Data S1 ...

Priming effects of soil organic matter decomposition are essential phenomena of terrestrial carbon cycling and affect the capacity of soils to serve as sources or sinks for atmospheric CO 2 in response to fresh carbon inputs. Yet, the general direction and intensity of soil priming in terrestrial ec...

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Bibliographic Details
Main Author: Xu, Shengwen
Format: Dataset
Language:unknown
Published: figshare 2024
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.25603185.v1
https://figshare.com/articles/dataset/Data_S1/25603185/1
id ftdatacite:10.6084/m9.figshare.25603185.v1
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.25603185.v1 2024-09-09T20:12:19+00:00 Data S1 ... Xu, Shengwen 2024 https://dx.doi.org/10.6084/m9.figshare.25603185.v1 https://figshare.com/articles/dataset/Data_S1/25603185/1 unknown figshare https://dx.doi.org/10.6084/m9.figshare.25603185 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Soil sciences not elsewhere classified Dataset dataset 2024 ftdatacite https://doi.org/10.6084/m9.figshare.25603185.v110.6084/m9.figshare.25603185 2024-07-03T11:28:03Z Priming effects of soil organic matter decomposition are essential phenomena of terrestrial carbon cycling and affect the capacity of soils to serve as sources or sinks for atmospheric CO 2 in response to fresh carbon inputs. Yet, the general direction and intensity of soil priming in terrestrial ecosystems remains under debate. A second-order meta-analysis was performed with 9296 paired observations from 363 primary studies to determine the intensity and general direction of priming effects depending on the compound type, nutrient availability, and ecosystem type. We found that fresh carbon inputs prevalently result in positive priming effects (+37%) in 97% of paired observations. Labile compounds induced higher priming effects (+73%) than complex organic compounds (+33%). Compound inputs with nutrient additions (N, P alone or together) reduced the intensity of priming effects compared to compounds without N and P. Notably, tundra, lake-beds, wetlands, and volcanic soils have much larger priming effects ... Dataset Tundra DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
topic Soil sciences not elsewhere classified
spellingShingle Soil sciences not elsewhere classified
Xu, Shengwen
Data S1 ...
topic_facet Soil sciences not elsewhere classified
description Priming effects of soil organic matter decomposition are essential phenomena of terrestrial carbon cycling and affect the capacity of soils to serve as sources or sinks for atmospheric CO 2 in response to fresh carbon inputs. Yet, the general direction and intensity of soil priming in terrestrial ecosystems remains under debate. A second-order meta-analysis was performed with 9296 paired observations from 363 primary studies to determine the intensity and general direction of priming effects depending on the compound type, nutrient availability, and ecosystem type. We found that fresh carbon inputs prevalently result in positive priming effects (+37%) in 97% of paired observations. Labile compounds induced higher priming effects (+73%) than complex organic compounds (+33%). Compound inputs with nutrient additions (N, P alone or together) reduced the intensity of priming effects compared to compounds without N and P. Notably, tundra, lake-beds, wetlands, and volcanic soils have much larger priming effects ...
format Dataset
author Xu, Shengwen
author_facet Xu, Shengwen
author_sort Xu, Shengwen
title Data S1 ...
title_short Data S1 ...
title_full Data S1 ...
title_fullStr Data S1 ...
title_full_unstemmed Data S1 ...
title_sort data s1 ...
publisher figshare
publishDate 2024
url https://dx.doi.org/10.6084/m9.figshare.25603185.v1
https://figshare.com/articles/dataset/Data_S1/25603185/1
genre Tundra
genre_facet Tundra
op_relation https://dx.doi.org/10.6084/m9.figshare.25603185
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.6084/m9.figshare.25603185.v110.6084/m9.figshare.25603185
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