As the Arctic rapidly warms, deciduous ectomycorrhizal (EcM) shrubs are expanding across
the tundra. While we know how EcM host plants respond to warming and the associated …

Shrub abundance is expected to increase with enhanced temperature and nutrient
availability in the Arctic, and associated changes in abundance of ectomycorrhizal (EM) …

Climate warming is leading to shrub expansion in Arctic tundra. Shrubs form ectomycorrhizal
(ECM) associations with soil fungi that are central to ecosystem carbon balance as …

Arctic regions are experiencing the greatest rates of climate warming on the planet and
marked changes have already been observed in terrestrial arctic ecosystems. While most …

Many arctic ecological processes are regulated by soil temperature that is tightly
interconnected with snow cover distribution and persistence. Recently, various climate …

Vegetation changes in a warming Arctic may affect plant-associated soil microbial
communities with possible consequences for the biogeochemical cycling of carbon (C) and …

Root‐associated fungi (RAF) and root traits regulate plant acquisition of nitrogen (N), which
is limiting to growth in Arctic ecosystems. With anthropogenic warming, a new N source from …

As Arctic soils warm, thawed permafrost releases nitrogen (N) that could stimulate plant
productivity and thus offset soil carbon losses from tundra ecosystems. Although mycorrhizal …

Changing climate is expected to alter precipitation patterns in the Arctic, with consequences
for subsurface temperature and moisture conditions, community structure, and nutrient …

Climate warming is severely affecting high‐latitude regions. In the Arctic tundra, it may lead
to enhanced soil nutrient availability and interact with simultaneous changes in grazing …