Estimating Sediment and Nutrient Loads in Four Western Lake Superior Streams

2014 ◽  
Vol 50 (5) ◽  
pp. 1138-1154 ◽  
Author(s):  
Elaine M. Ruzycki ◽  
Richard P. Axler ◽  
George E. Host ◽  
Jerald R. Henneck ◽  
Norman R. Will
2014 ◽  
Vol 40 (2) ◽  
pp. 455-462 ◽  
Author(s):  
Elizabeth C. Minor ◽  
Brandy Forsman ◽  
Stephanie J. Guildford

2005 ◽  
Vol 62 (6) ◽  
pp. 1254-1270 ◽  
Author(s):  
John C Brazner ◽  
Danny K Tanner ◽  
Naomi E Detenbeck ◽  
Sharon L Batterman ◽  
Stacey L Stark ◽  
...  

The relative importance of regional, watershed, and in-stream environmental factors on fish assemblage structure and function was investigated in western Lake Superior tributaries. We selected 48 second- and third-order watersheds from two hydrogeomorphic regions to examine fish assemblage response to differences in forest fragmentation, watershed storage, and a number of other watershed, riparian, and in-stream habitat conditions. Although a variety of regional, fragmentation, and storage-related factors had significant influences on the fish assemblages, water temperature appeared to be the single most important environmental factor. We found lower water temperatures and trout–sculpin assemblages at lower fragmentation sites and higher temperatures and minnow–sucker–darter assemblages as storage increased. Factors related to riparian shading and flow separated brook trout streams from brown trout (Salmo trutta) – rainbow trout (Oncorhynchus mykiss) streams. Functionally, fish assemblages at lower fragmentation sites were dominated by cold-water fishes that had low silt tolerance and preferred moderate current speeds, while fishes with higher silt tolerances, warmer temperature preferences, and weaker sustained swimming capabilities were most common at higher storage sites. Our results suggest that site-specific environmental conditions are highly dependent on regional- and watershed-scale characters and that a combination of these factors operates in concert to influence the structure and function of stream fish assemblages.


2003 ◽  
Vol 29 (1) ◽  
pp. 41-53 ◽  
Author(s):  
Matt F. Simcik ◽  
Jeff D. Jeremiason ◽  
Elizabeth Lipiatou ◽  
Steven J. Eisenreich

2011 ◽  
Vol 140 (6) ◽  
pp. 1504-1520 ◽  
Author(s):  
Tyler D. Ahrenstorff ◽  
Thomas R. Hrabik ◽  
Jason D. Stockwell ◽  
Daniel L. Yule ◽  
Greg G. Sass

1981 ◽  
Vol 103 (4) ◽  
pp. 262-264
Author(s):  
W. C. Huang ◽  
D. L. Nelson

The world’s first full-scale fluidized bed reactor co-disposal facility located at the Western Lake Superior Sanitary District’s (WLSSD) central waste-water treatment complex in Duluth, Minnesota, began its shakedown operation in the fall of 1979. The authors present herein basic design criteria, a system description, November 1979 system status, and areas of operational concern.


2005 ◽  
Vol 309 (1-4) ◽  
pp. 258-276 ◽  
Author(s):  
N.E. Detenbeck ◽  
V.J. Brady ◽  
D.L. Taylor ◽  
V.M. Snarski ◽  
S.L. Batterman

1994 ◽  
Vol 72 (1) ◽  
pp. 78-86
Author(s):  
S. A. Stephenson ◽  
W. T. Momot

Ichthyofaunal surveys of the Huron Mountains and Isle Royale, Michigan, and the Sibley Peninsula, Ontario, allow for both a comparative study of colonization events and the effects of sequential isostatic rebound within a large portion of the western Lake Superior basin. The distribution of some fish species in these areas is the result of catastrophic events related to glacial retreat. The highest Huron Mountain lakes were colonized during channel events occurring shortly after the Marquette readvance began its retreat. Some species present on the Sibley Peninsula were likely carried by overflows from Lake Agassiz. Most lakes within these areas, however, were colonized well after 9700 BP, when large numbers of species had gained entrance to Lake Superior, mainly from Mississippi basin refugia. Several species, presumably because of earlier warming periods, had a wider distribution than they exhibit today. Some colonization of Isle Royale was probably through the straying of a few individuals from these populations. Lake Superior remains a formidable barrier to many species, restricting them to favourable areas within the western basin.


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