Global subsoil organic carbon turnover times dominantly controlled by soil properties rather than climate
Soil organic carbon (SOC) in the subsoil below 0.3 m accounts for the majority of total SOC and may be as sensitive to climate change as topsoil SOC. Here we map global SOC turnover times (τ) in the subsoil layer at 1 km resolution using observational databases. Global mean τ is estimated to be [For...
| Published in: | Nature Communications |
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| Main Authors: | , , |
| Format: | Text |
| Language: | English |
| Published: |
Nature Publishing Group UK
2019
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| Subjects: | |
| Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6695437/ http://www.ncbi.nlm.nih.gov/pubmed/31417092 https://doi.org/10.1038/s41467-019-11597-9 |
| Summary: | Soil organic carbon (SOC) in the subsoil below 0.3 m accounts for the majority of total SOC and may be as sensitive to climate change as topsoil SOC. Here we map global SOC turnover times (τ) in the subsoil layer at 1 km resolution using observational databases. Global mean τ is estimated to be [Formula: see text] yr (mean with 95% confidence interval), and deserts and tundra show the shortest ([Formula: see text] yr) and longest ([Formula: see text] yr) τ respectively. Across the globe, mean τ ranges from 9 (the 5% quantile) to 6332 years (the 95% quantile). Temperature is the most important factor negatively affecting τ, but the overall effect of climate (including temperature and precipitation) is secondary compared with the overall effect of assessed soil properties (e.g., soil texture and pH). The high-resolution mapping of τ and the quantification of its controls provide a benchmark for diagnosing subsoil SOC dynamics under climate change. |
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