Role of Olfaction and Vision in the Behavior of American Shad (Alosa sapidissima) Homing to the Connecticut River from Long Island Sound

1974 ◽  
Vol 31 (10) ◽  
pp. 1607-1619 ◽  
Author(s):  
Julian J. Dodson ◽  
William C. Leggett

Twenty-two adult American shad (Alosa sapidissima), captured, sensory-impaired, sonic-tagged, and released adjacent to and 10 km west of the Connecticut River, were tracked in Long Island Sound in 1972. Both anosmic and blind/anosmic shad oriented into the tidal current and altered swimming speeds in relation to changes in tidal current velocity as do unimpaired fish. They did not, however, exhibit the consistency in these behavioral responses that resulted in westerly displacement in unimpaired shad. Blind shad exhibited neither of these behavior patterns but did tend to affect a westerly displacement in Long Island Sound.Dart-tagged adult shad that were sensory-impaired and released without displacement in the same areas of Long Island Sound in 1971 and 1972 homed less successfully to the Connecticut River than did unimpaired dart-tagged shad released in the same years. Anosmic dart-tagged shad located the Connecticut River less successfully than unimpaired shad. Blind shad successfully located the river from 10 km distance but failed to do so when released adjacent to the river. Blind/anosmic shad failed to locate the river from either release site.It was concluded that an olfactory–rheotaxic mechanism forms the basis of the location of the Connecticut River by shad. The preferred direction of displacement appears to be established by olfactory clues indicative of the Connecticut River whereas the orientation along the migratory path is maintained by reference to the rate and direction of tidal currents. Vision alone cannot account for this rheotaxic response.

1973 ◽  
Vol 30 (12) ◽  
pp. 1847-1860 ◽  
Author(s):  
Julian J. Dodson ◽  
William C. Leggett

The migratory behavior of American shad (Alosa sapidissima) approaching their natal river during the final saltwater stage of the spawning migration was studied using ultrasonic tracking and conventional tagging procedures. Initial displacement of most sonic-tagged shad released without displacement adjacent to and 10 km west of the Connecticut River was not in the direction of the home river. These fish, however, homed successfully to the Connecticut River as did dart-tagged shad released in the same areas.Shad exhibited two major behavior patterns; countercurrent orientation in response to the reversing tidal current and adjustment of swimming speed to changes in tidal velocity. Countercurrent orientation was equally significant during daylight and darkness, whereas the adjustment of swimming speeds to tidal current velocity was more significant during daylight than darkness.Shad tracked to the west exhibited a westerly bias inherent in the basic open water behavior patterns. Shad exhibited a greater degree of directed movement when oriented against the ebb tide and adjusted their swimming speeds to exceed the ebb tide velocity and to approximately equal the flood tide velocity. Shad tracked to the east exhibited the same major behavior patterns but with the opposite directional bias.A hypothesis is presented suggesting that the location of the home river is achieved by means of a nonrandom search. Environmental clues indicative of the Connecticut River act to establish a preferred direction of displacement while the actual unidirectional displacement is achieved by reference to the rate and direction of tidal currents.


2013 ◽  
Author(s):  
Lawrence J. Poppe ◽  
Katherine Y. McMullen ◽  
Seth D. Ackerman ◽  
Megan R. Guberski ◽  
Douglas A. Wood

<em>Abstract</em>.—Atlantic sturgeon <em>Acipenser oxyrinchus</em> are consistent visitors to specific areas of Long Island Sound and the lower portions of Connecticut rivers despite the fact that natal stocks have been extirpated. Atlantic sturgeon have been collected annually in the Connecticut River from 1988 through 2004. Similarly, annual utilization of selected areas in Long Island Sound points to the importance of these areas, probably as foraging sites. By means of pumped gastric lavage, 41 Atlantic sturgeon collected in Long Island Sound in October 2001 were examined to determine the prey items consumed. Ninety-three percent of the fish examined showed evidence of recent feeding. Among the fish that had fed, polychaetes (<em>Pherusa</em>, <em>Glycinde</em>, and <em>Clymenella </em>spp.) comprised 52% of stomach contents on average and all fish had consumed worms (range, 1 to 177). Polychaetes accounted for 2-100% of stomach contents by number and 63% of the diet by weight. Decapods (<em>Squilla</em>, <em>Gilvossius</em>, and <em>Upogebia</em> spp.) were also a prominent prey item, having been eaten by 63% of the fish that had fed. The number of these three mud shrimps eaten ranged from 0 to 49 (mean, 11/fish) and comprised up to 75% of the diet by number and up to 97% by weight (mean, 41%). Other prey included amphipods and pea crabs <em>Pinnixia</em> spp. Eleven subadult Atlantic sturgeon (<2 m total length) collected in the Connecticut River from 2000 to 2002 were also lavaged for stomach contents. Food was obtained from 73% of the fish examined; stomach contents were dominated by polychaetes <em>Scolecolepides</em> spp.


2016 ◽  
Vol 46 (8) ◽  
pp. 2351-2371 ◽  
Author(s):  
Michael M. Whitney ◽  
David S. Ullman ◽  
Daniel L. Codiga

AbstractLong Island Sound (LIS) is a large and wide macrotidal estuary with distributed river inputs, including the Connecticut River (the largest freshwater source) that flows into the eastern LIS near the mouth. In 2010, shipboard surveys of salinity, temperature, and currents were collected along an across-estuary transect in eastern LIS. Numerical model results are compared to these observations and used to study the spatial and temporal variability of salinity, velocity, and freshwater and salt fluxes over a 4-yr period. For all low wind conditions, observations and model results indicate an outward-flowing, low-salinity wedge on the south side with an inward-flowing, higher-salinity area underneath and to the north. Observations and model results during the low wind surveys indicate that stratification substantially decreases with increased tidal amplitude and decreased river discharge; the velocity field is less variable among surveys. Model analysis indicates strong sensitivities to both tides and river discharge; with discharge response strongest for salinity and freshwater flux and tidal response larger for velocities, volume flux, and salt flux. The long-term average net freshwater and salt fluxes are outward and inward, respectively. For both flux types, subtidal shear dispersion is twice tidal oscillatory diffusion, and both contributions are in the same direction as the net flux. The uniform flow contribution is small for freshwater flux, yet it is the largest single term for salt flux and partially counters the inward contributions.


2004 ◽  
Vol 90 (1-4) ◽  
pp. 53-74 ◽  
Author(s):  
Prentiss H. Balcom ◽  
William F. Fitzgerald ◽  
Grace M. Vandal ◽  
Carl H. Lamborg ◽  
Kristofer R. Rolfhus ◽  
...  

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