Understanding the alterations in soil microbial communities in response to climate warming
and their controls over soil carbon (C) processes is crucial for projecting permafrost C …

The rapid climatic and environmental changes observed in the Arctic and across the globe
in general call for reliable model projections. In recent years our understanding of ongoing …

Priming effects of soil organic matter decomposition are critical to determine carbon budget
and turnover in soil. Yet, the overall direction and intensity of soil priming remains under …

Climate change is exposing subarctic ecosystems to higher temperatures, increased nutrient
availability, and increasing cloud cover. In this study, we assessed how these factors affect …

Climate change can have positive and negative effects on the carbon pools and budgets in
soil and plant fractions, but net effects are unclear and expected to vary widely within the …

Environmental changes, such as climate warming and higher herbivory pressure, are
altering the carbon balance of Arctic ecosystems; yet, how these drivers modify the carbon …

Alpine tundra, covering 3% of the Earth's land surface, harbors approximately 4% of higher
plant species. Changes in this vegetation significantly impact biodiversity and ecosystem …

Global warming-induced permafrost thawing raises concerns about the release of dormant
microbes, including potentially harmful plant pathogens. However, the potential pathogenic …

Reed (Phragmites australis) dominated wetlands are commonly known as strong carbon (C)
sinks due to the high productivity of the reed plant and C fixation in the wetland soil …

The Caatinga biome has been severely devastated over the years due to the replacement of
native dry forests with grassland areas in the Brazilian semiarid region. Despite this …