Larval lake whitefish distribution in the open waters of Green Bay, Lake Michigan

Author(s):  
Andrew L. Ransom ◽  
Christopher J. Houghton ◽  
S. Dale Hanson ◽  
Scott P. Hansen ◽  
Marian Shaffer ◽  
...  
Author(s):  
Andrew L. Ransom ◽  
Christopher J. Houghton ◽  
S. Dale Hanson ◽  
Scott P. Hansen ◽  
Lydia R. Doerr ◽  
...  

1982 ◽  
Vol 39 (5) ◽  
pp. 700-709 ◽  
Author(s):  
A. L. Jensen ◽  
S. A. Spigarelli ◽  
M. M. Thommes

We applied a bioenergetic model to describe uptake of polychlorinated biphenyls (PCBs) by lake trout (Salvelinus namaycush), brown trout (Salmo trutta), lake whitefish (Coregonus clupeaformis), coho salmon (Oncorhynchus kisutch), and chinook salmon (Oncorhynchus tshawytscha) in Lake Michigan; lake trout and lake whitefish in Green Bay of Lake Michigan; and lake trout in Cayuga Lake, New York. The model describes PCB uptake in terms of metabolism, food consumption, size, and growth. Concentrations of PCBs differ significantly among species; for the same species there are large differences among habitats. The pattern of PCB uptake by brown trout is different from that of the other species. Application of the model with uptake and metabolic parameters estimated by Norstrom et al. describes the trend in the brown trout data; to describe uptake for other species we increased the exponent of weight for metabolism γ. An increase in γ changes the shape of the relation between PCB concentration and body weight from asymptotic to non-asymptotic. In all species tested except brown trout, uptake of PCBs was not asymptotic and concentrations did not approach an equilibrium; accumulation of contaminants was first rapid, decreased toward a plateau, and then began a second rapid increase. Simulation studies indicate that differences in PCB concentrations among species and in the same species among different environments result from differences in metabolic parameters, exposure, size, and rate of growth.Key words: PCBs, bioenergetic model, contaminant uptake, toxicology, fish, Great Lakes, salmon, trout, whitefish


1993 ◽  
Vol 27 (1) ◽  
pp. 75-87 ◽  
Author(s):  
Diane R. Achman ◽  
Keri C. Hornbuckle ◽  
Steven J. Eisenreich

Chemosphere ◽  
1993 ◽  
Vol 26 (11) ◽  
pp. 2079-2084 ◽  
Author(s):  
D.E. Tillitt ◽  
T.J. Kubiak ◽  
G.T. Ankley ◽  
J.P. Giesy

2018 ◽  
Vol 44 (5) ◽  
pp. 851-863 ◽  
Author(s):  
Brice K. Grunert ◽  
Shelby L. Brunner ◽  
Sajad A. Hamidi ◽  
Hector R. Bravo ◽  
J. Val Klump

1999 ◽  
Vol 45 (150) ◽  
pp. 201-213 ◽  
Author(s):  
E.M. Shoemaker

AbstractThe effect of subglacial lakes upon ice-sheet topography and the velocity patterns of subglacial water-sheet floods is investigated. A subglacial lake in the combined Michigan–Green Bay basin, Great Lakes, North America, leads to: (1) an ice-sheet lobe in the lee of Lake Michigan; (2) a change in orientations of flood velocities across the site of a supraglacial trough aligned closely with Green Bay, in agreement with drumlin orientations; (3) low water velocities in the lee of Lake Michigan where drumlins are absent; and (4) drumlinization occurring in regions of predicted high water velocities. The extraordinary divergence of drumlin orientations near Lake Ontario is explained by the presence of subglacial lakes in the Ontario and Erie basins, along with ice-sheet displacements of up to 30 km in eastern Lake Ontario. The megagrooves on the islands in western Lake Erie are likely to be the product of the late stage of a water-sheet flood when outflow from eastern Lake Ontario was dammed by displaced ice and instead flowed westward along the Erie basin. The Finger Lakes of northern New York state, northeastern U.S.A., occur in a region of likely ice-sheet grounding where water sheets became channelized. Green Bay and Grand Traverse Bay are probably the products of erosion along paths of strongly convergent water-sheet flow.


2018 ◽  
Vol 6 (1) ◽  
pp. 8-13 ◽  
Author(s):  
Charles P. Madenjian ◽  
Sarah E. Janssen ◽  
Ryan F. Lepak ◽  
Jacob M. Ogorek ◽  
Tylor J. Rosera ◽  
...  

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