The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland

Dissolved organic matter (DOM) leaching from thawing permafrost may promote a positive feedback on the climate if it is efficiently mineralized into greenhouse gases. However, many uncertainties remain on the extent of this mineralization, which depends on DOM lability that is seemingly quite variab...

Full description

Bibliographic Details
Published in:Biogeosciences
Main Authors: Mazoyer, Flora, Laurion, Isabelle, Rautio, Milla
Format: Text
Language:English
Published: 2022
Subjects:
Ice
Online Access:https://doi.org/10.5194/bg-19-3959-2022
https://bg.copernicus.org/articles/19/3959/2022/
id ftcopernicus:oai:publications.copernicus.org:bg101026
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:bg101026 2023-05-15T16:37:55+02:00 The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland Mazoyer, Flora Laurion, Isabelle Rautio, Milla 2022-08-31 application/pdf https://doi.org/10.5194/bg-19-3959-2022 https://bg.copernicus.org/articles/19/3959/2022/ eng eng doi:10.5194/bg-19-3959-2022 https://bg.copernicus.org/articles/19/3959/2022/ eISSN: 1726-4189 Text 2022 ftcopernicus https://doi.org/10.5194/bg-19-3959-2022 2022-09-05T16:22:54Z Dissolved organic matter (DOM) leaching from thawing permafrost may promote a positive feedback on the climate if it is efficiently mineralized into greenhouse gases. However, many uncertainties remain on the extent of this mineralization, which depends on DOM lability that is seemingly quite variable across landscapes. Thermokarst peatlands are organic-rich systems where some of the largest greenhouse gas (GHG) emission rates have been measured. At spring turnover, anoxic waters release the GHG accumulated in winter, and the DOM pool is exposed to sunlight. Here, we present an experiment where DOM photoreactivity and bioreactivity were investigated in water collected from a thermokarst lake in a subarctic peatland during late winter (after 6 months of darkness). We applied treatment with or without light exposure, and manipulated the bacterial abundance with the aim to quantify the unique and combined effects of light and bacteria on DOM reactivity at ice-off in spring. We demonstrate that sunlight was clearly driving the transformation of the DOM pool, part of which went through a complete mineralization into CO 2 . Up to 18 % of the initial dissolved organic carbon (DOC, a loss of 3.9 mgC L −1 ) was lost over 18 d of sunlight exposure in a treatment where bacterial abundance was initially reduced by 95 %. However, sunlight considerably stimulated bacterial growth when grazers were eliminated, leading to the recovery of the original bacterial abundance in about 8 d, which may have contributed to the DOC loss. Indeed, the highest DOC loss was observed for the treatment with the full bacterial community exposed to sunlight (5.0 mgC L −1 ), indicating an indirect effect of light through the bacterial consumption of photoproducts. Dark incubations led to very limited changes in DOC, regardless of the bacterial abundance and activity. The results also show that only half of the light-associated DOC losses were converted into CO 2 , and we suggest that the rest potentially turned into particles through ... Text Ice permafrost Subarctic Thermokarst Copernicus Publications: E-Journals Biogeosciences 19 17 3959 3977
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Dissolved organic matter (DOM) leaching from thawing permafrost may promote a positive feedback on the climate if it is efficiently mineralized into greenhouse gases. However, many uncertainties remain on the extent of this mineralization, which depends on DOM lability that is seemingly quite variable across landscapes. Thermokarst peatlands are organic-rich systems where some of the largest greenhouse gas (GHG) emission rates have been measured. At spring turnover, anoxic waters release the GHG accumulated in winter, and the DOM pool is exposed to sunlight. Here, we present an experiment where DOM photoreactivity and bioreactivity were investigated in water collected from a thermokarst lake in a subarctic peatland during late winter (after 6 months of darkness). We applied treatment with or without light exposure, and manipulated the bacterial abundance with the aim to quantify the unique and combined effects of light and bacteria on DOM reactivity at ice-off in spring. We demonstrate that sunlight was clearly driving the transformation of the DOM pool, part of which went through a complete mineralization into CO 2 . Up to 18 % of the initial dissolved organic carbon (DOC, a loss of 3.9 mgC L −1 ) was lost over 18 d of sunlight exposure in a treatment where bacterial abundance was initially reduced by 95 %. However, sunlight considerably stimulated bacterial growth when grazers were eliminated, leading to the recovery of the original bacterial abundance in about 8 d, which may have contributed to the DOC loss. Indeed, the highest DOC loss was observed for the treatment with the full bacterial community exposed to sunlight (5.0 mgC L −1 ), indicating an indirect effect of light through the bacterial consumption of photoproducts. Dark incubations led to very limited changes in DOC, regardless of the bacterial abundance and activity. The results also show that only half of the light-associated DOC losses were converted into CO 2 , and we suggest that the rest potentially turned into particles through ...
format Text
author Mazoyer, Flora
Laurion, Isabelle
Rautio, Milla
spellingShingle Mazoyer, Flora
Laurion, Isabelle
Rautio, Milla
The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
author_facet Mazoyer, Flora
Laurion, Isabelle
Rautio, Milla
author_sort Mazoyer, Flora
title The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
title_short The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
title_full The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
title_fullStr The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
title_full_unstemmed The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
title_sort dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
publishDate 2022
url https://doi.org/10.5194/bg-19-3959-2022
https://bg.copernicus.org/articles/19/3959/2022/
genre Ice
permafrost
Subarctic
Thermokarst
genre_facet Ice
permafrost
Subarctic
Thermokarst
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-19-3959-2022
https://bg.copernicus.org/articles/19/3959/2022/
op_doi https://doi.org/10.5194/bg-19-3959-2022
container_title Biogeosciences
container_volume 19
container_issue 17
container_start_page 3959
op_container_end_page 3977
_version_ 1766028219203452928