Climate Change in the Champlain Basin - The Nature Conservancy

Climate Change in the Champlain BasinThese fish apparently remain offshore for most of the year butenter shallow waters in late spring and early summer to spawn.If they do not have a long warm season in which to gain weight,alewives do not survive cold winters, which sometimes leads tomassive seasonal die-offs in the Great Lakes (Lepak and Kraft,Channel darter (Percina copelandi)2008). In winter they become stressed at temperatures colderthan 37°F (2.8°C), and they generally try to avoid habitats at orbelow 34°F (1°C) [O’Gorman, 2006]. If cold is a major limitingfactor for alewife populations, then warmer winters might lead totheir expansion in Lake Champlain, to the detriment of other fish.Slimy sculpin (Cottus cognatus)A small, cold-water, bottom-dwelling fish in tributaries as wellas in the lake itself, slimy sculpins are widely distributed throughoutCanada and the northern United States. They spawn in spring attemperatures of 4.5–15.5°C (40–60°F) and frequently occur withbrook trout in streams (Smith, 1985). They feed mostly on insectlarvae and nymphs but also on crustaceans, small fish and plantmaterials.Channel darters are rare in tributaries of the Champlain Basinand are listed as endangered in Vermont, the northeastern extremeof their range (Vermont Department of Fish and Wildlife[a],2005; Smith, 1985).Channel darters live and spawn in swift currents along thegravelly bottoms of the lower Winooski, LaPlatte and PoultneyRivers. There are also historical reports of channel darters inthe Great Chazy River, but none have been found there recently(Fisheries Technical Committee, 2009), perhaps becauseagricultural runoff has caused turbidity in the Chazy. These fishavoid silty or muddy substrates (Vermont Department of Fish andWildlife[a], 2005). If erosion continues to degrade tributary habitats,especially if heavy rainfall and winter runoff pulses becomemore frequent, channel darters could be vulnerable. Sand darters(Ammocrypta pellucida), which live further downstream, mightbe more affected by mud and silt deposition because they inhabitslower currents.On the other hand, if siltation is held in check, future warmingmight increase the viability of Champlain Basin channel darters,though it remains to be seen whether this isolated populationcould tolerate higher temperatures after having adapted to arelatively cool northern watershed (D. Facey, personal communication).It is as yet unknown how future warming will affect thedarters’ local food sources—mainly caddisfly, midge and mayflylarvae—and whether potentially reduced stream flows in summermight affect spawning (Smith, 1985).Slimy sculpins and close relatives mottled sculpins (C. bairdi)face aggressive competition in the Great Lakes region as roundgobies (Neogobius melanostomus) expand their range. Gobieshave food, habitat and spawning requirements similar to thoseof sculpins and appear to be replacing them where the speciesoverlap (Janssen and Jude, 2001; Chotkowski and Marsden,1999). Round gobies have been moving eastward from Lake Erievia the Erie Canal, and they are better able to feed and spawn invery warm or murky water than slimy sculpins. As a result, warmingand potentially increased runoff in the Champlain Basin could helpgobies to outcompete native sculpins if they find their way into thewatershed.Fish images in this section provided by the New York StateDepartment of Environmental Conservation. All rights reserved.30