The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams

In the Alaskan Arctic, rapid climate change is increasing the frequency of disturbance including wildfire and permafrost collapse. These pulse disturbances may influence the delivery of dissolved organic carbon (DOC) to aquatic ecosystems, however the magnitude of these effects compared to the natur...

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Published in:Biogeosciences
Main Authors: Larouche, J. R., Abbott, B. W., Bowden, W. B., Jones, J. B.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/bg-12-4221-2015
https://www.biogeosciences.net/12/4221/2015/
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spelling ftcopernicus:oai:publications.copernicus.org:bg28856 2023-05-15T14:54:14+02:00 The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams Larouche, J. R. Abbott, B. W. Bowden, W. B. Jones, J. B. 2018-09-27 application/pdf https://doi.org/10.5194/bg-12-4221-2015 https://www.biogeosciences.net/12/4221/2015/ eng eng doi:10.5194/bg-12-4221-2015 https://www.biogeosciences.net/12/4221/2015/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-12-4221-2015 2019-12-24T09:53:18Z In the Alaskan Arctic, rapid climate change is increasing the frequency of disturbance including wildfire and permafrost collapse. These pulse disturbances may influence the delivery of dissolved organic carbon (DOC) to aquatic ecosystems, however the magnitude of these effects compared to the natural background variability of DOC at the watershed scale is not well known. We measured DOC quantity, composition, and biodegradability from 14 river and stream reaches (watershed sizes ranging from 1.5–167 km 2 ) some of which were impacted by permafrost collapse (thermokarst) and fire. We found that region had a significant impact on quantity and biodegradability of DOC, likely driven by landscape and watershed characteristics such as lithology, soil and vegetation type, elevation, and glacial age. However, contrary to our hypothesis, we found that streams disturbed by thermokarst and fire did not contain significantly altered labile DOC fractions compared to adjacent reference waters, potentially due to rapid ecosystem recovery after fire and thermokarst as well as the limited spatial extent of thermokarst. Overall, biodegradable DOC ranged from 4 to 46 % and contrary to patterns of DOC biodegradability in large Arctic rivers, seasonal variation in DOC biodegradability showed no clear pattern between sites, potentially related to stream geomorphology and position along the river network. While thermokarst and fire can alter DOC quantity and biodegradability at the scale of the feature, we conclude that tundra ecosystems are resilient to these types of disturbance. Text Arctic Climate change permafrost Thermokarst Tundra Copernicus Publications: E-Journals Arctic Biogeosciences 12 14 4221 4233
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collection Copernicus Publications: E-Journals
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language English
description In the Alaskan Arctic, rapid climate change is increasing the frequency of disturbance including wildfire and permafrost collapse. These pulse disturbances may influence the delivery of dissolved organic carbon (DOC) to aquatic ecosystems, however the magnitude of these effects compared to the natural background variability of DOC at the watershed scale is not well known. We measured DOC quantity, composition, and biodegradability from 14 river and stream reaches (watershed sizes ranging from 1.5–167 km 2 ) some of which were impacted by permafrost collapse (thermokarst) and fire. We found that region had a significant impact on quantity and biodegradability of DOC, likely driven by landscape and watershed characteristics such as lithology, soil and vegetation type, elevation, and glacial age. However, contrary to our hypothesis, we found that streams disturbed by thermokarst and fire did not contain significantly altered labile DOC fractions compared to adjacent reference waters, potentially due to rapid ecosystem recovery after fire and thermokarst as well as the limited spatial extent of thermokarst. Overall, biodegradable DOC ranged from 4 to 46 % and contrary to patterns of DOC biodegradability in large Arctic rivers, seasonal variation in DOC biodegradability showed no clear pattern between sites, potentially related to stream geomorphology and position along the river network. While thermokarst and fire can alter DOC quantity and biodegradability at the scale of the feature, we conclude that tundra ecosystems are resilient to these types of disturbance.
format Text
author Larouche, J. R.
Abbott, B. W.
Bowden, W. B.
Jones, J. B.
spellingShingle Larouche, J. R.
Abbott, B. W.
Bowden, W. B.
Jones, J. B.
The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
author_facet Larouche, J. R.
Abbott, B. W.
Bowden, W. B.
Jones, J. B.
author_sort Larouche, J. R.
title The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
title_short The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
title_full The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
title_fullStr The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
title_full_unstemmed The role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in Arctic headwater streams
title_sort role of watershed characteristics, permafrost thaw, and wildfire on dissolved organic carbon biodegradability and water chemistry in arctic headwater streams
publishDate 2018
url https://doi.org/10.5194/bg-12-4221-2015
https://www.biogeosciences.net/12/4221/2015/
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
permafrost
Thermokarst
Tundra
genre_facet Arctic
Climate change
permafrost
Thermokarst
Tundra
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-12-4221-2015
https://www.biogeosciences.net/12/4221/2015/
op_doi https://doi.org/10.5194/bg-12-4221-2015
container_title Biogeosciences
container_volume 12
container_issue 14
container_start_page 4221
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