Mercury Isotopes Reveal an Ontogenetic Shift in Habitat Use by Walleye in Lower Green Bay of Lake Michigan

2018 ◽  
Vol 6 (1) ◽  
pp. 8-13 ◽  
Author(s):  
Charles P. Madenjian ◽  
Sarah E. Janssen ◽  
Ryan F. Lepak ◽  
Jacob M. Ogorek ◽  
Tylor J. Rosera ◽  
...  
1993 ◽  
Vol 27 (1) ◽  
pp. 75-87 ◽  
Author(s):  
Diane R. Achman ◽  
Keri C. Hornbuckle ◽  
Steven J. Eisenreich

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

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.


Author(s):  
Amelia T McReynolds ◽  
Megan L. Hoff ◽  
Angelena A. Sikora ◽  
Cynthia I. Nau ◽  
Michael J. Pietraszek ◽  
...  

Small tributaries of the Great Lakes serve as important habitat during critical life stages of many fish species, though temporal and spatial dynamics of the assemblage that uses these systems are seldom investigated. This study quantifies larval and adult fish assemblages captured by fyke net and light traps among small tributary mouths of Green Bay, Lake Michigan. Ten tributaries harbored a total of forty-five species representing seventeen families, with the most abundant including spottail shiner (Notropis hudsonius (Clinton 1824)) in adult assemblages and white sucker (Catostomus commersonii (Lacepède 1803)) in larval assemblages. Larval fish assemblage structures differed over five biweekly sampling events in May and June. Adult fish assemblage structures varied among tributaries but not among spring, summer, and fall samples. Larval and adult species assemblages at these rivermouths are likely influenced by hydrology, habitat structure, and species-specific ecology. Water movement may transport larvae into rivermouths, as larval assemblages were dominated by species that spawn in coastal habitats. Adult species richness varied with longitude, with the greatest diversity in tributaries on the west shore. This investigation of fish assemblages highlights the spatial and temporal variation that occurs in these systems and their role in shaping fish populations in Green Bay.


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