Punctuated equilibria argue for intervals of long-term net stasis and comparatively abrupt change in the morphology of individual species lineages resulting from the process of allopatric speciation as recorded in the stratigraphic and fossil record. The concept of coordinated stasis extends punctuated equilibria to posit that not only individual species, but groups of coexisting lineages within a basin, display concurrent morphological and ecological stability over the same extended intervals of geologic time (105 to 106 yr). These blocks of stability termed ecological–evolutionary subunits (EESUs) are separated by shorter-lived (on the order of 103 to 104 yr) episodes of change characterized by varying combinations of speciation, extinction, immigration, and emigration. The result is a pattern of evolutionary and ecological stasis and change that is coincident and highly punctuational.

Here, we assess the connections among environment, evolution, and ecology by documenting patterns of stability, geographic extent, and synchronous turnover during medium-scale bioevents in the Middle Devonian of the eastern United States, and we briefly compare these with patterns of EESUs across the Late Ordovician mass extinction (LOME) based on ongoing work. We quantify the geographic extent and stability of faunas originally documented in the Appalachian Basin and identify their likely places of origin and refugia during turnovers. Faunas are geographically widespread during times of stability and border comparably stable faunas in adjacent provinces. During geologically brief intervals, assemblages display near-synchronous shifts involving local extirpation/extinction and coordinated migration of biogeographic boundaries over very long distances. Allopatric speciation in small, locally isolated populations along the edges of basins during brief windows of dramatically altered environmental conditions is more consistent with the geological record, emphasizes the role of environment and biogeography in driving evolutionary change, and confirms the prevalence of punctuated equilibria.

Volcanic monitoring in Antarctica provides dual benefits by facilitating the study of highly volcanically active yet underexplored regions and by serving as an essential tool for maintaining the safety of both national and international Antarctic bases. Deception Island, one of the most volcanically active areas on the Antarctic continent, is now equipped with an enhanced monitoring system, modernized by the Spanish National Geographic Institute (IGN), which assumed its management in September 2020, pursuant to a protocol established between the Spanish Ministry of Transport, Mobility, and Urban Agenda and Ministry of Science and Innovation. In order to meet the challenging conditions of the polar region, six permanent stainless-steel shelters have been installed over the course of the last four Spanish Antarctic campaigns. Each shelter is outfitted with batteries, solar panels, Wi-Fi and data acquisition systems for seismic and Global Navigation Satellite System (GNSS) stations. This monitoring network also comprises a station dedicated to measuring temperature within a thermal located where there is the anomaly on the island, a visual surveillance camera, seven seismic stations and six GNSS stations. All data collected are transmitted in real time to IGN headquarters in Madrid through Gabriel de Castilla Base, operated by the Spanish Army. Due to the growing volume of recorded data, it became necessary to upgrade transmission systems, leading to the installation of a next-generation satellite telemetry system during the 2023–2024 campaign. All seismic information is continuously and immediately analysed by the IGN’s National Seismic Network and is stored at the National Polar Data Center, housed within the Marine Technical Unit of the Spanish National Research Council, in accordance with the guidelines of the Spanish Polar Committee. The establishment of this infrastructure on Deception Island delivers a robust operational model that can be replicated in other polar settings, thereby contributing to the advancement of volcanic monitoring across the continent.

The current state of Arctic research and its community continues to exhibit high levels of political polarization and fragmentation by establishing a number of questions regarding the societal relevance of the process and its results for the benefit of present and future generations. The ASSW2025 (Arctic Science Summit Week) conference devoted to the ICARP IV (International Conference on Arctic Research Planning) process took place in Boulder, Colorado (March 2025), and had special importance in this regard. The conference was a summary meeting of the Arctic research planning process for the next 10 years and set the foundation for the upcoming IPY-5 (International Polar Year). The Summit, attended by nearly 1200 international scientists and researchers, Indigenous Knowledge holders, and community members from across the Arctic and beyond, exhibited the lowest ever attendance of Russian Arctic scientists representing Russian science organizations. This group studies and advocates for almost half of the Arctic’s social and human capital (roughly 2.4 million people live in Arctic Russia). In order to preserve scientific discourse and guarantee the societal and environmental benefits of science for the fragile socio-ecological systems of polar regions and their delicate geopolitics, effective transition strategies and approaches should be taken into consideration where possible.

Numerous fish microremains, including diverse chondrichthyans, have been recovered for the first time in the Carboniferous–lower Permian of the Naqing, Narao, and Shanglong deep-water sections from Guizhou Province, South China, as well as in the Serpukhovian–lower Bashkirian of the Sholaksay section from Kazakhstan. The richest assemblage was found in the Bashkirian strata of the three South China sections. These findings are the first reliable record of Pennsylvanian fishes in China. The fish assemblage from the Sholaksay section and the Bashkirian of China closely resemble those from the same interval in the Aksu section, Uzbekistan. All studied fish faunas from these three Asian regions are associated with the Paleotethys. Notably, while Bashkirian chondrichthyan faunas generally exhibit low taxonomical diversity in many regions of the world, the deep-water fish assemblages from South China, Kazakhstan, and Uzbekistan are characterized by high taxonomical diversity. The fish fauna includes widely distributed chondrichthyan taxa; however, Gissarodus occurs only in these three Asian regions.

Good air quality is a critical determinant of public health, influencing life expectancy, respiratory health, work productivity, and the prevention of chronic diseases. This study presents a novel approach to classifying the Air Quality Index (AQI) using deep learning techniques, specifically convolutional neural networks (CNNs). We collected and curated a dataset comprising 11,000 digital images from three distinct regions in Indonesia—Jakarta, Malang, and Semarang—ensuring uniformity through standardized acquisition settings. The images were categorized into four air quality classes: good, moderate, unhealthy for sensitive groups, and unhealthy. We designed and implemented a CNN architecture optimized for AQI classification. The model achieved an impressive accuracy of 99.81% using K-fold cross-validation. In addition, the model’s interpretative capabilities were examined using techniques such as Grad-CAM, providing valuable insights into how the CNN identifies and classifies air quality conditions based on image features. These findings underscore the effectiveness of CNNs for AQI classification and highlight the potential for future work to incorporate a more diverse set of digital images captured from various perspectives to enhance dataset complexity and model robustness. The dataset is publicly accessible at https://doi.org/10.5281/zenodo.15727522.

Despite the lesser preservation of bat fossils compared to karstic sites, fluviolacustrine deposits are of crucial importance for assessing the local palaeodiversity of bats. This was confirmed by three faunas from the upper Miocene of Slovakia (Borský Svätý Jur, MN9; Studienka A, MN9; Krásno, MN11), which comprise seven species—Miostrellus cf. Miostrellus noctuloides (Lartet, 1851), Myotis cf. Myotis murinoides (Lartet, 1851), ‘Otonycteris’ sp. indet., Miniopterus sp. indet., Vespertilionidae gen. indet. sp. indet. 1, Vespertilionidae gen. indet. sp. indet. 2, and Rhinolophus cf. Rhinolophus grivensis Depéret, 1892. Bats represent ~ 1.40% of the small mammal remains from Borský Svätý Jur, ~ 0.25% of those from Studienka A, and ~ 1.78% of those from Krásno. The MN11 fauna from Krásno consists of six distinct species, which is unusual for a Miocene fluviolacustrine deposit. Most likely, this is the consequence of the relatively high frequency of bats in the taphocoenosis, therefore providing a more complete and more accurate picture of the Carpathian late Miocene bat faunas. This material encourages the study of fluviolacustrine deposits to unravel the cryptic diversity of Neogene taxa.