Grasslands store approximately one third of the global terrestrial carbon stocks and can act
as an important soil carbon sink. Recent studies show that plant diversity increases soil …

Soil microorganisms shape global element cycles in life and death. Living soil
microorganisms are a major engine of terrestrial biogeochemistry, driving the turnover of soil …

Despite the recognized importance of the contribution of microbial necromass to soil organic
carbon (SOC) sequestration, at a global scale, there has been no quantification for cropland …

Soil organic matter (SOM) represents a major reservoir of stored carbon (C). However,
uncertainties regarding the composition and origin of stabilized SOM hinder the …

Soil carbon sequestration (SCS) refers to the uptake of carbon (C) containing substances
from the atmosphere and its storage in soil C pools. Soil microbial community (SMC) play a …

Soil carbon transformation and sequestration have received significant interest in recent
years due to a growing need for quantitating its role in mitigating climate change. Even …

Grassland restoration across the world increases soil organic carbon (SOC) sequestration
which is critical for global C cycling and CO 2 removal from the atmosphere. However, the …

Mechanisms of soil organic carbon (SOC) stabilization have been widely studied due to their
relevance in the global carbon cycle. No‐till (NT) has been frequently adopted to sequester …

Paddy soils make up the largest anthropogenic wetlands on earth, and are characterized by
a prominent potential for organic carbon (C) sequestration. By quantifying the plant‐and …

Increasing phosphorus (P) inputs induced by anthropogenic activities have increased P
availability in soils considerably, with dramatic effects on carbon (C) cycling and storage …