Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada

A compilation of published and new limnological data from 1489 shallow lakes and ponds in northern Canada, sampled between 1979 and 2009, revealed significant patterns that correlated with landscape features and climate. Lakes and ponds underlain by Archean or Proterozoic bedrock had lower specific...

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Published in:Arctic Science
Main Authors: Stefana Aurora Dranga, Simon Hayles, Konrad Gajewski
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2018
Subjects:
Online Access:https://doi.org/10.1139/as-2017-0039
https://doaj.org/article/ec1e4ace44164c289000c36838156200
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spelling ftdoajarticles:oai:doaj.org/article:ec1e4ace44164c289000c36838156200 2023-05-15T14:23:42+02:00 Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada Stefana Aurora Dranga Simon Hayles Konrad Gajewski 2018-06-01T00:00:00Z https://doi.org/10.1139/as-2017-0039 https://doaj.org/article/ec1e4ace44164c289000c36838156200 EN FR eng fre Canadian Science Publishing https://doi.org/10.1139/as-2017-0039 https://doaj.org/toc/2368-7460 doi:10.1139/as-2017-0039 2368-7460 https://doaj.org/article/ec1e4ace44164c289000c36838156200 Arctic Science, Vol 4, Iss 2, Pp 167-185 (2018) freshwater aquatic productivity water chemistry nutrients Environmental sciences GE1-350 Environmental engineering TA170-171 article 2018 ftdoajarticles https://doi.org/10.1139/as-2017-0039 2022-12-31T12:52:37Z A compilation of published and new limnological data from 1489 shallow lakes and ponds in northern Canada, sampled between 1979 and 2009, revealed significant patterns that correlated with landscape features and climate. Lakes and ponds underlain by Archean or Proterozoic bedrock had lower specific conductivity and pH. Vegetation cover had a lesser influence on these parameters. Forested landscapes tended to have higher phosphorus and nitrogen, as did younger rock types. Dissolved organic carbon was higher, but dissolved inorganic carbon was lower in forested regions. Phytoplankton biomass of the surface waters, as estimated by chlorophyll a concentrations, was positively correlated with July air temperature and nutrients, and was higher in forested relative to polar desert regions. There were no significant differences in the measured limnological variables between shallow (<2 m depth) and deep lakes (>2 m); however, all water chemistry parameters were negatively correlated with depth. Despite large variability within and among regions, spatial trends in water chemistry were associated with geology, vegetation, and climate at a continental scale. Article in Journal/Newspaper Arctic Arctic Phytoplankton polar desert Directory of Open Access Journals: DOAJ Articles Arctic Canada Arctic Science 4 2 167 185
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic freshwater
aquatic productivity
water chemistry
nutrients
Environmental sciences
GE1-350
Environmental engineering
TA170-171
spellingShingle freshwater
aquatic productivity
water chemistry
nutrients
Environmental sciences
GE1-350
Environmental engineering
TA170-171
Stefana Aurora Dranga
Simon Hayles
Konrad Gajewski
Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
topic_facet freshwater
aquatic productivity
water chemistry
nutrients
Environmental sciences
GE1-350
Environmental engineering
TA170-171
description A compilation of published and new limnological data from 1489 shallow lakes and ponds in northern Canada, sampled between 1979 and 2009, revealed significant patterns that correlated with landscape features and climate. Lakes and ponds underlain by Archean or Proterozoic bedrock had lower specific conductivity and pH. Vegetation cover had a lesser influence on these parameters. Forested landscapes tended to have higher phosphorus and nitrogen, as did younger rock types. Dissolved organic carbon was higher, but dissolved inorganic carbon was lower in forested regions. Phytoplankton biomass of the surface waters, as estimated by chlorophyll a concentrations, was positively correlated with July air temperature and nutrients, and was higher in forested relative to polar desert regions. There were no significant differences in the measured limnological variables between shallow (<2 m depth) and deep lakes (>2 m); however, all water chemistry parameters were negatively correlated with depth. Despite large variability within and among regions, spatial trends in water chemistry were associated with geology, vegetation, and climate at a continental scale.
format Article in Journal/Newspaper
author Stefana Aurora Dranga
Simon Hayles
Konrad Gajewski
author_facet Stefana Aurora Dranga
Simon Hayles
Konrad Gajewski
author_sort Stefana Aurora Dranga
title Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
title_short Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
title_full Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
title_fullStr Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
title_full_unstemmed Synthesis of limnological data from lakes and ponds across Arctic and Boreal Canada
title_sort synthesis of limnological data from lakes and ponds across arctic and boreal canada
publisher Canadian Science Publishing
publishDate 2018
url https://doi.org/10.1139/as-2017-0039
https://doaj.org/article/ec1e4ace44164c289000c36838156200
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Arctic
Phytoplankton
polar desert
genre_facet Arctic
Arctic
Phytoplankton
polar desert
op_source Arctic Science, Vol 4, Iss 2, Pp 167-185 (2018)
op_relation https://doi.org/10.1139/as-2017-0039
https://doaj.org/toc/2368-7460
doi:10.1139/as-2017-0039
2368-7460
https://doaj.org/article/ec1e4ace44164c289000c36838156200
op_doi https://doi.org/10.1139/as-2017-0039
container_title Arctic Science
container_volume 4
container_issue 2
container_start_page 167
op_container_end_page 185
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