Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate

The sensitivity of soil organic carbon (SOC) in subsoil (below 0.3 m) to climate change is poorly constrained. Here, the authors map global subsoil (0.3–1 m soil layer) SOC turnover times and find that temperature and in general climate effects are secondary to effects due to soil properties at both...

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Autores principales:	Zhongkui Luo, Guocheng Wang, Enli Wang
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/06fb8b200a124e11ae089ae5fd9b6790
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id	oai:doaj.org-article:06fb8b200a124e11ae089ae5fd9b6790
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spelling	oai:doaj.org-article:06fb8b200a124e11ae089ae5fd9b67902021-12-02T15:35:07ZGlobal subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate10.1038/s41467-019-11597-92041-1723https://doaj.org/article/06fb8b200a124e11ae089ae5fd9b67902019-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-11597-9https://doaj.org/toc/2041-1723The sensitivity of soil organic carbon (SOC) in subsoil (below 0.3 m) to climate change is poorly constrained. Here, the authors map global subsoil (0.3–1 m soil layer) SOC turnover times and find that temperature and in general climate effects are secondary to effects due to soil properties at both local and global scales—this now needs to be regarded for diagnosing subsoil SOC dynamics.Zhongkui LuoGuocheng WangEnli WangNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-10 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Zhongkui Luo Guocheng Wang Enli Wang Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
description	The sensitivity of soil organic carbon (SOC) in subsoil (below 0.3 m) to climate change is poorly constrained. Here, the authors map global subsoil (0.3–1 m soil layer) SOC turnover times and find that temperature and in general climate effects are secondary to effects due to soil properties at both local and global scales—this now needs to be regarded for diagnosing subsoil SOC dynamics.
format	article
author	Zhongkui Luo Guocheng Wang Enli Wang
author_facet	Zhongkui Luo Guocheng Wang Enli Wang
author_sort	Zhongkui Luo
title	Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
title_short	Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
title_full	Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
title_fullStr	Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
title_full_unstemmed	Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
title_sort	global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/06fb8b200a124e11ae089ae5fd9b6790
work_keys_str_mv	AT zhongkuiluo globalsubsoilorganiccarbonturnovertimesdominantlycontrolledbysoilpropertiesratherthanclimate AT guochengwang globalsubsoilorganiccarbonturnovertimesdominantlycontrolledbysoilpropertiesratherthanclimate AT enliwang globalsubsoilorganiccarbonturnovertimesdominantlycontrolledbysoilpropertiesratherthanclimate
_version_	1718386637588660224

Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate

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