Rising Temperature May Trigger Deep Soil Carbon Loss Across Forest Ecosystems.
Ontology highlight
ABSTRACT: Significantly more carbon (C) is stored in deep soil than in shallow horizons, yet how the decomposition of deep soil organic C (SOC) will respond to rising temperature remains unexplored on large scales, leading to considerable uncertainties to predictions of the magnitude and direction of C-cycle feedbacks to climate change. Herein, short-term temperature sensitivity of SOC decomposition (expressed as Q 10) from six depths within the top 1 m soil from 90 upland forest sites (540 soil samples) across China is reported. Results show that Q 10 significantly increases with soil depth, suggesting that deep SOC is more vulnerable to loss with rising temperature in comparison to shallow SOC. Climate is the primary regulator of shallow soil Q 10
SUBMITTER: Li J
PROVIDER: S-EPMC7539220 | biostudies-literature | 2020 Oct
REPOSITORIES: biostudies-literature
ACCESS DATA