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The Determination of Minimum Flows for Sulphur Springs, Tampa

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DRAFT<br />

species (10 to 13) were collected during periods <strong>of</strong> no flow and normal flow; while low<br />

numbers <strong>of</strong> species (5 to 7) were also collected during periods <strong>of</strong> no flow and normal<br />

flow.<br />

<strong>The</strong> presence <strong>of</strong> fishes in <strong>Sulphur</strong> <strong>Springs</strong> may be related to flow and water quality<br />

conditions in the Lower Hillsborough River, but such relationships are only speculative.<br />

During periods <strong>of</strong> no flow from the dam, salinity in the spring run is generally<br />

considerably lower than in the river. This may attract some species to the spring run, but<br />

factors such as the temperature, clarity and dissolved oxygen in the spring run might be<br />

equally as important. Conversely, it could be argued that during high flows, suitable<br />

habitat becomes more available in the lower river, thus not concentrating fish in the<br />

spring run.<br />

It can be concluded that the spring run provides a valuable low salinity refuge <strong>for</strong><br />

freshwater species during periods <strong>of</strong> no flow from the Hillsborough River dam.<br />

Freshwater species, such as largemouth bass and bluegill, are <strong>of</strong>ten collected in the low<br />

salinity areas <strong>of</strong> tidal creeks and rivers where they can feed on the food resources found<br />

there. A review <strong>of</strong> the effects <strong>of</strong> salinity on freshwater fishes in the coastal plain <strong>of</strong> the<br />

southeastern U.S. is provided by Peterson and Meador (1994). Elevated salinity can<br />

influence fish behavior, physiology, growth, or reproduction. However, the salinity<br />

values that are generally reported <strong>for</strong> these effects are well above the background<br />

salinity that occurs in <strong>Sulphur</strong> <strong>Springs</strong> under normal flows, and even during some<br />

periods <strong>of</strong> salinity incursion from the river. Acknowledging that salinity tolerances vary<br />

considerably between fish families, Peterson and Meador state that many freshwater<br />

species can withstand extended exposures up to 9 ppt salinity, and tolerate brief<br />

exposures at higher values. <strong>The</strong>y furthermore state that some studies suggest that most<br />

freshwater fishes cannot reproduce in salinities greater than 3-4 ppt, but few studies<br />

have addressed this issue.<br />

It is unlikely that salinity incursions in the spring run observed during this study<br />

jeopardized the survivability <strong>of</strong> the estuarine/marine fish that inhabit the spring run.<br />

However, the prolonged high salinity values (8-16 ppt) that resulted from the large<br />

withdrawals from <strong>Sulphur</strong> <strong>Springs</strong> during the 2000-2001 drought likely caused the<br />

spring run to be unsuitable habitat <strong>for</strong> most freshwater fishes found in the Lower<br />

Hillsborough River. However, salinity incursions <strong>of</strong> lesser magnitude or duration, such<br />

as occurred during the fall <strong>of</strong> 2001 and spring 2002 (Figure 3-5), may not have<br />

jeopardized the survivability <strong>of</strong> these species or possibly their reproduction.<br />

<strong>The</strong> use <strong>of</strong> the spring run by fishes will be dependent not only on salinity, but also on<br />

food resources available in the run. Given the findings <strong>for</strong> invertebrates presented in<br />

Section 3.7, the species composition <strong>of</strong> the invertebrate community is likely more<br />

sensitive to changes in salinity in the low range than the fish fauna. It is unclear,<br />

however, if such a community shift in the invertebrates would result in less total prey <strong>for</strong><br />

fishes. <strong>The</strong> potential biological effects <strong>of</strong> salinity incursions into the spring run resulting<br />

from different flow rates from the spring are considered in Chapter 5.<br />

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