Urbanization alters habitat structure and resource availability, influencing wildlife distribution and behavior. In particular, invertebrates are affected by the differences in urban landscape that are caused by distinct socio-economic differences throughout urban areas. These changes in invertebrate abundance and diversity may affect bat populations that rely on these invertebrates as a food source. This study investigates how neighborhood income influences invertebrate diversity and bat foraging activity in Fort Worth, Texas, USA. We hypothesize that variations in landscape management and the income-driven use of pesticides can alter invertebrate diversity and subsequently bat activity. We conducted invertebrate sampling and acoustic bat monitoring across ten urban greenspaces; five high-income and five low-income neighborhoods in Tarrant County, TX, USA. We then quantified invertebrate and bat abundance and diversity using Shannon’s and Simpson’s diversity indices and examined correlations between invertebrate diversity, bat activity, and household income. This study will help to understand the ecological consequences of socio-economic disparities in urban habitats, which can inform conservation strategies to enhance urban biodiversity and bat conservation efforts.

Fort Worth, the fastest-growing city in Texas, contains many vacant land plots suitable for urban agriculture—an opportunity to address local food deserts. However, unsustainable farming can degrade soil organic carbon and reduce productivity. This study assessed soil carbon dynamics in a food waste compost–amended urban farm in Fort Worth. Experimental plots, including compost-amended and control treatments (triplicated), were established and monitored monthly from January 2023 to July 2024. Thermo-gravimetric Analysis (TGA) was used to calculate the recalcitrance index (R50), indicating carbon stability. Results showed compost-treated soils had more stable carbon and structured lignin degradation. In contrast, untreated soils exhibited unstructured decomposition and faster carbon loss. Compost enhances soil health and carbon cycling, and future research should explore combining compost with cover crops to maximize carbon sequestration and microbial activity in urban farming systems.

Leaking underground storage tanks (USTs) pose a significant environmental hazard in Norfolk, Virginia, where factors such as weather, casing materials, and varying ground conditions contribute to potential leaks over time. Corrosion, exacerbated by Norfolk's coastal location and harsh soil conditions, is a primary cause of these leaks. Geographic Information System (GIS) tools can be utilized to develop a predictive model for identifying at-risk UST locations by integrating data from multiple sources, including UST records from the state of Virginia and other relevant datasets. This model would employ various spatial analysis techniques to generate maps and web applications, enabling field teams to validate its accuracy and support the City of Norfolk in mitigating risks associated with leaking USTs. The goal of this research is to produce valuable insights that help safeguard the health of Norfolk's residents and protect the delicate surrounding ecosystem, including the Atlantic Ocean, marshes, rivers, and Chesapeake Bay.

The Tremp-Graus basin, located in Northern Spain, is a foreland piggyback basin that sits on the foot of Pyrenees Mountains. More specifically within the Montsec range, North of the Montsec thrust belt. The basin is a result of an east to west trending syncline area between the Boxial and Montsec Thrusts, North and South of Tremp, Spain, respectively. During the end of the Cretaceous period, syntectonic sedimentation began and carried throughout the Miocene. Thus, forming the basin that is structurally open in the west and open in the east, possibly due to structural events and quite possibly a shallow sea that protruded the area during the Ypresian (56 – 47.8 Ma). The sediments came from sources in the North, East, and the South in less quantities. The Pyrenees Mountains to the north are the main source of the sedimentation in the area as an influx of sediment occurred over time as the thrust sheets became proximal to the basin. The Boxial thrust supplied alluvial fans during the Maastrichtian in a localized setting (Arevalo, 2022; Busquests, 2022).
There is an overall transition from continental to deltaic sediments in the east to a western section that is mainly slope mudstones, thin-bedded turbidite wedges, proximal turbidites, channel-fills, distal turbidities and basin-plain deposits. This study will focus on a vertical section in the Coll del Montllobar Cliffs to help identify and differentiate channel characteristics as the rocks shift from continental/terrestrial deposits to marine influence deposits (tracking transgressive-regressive cycles) within the Upper Ager Group through the Lower Montanyana Group. The study will include at least five highly detailed measured sections, fluvial mapping conducted through drone footage and 3D modeling as well as possible point counting root density within the sections. In the conclusion of this study researchers will have a reliable Type Section as well as a basic understanding of how transgressive – regressive cycles alter channel behavior within the region, as well as the defining characteristics of the fluvial channels.

The Wichita Mountains in southwestern Oklahoma hold over a billion years of geological history, offering valuable insights into rift dynamics, magmatism, and basin evolution. These mountains are remnants of the Southern Oklahoma Aulacogen, a failed rift that initially formed during the Cambrian period through crustal extension but was later uplifted due to tectonic inversion. The region features a diverse range of igneous and sedimentary rocks, including the Carlton Rhyolites, gabbroic anorthosites, and granites of the Wichita Granite Group, which reflect a complex magmatic history. Over time, major tectonic events such as the Pennsylvanian uplift during the formation of Pangea and subsequent Permian burial played a key role in shaping the area's present landscape. This study utilizes Geographic Information Systems (GIS) tools to examine the spatial relationships, structural features, and lithological distribution of the Wichita Mountains. Using remote sensing, digital elevation models (DEMs), and geospatial analysis, this research provides a deeper understanding of the regions geological history and demonstrates the effectiveness of GIS technology in structural geology and regional mapping.