Carbon dynamics in highly heterotrophic subarctic thaw ponds

Global warming has accelerated the formation of permafrost thaw ponds in several subarctic and arctic regions. These ponds are net heterotrophic as evidenced by their greenhouse gas (GHG) supersaturation levels (CO2 and CH4), and generally receive large terrestrial carbon inputs from the thawing and...

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Main Authors: Roiha, Toni, Laurion, I., Rautio, Milla
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH; European Geosciences Union 2015
Subjects:
Ice
Online Access:http://urn.fi/URN:NBN:fi:jyu-201604202274
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spelling ftjyvaeskylaenun:oai:jyx.jyu.fi:123456789/49396 2023-05-15T15:11:37+02:00 Carbon dynamics in highly heterotrophic subarctic thaw ponds Roiha, Toni Laurion, I. Rautio, Milla 2015 7223-7237 application/pdf http://urn.fi/URN:NBN:fi:jyu-201604202274 eng eng Copernicus GmbH; European Geosciences Union Biogeosciences 1726-4170 23 12 10.5194/bg-12-7223-2015 Roiha, T., Laurion, I., & Rautio, M. (2015). Carbon dynamics in highly heterotrophic subarctic thaw ponds. Biogeosciences , 12 (23), 7223-7237. https://doi.org/10.5194/bg-12-7223-2015 CONVID_25662548 TUTKAID_69802 URN:NBN:fi:jyu-201604202274 http://urn.fi/URN:NBN:fi:jyu-201604202274 © Author(s) 2015. This is an open access article distributed under the CC Attribution 3.0 License. openAccess https://creativecommons.org/licenses/by/3.0/ CC-BY subarctic region permafrost thaw ponds thermokarst dissolved organic matter bacterioplankton liuennut orgaaninen hiili article http://purl.org/eprint/type/JournalArticle journal article publishedVersion 2015 ftjyvaeskylaenun 2023-03-01T23:59:43Z Global warming has accelerated the formation of permafrost thaw ponds in several subarctic and arctic regions. These ponds are net heterotrophic as evidenced by their greenhouse gas (GHG) supersaturation levels (CO2 and CH4), and generally receive large terrestrial carbon inputs from the thawing and eroding permafrost. We measured seasonal and vertical variations in the concentration and type of dissolved organic matter (DOM) in five subarctic thaw (thermokarst) ponds in northern Quebec, and explored how environmental gradients influenced heterotrophic and phototrophic biomass and productivity. Late winter DOM had low aromaticity indicating reduced inputs of terrestrial carbon, while the high concentration of dissolved organic carbon (DOC) suggests that some production of nonchromophoric dissolved compounds by the microbial food web took place under the ice cover. Summer DOM had a strong terrestrial signature, but was also characterized with significant inputs of algal-derived carbon, especially at the pond surface. During late winter, bacterial production was low (maximum of 0.8 mg C m−3 d −1 ) and was largely based on free-living bacterioplankton (58 %). Bacterial production in summer was high (up to 58 mg C m−3 d −1 ), dominated by particle-attached bacteria (67 %), and strongly correlated with the amount of terrestrial carbon. Primary production was restricted to summer surface waters due to strong light limitation deeper in the water column or in winter. The phototrophic biomass was equal to the heterotrophic biomass, but as the algae were mostly composed of mixotrophic species, most probably they used bacteria rather than solar energy in such shaded ponds. Our results point to a strong heterotrophic energy pathway in these thaw pond ecosystems, where bacterioplankton dominates the production of new carbon biomass in both summer and winter. peerReviewed Article in Journal/Newspaper Arctic Global warming Ice permafrost Subarctic Thermokarst JYX - Jyväskylä University Digital Archive Arctic
institution Open Polar
collection JYX - Jyväskylä University Digital Archive
op_collection_id ftjyvaeskylaenun
language English
topic subarctic region
permafrost thaw ponds
thermokarst
dissolved organic matter
bacterioplankton
liuennut orgaaninen hiili
spellingShingle subarctic region
permafrost thaw ponds
thermokarst
dissolved organic matter
bacterioplankton
liuennut orgaaninen hiili
Roiha, Toni
Laurion, I.
Rautio, Milla
Carbon dynamics in highly heterotrophic subarctic thaw ponds
topic_facet subarctic region
permafrost thaw ponds
thermokarst
dissolved organic matter
bacterioplankton
liuennut orgaaninen hiili
description Global warming has accelerated the formation of permafrost thaw ponds in several subarctic and arctic regions. These ponds are net heterotrophic as evidenced by their greenhouse gas (GHG) supersaturation levels (CO2 and CH4), and generally receive large terrestrial carbon inputs from the thawing and eroding permafrost. We measured seasonal and vertical variations in the concentration and type of dissolved organic matter (DOM) in five subarctic thaw (thermokarst) ponds in northern Quebec, and explored how environmental gradients influenced heterotrophic and phototrophic biomass and productivity. Late winter DOM had low aromaticity indicating reduced inputs of terrestrial carbon, while the high concentration of dissolved organic carbon (DOC) suggests that some production of nonchromophoric dissolved compounds by the microbial food web took place under the ice cover. Summer DOM had a strong terrestrial signature, but was also characterized with significant inputs of algal-derived carbon, especially at the pond surface. During late winter, bacterial production was low (maximum of 0.8 mg C m−3 d −1 ) and was largely based on free-living bacterioplankton (58 %). Bacterial production in summer was high (up to 58 mg C m−3 d −1 ), dominated by particle-attached bacteria (67 %), and strongly correlated with the amount of terrestrial carbon. Primary production was restricted to summer surface waters due to strong light limitation deeper in the water column or in winter. The phototrophic biomass was equal to the heterotrophic biomass, but as the algae were mostly composed of mixotrophic species, most probably they used bacteria rather than solar energy in such shaded ponds. Our results point to a strong heterotrophic energy pathway in these thaw pond ecosystems, where bacterioplankton dominates the production of new carbon biomass in both summer and winter. peerReviewed
format Article in Journal/Newspaper
author Roiha, Toni
Laurion, I.
Rautio, Milla
author_facet Roiha, Toni
Laurion, I.
Rautio, Milla
author_sort Roiha, Toni
title Carbon dynamics in highly heterotrophic subarctic thaw ponds
title_short Carbon dynamics in highly heterotrophic subarctic thaw ponds
title_full Carbon dynamics in highly heterotrophic subarctic thaw ponds
title_fullStr Carbon dynamics in highly heterotrophic subarctic thaw ponds
title_full_unstemmed Carbon dynamics in highly heterotrophic subarctic thaw ponds
title_sort carbon dynamics in highly heterotrophic subarctic thaw ponds
publisher Copernicus GmbH; European Geosciences Union
publishDate 2015
url http://urn.fi/URN:NBN:fi:jyu-201604202274
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Ice
permafrost
Subarctic
Thermokarst
genre_facet Arctic
Global warming
Ice
permafrost
Subarctic
Thermokarst
op_relation Biogeosciences
1726-4170
23
12
10.5194/bg-12-7223-2015
Roiha, T., Laurion, I., & Rautio, M. (2015). Carbon dynamics in highly heterotrophic subarctic thaw ponds. Biogeosciences , 12 (23), 7223-7237. https://doi.org/10.5194/bg-12-7223-2015
CONVID_25662548
TUTKAID_69802
URN:NBN:fi:jyu-201604202274
http://urn.fi/URN:NBN:fi:jyu-201604202274
op_rights © Author(s) 2015. This is an open access article distributed under the CC Attribution 3.0 License.
openAccess
https://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
_version_ 1766342457549651968