Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean

The northern coast of Ellesmere Island in the Canadian High Arctic is undergoing amplified warming that parallels the rapid decline in Arctic Ocean sea ice extent, and many lakes in this region have already shown changes in response to warming. However, biogeochemical data from High Arctic freshwate...

Full description

Bibliographic Details
Main Authors: Klanten, Yohanna, Triglav, Katherine, Marois, Catherine, Antoniades, Dermot
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2021
Subjects:
geo
Online Access:https://hdl.handle.net/20.500.11794/68504
id fttriple:oai:gotriple.eu:http://hdl.handle.net/20.500.11794/68504
record_format openpolar
spelling fttriple:oai:gotriple.eu:http://hdl.handle.net/20.500.11794/68504 2023-05-15T14:48:11+02:00 Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean Klanten, Yohanna Triglav, Katherine Marois, Catherine Antoniades, Dermot Arctique Nunavut -- Ellesmere, Île d' 2021-03-15 https://hdl.handle.net/20.500.11794/68504 en eng Canadian Science Publishing http://hdl.handle.net/20.500.11794/68504 other CorpusUL geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple https://doi.org/20.500.11794/68504 2023-01-22T16:44:28Z The northern coast of Ellesmere Island in the Canadian High Arctic is undergoing amplified warming that parallels the rapid decline in Arctic Ocean sea ice extent, and many lakes in this region have already shown changes in response to warming. However, biogeochemical data from High Arctic freshwaters are limited, and mostly restricted to the short, ice-free period. We sampled four coastal lakes in Stuckberry Valley (82° 54’ N, 66° 56’ W) before the onset of spring melting in 2017, 2018 and 2019, to assess biogeochemical gradients in their water columns and characteristics of their surface sediments. Despite their proximity, there were large differences in limnological properties. The two shallower lakes closer to the ocean were oxygen deficient while the two deeper, more distant lakes were more oxygenated. There were pronounced vertical gradients in major ions, metals and nutrients that suggested large differences in the extent of anaerobic microbial processes among the lakes. Morphometry and dissolved oxygen were the overriding determinants of biogeochemical differences rather than position along this short oceaninland gradient. The diversity of limnological conditions, and the sensitivity of these characteristics to changes in ice cover, underlines the need for further study of under-ice processes in extreme northern lakes. Article in Journal/Newspaper Arctic Arctic Ocean Arctique* Ellesmere Island Nunavut Sea ice Unknown Arctic Arctic Ocean Nunavut Ellesmere Island
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Klanten, Yohanna
Triglav, Katherine
Marois, Catherine
Antoniades, Dermot
Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
topic_facet geo
envir
description The northern coast of Ellesmere Island in the Canadian High Arctic is undergoing amplified warming that parallels the rapid decline in Arctic Ocean sea ice extent, and many lakes in this region have already shown changes in response to warming. However, biogeochemical data from High Arctic freshwaters are limited, and mostly restricted to the short, ice-free period. We sampled four coastal lakes in Stuckberry Valley (82° 54’ N, 66° 56’ W) before the onset of spring melting in 2017, 2018 and 2019, to assess biogeochemical gradients in their water columns and characteristics of their surface sediments. Despite their proximity, there were large differences in limnological properties. The two shallower lakes closer to the ocean were oxygen deficient while the two deeper, more distant lakes were more oxygenated. There were pronounced vertical gradients in major ions, metals and nutrients that suggested large differences in the extent of anaerobic microbial processes among the lakes. Morphometry and dissolved oxygen were the overriding determinants of biogeochemical differences rather than position along this short oceaninland gradient. The diversity of limnological conditions, and the sensitivity of these characteristics to changes in ice cover, underlines the need for further study of under-ice processes in extreme northern lakes.
format Article in Journal/Newspaper
author Klanten, Yohanna
Triglav, Katherine
Marois, Catherine
Antoniades, Dermot
author_facet Klanten, Yohanna
Triglav, Katherine
Marois, Catherine
Antoniades, Dermot
author_sort Klanten, Yohanna
title Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
title_short Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
title_full Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
title_fullStr Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
title_full_unstemmed Under-ice limnology of coastal valley lakes at the edge of the Arctic Ocean
title_sort under-ice limnology of coastal valley lakes at the edge of the arctic ocean
publisher Canadian Science Publishing
publishDate 2021
url https://hdl.handle.net/20.500.11794/68504
op_coverage Arctique
Nunavut -- Ellesmere, Île d'
geographic Arctic
Arctic Ocean
Nunavut
Ellesmere Island
geographic_facet Arctic
Arctic Ocean
Nunavut
Ellesmere Island
genre Arctic
Arctic Ocean
Arctique*
Ellesmere Island
Nunavut
Sea ice
genre_facet Arctic
Arctic Ocean
Arctique*
Ellesmere Island
Nunavut
Sea ice
op_source CorpusUL
op_relation http://hdl.handle.net/20.500.11794/68504
op_rights other
op_doi https://doi.org/20.500.11794/68504
_version_ 1766319287273783296