Let’s call it the Clinch Dace. It’s a small minnow, which the locals call “yeller finned minners.” When Freshwater Fishes of Virginia was first published in 1994, this minnow was not known, at least to scientists. It’s referred to as Chrosomus sp. cf. saylori. This means we are sure it is a member of the genus Chrosomus, the fine-scale daces. The sp. is an abbreviation for species, meaning we are not sure what the species really is. The cf. is an abbreviation for the Latin verb conferre. This tells one to consult with or compare with the species saylori, because it is most similar to the Laurel Dace Chrosomus saylori. The Laurel Dace was described by Dr. Christopher Skelton (2001) and was listed as endangered by the U.S. Fish and Wildlife Service in 2011. The Clinch Dace was encountered in surveys associated with gas pipeline planning and construction. The fish was considered a unique species due to differences in morphological and meristic traits (White and Orth 2013). Because it has not yet been described as a species it has no federal protection. In Virginia, it is a Tier I species (very high conservation need) in the Virginia Wildlife Action Plan.
|A, Laurel Dace Chrosomus saylori Photo by Chris Skelton, B. Clinch Dace Chrosomus sp. cf. saylori Photo by Dave Neely|
|Dashed line shows range of all collections of Clinch Dace.|
Coal mining, logging, gas wells, cattle pastures, roads and culverts occur throughout the highly dissected landscape where the Clinch Dace may be found. Here, the impacts of surface mining outweigh current mitigation actions, which have been largely criticized (Bernhardt et al. 2012). The surface mine impacts can have long-lasting and significant effects on aquatic life. For example, one isolated population of Clinch Dace exists upstream from a large surface mine in Left Fork Coal Creek (see photo). Here the conductivity is less than 200 μS/cm. However, downstream of the discharge from the surface mine, conductivity values increase to over 1,000 μS/cm. Different ionic constituents are part of the dissolved solids loading, though these are not regulated. Of further concern, is that the community of Fork Ridge, Virginia, is one of 50 communities at highest risk of mountaintop mining.
|Aerial photo of Fork Ridge surface mine and isolated Clinch Dace habitat. Photo by D.J. Orth|
The landscapes where the Clinch Dace reside provide a microcosm of what is occurring throughout the coal-mining region of Appalachia. Coal is removed by a method known as contour highwall mining or mountaintop removal and valleys are filled with mine spoil. Drainage from these surface mines and valley fills have high levels of dissolved solids, which remain elevated for long distances downstream and for 2 decades or more after the mine is “reclaimed” (Evans et al. 2014). Aquatic macroinvertebrate communities are impaired by high ionic concentrations; these same small creatures are part of the food base for many fishes, including the Clinch Dace. It is unlikely that eggs and larvae can survive the elevated ionic concentrations. Others have also detected a conductivity threshold for stream fishes. A threshold of conductivity likely exists, above which Clinch Dace and other fishes cannot persist. With the small, and isolated pattern of the Clinch Dace populations, any further losses in habitat are troublesome. At present, four of the largest populations in the least disturbed watersheds are the hope for the future of the species.
We still need to quantify the levels of genetic diversity remaining in these small populations. Habitats that are important for Clinch Dace spawning need to be identified and protected. With cooperative landowners we need to identify and remove barriers to population expansion and monitor responses. These yeller finned minners belong in the small streams that drain these hollers. There are no alternative habitats once a valley is filled in.
|Landscape in the region occupied by Clinch Dace. Photo by D.J. Orth.|
Bernhardt, E.S., et al. 2012. How many mountains can we mine? Assessing the regional degradation of central Appalachian rivers by surface coal mining. Environmental Science and Technology 46(15):8115-8122.
Evans, D.M., C.E. Zipper, P.F. Donovan, and W.L. Daniels. 2014. Long-term trends of specific conductance in waters discharged by coal-mine valley fills in central Appalachia, USA. Journal of the American Water Resources Association 50(6):1449-1460.
Skelton, C.E. 2001. New dace of the genus Phoxinus (Cyprinidae: Cypriniformes) from the Tennessee River drainage, Tennessee. Copeia 2001:118-128.
White, S.L, and D.J. Orth. 2013. Ontogenetic and comparative morphology of Clinch Dace (Chrosomus sp. cf. saylori). Copeia 2013(4):750-756.