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1. Increasing numbers of global change stressors reduce soil carbon worldwide

4. Rhizosheath drought responsiveness is variety‐specific and a key component of belowground plant adaptation

6. Microbial impact on initial soil formation in arid and semiarid environments under simulated climate change

7. Dominance of particulate organic carbon in top mineral soils in cold regions

9. Getting to the Root of the Problem: Disentangling Interactions between Modern Root Inputs, Microbial Activity, and Carbon Destabilization in Buried Paleosols

15. Soil carbon and nitrogen cycling at the atmosphere-soil interface: quantifying the response of biocrust-soil interactions to climate change

16. Functional traits of Zea mays L. varieties determine drought effects on soil structure and carbon allocation in the rhizosheath

19. Getting to the Root of the Problem: Disentangling Interactions between Modern Root Inputs, Microbial Activity, and Carbon Destabilization in Buried Paleosols

20. Above and belowground traits impacting transpiration decline during soil drying in 48 maize (Zea mays) genotypes

24. Alder-induced stimulation of soil gross nitrogen turnover in a permafrost-affected peatland of Northeast China

32. Microbial iron cycling during palsa hillslope collapse promotes greenhouse gas emissions before complete permafrost thaw

34. Alder-induced stimulation of soil gross nitrogen turnover in permafrost-affected peatlands of Northeast China

36. A review of the importance of mineral nitrogen cycling in the plant-soil-microbe system of permafrost-affected soils – changing the paradigm

41. High-resolution stalagmite stratigraphy supports the Late Holocene tephrochronology of southernmost Patagonia

44. Ensuring planetary survival: the centrality of organic carbon in balancing the multifunctional nature of soils

46. A review of the importance of mineral nitrogen cycling in the plant-soil-microbe system of permafrost-affected soils—changing the paradigm

50. Probing the nature of soil organic matter

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