Academic literature on the topic 'Black lake'

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Journal articles on the topic "Black lake"

1

Moreira, Amanda L., and Eric B. Taylor. "The origin and genetic divergence of “black” kokanee, a novel reproductive ecotype of Oncorhynchus nerka." Canadian Journal of Fisheries and Aquatic Sciences 72, no. 10 (2015): 1584–95. http://dx.doi.org/10.1139/cjfas-2015-0145.

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Kokanee and sockeye salmon are the freshwater-resident and anadromous forms, respectively, of Oncorhynchus nerka. Unique populations of “black” kokanee are found in Lake Saiko, Japan, and in Anderson and Seton lakes in the southwestern interior of British Columbia. They are distinct from other populations of O. nerka in that black kokanee display black nuptial colouration and they spawn between 20 to 70 m below the surface of lakes in the winter or early spring. Analysis of mitochondrial DNA and nine microsatellite loci supported the hypothesis that black kokanee in Lake Saiko and in Anderson
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2

Becker, Arnfried, Brigitta Ammann, Flavio S. Anselmetti, et al. "Paleoenvironmental studies on Lake Bergsee, Black Forest, Germany." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 240, no. 3 (2006): 405–45. http://dx.doi.org/10.1127/njgpa/240/2006/405.

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3

Adams, W. P., and D. C. Lasenby. "The Roles of Snow, Lake Ice and Lake Water in the Distribution of Major Ions in the Ice Cover of a Lake." Annals of Glaciology 7 (1985): 202–7. http://dx.doi.org/10.1017/s0260305500006170.

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The stratigraphic variability of ion concentration in lake ice was examined and related to the processes of lake-ice formation. Ice blocks obtained from Elizabeth Lake, Labrador and Knob Lake, Quebec showed marked vertical variation in the concentration of major ions, with peaks in conductivity occurring in the white ice and an overall increase in conductivity upwards from the black-ice/white-ice interface to the top of the block. Exsolution of ions from the black ice into the water body appears to be very efficient, producing low concentrations of ions in the black ice and high concentrations
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4

Adams, W. P., and D. C. Lasenby. "The Roles of Snow, Lake Ice and Lake Water in the Distribution of Major Ions in the Ice Cover of a Lake." Annals of Glaciology 7 (1985): 202–7. http://dx.doi.org/10.3189/s0260305500006170.

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The stratigraphic variability of ion concentration in lake ice was examined and related to the processes of lake-ice formation. Ice blocks obtained from Elizabeth Lake, Labrador and Knob Lake, Quebec showed marked vertical variation in the concentration of major ions, with peaks in conductivity occurring in the white ice and an overall increase in conductivity upwards from the black-ice/white-ice interface to the top of the block. Exsolution of ions from the black ice into the water body appears to be very efficient, producing low concentrations of ions in the black ice and high concentrations
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5

Filipic, Brankica, Katarina Novovic, David J. Studholme, et al. "Shotgun metagenomics reveals differences in antibiotic resistance genes among bacterial communities in Western Balkans glacial lakes sediments." Journal of Water and Health 18, no. 3 (2020): 383–97. http://dx.doi.org/10.2166/wh.2020.227.

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Abstract Long-term overuse of antibiotics has driven the propagation and spreading of antibiotic resistance genes (ARGs) such as efflux pumps in the environment, which can be transferred to clinically relevant pathogens. This study explored the abundance and diversity of ARGs and mobile genetic elements within bacterial communities from sediments of three Western Balkans glacial lakes: Plav Lake (high impact of human population), Black Lake (medium impact of human population) and Donje Bare Lake (remote lake, minimal impact of human population) via shotgun metagenomics. Assembled metagenomic s
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6

Cintra, Renato. "Ecological Gradients Influencing Waterbird Communities in Black Water Lakes in the Anavilhanas Archipelago, Central Amazonia." International Journal of Ecology 2012 (2012): 1–21. http://dx.doi.org/10.1155/2012/801683.

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For the first time, and in a large spatial scale, the influence of ecological properties on the aquatic bird community of black water lakes in Brazilian Amazonia is evaluated. Bird surveys were conducted in 45 lakes. A total of 3626 individuals in 48 bird species were recorded; of these, 31 are aquatic, and 18 of these are primarily piscivorous. Bird richness and abundance were not significantly related to lake shape and productivity but were influenced by hydrological period (low versus high), water depth, transparency, lake isolation, and habitat richness. Matrices of bird species by lake we
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7

Jacobson, Lawrence D., Wayne R. MacCallum, and George R. Spangler. "Biomass Dynamics of Lake Superior Lake Herring (Coregonus artedii): Application of Schnute's Difference Model." Canadian Journal of Fisheries and Aquatic Sciences 44, S2 (1987): s275—s288. http://dx.doi.org/10.1139/f87-329.

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Schnute's (1985. Can. J. Fish. Aquat. Sci. 42: 414–429) difference model was used to study the biomass dynamics of lake herring (Coregonus artedii) in Thunder Bay and Black Bay, Lake Superior, during 1948–79. Recruitment to both fisheries appeared to be independent of escapement during previous years. Abundance of lake herring in Black Bay varied without trend during the study period despite a strong peak in effective fishing effort during 1968–70 and a general trend of increasing effort throughout the study period. Abundance of Thunder Bay lake herring declined during 1948–50 and 1959–67 and
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8

Michalczyk, Zdzisław, Stanisław Chmiel, and Marek Turczyński. "Lake water stage dynamics in the Łęczna-Włodawa Lake District in 1991-2010." Limnological Review 11, no. 3 (2011): 113–22. http://dx.doi.org/10.2478/v10194-011-0033-1.

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Lake water stage dynamics in the Łęczna-Włodawa Lake District in 1991-2010In the years 1991-2010 the water stages of 38 lakes in the Łęczna-Włodawa Lake District were observed. Water stage dynamics of the Łęczna-Włodawa lakes was varied. A multi-annual trend with seasonal water stage variability was clearly observable. Low water stages were observed in the years 1994-1996 and 2004-2005, whereas the highest water stages were reported for 2002 and 2010. The water stages of Lake Piaseczno, the deepest lake, were consistent with solar activity changes. Land improvement works in the Łęczna-Włodawa
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9

Elliott, R. T. "Lake Nakuru Black Rhinoceros Sanctuary." Oryx 26, no. 3 (1992): 174–75. http://dx.doi.org/10.1017/s0030605300023656.

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10

Ansell, W. F. H. "Lake Nakuru Black Rhinoceros Sanctuary." Oryx 26, no. 4 (1992): 236. http://dx.doi.org/10.1017/s0030605300023784.

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