Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil

Data description This dataset is associated with the paper "Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil".This dataset includes the soil organic carbon turnover time (τ soc ) based on radiocarbon signals at the global and regional sca...

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Main Authors: Wang, Jing, Xia, Jianyang
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2023
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Online Access:https://doi.org/10.5281/zenodo.7623837
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spelling ftzenodo:oai:zenodo.org:7623837 2024-09-15T18:30:14+00:00 Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil Wang, Jing Xia, Jianyang 2023-02-03 https://doi.org/10.5281/zenodo.7623837 unknown Zenodo https://doi.org/10.5281/zenodo.7623836 https://doi.org/10.5281/zenodo.7623837 oai:zenodo.org:7623837 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/other 2023 ftzenodo https://doi.org/10.5281/zenodo.762383710.5281/zenodo.7623836 2024-07-27T05:42:22Z Data description This dataset is associated with the paper "Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil".This dataset includes the soil organic carbon turnover time (τ soc ) based on radiocarbon signals at the global and regional scales. Global synthesis The analysis of global soil radiocarbon data was done using the International Soil Radiocarbon Database (ISRaD v.1.0; Lawrence et al., 2020). ISRaD is an open source data with the records of 8 biomes ( i.e., forest, grassland, cropland, shrubland, savanna, tundra, permafrost, and others). Since we focus on the turnover time of SOC (τ soc ) based on radiocarbon occurring in the natural forest ecosystem, so we limited our study to data from soil depth within 200 cm in the forest ecosystem. We built a database of radiocarbon-based soil turnover time (τ soc ) of 1897 soil samples from 245 forest locations worldwide. It covers a wide geographical range (35.65 o S ‒ 68.8 o N; 159.64 °W – 173.57 °E) and a broad nature climate zone (-5.2 o C to 40.0 o C; 58.66 mm to 6900 mm) over the half a century (1958 – 2017).Where forest age is missing, we derived it from The global forest age dataset (GFAD v 1.0; Poulter et al., 2018). The GFAD database represents the distribution of forest stand age during 2000 – 2010 years. Regional analysis Soil sampling in forests across the Eastern Asian Monsoon region We sampled soils from twelve permanent forest plots in five mountains in the Eastern Asian Monsoon region (Table 1, Figure 1, and S1). Five of the twelve forest plots are members of the Smithsonian Forest Global Earth Observatory network (ForestGEO, https://forestgeo.si.edu/; Anderson-Teixeira et al., 2018; Chu et al., 2019). The other seven forest plots are members of China's National Ecosystem Research Network (CNERN, http://www.cern.ac.cn). In the Eastern Asian Monsoon region, more than half of the total annual rainfall occurs in the summer season ( i.e. , June, July, and August) (Tardif et al., 2020; Tian et al., ... Other/Unknown Material permafrost Tundra Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Data description This dataset is associated with the paper "Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil".This dataset includes the soil organic carbon turnover time (τ soc ) based on radiocarbon signals at the global and regional scales. Global synthesis The analysis of global soil radiocarbon data was done using the International Soil Radiocarbon Database (ISRaD v.1.0; Lawrence et al., 2020). ISRaD is an open source data with the records of 8 biomes ( i.e., forest, grassland, cropland, shrubland, savanna, tundra, permafrost, and others). Since we focus on the turnover time of SOC (τ soc ) based on radiocarbon occurring in the natural forest ecosystem, so we limited our study to data from soil depth within 200 cm in the forest ecosystem. We built a database of radiocarbon-based soil turnover time (τ soc ) of 1897 soil samples from 245 forest locations worldwide. It covers a wide geographical range (35.65 o S ‒ 68.8 o N; 159.64 °W – 173.57 °E) and a broad nature climate zone (-5.2 o C to 40.0 o C; 58.66 mm to 6900 mm) over the half a century (1958 – 2017).Where forest age is missing, we derived it from The global forest age dataset (GFAD v 1.0; Poulter et al., 2018). The GFAD database represents the distribution of forest stand age during 2000 – 2010 years. Regional analysis Soil sampling in forests across the Eastern Asian Monsoon region We sampled soils from twelve permanent forest plots in five mountains in the Eastern Asian Monsoon region (Table 1, Figure 1, and S1). Five of the twelve forest plots are members of the Smithsonian Forest Global Earth Observatory network (ForestGEO, https://forestgeo.si.edu/; Anderson-Teixeira et al., 2018; Chu et al., 2019). The other seven forest plots are members of China's National Ecosystem Research Network (CNERN, http://www.cern.ac.cn). In the Eastern Asian Monsoon region, more than half of the total annual rainfall occurs in the summer season ( i.e. , June, July, and August) (Tardif et al., 2020; Tian et al., ...
format Other/Unknown Material
author Wang, Jing
Xia, Jianyang
spellingShingle Wang, Jing
Xia, Jianyang
Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
author_facet Wang, Jing
Xia, Jianyang
author_sort Wang, Jing
title Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
title_short Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
title_full Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
title_fullStr Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
title_full_unstemmed Biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
title_sort biotic and abiotic factors controlling spatial variation of mean carbon turnover time in forest soil
publisher Zenodo
publishDate 2023
url https://doi.org/10.5281/zenodo.7623837
genre permafrost
Tundra
genre_facet permafrost
Tundra
op_relation https://doi.org/10.5281/zenodo.7623836
https://doi.org/10.5281/zenodo.7623837
oai:zenodo.org:7623837
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.762383710.5281/zenodo.7623836
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