Permafrost carbon emissions in a changing Arctic
Arctic permafrost stores nearly 1,700 billion metric tons of frozen and thawing carbon.
Anthropogenic warming threatens to release an unknown quantity of this carbon to the …
Anthropogenic warming threatens to release an unknown quantity of this carbon to the …
Soil organic matter formation, persistence, and functioning: A synthesis of current understanding to inform its conservation and regeneration
Soil organic matter (SOM) provides vital services to humanity. Its preservation and further
accrual are key to sustain food production and avoid an irreversible climate crisis. Here we …
accrual are key to sustain food production and avoid an irreversible climate crisis. Here we …
Emergent biogeochemical risks from Arctic permafrost degradation
The Arctic cryosphere is collapsing, posing overlap** environmental risks. In particular,
thawing permafrost threatens to release biological, chemical and radioactive materials that …
thawing permafrost threatens to release biological, chemical and radioactive materials that …
Salinity controls soil microbial community structure and function in coastal estuarine wetlands
Soil salinity acts as a critical environmental filter on microbial communities, but the
consequences for microbial diversity and biogeochemical processes are poorly understood …
consequences for microbial diversity and biogeochemical processes are poorly understood …
Microbiome assembly in thawing permafrost and its feedbacks to climate
The physical and chemical changes that accompany permafrost thaw directly influence the
microbial communities that mediate the decomposition of formerly frozen organic matter …
microbial communities that mediate the decomposition of formerly frozen organic matter …
Microbial traits determine soil C emission in response to fresh carbon inputs in forests across biomes
Soil priming is a microbial‐driven process, which determines key soil–climate feedbacks in
response to fresh carbon inputs. Despite its importance, the microbial traits behind this …
response to fresh carbon inputs. Despite its importance, the microbial traits behind this …
Meta-analysis of the impact of freeze–thaw cycles on soil microbial diversity and C and N dynamics
X Ji, M Liu, J Yang, F Feng - Soil Biology and Biochemistry, 2022 - Elsevier
Reduction in snow cover is a prominent aspect of global change. Freeze–thaw cycles
(FTCs) of different amplitudes and durations in soil due to insufficient thermal insulation may …
(FTCs) of different amplitudes and durations in soil due to insufficient thermal insulation may …
Emission mitigation of CH4 and N2O during semi-permeable membrane covered hyperthermophilic aerobic composting of livestock manure
B Sun, Z Bai, Y Li, R Li, M Song, S Xu, H Zhang… - Journal of Cleaner …, 2022 - Elsevier
Membrane-covered composting and hyperthermophilic composting technologies have been
proven to be effective and have been widely applied as organic waste recycling strategies …
proven to be effective and have been widely applied as organic waste recycling strategies …
Distinct patterns of soil bacterial and fungal community assemblages in subtropical forest ecosystems under warming
Climate change globally affects soil microbial community assembly across ecosystems.
However, little is known about the impact of warming on the structure of soil microbial …
However, little is known about the impact of warming on the structure of soil microbial …
Asymmetric winter warming reduces microbial carbon use efficiency and growth more than symmetric year-round warming in alpine soils
Asymmetric seasonal warming trends are evident across terrestrial ecosystems, with winter
temperatures rising more than summer ones. Yet, the impact of such asymmetric seasonal …
temperatures rising more than summer ones. Yet, the impact of such asymmetric seasonal …