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Sulphur Springs:
Chemical Barriers to Fish Movement
Several
cold water sulphur springs flow into tributaries of the
Welland River on the Niagara Peninsula. Sulphur spring
water temperature is approximately 9 şC throughout the
year and it contains little or no dissolved oxygen. The
water contains high levels of dissolved hydrogen sulphide
(> 11 ppm) and it is lethal to fish. Since 2004 we have
conducted a series of experiments designed to illustrate
the biological ramifications of the sulphur springs on
fish and other organisms. At the Buckhorn Creek sulphur
spring, there is a “dead zone” with very little dissolved
oxygen, high conductivity >3500 µS/cm, and redox
potentials < -200 eV, that extends over 500 m downstream
from the spring outlet. In an electro-fishing survey
conducted in 2006, fish were present upstream and
downstream from the “dead zone”, suggesting that fish
passage may be possible during periods of elevated
discharge; however, during low flow situations, this
spring would be a barrier to fish movement and it reduces
the amount of available aquatic habitat in Buckhorn
Creek. The Buckhorn Creek spring supports a diverse
assemblage of chemotrophic algae and bacteria that may be
regionally unique, ecologically significant and worth
preserving. The spring also contributes to base-flow in
the creek during the summer months.
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