Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed
With the strongest climate warming occurring and predicted in the high-latitudes, understanding arctic carbon (C) cycling and the feedback of terrestrial C pools is increasingly important. Arctic terrestrial ecosystems comprise about one-third of the global terrestrial ecosystem C total with most of...
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ftdatacite:10.25710/nahj-nw20 2023-05-15T14:46:06+02:00 Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed Heard, Kathryn E. 2014 https://dx.doi.org/10.25710/nahj-nw20 https://cedar.wwu.edu/wwuet/352 unknown Western Washington University Text Masters Thesis article-journal ScholarlyArticle 2014 ftdatacite https://doi.org/10.25710/nahj-nw20 2021-11-05T12:55:41Z With the strongest climate warming occurring and predicted in the high-latitudes, understanding arctic carbon (C) cycling and the feedback of terrestrial C pools is increasingly important. Arctic terrestrial ecosystems comprise about one-third of the global terrestrial ecosystem C total with most of the C stored in soils, making the response of arctic systems to accelerated warming an issue of global concern. For this research, above- and belowground C stocks were quantified in a small catchment of the Kolyma River watershed in northeastern Siberia, with the primary goal of contributing to a more precise estimate of arctic C pools. Eighteen sites were chosen based on four categories of tree density. We assessed the correlation between soil C, vegetation C, and four environmental correlates -- slope, solar insolation, canopy density, and leaf area index. Carbon in the surface O horizon (2414 ± 391 g C m -2 , mean +/- SE) and underlying mineral soil layer to a depth of 10 cm or to the bottom of the active layer, whichever was less, (2231 ± 432 g C m -2 ) were, together, approximately four times that of the aboveground C pools (1128 ± 273 g C m -2 ). Of the environmental correlates considered, canopy cover had the most robust association with aboveground C pools (p < 0.001; r = 0.812), while no environmental variables correlated significantly with soil C pools (p > 0.05). Greater quantities of belowground C storage are consistent with previous studies in arctic terrestrial ecosystems, but a high degree of variability existed in both above- and belowground C pools. High variability will make it more difficult to accurately quantify C pools at larger spatial scales. Additionally, the identification of canopy cover as a robust biotic correlate presents alternatives to directly measuring C stocks, but this relationship needs to be verified elsewhere in the Arctic before using it in lieu of field data collection. Text Arctic kolyma river Siberia DataCite Metadata Store (German National Library of Science and Technology) Arctic Kolyma ENVELOPE(161.000,161.000,69.500,69.500) |
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With the strongest climate warming occurring and predicted in the high-latitudes, understanding arctic carbon (C) cycling and the feedback of terrestrial C pools is increasingly important. Arctic terrestrial ecosystems comprise about one-third of the global terrestrial ecosystem C total with most of the C stored in soils, making the response of arctic systems to accelerated warming an issue of global concern. For this research, above- and belowground C stocks were quantified in a small catchment of the Kolyma River watershed in northeastern Siberia, with the primary goal of contributing to a more precise estimate of arctic C pools. Eighteen sites were chosen based on four categories of tree density. We assessed the correlation between soil C, vegetation C, and four environmental correlates -- slope, solar insolation, canopy density, and leaf area index. Carbon in the surface O horizon (2414 ± 391 g C m -2 , mean +/- SE) and underlying mineral soil layer to a depth of 10 cm or to the bottom of the active layer, whichever was less, (2231 ± 432 g C m -2 ) were, together, approximately four times that of the aboveground C pools (1128 ± 273 g C m -2 ). Of the environmental correlates considered, canopy cover had the most robust association with aboveground C pools (p < 0.001; r = 0.812), while no environmental variables correlated significantly with soil C pools (p > 0.05). Greater quantities of belowground C storage are consistent with previous studies in arctic terrestrial ecosystems, but a high degree of variability existed in both above- and belowground C pools. High variability will make it more difficult to accurately quantify C pools at larger spatial scales. Additionally, the identification of canopy cover as a robust biotic correlate presents alternatives to directly measuring C stocks, but this relationship needs to be verified elsewhere in the Arctic before using it in lieu of field data collection. |
format |
Text |
author |
Heard, Kathryn E. |
spellingShingle |
Heard, Kathryn E. Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
author_facet |
Heard, Kathryn E. |
author_sort |
Heard, Kathryn E. |
title |
Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
title_short |
Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
title_full |
Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
title_fullStr |
Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
title_full_unstemmed |
Systematic analysis of terrestrial carbon stocks in a small catchment of the Kolyma watershed |
title_sort |
systematic analysis of terrestrial carbon stocks in a small catchment of the kolyma watershed |
publisher |
Western Washington University |
publishDate |
2014 |
url |
https://dx.doi.org/10.25710/nahj-nw20 https://cedar.wwu.edu/wwuet/352 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) |
geographic |
Arctic Kolyma |
geographic_facet |
Arctic Kolyma |
genre |
Arctic kolyma river Siberia |
genre_facet |
Arctic kolyma river Siberia |
op_doi |
https://doi.org/10.25710/nahj-nw20 |
_version_ |
1766317365793914880 |