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Research about Wind River basin

Source-linked reports with geographic coverage including Wind River basin.

7 recordsLinked to original sources

Chronic wasting disease reduces mule deer survival and hunter success in the Wind River Basin of Wyoming

Chronic wasting disease (CWD) is a fatal prion disease of cervids that has spread across much of North America and has recently become a global concern. Although CWD typically emerges gradually in new geographic regions, some areas experience rapid increases in prevalence for reasons that remain unclear. Herein, we describe the establishment of CWD in a mule deer (Odocoileus hemionus) population in the eastern portion of the Wind River Basin, WY, USA, where CWD prevalence in adult males (n=249) increased from 0% to 63% within a decade. We provide historical context, including a description of regional anthropogenic changes, and examine the epizootic’s impact on deer survival and hunting. From 2023 to 2025, we captured and monitored 96 adult mule deer. Annual survival was low: 0.38 for adult males (n=21) and 0.53 for adult females (n=75). Before CWD detection in 2012, mean hunter success was 72% (2000 to 2011). After detection, hunter success declined to 30% in 2022. We propose three hypotheses to explain the rapid rise in CWD prevalence, including food hotspots created by agriculture, increased agricultural dependency due to habitat degradation, and declining migratory behavior. Our case study highlights the potential effects of CWD and provides insights into possible drivers of transmission, to support more targeted management.

Wyoming↗

Geochemistry of the Cretaceous Mowry Shale in the Wind River Basin, Wyoming

The siliceous nature of the Mowry Shale distinguishes it from many of the well-studied organic-rich mudstones of the Cretaceous Western Interior Seaway. Available models of organic enrichment in mudstones rarely incorporate detailed biomarker, bulk organic, inorganic, and mineralogy data. Here, we used these data to evaluate how variations in organic matter source, productivity, dilution, and preservation modulated organic matter accumulation during the deposition of the Mowry Shale, while also demonstrating the benefits of this integrated approach. An organic stable carbon isotope vertical profile for the Mowry Shale is presented to test whether the Mowry Shale was deposited during oceanic anoxic event 1d (OAE 1d), thereby contributing to organic enrichment in the Mowry Shale.

Wyoming↗