Natural History Museum Vienna

Wild bees (Hymenoptera: Anthophila) and hoverflies (Diptera: Syrphidae), the two major groups of insect pollinators, are undergoing alarming declines worldwide, including Europe. The lack of accessible and verified spatial and temporal occurrence records currently challenges efforts to understand and mitigate this decline. Here, we compiled datasets from diverse sources, including taxonomists, national experts, public repositories, museum collections, published literature, verified open-access platforms, and aggregated datasets from previous European projects. The collected data were standardised, cleaned and validated by taxonomists and national experts. This collective effort resulted in two databases comprising more than 4.34 million and 1.04 million records for wild bees and hoverflies, respectively. The databases cover 97% of the European bee fauna (2,083 species out of 2,138 recorded in Europe) and 97% of the European hoverfly fauna (886 species out of 913 recorded in Europe). These standardised databases constitute essential resources for future assessments of status and trends, habitat associations, and other research and conservation initiatives to protect and understand wild pollinators on the European continent.

In the Dinarides, a series of long-lived lakes, known as the Dinarides Lake System (DLS) developed during the Miocene. The Sinj Basin, situated in southern Croatia, is one of the best studied among them, providing valuable insights into the paleogeographic evolution of the region. Previous research established a chronostratigraphic framework in the NW part of the basin using paleomagnetic data calibrated by 40Ar/39Ar dating. Subsequent studies demonstrated that lacustrine flooding was diachronous. However, the influence of the Miocene Climatic Optimum (MCO) or the regional Miocene extensional tectonics is still debated. This study provides new constraints on the evolution of the Sinj Basin by integrating previous dating results with new LA–ICP–MS U–Pb–zircon dating of volcaniclastic and residual deposits from the NW, central, and SE parts of the basin. The obtained U-Pb ages range between 17.7 and 15.3 Ma and provide new constraints on the timing of initial lacustrine flooding. Correlation with the MCO suggests a close relationship between climate change and lacustrine development. Lake-level falls reflected by conglomerates and coals deposited in marginal and more distal parts of the basin, respectively, suggest environmental instability after 15.3 Ma, towards the end of the MCO. Detrital zircon grains reveal a wide spectrum of ages from the Neoproterozoic to the Early Miocene, suggesting multiple redeposition cycles, starting with the Cadomian and Variscan orogenies, followed by Cretaceous–Oligocene uplift of the Dinarides, and the recycling of foreland basin deposits into the Miocene Sinj Basin. Finally, this study demonstrates the usefulness of LA–ICP–MS U–Pb dating for the reconstruction and correlation of isolated intramontane basins.

A bright fireball was seen at 4:46 a.m. CET on November 19, 2020, over Austria, and also eye witnessed in Italy and Germany. The resulting Kindberg meteorite was the fifth well‐approved meteorite fall in Austria, and all rocks represent ordinary chondrites. One specimen of Kindberg, measuring 233.08 g, was recovered on July 4, 2021, largely covered by a dark brownish fusion crust. The meteorite is an L6 ordinary chondrite (OC) breccia; Kindberg's highly equilibrated type 6 character is also supported by the large‐sized plagioclase grains (An 9‐12 ; with grains >100 μm) and the homogeneous compositions of olivine (Fa 24.4±0.4 ) and low‐Ca pyroxene (Fs 20.6±0.3 ). The meteorite shows remarkable shock effects in the form of easily visible dark shock veins cross‐cutting the bulk rock. The olivine in Kindberg is dominated by grains with undulous extinction or planar fractures, indicating a weakly shocked (S3 [C‐S3]) chondritic rock. Close to the shock veins, olivine can also show mosaicism. In addition, wadsleyite, a high‐pressure polymorph of olivine, was identified by Raman and IR spectroscopy. Wadsleyite, sometimes in paragenesis with maskelynite and locally part of an intergrowth with majorite and perhaps ringwoodite, was found within and close to the veins. The occurrence of high‐pressure phases of olivine and maskelynite in a weakly shocked bulk rock clearly indicates their formation at relatively low equilibrium shock pressures of <20 GPa (S3/S4 transition). Equilibrium shock pressures consistent with those experienced by bulk rocks shocked to S5 (>30–35 GPa) and S6 (>45 GPa; S5/S6 transition) are not required to form high‐pressure polymorphs of olivine. The L‐chondrite classification is confirmed by O isotope data. The bulk chemical composition also supports L‐group membership.

The insect threat to heritage objects can increase with climate change, increased travel, movement of goods and loan exhibitions. This study used catch from 30 heritage environments across Austria. Overall arthropod catch rate in storerooms was lower than in museums and libraries. Taxonomic richness of the ecosystem in the buildings was a product of building size, perhaps paralleling island biogeography. Heritage pests are distributed independently and follow environmental gradients, perhaps aligning with Henry Gleason’s continuum theory of ecological communities. Catch rates for some abundant pests are evenly distributed among buildings (e.g., Psocoptera booklice, Lepisma saccharinum common silverfish), but Tineola bisselliella, the webbing clothes moth, is unevenly distributed because some locations have large infestations. Rare species are unevenly distributed, as these are found in only a few buildings. A characteristic set of insect pests appear to dominate indoor heritage environments in Austria: Psocoptera, Lepismatidae silverfish, Tineola bisselliella webbing clothes moth and carpet beetles like Anthrenus spp. and Attagenus spp. These pests are also common in the interiors of heritage buildings in some other European countries.

Phoresy is an important dispersal strategy in pseudoscorpions, yet associations with Diptera have not been comprehensively revised for more than two decades. An updated synthesis of pseudoscorpion-Diptera phoresy is presented based on newly collected European material, a revision of previously studied Slovak material, a critical reassessment of worldwide published records, and available fossil evidence. In total, 11 previously unreported cases of pseudoscorpion phoresy from four European countries are documented, including the first records of Dactylochelifer degeerii (C.L. Koch, 1835) from France and of Pselaphochernes scorpioides (Hermann, 1804) from Slovenia. Seven dipteran species and three dipteran families are newly recorded worldwide as hosts of pseudoscorpion phoresy, and one case of multiple phoresy was recorded from Slovakia. Altogether, 172 records spanning the period from 1761 to 2025 were compiled and evaluated. Compared with previous syntheses, the number of known dipteran hosts was increased to 74 species from 30 families, and pseudoscorpion phoronts to 39 species from seven families. This study provides the most comprehensive overview of pseudoscorpion-Diptera phoresy to date and establishes a robust framework for future taxonomic, ecological, and evolutionary studies.