@article{hall_limnological_1999,
	title = {Limnological succession in reservoirs: a paleolimnological comparison of two methods of reservoir formation},
	volume = {56},
	issn = {0706-652X},
	shorttitle = {Limnological succession in reservoirs},
	url = {http://www.nrcresearchpress.com/doi/abs/10.1139/f99-047},
	doi = {10.1139/f99-047},
	abstract = {Analysis of diatoms, algal pigments, and chironomids in sediment cores from two otherwise similar prairie reservoirs demonstrated that differences in reservoir formation (river valley impoundment versus lake inundation) and hydrological regime (variable versus stable water level) resulted in distinct patterns of aquatic community change. Lake Diefenbaker, a 500-km2 reservoir created by damming the South Saskatchewan River in 1968, experiences water level fluctuations of 6 m·year-1. In contrast, impoundment of Buffalo Pound Lake in 1952 flooded a natural lake, raised mean water levels {\textasciitilde}2.0 m, and reduced water level fluctuations from {\textasciitilde}3 to {\textless}1 m·year-1. Comparison of fossil records showed that reservoir formation did not inevitably lead to eutrophication. Lake Diefenbaker exhibited typical reservoir ontogeny with three trophic periods, including an initial {\textasciitilde}4-year period of eutrophy, a decade of mesotrophy, and a gradual shift to modern productive conditions. Planktonic taxa dominated diatom communities at ..., L'analyse des diatomées, des pigments algaux et des chironomides dans des carottes de sédiments de deux réservoirs de prairie semblables par ailleurs montre que les différences dans la formation des réservoirs (endiguement de rivière dans une vallée ou inondation d'un lac) et le régime hydrologique (niveau de l'eau variable ou stable) ont donné des profils distincts de changement dans les communautés aquatiques. Au lac Diefenbaker, un réservoir de 500 km2 créé par l'endiguement de la rivière Saskatchewan Sud en 1968, on observe des fluctuations du niveau de l'eau de 6 m·an-1. Par contre, l'endiguement du lac Buffalo Pound en 1952 a agrandi ce lac naturel et élevé le niveau moyen de l'eau d'environ 2,0 m tout en réduisant les fluctuations du niveau d'environ 3 m·an-1 à moins de 1 m·an-1. La comparaison des registres fossiles a montré que la formation d'un réservoir ne conduit pas nécessairement à une eutrophisation. On a observé au lac Diefenbaker une ontogénie typique de réservoir avec trois périodes trop...},
	number = {6},
	urldate = {2018-06-08},
	journal = {Canadian Journal of Fisheries and Aquatic Sciences},
	author = {Hall, Roland I and Leavitt, Peter R and Dixit, Aruna S and Quinlan, Roberto and Smol, John P},
	month = jun,
	year = {1999},
	note = {00067},
	keywords = {\#nosource},
	pages = {1109--1121},
}

{"_id":"taJFrmbZM6R9JrJnk","bibbaseid":"hall-leavitt-dixit-quinlan-smol-limnologicalsuccessioninreservoirsapaleolimnologicalcomparisonoftwomethodsofreservoirformation-1999","author_short":["Hall, R. I","Leavitt, P. R","Dixit, A. S","Quinlan, R.","Smol, J. P"],"bibdata":{"bibtype":"article","type":"article","title":"Limnological succession in reservoirs: a paleolimnological comparison of two methods of reservoir formation","volume":"56","issn":"0706-652X","shorttitle":"Limnological succession in reservoirs","url":"http://www.nrcresearchpress.com/doi/abs/10.1139/f99-047","doi":"10.1139/f99-047","abstract":"Analysis of diatoms, algal pigments, and chironomids in sediment cores from two otherwise similar prairie reservoirs demonstrated that differences in reservoir formation (river valley impoundment versus lake inundation) and hydrological regime (variable versus stable water level) resulted in distinct patterns of aquatic community change. Lake Diefenbaker, a 500-km2 reservoir created by damming the South Saskatchewan River in 1968, experiences water level fluctuations of 6 m·year-1. In contrast, impoundment of Buffalo Pound Lake in 1952 flooded a natural lake, raised mean water levels ~2.0 m, and reduced water level fluctuations from ~3 to \\textless1 m·year-1. Comparison of fossil records showed that reservoir formation did not inevitably lead to eutrophication. Lake Diefenbaker exhibited typical reservoir ontogeny with three trophic periods, including an initial ~4-year period of eutrophy, a decade of mesotrophy, and a gradual shift to modern productive conditions. Planktonic taxa dominated diatom communities at ..., L'analyse des diatomées, des pigments algaux et des chironomides dans des carottes de sédiments de deux réservoirs de prairie semblables par ailleurs montre que les différences dans la formation des réservoirs (endiguement de rivière dans une vallée ou inondation d'un lac) et le régime hydrologique (niveau de l'eau variable ou stable) ont donné des profils distincts de changement dans les communautés aquatiques. Au lac Diefenbaker, un réservoir de 500 km2 créé par l'endiguement de la rivière Saskatchewan Sud en 1968, on observe des fluctuations du niveau de l'eau de 6 m·an-1. Par contre, l'endiguement du lac Buffalo Pound en 1952 a agrandi ce lac naturel et élevé le niveau moyen de l'eau d'environ 2,0 m tout en réduisant les fluctuations du niveau d'environ 3 m·an-1 à moins de 1 m·an-1. La comparaison des registres fossiles a montré que la formation d'un réservoir ne conduit pas nécessairement à une eutrophisation. On a observé au lac Diefenbaker une ontogénie typique de réservoir avec trois périodes trop...","number":"6","urldate":"2018-06-08","journal":"Canadian Journal of Fisheries and Aquatic Sciences","author":[{"propositions":[],"lastnames":["Hall"],"firstnames":["Roland","I"],"suffixes":[]},{"propositions":[],"lastnames":["Leavitt"],"firstnames":["Peter","R"],"suffixes":[]},{"propositions":[],"lastnames":["Dixit"],"firstnames":["Aruna","S"],"suffixes":[]},{"propositions":[],"lastnames":["Quinlan"],"firstnames":["Roberto"],"suffixes":[]},{"propositions":[],"lastnames":["Smol"],"firstnames":["John","P"],"suffixes":[]}],"month":"June","year":"1999","note":"00067","keywords":"#nosource","pages":"1109–1121","bibtex":"@article{hall_limnological_1999,\n\ttitle = {Limnological succession in reservoirs: a paleolimnological comparison of two methods of reservoir formation},\n\tvolume = {56},\n\tissn = {0706-652X},\n\tshorttitle = {Limnological succession in reservoirs},\n\turl = {http://www.nrcresearchpress.com/doi/abs/10.1139/f99-047},\n\tdoi = {10.1139/f99-047},\n\tabstract = {Analysis of diatoms, algal pigments, and chironomids in sediment cores from two otherwise similar prairie reservoirs demonstrated that differences in reservoir formation (river valley impoundment versus lake inundation) and hydrological regime (variable versus stable water level) resulted in distinct patterns of aquatic community change. Lake Diefenbaker, a 500-km2 reservoir created by damming the South Saskatchewan River in 1968, experiences water level fluctuations of 6 m·year-1. In contrast, impoundment of Buffalo Pound Lake in 1952 flooded a natural lake, raised mean water levels {\\textasciitilde}2.0 m, and reduced water level fluctuations from {\\textasciitilde}3 to {\\textless}1 m·year-1. Comparison of fossil records showed that reservoir formation did not inevitably lead to eutrophication. Lake Diefenbaker exhibited typical reservoir ontogeny with three trophic periods, including an initial {\\textasciitilde}4-year period of eutrophy, a decade of mesotrophy, and a gradual shift to modern productive conditions. Planktonic taxa dominated diatom communities at ..., L'analyse des diatomées, des pigments algaux et des chironomides dans des carottes de sédiments de deux réservoirs de prairie semblables par ailleurs montre que les différences dans la formation des réservoirs (endiguement de rivière dans une vallée ou inondation d'un lac) et le régime hydrologique (niveau de l'eau variable ou stable) ont donné des profils distincts de changement dans les communautés aquatiques. Au lac Diefenbaker, un réservoir de 500 km2 créé par l'endiguement de la rivière Saskatchewan Sud en 1968, on observe des fluctuations du niveau de l'eau de 6 m·an-1. Par contre, l'endiguement du lac Buffalo Pound en 1952 a agrandi ce lac naturel et élevé le niveau moyen de l'eau d'environ 2,0 m tout en réduisant les fluctuations du niveau d'environ 3 m·an-1 à moins de 1 m·an-1. La comparaison des registres fossiles a montré que la formation d'un réservoir ne conduit pas nécessairement à une eutrophisation. On a observé au lac Diefenbaker une ontogénie typique de réservoir avec trois périodes trop...},\n\tnumber = {6},\n\turldate = {2018-06-08},\n\tjournal = {Canadian Journal of Fisheries and Aquatic Sciences},\n\tauthor = {Hall, Roland I and Leavitt, Peter R and Dixit, Aruna S and Quinlan, Roberto and Smol, John P},\n\tmonth = jun,\n\tyear = {1999},\n\tnote = {00067},\n\tkeywords = {\\#nosource},\n\tpages = {1109--1121},\n}\n\n\n\n","author_short":["Hall, R. I","Leavitt, P. R","Dixit, A. S","Quinlan, R.","Smol, J. 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