrolycorine, crinine, pancracine, 11-hydroxyvittatine and lycorine in in vitro cultures. Alkaloid biosynthesis is closely related to tissue differentiation. Callus and somatic embryos did not produce galanthamine and accumulated small amounts of lycorine. The bulbs and plants showed the highest capacity for biosynthesis of these alkaloids.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105047316199,

title = {Mutation Breeding as a Tool for Sustainable Crop Production and Climate Resilience: Experiences from the South-Eastern Europe (SEE) and Central Asia (CA)},

author = { S. Cvejić and A. Radanović and D. Trkulja and S. Glogovac and I.D. Vukelić and M.K. Zejković and M. Antić and S. Umićević and J. Grahić and M. Jankulovska and N. Sandeva Atanasova and B. Kuzmanovska and B. Lazarević and E.M. Abraham and E.E. Tani and E. Sarri and D.Ν. Vlachostergios and C. Petsoulas and A. Kargiotidou and C.I. Pankou and R.M. Usmanov and B. Anapiyayev and K.M. Iskakova and N.B. Tomlekova and E.K. Nacheva and D.G. Ganeva and S.D. Aziz and A. Şenay and H. Peşkircioğlu and E. Seçer and A. Gőktuğ and K.Y. Kantoglu and J. Kwaśniewska and S.B. Jocić and A.D. Kondić-Špika and D. Miladinović},

url = {https://doi.org/10.3390/agronomy16151488},

doi = {10.3390/agronomy16151488},

issn = {20734395},

year  = {2026},

date = {2026-01-01},

journal = {Agronomy},

volume = {16},

number = {15},

publisher = {Multidisciplinary Digital Publishing Institute (MDPI)},

abstract = {The review summarizes practical experiences in using mutation breeding for crop improvement in South-Eastern Europe (SEE) and Central Asia (CA), demonstrating that mutation breeding can be a field-validated, effective approach for developing climate-resilient crops. Drawing on coordinated research conducted within national breeding programs and international initiatives supported by FAO/IAEA, applied methodologies, trait-evaluation strategies, and concrete breeding outputs in cereals, legumes, and industrial crops are presented. The use of gamma irradiation, fast neutrons, and chemical mutagens has successfully generated stable mutant lines stable mutant lines with enhanced traits, such as increased thousand-grain weight in wheat, altered oil quality in sunflower, and improved drought tolerance in common bean and sesame. The integration of classical pedigree selection with modern breeding tools such as high-throughput phenotyping, molecular and biochemical markers, and doubled-haploid technology has enabled earlier and more efficient identification of superior genotypes in mutation breeding programs. The review underscores the practical relevance of mutation breeding in contemporary pipelines to maintain yield stability and quality under adverse environmental conditions.},

note = {1},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105050600602,

title = {Have we entered a ‘post-model’ era in plant biology?},

author = { R. Hasterok and N. Borowska-Zuchowska and B.A. Kolano and H. Shimomai and Z. Yin and K. Wang and L.A.J. Mur},

url = {https://doi.org/10.1016/j.tplants.2026.08.013},

doi = {10.1016/j.tplants.2026.08.013},

issn = {13601385},

year  = {2026},

date = {2026-01-01},

journal = {Trends in Plant Science},

publisher = {Elsevier Ltd},

abstract = {Models such as arabidopsis ( Arabidopsis thaliana ) have underpinned genomic and physiological research in plant science. Advances in genome sequencing, pangenomics, and genome editing have prompted claims of a ‘post-model’ era, with model–crops and crops such as rice and bread wheat combining agricultural relevance with experimental tractability. We argue that the ‘simplicity-to-complexity’ approach remains valid, although model systems have evolved. Arabidopsis remains indispensable for interpreting multi-omics data, testing developmental hypotheses, and generating mechanistic insights difficult to obtain in crops. Linking these strengths to model–crops adds translational value by bridging discovery and breeding, while niche models such as Brachypodium distachyon and legumes address grass cell wall biology and nitrogen fixation. Future progress depends on diverse species with complementary strengths across fundamental and applied plant biology.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105050642090,

title = {Bathymetry, sediment architecture and buried subglacial topography of two contrasting high-mountain lakes from ground-penetrating radar (Tatra Mts., Poland)},

author = { B. Gądek and M. Grabiec and S. Kedzia},

url = {https://doi.org/10.1016/j.geomorph.2026.110541},

doi = {10.1016/j.geomorph.2026.110541},

issn = {0169555X},

year  = {2026},

date = {2026-01-01},

journal = {Geomorphology},

volume = {514},

publisher = {Elsevier B.V.},

abstract = {Small high-mountain lakes archive Holocene environmental change in their bottom sediments, and the older glacial history of the region in the relief of their buried bedrock. Deciphering both records requires characterizing lake bathymetry and fill architecture. This paper presents the results of such an integrated investigation of two adjacent, morphologically contrasting glacial lakes in the High Tatra Mountains (Zielony Staw Gąsienicowy and Kurtkowiec). The surveys were carried out in winter, from a stable ice cover, using a dual-channel GPR (50 and 100 MHz) coupled with a GNSS receiver. The dielectric properties of the subsurface media were determined from WARR velocity soundings. The new bathymetric models revealed the uncertainty of the archival data. Within the lake fills, four radar facies with contrasting thickness distributions were identified: laminated lacustrine sediments (RF1), weakly laminated and transparent (glacio)lacustrine sediments (RF2), coarse-clastic slope deposits (RF3), and morainic deposits (RF4). The bedrock beneath both lakes occupies the same preglacial valley level; Zielony Staw, however, formed in a glacial overdeepening, whereas Kurtkowiec is an intramorainic basin. The buried N-channels and potholes identified here point to the presence of pressurized subglacial water, to basal sliding of the former temperate-based Tatra glaciers, and to the inheritance of the subglacial drainage course by present-day streams. The results confirm the usefulness of GPR in studies of small high-mountain lakes and highlight the potential of geophysical surveying for planning sediment coring.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105045157554,

title = {Integrative study of two invasive North American pine aphids (Cinara atlantica and C. watsoni) in South Korea},

author = { Mi. Lee and M. Kanturski and C. Favret and S. Lee},

url = {https://doi.org/10.1038/s41598-026-46921-z},

doi = {10.1038/s41598-026-46921-z},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

publisher = {Nature Research},

abstract = {This study investigates the seasonal ecology, morphology, and invasion history of the aphids Cinara atlantica and C. watsoni (Hemiptera: Aphididae: Lachninae) in South Korea and assesses their potential ecological impacts. Historically, C. atlantica was recorded only on non-native pines, but we provide the first evidence of host expansion to the native pine Pinus densiflora. C. watsoni is recorded for the first time in South Korea on imported pines, indicating a potential risk of spread to native hosts. Field surveys conducted between 2020 and 2025, including monthly monitoring, showed that both species reproduce anholocyclically, with colony densities peaking in June and October–November. Honeydew accumulation promoted sooty mold development, and heavy infestations caused needle yellowing. Morphological redescriptions, DNA barcoding, and haplotype analyses confirmed species identities and revealed minimal genetic divergence between South Korean and Nearctic populations. Shared haplotypes with North American material suggest a recent introduction possibly mediated by international plant trade, although the precise source remains uncertain. These findings highlight the high invasion potential of Cinara species and emphasize the need for strengthened phytosanitary measures and continuous monitoring of conifer-associated aphids in East Asia.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105049249343,

title = {Human-Environment Interactions Within the Landscape Mosaic of the Central European Section of the Dune Belt in the Light of Palaeobotanical Studies (Włoszczowa Basin, Southern Poland)},

author = { A. Szymczyk and M. Nita and S. Skreczko},

url = {https://doi.org/10.1080/14614103.2026.2715199},

doi = {10.1080/14614103.2026.2715199},

issn = {14614103},

year  = {2026},

date = {2026-01-01},

journal = {Environmental Archaeology},

publisher = {Taylor and Francis Ltd.},

abstract = {The study aimed to trace the impact of settlement and farming by cultures in the Late Holocene on the landscape mosaic of the eastern part of the Włoszczowa Basin in southern Poland. Despite the presence of many different cultures, settlement there was much sparser than in neighbouring areas. This was influenced by the small size and fragmented nature of fertile soil patches and was reflected in the minor scale and reversible nature of environmental changes, which were limited to the immediate vicinity of settlements. No deforestation or changes in the composition of forest species were recorded. Pollen spectra made it possible to distinguish several phases of intensified settlement and environmental pressure. The first traces of settlement date back to the Younger Neolithic, and a marked increase in indicators of human activity was recorded at the end of that period. Intensified human activity in the region was also recorded in the second half of the Bronze Age, which can be attributed to settlements of the Lusatian culture, as well as during the period of Roman influence when the Przeworsk culture emerged. Clear evidence of human impact on the environment and landscape was only recorded in the Early Middle Ages.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105046296749,

title = {Deep subsurface architecture of the Hans Glacier forefield, Svalbard. Seismic evidence for permafrost degradation and groundwater pathways},

author = { A. Marciniak and E. Roshdy and S.J. Oryński and M. Osuch and W. Dobiński and M. Majdański},

url = {https://doi.org/10.1016/j.catena.2026.110487},

doi = {10.1016/j.catena.2026.110487},

issn = {03418162},

year  = {2026},

date = {2026-01-01},

journal = {Catena},

volume = {273},

publisher = {Elsevier B.V.},

abstract = {The Arctic and Antarctic regions are experiencing polar amplification, with warming rates significantly exceeding the global average. This rapid increase in thermal conditions drives permafrost degradation, threatening the structural integrity of cryospheric landscapes. While extensive research has focused on surface-level phenomena and active layer dynamics, a profound knowledge gap persists regarding deeper, stable cryotic structures and their role in landscape evolution. In glacier forefields, such as those in Svalbard, the transition from glacial to periglacial environments is critical, yet the deep subsurface architecture remains poorly understood due to the logistical challenges of Arctic fieldwork. This study employs high-resolution seismic reflection imaging to investigate the complex subsurface architecture of the Hans Glacier terminal moraine and its associated forefield in southern Spitsbergen. We present data from two field campaigns (September/October 2017 and April/May 2018) that cover profiles up to 1130 m in length. A comparative analysis reveals an important methodological paradox: while thick snow cover attenuates high-frequency signals, the seasonal freezing of the near-surface active layer significantly improves deep seismic coupling, extending the imaging range. The results provide high-resolution evidence of post-glacial sedimentary sequences and detect buried ice cores. Beneath this cryotic barrier, we observe laterally persistent structural elements that suggest the presence of a deeper, unfrozen system. These findings indicate that the Hans Glacier forefield is an active component of a complex hydrogeological system, where degrading permafrost and deep structural pathways may facilitate critical groundwater-seawater interactions and submarine groundwater discharge from the terrestrial forefield into the adjacent fjord.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105035893697,

title = {Integrative taxonomic study reveals a new species of Maculolachnus (Hemiptera: Aphididae) from South Korea},

author = { Mi. Lee and M. Kanturski and S. Lee},

url = {https://doi.org/10.1038/s41598-026-40274-3},

doi = {10.1038/s41598-026-40274-3},

issn = {20452322},

year  = {2026},

date = {2026-01-01},

journal = {Scientific Reports},

volume = {16},

number = {1},

publisher = {Nature Research},

abstract = {The genus Maculolachnus Gaumont, 1920 (Hemiptera: Aphididae: Lachninae) exhibits substantial hidden diversity, yet its life history remains poorly understood. Here, we present an integrative taxonomic study of Maculolachnus in South Korea, revealing a previously unrecognized species closely related to M. submacula and providing the first biological insights into the group. We combined detailed morphological examinations, mitochondrial COI sequence analyses, and field observations of colony structure and phenology to clarify species boundaries and elucidate life history traits. Populations formerly identified as M. submacula exhibited distinct morphological characters and significant COI divergence. Phylogenetic reconstructions (BI; ML; NJ), species delimitation methods (ABGD; ASAP; bPTP), and haplotype network analyses consistently supported four distinct species: M. submacula, M. sijpkensi, M. paiki, and a new species described herein as Maculolachnus koreanus sp. nov. The COI distance between M. koreanus sp. nov. and M. submacula exceeded 2.4%, surpassing the typical aphid barcode gap. We redescribe the rare alate viviparous female of M. paiki, which is endemic to South Korea. Observations on M. koreanus sp. nov. revealed ant attendance and seasonal reproductive strategies. Scanning electron microscopy (SEM) provided the first detailed characterization of sensorial structures. This study highlights the value of integrative taxonomy in revealing hidden diversity within Lachninae. International Commission on Zoological Nomenclature (ICZN). International Code of ZoologicalNomenclature 4th edn, i–xxix, 1–306 (The International Trust for Zoological Nomenclature;1999). urn:lsid:zoobank.org:pub:F4BF9295-FF83-434C-9A29-74FDB7A64A9E.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105043920865,

title = {Built to last: Long-term stability of steep deglaciated slopes of alpine karst plateaus (Northern Calcareous Alps, Austria)},

author = { J. Szczygieł and M. Dąbrowski and O. Fernández and J.C. Hellstrom and B. Grasemann},

url = {https://doi.org/10.1016/j.enggeo.2026.108924},

doi = {10.1016/j.enggeo.2026.108924},

issn = {00137952},

year  = {2026},

date = {2026-01-01},

journal = {Engineering Geology},

volume = {372},

publisher = {Elsevier B.V.},

abstract = {Steep limestone plateaus of the Northern Calcareous Alps rise abruptly above deeply incised valleys, yet despite their sharp relief, they rarely experience large-scale slope failures. To understand why these massifs remain remarkably stable, we investigated five alpine karst plateaus: Göll, Untersberg, Hagengebirge, Tennengebirge, and Totes Gebirge, using a combination of speleothem geochronology, structural mapping, limit equilibrium analysis and elastic stress modelling. Cave archives reveal a long-lived history of episodic gravitational deformation spanning the last 550 ka. Individual slip events remained small (<40 cm) and did not evolve into continuous rupture surfaces, even though the region experienced repeated glaciations and intermittent tectonic reactivation along the Königssee–Lammertal–Traunsee and Lammertal fault systems. Both stress modelling and structural data show that near-surface deformation is governed mostly by gravitational loading and steep topography, whereas far-field tectonic stresses prevail in the deeper parts of the massifs, with the greatest disturbances in the ridges and edge of the plateaus. Limit equilibrium analyses further demonstrate that the thick-bedded, high-cohesion Dachstein limestones remain stable under dry static conditions, with slip reactivation requiring transient triggers such as seismic loading. Together, these results highlight the stabilizing role of cohesive limestone, the limited persistence of discontinuities, and efficient karst drainage. Even under strong climatic and tectonic perturbations, deep-seated slope deformation in these massifs remained limited in magnitude. This provides new insight into the mechanical resilience of Alpine karst plateaus and constrains the long-term behaviour of carbonate slopes subjected to combined geodynamic and climatic forcing.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

@article{2-s2.0-105044404431,

title = {Reply to Segit's Discussion of “Middle Jurassic black shale deposits from the Pieniny Klippen Belt, Western Carpathians: Insights into organic matter composition, thermal maturity, depositional, and palaeoenvironmental variations},

author = { M. Zielińska and J. Kus and J.G.M. Filho and E. Szram and M. Blumenberg and M.J. Fabiańska},

url = {https://doi.org/10.1016/j.coal.2026.105070},

doi = {10.1016/j.coal.2026.105070},

issn = {01665162},

year  = {2026},

date = {2026-01-01},

journal = {International Journal of Coal Geology},

volume = {324},

publisher = {Elsevier B.V.},

abstract = {We respond to Segit's Discussion concerning lithological terminology, sampling strategy, stratigraphic interpretation, palaeo‑oxygenation, and the tectono-sedimentary context of Middle Jurassic organic-matter-bearing deposits of the Szlachtowa Formation in the Pieniny Klippen Belt. We clarify that our study deliberately examined lithologically variable, dark, organic-bearing siliciclastic deposits within a heterolithic turbiditic succession, and that the term “black shale deposits” was not intended as a strict classification of all analysed samples. The lithology of each sample was explicitly reported, and additional field documentation is provided to clarify the sedimentological context of the sampled material. We further emphasize that tectonic fragmentation and discontinuous exposure within the Pieniny Klippen Belt limit the possibility of geographically uniform sampling and broad basin-scale extrapolation. The assignment of sample 50SL from Vršatské Podhradie to the Szlachtowa Formation remains plausible, although the structurally complex setting of this locality requires caution and further independent verification. The dinoflagellate cyst assemblages support a broad Middle Jurassic affinity for the analysed material, with a well-supported Lower Bajocian component and evidence that some horizons may extend into the Bathonian. The proposed Toarcian–Aalenian affinity of selected samples is retained only as a tentative interpretation requiring further biostratigraphic confirmation. We also clarify that our palaeoenvironmental interpretation did not imply persistent basin-wide anoxia or a Toarcian Oceanic Anoxic Event-type euxinic system. Rather, the integrated organic-petrological, palynofacies, Rock-Eval, and biomarker dataset indicates a terrigenously influenced, heterolithic depositional system characterized predominantly by dysoxic to suboxic conditions, with local and potentially episodic shifts towards more reducing conditions. Overall, the discussion concerns the scope and wording of selected interpretations rather than the validity of the underlying analytical dataset.},

note = {0},

keywords = {},

pubstate = {published},

tppubtype = {article}

}