Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.

Soil microbes are not only key drivers for nutrient and energy cycles, but they are also fast responders to changes in their environment- and as such act as bioindicators of climate change. The temperatures in the Arctic are warming two times faster than at lower latitudes and lead to warming of per...

Full description

Bibliographic Details
Main Authors: Ina Timling, Lee Taylor, Cristina Takacs-Vesbach, Skip Walker
Format: Dataset
Language:unknown
Published: Arctic Data Center 2022
Subjects:
Ice
Online Access:https://doi.org/10.18739/A2T14TQ8P
id dataone:doi:10.18739/A2T14TQ8P
record_format openpolar
spelling dataone:doi:10.18739/A2T14TQ8P 2023-11-08T14:14:16+01:00 Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021. Ina Timling Lee Taylor Cristina Takacs-Vesbach Skip Walker Isachsen, Ellef Ringnes Island, Nunawut, Canada Mould Bay, Prince Patrick Island, Northwest Territories, Canada Green Cabin, Banks Island, Northwest Territories, Canada ENVELOPE(-103.54,-103.54,78.79,78.79) BEGINDATE: 2005-01-01T00:00:00Z ENDDATE: 2021-01-01T00:00:00Z 2022-01-01T00:00:00Z https://doi.org/10.18739/A2T14TQ8P unknown Arctic Data Center High Canadian Arctic permafrost soils fungi bacteria warming thermokarst Dataset 2022 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2T14TQ8P 2023-11-08T13:47:40Z Soil microbes are not only key drivers for nutrient and energy cycles, but they are also fast responders to changes in their environment- and as such act as bioindicators of climate change. The temperatures in the Arctic are warming two times faster than at lower latitudes and lead to warming of permafrost soils, an increase of the active layer and eventually to thermokarst, the thawing of permafrost. Thawing permafrost affects the hydrological systems and increases the potential of old carbon becoming available for decomposition. The fate of carbon stores will rest largely on the response of plant and microbial communities to the changed conditions. Especially the ice rich permafrost soils in the High Arctic are highly sensitive to increasing air temperatures, because the permafrost occurs close to the surface and the soils lack the insulation provided by a thick vegetation cover and organic soil horizons as found in the Low Arctic (Farquharson et al. 2019). This study examines the effects of soil warming and thermokarst on fungal and bacterial communities of active layer soils in the three most northern bioclimatic subzones (A, B, C) of the Arctic that occurred over 10 years (2005-2016). We used Illumina sequencing to analyze the fungal and bacterial communities and obtained environmental data to investigate the effect of warming and thermokarst on fungal and bacterial communities in the High Arctic. Here we present the assembled fungal, bacterial and environmental data sets. Dataset Arctic Banks Island Climate change Ellef Ringnes Island Ice Mould Bay Northwest Territories permafrost Prince Patrick Island Thermokarst Arctic Data Center (via DataONE) Arctic Northwest Territories Canada Isachsen ENVELOPE(-103.505,-103.505,78.785,78.785) Mould Bay ENVELOPE(-119.436,-119.436,76.197,76.197) Ellef Ringnes Island ENVELOPE(-102.256,-102.256,78.502,78.502) Prince Patrick Island ENVELOPE(-119.507,-119.507,76.751,76.751) ENVELOPE(-103.54,-103.54,78.79,78.79)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic High Canadian Arctic
permafrost soils
fungi
bacteria
warming
thermokarst
spellingShingle High Canadian Arctic
permafrost soils
fungi
bacteria
warming
thermokarst
Ina Timling
Lee Taylor
Cristina Takacs-Vesbach
Skip Walker
Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
topic_facet High Canadian Arctic
permafrost soils
fungi
bacteria
warming
thermokarst
description Soil microbes are not only key drivers for nutrient and energy cycles, but they are also fast responders to changes in their environment- and as such act as bioindicators of climate change. The temperatures in the Arctic are warming two times faster than at lower latitudes and lead to warming of permafrost soils, an increase of the active layer and eventually to thermokarst, the thawing of permafrost. Thawing permafrost affects the hydrological systems and increases the potential of old carbon becoming available for decomposition. The fate of carbon stores will rest largely on the response of plant and microbial communities to the changed conditions. Especially the ice rich permafrost soils in the High Arctic are highly sensitive to increasing air temperatures, because the permafrost occurs close to the surface and the soils lack the insulation provided by a thick vegetation cover and organic soil horizons as found in the Low Arctic (Farquharson et al. 2019). This study examines the effects of soil warming and thermokarst on fungal and bacterial communities of active layer soils in the three most northern bioclimatic subzones (A, B, C) of the Arctic that occurred over 10 years (2005-2016). We used Illumina sequencing to analyze the fungal and bacterial communities and obtained environmental data to investigate the effect of warming and thermokarst on fungal and bacterial communities in the High Arctic. Here we present the assembled fungal, bacterial and environmental data sets.
format Dataset
author Ina Timling
Lee Taylor
Cristina Takacs-Vesbach
Skip Walker
author_facet Ina Timling
Lee Taylor
Cristina Takacs-Vesbach
Skip Walker
author_sort Ina Timling
title Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
title_short Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
title_full Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
title_fullStr Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
title_full_unstemmed Effects of soil warming and thermokarst on soil microbial communities in the High Canadian Arctic, 2005-2021.
title_sort effects of soil warming and thermokarst on soil microbial communities in the high canadian arctic, 2005-2021.
publisher Arctic Data Center
publishDate 2022
url https://doi.org/10.18739/A2T14TQ8P
op_coverage Isachsen, Ellef Ringnes Island, Nunawut, Canada
Mould Bay, Prince Patrick Island, Northwest Territories, Canada
Green Cabin, Banks Island, Northwest Territories, Canada
ENVELOPE(-103.54,-103.54,78.79,78.79)
BEGINDATE: 2005-01-01T00:00:00Z ENDDATE: 2021-01-01T00:00:00Z
long_lat ENVELOPE(-103.505,-103.505,78.785,78.785)
ENVELOPE(-119.436,-119.436,76.197,76.197)
ENVELOPE(-102.256,-102.256,78.502,78.502)
ENVELOPE(-119.507,-119.507,76.751,76.751)
ENVELOPE(-103.54,-103.54,78.79,78.79)
geographic Arctic
Northwest Territories
Canada
Isachsen
Mould Bay
Ellef Ringnes Island
Prince Patrick Island
geographic_facet Arctic
Northwest Territories
Canada
Isachsen
Mould Bay
Ellef Ringnes Island
Prince Patrick Island
genre Arctic
Banks Island
Climate change
Ellef Ringnes Island
Ice
Mould Bay
Northwest Territories
permafrost
Prince Patrick Island
Thermokarst
genre_facet Arctic
Banks Island
Climate change
Ellef Ringnes Island
Ice
Mould Bay
Northwest Territories
permafrost
Prince Patrick Island
Thermokarst
op_doi https://doi.org/10.18739/A2T14TQ8P
_version_ 1782012694482649088