Results 21 to 30 of about 507 (166)
Patterns of free amino acids in tundra soils reflect mycorrhizal type, shrubification, and warming. [PDF]
AbstractThe soil nitrogen (N) cycle in cold terrestrial ecosystems is slow and organically bound N is an important source of N for plants in these ecosystems. Many plant species can take up free amino acids from these infertile soils, either directly or indirectly via their mycorrhizal fungi. We hypothesized that plant community changes and local plant
Andresen LC +9 more
europepmc +6 more sources
Permafrost is warming globally and the extent of this warming is locally variable in space and time due to an array of factors. In the Arctic, vegetation is one of these factors, whichever influenced by climate change is undergoing a transformation through an increase in height and extent of shrubs on the tundra.
Haagmans, Vincent J.T. +1 more
openaire +2 more sources
Terrestrial Arthropod Responses to Arctic Cryosphere Degradation. [PDF]
Changes in Arctic snow and ice are impacting terrestrial arthropods—for example, thinner snowpacks alter phenological synchrony and soil fauna survival; thawing permafrost increases decomposition, and glacial ice loss leads to the disappearance of adapted specialists; sea ice decline will have many indirect impacts for arthropods.
Gillespie MAK, Høye TT.
europepmc +2 more sources
Simulated rhizosphere deposits induce microbial N‐mining that may accelerate shrubification in the subarctic [PDF]
AbstractClimate change is exposing high‐latitude systems to warming and a shift towards more shrub‐dominated plant communities, resulting in increased leaf‐litter inputs at the soil surface, and more labile root‐derived organic matter (OM) input in the soil profile.
Lettice C. Hicks +4 more
openaire +4 more sources
Implications of alder shrub growth for alpine tundra soil properties in Interior Alaska
The increase in deciduous shrub growth in response to climate change throughout the Arctic tundra has uncertain implications, in part due to a lack of field observations.
Allison M. Welch +8 more
doaj +1 more source
Shrubification of peatlands [PDF]
Biogeography Soil is a key player in the global carbon cycle. Peatlands are important because they contain more than half of global soil carbon, much of which is sequestered in slow-decaying Sphagnum moss. Hence, there is a need to understand how peatlands will respond to the rapidly changing climate. Malhotra et al.
openaire +1 more source
Global warming leads to drastic changes in the diversity and structure of Arctic plant communities. Studies of functional diversity within the Arctic tundra biome have improved our understanding of plant responses to warming. However, these studies still
Ruud Scharn +8 more
doaj +1 more source
Plant growth and distribution in high-latitude tundra ecosystems is strongly limited by nutrient availability and is critical for quantifying centennial-scale carbon-climate interactions. However, land model representations of plant–nutrient interactions
William J Riley +5 more
doaj +1 more source
Rapid Ecosystem Change at the Southern Limit of the Canadian Arctic, Torngat Mountains National Park
Northern protected areas guard against habitat and species loss but are themselves highly vulnerable to environmental change due to their fixed spatial boundaries.
Emma L. Davis +4 more
doaj +1 more source
Vegetation is responding to climate change, which is especially prominent in the Arctic. Vegetation change is manifest in different ways and varies regionally, depending on the characteristics of the investigated area.
Iuliia Shevtsova +7 more
doaj +1 more source

