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Research about Virginia, Tennessee

Source-linked reports with geographic coverage including Virginia, Tennessee.

2 recordsLinked to original sources

Mass mortality in freshwater mussels (Actinonaias pectorosa) in the Clinch River, USA, linked to a novel densovirus

Freshwater mussels (order Unionida) are among the world’s most biodiverse but imperiled taxa. Recent unionid mass mortality events around the world threaten ecosystem services such as water filtration, nutrient cycling, habitat stabilization, and food web enhancement, but causes have remained elusive. To examine potential infectious causes of these declines, we studied mussels in Clinch River, Virginia and Tennessee, USA, where the endemic and once-predominant pheasantshell ( Actinonaias pectorosa ) has suffered precipitous declines since approximately 2016. Using metagenomics, we identified 17 novel viruses in Clinch River pheasantshells. However, only one virus, a novel densovirus ( Parvoviridae ; Densovirinae ), was epidemiologically linked to morbidity. Clinch densovirus 1 was 11.2 times more likely to be found in cases (moribund mussels) than controls (apparently healthy mussels from the same or matched sites), and cases had 2.7 (log 10 ) times higher viral loads than controls. Densoviruses cause lethal epidemic disease in invertebrates, including shrimp, cockroaches, crickets, moths, crayfish, and sea stars. Viral infection warrants consideration as a factor in unionid mass mortality events either as a direct cause, an indirect consequence of physiological compromise, or a factor interacting with other biological and ecological stressors to precipitate mortality.

Virginia, Tennessee

A lower paleozoic paleoaquifer; the Kingsport Formation and Mascot dolomite of Tennessee and southwest Virginia

The Kingsport Formation (Lower Ordovician) in one section may be composed of two dominant rock types--limestone and medium to coarsely crystalline dolomite--whereas in an adjacent section, most of the formation may be largely composed of breccia. The breccia bodies, which are interpreted to be solution-collapse features, range in width from 30 feet to several hundred feet, in thickness from a few feet to more than 200 feet, and are hundreds of feet long. Many of the complexities of the Kingsport can be directly related to the development of an unconformity at the top of the overlying Mascot Dolomite. Erosion associated with the unconformity produced a widespread karst topography with an attendant paleoaquifer system. Ground water, apparently reacting to differences in solubility between limestone of the Kingsport and dense dolomite of the Mascot, is thought to be a major contributing factor in regional dolomitization and localization of solution-thinning and collapse features at the contact of the Kingsport and Mascot. Later mineralizing solutions invaded the paleoaquifer, locally depositing commercial quantities of zinc ore.

Virginia, Tennessee