Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores.
19 páginas, 5 figuras, 2 tablas. The extraction of bitumen from the Athabasca oil sands is rapidly expanding, and emission of sulphur and nitrogen oxides has substantially increased. To determine whether lakes downwind of this development in northwest Saskatchewan have been detrimentally impacted si...
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Online Access: | http://hdl.handle.net/10261/88868 https://doi.org/10.1007/s10750-013-1623-5 |
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ftcsic:oai:digital.csic.es:10261/88868 2024-02-11T10:03:53+01:00 Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. Laird, K. Das, B. Kingsbury, M. Moos, Melissa T. Pla-Rabes, S. Ahad, J. E. Wiltse, B. Cumming, B. 2013-12 http://hdl.handle.net/10261/88868 https://doi.org/10.1007/s10750-013-1623-5 en eng Springer http://dx.doi.org/10.1007/s10750-013-1623-5 Hydrobiologia 720 : 1-19 (2013) 0018-8158 http://hdl.handle.net/10261/88868 doi:10.1007/s10750-013-1623-5 none Athabasca oil sands Saskatchewan Lake acidification Climate change Diatoms Chrysophyte scales Trace metals artículo http://purl.org/coar/resource_type/c_6501 2013 ftcsic https://doi.org/10.1007/s10750-013-1623-5 2024-01-16T09:55:08Z 19 páginas, 5 figuras, 2 tablas. The extraction of bitumen from the Athabasca oil sands is rapidly expanding, and emission of sulphur and nitrogen oxides has substantially increased. To determine whether lakes downwind of this development in northwest Saskatchewan have been detrimentally impacted since development of the oil sands, a paleolimnological assessment of ten lakes was carried out. Analysis of diatom valves and inferences of diatom-inferred pH indicated that emissions have not resulted in widespread chronic acidification of acidsensitive lakes *80–250 km east and northeast of the oil sands development around Fort McMurray and Fort Mackay. However, one of the closest sites to the development indicated a slight decline in diatominferred pH, but the two next closest sites, both ofwhich had higher alkalinity, did not show any evidence of acidification. There were also no consistent trends in the concentration or flux of total or individual priority pollutants including lead, mercury, copper, zinc and vanadium. The sedimentation rates in most lakes increased since the mid-1900s, along with increased flux of both diatoms and scaled chrysophytes. Subtle changes in the species assemblages of diatoms and increased flux of diatoms and chrysophyte scales are consistent with recent climate change in this region. This project was funded by the Saskatchewan Ministry of the Environment Peer reviewed Article in Journal/Newspaper Fort McMurray Digital.CSIC (Spanish National Research Council) Fort MacKay ENVELOPE(-111.619,-111.619,57.184,57.184) Fort McMurray Mackay ENVELOPE(168.517,168.517,-77.700,-77.700) Hydrobiologia 720 1 55 73 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Athabasca oil sands Saskatchewan Lake acidification Climate change Diatoms Chrysophyte scales Trace metals |
spellingShingle |
Athabasca oil sands Saskatchewan Lake acidification Climate change Diatoms Chrysophyte scales Trace metals Laird, K. Das, B. Kingsbury, M. Moos, Melissa T. Pla-Rabes, S. Ahad, J. E. Wiltse, B. Cumming, B. Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
topic_facet |
Athabasca oil sands Saskatchewan Lake acidification Climate change Diatoms Chrysophyte scales Trace metals |
description |
19 páginas, 5 figuras, 2 tablas. The extraction of bitumen from the Athabasca oil sands is rapidly expanding, and emission of sulphur and nitrogen oxides has substantially increased. To determine whether lakes downwind of this development in northwest Saskatchewan have been detrimentally impacted since development of the oil sands, a paleolimnological assessment of ten lakes was carried out. Analysis of diatom valves and inferences of diatom-inferred pH indicated that emissions have not resulted in widespread chronic acidification of acidsensitive lakes *80–250 km east and northeast of the oil sands development around Fort McMurray and Fort Mackay. However, one of the closest sites to the development indicated a slight decline in diatominferred pH, but the two next closest sites, both ofwhich had higher alkalinity, did not show any evidence of acidification. There were also no consistent trends in the concentration or flux of total or individual priority pollutants including lead, mercury, copper, zinc and vanadium. The sedimentation rates in most lakes increased since the mid-1900s, along with increased flux of both diatoms and scaled chrysophytes. Subtle changes in the species assemblages of diatoms and increased flux of diatoms and chrysophyte scales are consistent with recent climate change in this region. This project was funded by the Saskatchewan Ministry of the Environment Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Laird, K. Das, B. Kingsbury, M. Moos, Melissa T. Pla-Rabes, S. Ahad, J. E. Wiltse, B. Cumming, B. |
author_facet |
Laird, K. Das, B. Kingsbury, M. Moos, Melissa T. Pla-Rabes, S. Ahad, J. E. Wiltse, B. Cumming, B. |
author_sort |
Laird, K. |
title |
Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
title_short |
Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
title_full |
Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
title_fullStr |
Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
title_full_unstemmed |
Paleolimnological assessment of limnological change in 10 lakes from northwest Saskatchewan downwind of the Athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
title_sort |
paleolimnological assessment of limnological change in 10 lakes from northwest saskatchewan downwind of the athabasca oils sands based on analysis of siliceous algae and trace metals in sediment cores. |
publisher |
Springer |
publishDate |
2013 |
url |
http://hdl.handle.net/10261/88868 https://doi.org/10.1007/s10750-013-1623-5 |
long_lat |
ENVELOPE(-111.619,-111.619,57.184,57.184) ENVELOPE(168.517,168.517,-77.700,-77.700) |
geographic |
Fort MacKay Fort McMurray Mackay |
geographic_facet |
Fort MacKay Fort McMurray Mackay |
genre |
Fort McMurray |
genre_facet |
Fort McMurray |
op_relation |
http://dx.doi.org/10.1007/s10750-013-1623-5 Hydrobiologia 720 : 1-19 (2013) 0018-8158 http://hdl.handle.net/10261/88868 doi:10.1007/s10750-013-1623-5 |
op_rights |
none |
op_doi |
https://doi.org/10.1007/s10750-013-1623-5 |
container_title |
Hydrobiologia |
container_volume |
720 |
container_issue |
1 |
container_start_page |
55 |
op_container_end_page |
73 |
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1790600227645816832 |