Surficial geologic map of the upper Bear River and Bear Lake drainage basins, Idaho, Utah, and Wyoming

Author(s):  
Marith C. Reheis
1975 ◽  
Vol 32 (11) ◽  
pp. 1989-2004 ◽  
Author(s):  
Lionel Johnson

Benthic invertebrates in Great Bear Lake are most highly concentrated in the upper 20 m. Densities between 20 and 100 m are low; below 100 m only Mysis relicta and Myoxocephalus quadricornis exist at measurable densities. All benthic organisms exhibit a high degree of patchiness.Lake trout, Salvelinus namaycush, and M. quadricornis are two species that inhabit the lake at all depths (3–400 m) and temperatures (13.2 C for M. quadricornis and 15 C for S. namaycush).Whitefish, Coregonus clupeaformis, inhabit only the bays, seldom being caught in water over 20 m deep. The distribution of whitefish is considered to be restricted mainly by the density of benthic organisms.Three species are confined to the periphery of the lake, Stizostedion vitreum, Lota lota, and Catostomus catostomus. Two species, Couesius plumbeus and Percopsis omiscomaycus, are present in the headwaters and Great Bear River but have not been able to establish themselves in Great Bear Lake. Extreme oligotrophy is considered to have had the effect of reducing species diversity.


2014 ◽  
Vol 1 (2) ◽  
pp. 64-77
Author(s):  
Dávid Murányi ◽  
Tibor Kovács ◽  
Kirill Márk Orci

The stoneflies Leuctra graeca Zwick, 1978, Zwicknia acuta Murányi & Orci, 2014 and Isoperla pesici Murányi, 2011 are reported for the first time from the (FY) Republic of Macedonia. An apparently new species of Zwicknia Murányi, 2014 is referred but not named. The hitherto unknown larva of Rhabdiopteryx doiranensis Ikonomov, 1983 is described from both sexes. Further stonefly occurrences are also enumerated from the Anska Reka and Dojran Lake drainage basins, including the first early spring records of the autumnal Leuctra bronislawi Sowa, 1970 and L. graeca.


2007 ◽  
Vol 52 (3) ◽  
pp. 1094-1111 ◽  
Author(s):  
Walter E. Dean ◽  
Richard M. Forester ◽  
Jordon Bright ◽  
Roger Y. Anderson

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