Feeding Ecology of Juvenile Lake Sturgeon in the St. Lawrence River System

2006 ◽  
Vol 135 (4) ◽  
pp. 1044-1055 ◽  
Author(s):  
Pedro Nilo ◽  
Serge Tremblay ◽  
Aline Bolon ◽  
Julian Dodson ◽  
Pierre Dumont ◽  
...  
Keyword(s):  
Feeding Ecology ◽  
River System ◽  
Lake Sturgeon ◽  
St Lawrence River

Comparison of lake sturgeon (Acipenser fulvescens), Stizostedion spp., Catostomus spp., Moxostoma spp., quillback (Carpiodes cyprinus), and mooneye (Hiodon tergisus) larval drift in Des Prairies River, Quebec

2001 ◽  
Vol 79 (8) ◽  
pp. 1472-1489 ◽  
Author(s):  
Julie D'Amours ◽  
Stéphanie Thibodeau ◽  
Réjean Fortin
Keyword(s):  
River System ◽  
Lake Sturgeon ◽  
Acipenser Fulvescens ◽  
Larval Drift ◽  
Power House ◽  
Spawning Areas ◽  
Vertical Variations ◽  
Reverse Situation ◽  
The Right ◽  
St Lawrence River

Several fish species that spawn in lotic habitats have a larval-drift phase which is a major determinant of their reproductive success. The main objective of this study was to compare seasonal, diel, longitudinal, transverse, and vertical variations in rates of lake sturgeon (Acipenser fulvescens), Stizostedion spp., Catostomus spp., Moxostoma spp., quillback (Carpiodes cyprinus), and mooneye (Hiodon tergisus) larval drift in Des Prairies River (DPR) near Montreal (Quebec), which is one of the major lotic spawning habitats of the St. Lawrence River system. Larval sampling was conducted in the spring of 1994 and 1995 for the six taxa, and on a more restricted basis for lake sturgeon in 1996–1998, using drift nets set at several transects, stations, depths, and periods of the day, along a 19 km long section of river beginning ca. 2 km downstream from the DPR power house. For all taxa except lake sturgeon, peak larval drift occurred ca. 1 week earlier in 1995 than in 1994. The sequence was very similar between years, beginning with Stizostedion spp., followed by Catostomus spp., then lake sturgeon, quillback, and mooneye drifting simultaneously, and finally Moxostoma spp. Generally, for all taxa except quillback, whose multimodal drift pattern suggests intermittent, prolonged spawning, larval-drift profiles showed one major seasonal mode, which was observed simultaneously at all transects. For all taxa except quillback, drift rates peaked between 21:00 and 03:00 and were minimal during daylight hours. Lake sturgeon and Stizostedion spp. larval drift rates decreased radically from the most upstream to the most downstream transect, suggesting that both taxa spawn mostly in the vicinity of the DPR power house. More studies are required to explain this longitudinal decline in drift rates, particularly for lake sturgeon. The other taxa showed longitudinal variation in larval drift rates, suggesting that they spawn near the DPR power house and (or) in the Île de Pierre Rapids, ca. 12 km downstream. At all transects, larval drift rates for the six taxa were generally higher in the right half (Montreal) of the river, suggesting that eggs are deposited mostly in this part of the river at the two major spawning areas and that larvae tend to remain in the same general corridors during downstream migration. For all taxa, though to a lesser extent for lake sturgeon, nocturnal drift rates tend to be higher near the surface than at mid-depth and near the bottom, the reverse situation being observed for diurnal drift rates.

Movements and biological statistics of lake sturgeon (Acipenser fulvescens) populations from the St. Lawrence and Ottawa River system, Quebec

1993 ◽  
Vol 71 (3) ◽  
pp. 638-650 ◽  
Author(s):  
Réjean Fortin ◽  
Jean-René Mongeau ◽  
Gilles Desjardins ◽  
Pierre Dumont
Keyword(s):  
Total Mortality ◽  
River System ◽  
Lake Sturgeon ◽  
Acipenser Fulvescens ◽  
Commercial Fishing ◽  
Commercial Catch ◽  
Saint Louis ◽  
Ottawa River ◽  
Biological Statistics ◽  
St Lawrence River

Our objective was to compare movements and biological statistics of lake sturgeon (Acipenser fulvescens) populations from two fluvial lakes on the St. Lawrence River, Lac Saint-Louis and Lac Saint-Pierre, which are main commercial fishing sectors, and from Lac des Deux Montagnes on the Ottawa River. Sturgeon can move freely among these three lakes. Lac des Deux Montagnes sturgeon differ from the other groups by their higher degree of sedentariness, slower growth, and lower condition factor. Lac Saint-Louis and Lac Saint-Pierre sturgeon are also sedentary, but some movement between the two lakes was observed. Sturgeon tagged on the Rivière des Prairies and Rivière L'Assomption spawning grounds, located in the central part of the study area, and also on pre- and post-spawning concentration sites, were recaptured throughout the St. Lawrence River, from Lac Saint-Louis to Lac Saint-Pierre. Length, weight, and age composition of the commercial catch, growth, and total mortality varied between Lac Saint-Louis and Lac Saint-Pierre. Higher commercial exploitation rates in the latter could be responsible for some differences. The management implications of these results are discussed.

Loadings of Selected Chemicals into the St. Lawrence River System from Lake Ontario, 1986/87

1989 ◽  
Vol 24 (4) ◽  
pp. 589-608 ◽  
Author(s):  
I.K. Tsanis ◽  
J. Biberhofer ◽  
C.R. Murthy ◽  
A. Sylvestre
Keyword(s):  
Mass Balance ◽  
Lake Ontario ◽  
River System ◽  
Vertical Gradient ◽  
The South ◽  
Measured Concentration ◽  
Chemical Monitoring ◽  
The North ◽  
Loading Estimates ◽  
St Lawrence River

Abstract Determination of the mass output through the St. Lawrence River outflow system is an important component in computing mass balance of chemical loadings to Lake Ontario. The total flow rate in the St. Lawrence River System at the Wolfe Island area was calculated from detailed time series current meter measurements from a network of current meters and Lagrangian drifter experiments. This flow is roughly distributed in the ratio of 55% to 45% in the South and North channel, respectively. Loading estimates of selected chemicals have been made by combining the above transport calculations with the ongoing chemical monitoring data at the St. Lawrence outflow. A vertical gradient in the concentration of some organic and inorganic chemicals was observed. The measured concentration for some of the chemicals was higher during the summer months and also is higher in the South Channel than in the North Channel of the St. Lawrence River. These loading estimates are useful not only for modelling the mass balance of chemicals in Lake Ontario but also for serving as input loadings to the St. Lawrence River system from Lake Ontario.

Lake sturgeon spawning on artificial habitat in the St Lawrence River

2006 ◽  
Vol 22 (6) ◽  
pp. 465-470 ◽  
Author(s):  
J. H. Johnson ◽  
S. R. LaPan ◽  
R. M. Klindt ◽  
A. Schiavone
Keyword(s):  
Lake Sturgeon ◽  
Artificial Habitat ◽  
St Lawrence River

Efficacy of Iodine for Disinfection of Lake Sturgeon Eggs from the St. Lawrence River, New York

2014 ◽  
Vol 77 (1) ◽  
pp. 82-89 ◽  
Author(s):  
Marc Chalupnicki ◽  
Dawn Dittman ◽  
Clifford E. Starliper ◽  
Deborah D. Iwanowicz
Keyword(s):  
New York ◽  
Lake Sturgeon ◽  
St Lawrence River

Reference intervals for select hematologic and plasma biochemical analytes of wild Lake Sturgeon (Acipenser fulvescens) from the St. Lawrence River in New York

2012 ◽  
Vol 42 (1) ◽  
pp. 19-26 ◽  
Author(s):  
Louis DiVincenti ◽  
Jeff Wyatt ◽  
Heather Priest ◽  
Dawn Dittman ◽  
Rodger Klindt ◽  
...  
Keyword(s):  
New York ◽  
Reference Intervals ◽  
Lake Sturgeon ◽  
Acipenser Fulvescens ◽  
St Lawrence River

Oil Spill Simulation in Rivers

1991 ◽  
Vol 1991 (1) ◽  
pp. 593-600
Author(s):  
Poojitha D. Yapa ◽  
Hung Tao Shen ◽  
Steven F. Daly ◽  
Stephen C. Hung
Keyword(s):  
Great Lakes ◽  
Oil Spill ◽  
Vertical Mixing ◽  
River System ◽  
Open Water ◽  
Ohio River ◽  
Oil Slick ◽  
Oil Spill Response ◽  
Dimensional Surface ◽  
St Lawrence River

ABSTRACT Computer models recently have been developed for simulating oil slick transport in rivers, including the connecting channels of the Great Lakes, the upper St. Lawrence River, and the Allegheny-Monongahela-Ohio River system. In these models, a Lagrangian discrete-parcel algorithm is used to determine the location and concentration distribution of the oil in the river as well as the deposition of oil on the shore. The model for the Great Lakes connecting channels (ROSS) is a two-dimensional surface slick model which considers advection, spreading, horizontal diffusion, evaporation, dissolution, and shoreline deposition. The model is applicable to both open water and ice covered conditions. Models for the St. Lawrence River and the Ohio River System are developed based on a two-layer scheme (ROSS2) which considers vertical mixing and emulsiflcation processes in addition to the processes considered in the surface slick model. All of these models are implemented on microcomputers and can be used as integral parts of oil spill response programs to assist cleanup actions.

Under-ice observations of behavior of selected native and exotic fishes of the St. Lawrence river system

Zoo Biology ◽  
1994 ◽  
Vol 13 (6) ◽  
pp. 545-555 ◽  
Author(s):  
F. G. Whoriskey ◽  
K. Brown
Keyword(s):  
River System ◽  
Exotic Fishes ◽  
St Lawrence River
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