The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada

Abstract In the lake‐rich tundra uplands east of the Mackenzie Delta, almost one in ten lakes has been affected by retrogressive thaw slumping. In this study, we assessed water chemistry for 34 slump‐affected and 39 undisturbed upland lakes across this region and found that environmental factors typ...

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Published in:Permafrost and Periglacial Processes
Main Authors: Kokelj, S. V., Zajdlik, B., Thompson, M. S.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.641
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spelling crwiley:10.1002/ppp.641 2024-06-23T07:50:36+00:00 The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada Kokelj, S. V. Zajdlik, B. Thompson, M. S. 2009 http://dx.doi.org/10.1002/ppp.641 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.641 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.641 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 2, page 185-199 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.641 2024-06-11T04:46:21Z Abstract In the lake‐rich tundra uplands east of the Mackenzie Delta, almost one in ten lakes has been affected by retrogressive thaw slumping. In this study, we assessed water chemistry for 34 slump‐affected and 39 undisturbed upland lakes across this region and found that environmental factors typically evoked to explain variation in tundra lake water quality including surficial geology and proximity to the treeline or coast were subordinate to the main driver, permafrost degradation. Thaw slump‐affected lakes had elevated ionic concentrations and water clarity in comparison with undisturbed lakes. The strength of the ionic impact was positively associated with the proportion of catchment affected by slumping and inversely related to disturbance age. Slumping did not have a significant effect on total organic carbon (TOC) concentrations, although water clarity increased significantly with decreasing age of disturbance. In lakes undisturbed by slumping, fire‐induced active‐layer deepening had a detectable influence on lake water ionic strength. Surficial deposits influenced TOC concentrations with the highest concentrations and colour in undisturbed lakes with lacustrine catchments. In a warming Arctic, thermokarst processes may increase in importance as a driver of ionic chemistry and optical properties of small lakes and ponds, and shifts in aquatic food webs can be anticipated. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada. Article in Journal/Newspaper Arctic Mackenzie Delta permafrost Permafrost and Periglacial Processes Subarctic Thermokarst Tundra Wiley Online Library Arctic Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Permafrost and Periglacial Processes 20 2 185 199
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language English
description Abstract In the lake‐rich tundra uplands east of the Mackenzie Delta, almost one in ten lakes has been affected by retrogressive thaw slumping. In this study, we assessed water chemistry for 34 slump‐affected and 39 undisturbed upland lakes across this region and found that environmental factors typically evoked to explain variation in tundra lake water quality including surficial geology and proximity to the treeline or coast were subordinate to the main driver, permafrost degradation. Thaw slump‐affected lakes had elevated ionic concentrations and water clarity in comparison with undisturbed lakes. The strength of the ionic impact was positively associated with the proportion of catchment affected by slumping and inversely related to disturbance age. Slumping did not have a significant effect on total organic carbon (TOC) concentrations, although water clarity increased significantly with decreasing age of disturbance. In lakes undisturbed by slumping, fire‐induced active‐layer deepening had a detectable influence on lake water ionic strength. Surficial deposits influenced TOC concentrations with the highest concentrations and colour in undisturbed lakes with lacustrine catchments. In a warming Arctic, thermokarst processes may increase in importance as a driver of ionic chemistry and optical properties of small lakes and ponds, and shifts in aquatic food webs can be anticipated. Copyright © 2009 John Wiley & Sons, Ltd. and Her Majesty the Queen in right of Canada.
format Article in Journal/Newspaper
author Kokelj, S. V.
Zajdlik, B.
Thompson, M. S.
spellingShingle Kokelj, S. V.
Zajdlik, B.
Thompson, M. S.
The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
author_facet Kokelj, S. V.
Zajdlik, B.
Thompson, M. S.
author_sort Kokelj, S. V.
title The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
title_short The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
title_full The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
title_fullStr The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
title_full_unstemmed The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada
title_sort impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, mackenzie delta region, canada
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/ppp.641
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.641
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.641
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Arctic
Canada
Mackenzie Delta
geographic_facet Arctic
Canada
Mackenzie Delta
genre Arctic
Mackenzie Delta
permafrost
Permafrost and Periglacial Processes
Subarctic
Thermokarst
Tundra
genre_facet Arctic
Mackenzie Delta
permafrost
Permafrost and Periglacial Processes
Subarctic
Thermokarst
Tundra
op_source Permafrost and Periglacial Processes
volume 20, issue 2, page 185-199
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.641
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