Structural characterization of dissolved organic matter in Permafrost Peatland Lakes

Thermokarst lakes result from the thawing of ice-rich permafrost and are widespread across northern landscapes. These waters are strong emitters of methane, especially in permafrost peatland regions, where they are stained black by high concentrations of dissolved organic matter (DOM). In the presen...

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Published in:Water
Main Authors: Folhas, Diogo, Duarte, Armando C., Pilote, Martin, Vincent, Warwick F., Freitas, Pedro, Vieira, Gonçalo, Silva, Artur M. S., Duarte, Regina M. B. O., Canário, João
Format: Article in Journal/Newspaper
Language:English
Published: MDPI 2020
Subjects:
DOM
Ice
Online Access:http://hdl.handle.net/10451/44840
https://doi.org/10.3390/w12113059
id ftunivlisboa:oai:repositorio.ul.pt:10451/44840
record_format openpolar
spelling ftunivlisboa:oai:repositorio.ul.pt:10451/44840 2023-05-15T16:35:28+02:00 Structural characterization of dissolved organic matter in Permafrost Peatland Lakes Folhas, Diogo Duarte, Armando C. Pilote, Martin Vincent, Warwick F. Freitas, Pedro Vieira, Gonçalo Silva, Artur M. S. Duarte, Regina M. B. O. Canário, João 2020-11-11T15:37:54Z http://hdl.handle.net/10451/44840 https://doi.org/10.3390/w12113059 eng eng MDPI https://www.mdpi.com/2073-4441/12/11/3059 Folhas, D., Duarte, A.C., Pilote, M., Vincent, W.F., Freitas, P., Vieira, G., Silva, A.M.S., Duarte, R.M.B.O., Canário, J. (2020). Structural characterization of dissolved organic matter in Permafrost Peatland Lakes. Water, 12(11), 3059. https://doi.org/10.3390/w12113059 http://hdl.handle.net/10451/44840 doi:10.3390/w12113059 2073-4441 openAccess http://creativecommons.org/licenses/by/4.0/ CC-BY Permafrost Thermokarst Peatlands Subarctic DOM Carbon cycle article 2020 ftunivlisboa https://doi.org/10.3390/w12113059 2023-03-01T01:08:16Z Thermokarst lakes result from the thawing of ice-rich permafrost and are widespread across northern landscapes. These waters are strong emitters of methane, especially in permafrost peatland regions, where they are stained black by high concentrations of dissolved organic matter (DOM). In the present study, we aimed to structurally characterize the DOM from a set of peatland thermokarst lakes that are known to be intense sites of microbial decomposition and methane emission. Samples were collected at different depths from three thermokarst lakes in the Sasapimakwananisikw (SAS) River valley near the eastern Hudson Bay community of Kuujjuarapik–Whapmagoostui (Nunavik, Canada). Samples were analyzed by spectrofluorometry, Fourier-transform infrared spectroscopy (FTIR), nuclear magnetic resonance spectroscopy (NMR), and elemental analysis. Fluorescence analyses indicated considerable amounts of autochthonous DOM in the surface waters of one of SAS 1A, indicating a strong bioavailability of labile DOM, and consequently a greater methanogenic potential. The three lakes differed in their chemical composition and diversity, suggesting various DOM transformations phenomena. The usefulness of complementary analytical approaches to characterize the complex mixture of DOM in permafrost peatland waters cannot be overlooked, representing a first step towards greater comprehension of the organic geochemical properties of these permafrost-derived systems info:eu-repo/semantics/publishedVersion Article in Journal/Newspaper Hudson Bay Ice Kuujjuarapik permafrost Subarctic Thermokarst Nunavik Universidade de Lisboa: repositório.UL Hudson Bay Nunavik Canada Hudson Kuujjuarapik ENVELOPE(-77.762,-77.762,55.276,55.276) Whapmagoostui ENVELOPE(-77.750,-77.750,55.250,55.250) Water 12 11 3059
institution Open Polar
collection Universidade de Lisboa: repositório.UL
op_collection_id ftunivlisboa
language English
topic Permafrost
Thermokarst
Peatlands
Subarctic
DOM
Carbon cycle
spellingShingle Permafrost
Thermokarst
Peatlands
Subarctic
DOM
Carbon cycle
Folhas, Diogo
Duarte, Armando C.
Pilote, Martin
Vincent, Warwick F.
Freitas, Pedro
Vieira, Gonçalo
Silva, Artur M. S.
Duarte, Regina M. B. O.
Canário, João
Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
topic_facet Permafrost
Thermokarst
Peatlands
Subarctic
DOM
Carbon cycle
description Thermokarst lakes result from the thawing of ice-rich permafrost and are widespread across northern landscapes. These waters are strong emitters of methane, especially in permafrost peatland regions, where they are stained black by high concentrations of dissolved organic matter (DOM). In the present study, we aimed to structurally characterize the DOM from a set of peatland thermokarst lakes that are known to be intense sites of microbial decomposition and methane emission. Samples were collected at different depths from three thermokarst lakes in the Sasapimakwananisikw (SAS) River valley near the eastern Hudson Bay community of Kuujjuarapik–Whapmagoostui (Nunavik, Canada). Samples were analyzed by spectrofluorometry, Fourier-transform infrared spectroscopy (FTIR), nuclear magnetic resonance spectroscopy (NMR), and elemental analysis. Fluorescence analyses indicated considerable amounts of autochthonous DOM in the surface waters of one of SAS 1A, indicating a strong bioavailability of labile DOM, and consequently a greater methanogenic potential. The three lakes differed in their chemical composition and diversity, suggesting various DOM transformations phenomena. The usefulness of complementary analytical approaches to characterize the complex mixture of DOM in permafrost peatland waters cannot be overlooked, representing a first step towards greater comprehension of the organic geochemical properties of these permafrost-derived systems info:eu-repo/semantics/publishedVersion
format Article in Journal/Newspaper
author Folhas, Diogo
Duarte, Armando C.
Pilote, Martin
Vincent, Warwick F.
Freitas, Pedro
Vieira, Gonçalo
Silva, Artur M. S.
Duarte, Regina M. B. O.
Canário, João
author_facet Folhas, Diogo
Duarte, Armando C.
Pilote, Martin
Vincent, Warwick F.
Freitas, Pedro
Vieira, Gonçalo
Silva, Artur M. S.
Duarte, Regina M. B. O.
Canário, João
author_sort Folhas, Diogo
title Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
title_short Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
title_full Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
title_fullStr Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
title_full_unstemmed Structural characterization of dissolved organic matter in Permafrost Peatland Lakes
title_sort structural characterization of dissolved organic matter in permafrost peatland lakes
publisher MDPI
publishDate 2020
url http://hdl.handle.net/10451/44840
https://doi.org/10.3390/w12113059
long_lat ENVELOPE(-77.762,-77.762,55.276,55.276)
ENVELOPE(-77.750,-77.750,55.250,55.250)
geographic Hudson Bay
Nunavik
Canada
Hudson
Kuujjuarapik
Whapmagoostui
geographic_facet Hudson Bay
Nunavik
Canada
Hudson
Kuujjuarapik
Whapmagoostui
genre Hudson Bay
Ice
Kuujjuarapik
permafrost
Subarctic
Thermokarst
Nunavik
genre_facet Hudson Bay
Ice
Kuujjuarapik
permafrost
Subarctic
Thermokarst
Nunavik
op_relation https://www.mdpi.com/2073-4441/12/11/3059
Folhas, D., Duarte, A.C., Pilote, M., Vincent, W.F., Freitas, P., Vieira, G., Silva, A.M.S., Duarte, R.M.B.O., Canário, J. (2020). Structural characterization of dissolved organic matter in Permafrost Peatland Lakes. Water, 12(11), 3059. https://doi.org/10.3390/w12113059
http://hdl.handle.net/10451/44840
doi:10.3390/w12113059
2073-4441
op_rights openAccess
http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.3390/w12113059
container_title Water
container_volume 12
container_issue 11
container_start_page 3059
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