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Differential responses of grass and a dwarf shrub to longāterm changes in soil m...
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Fast Responses of Root Dynamics to Increased Snow Deposition and Summer Air Temp...
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Inhibition of growth, and effects on nutrient uptake of arctic graminoids by lea...
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Environmental control and intersite variations of phenolics in Betula nana in tu...
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Environmental control and intersite variations of phenolics in Betula nana in tu...
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Environmental control and intersite varations of phenolics in Betula nana in tun...
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Soil microarthropods are only weakly impacted after 13 years of repeated drought...
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Changes in the onset of spring growth in shrubland species in response to experi...
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Changes in the onset of spring growth in shrubland species in response to experi...
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Changes in the onset of spring growth in shrubland species in response to experi...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Global negative vegetation feedback to climate warming responses of leaf litter...
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Related Subjects
Arctic
boreal
dissolved organic carbon
particulate organic carbon
permafrost carbon
wildfire
Ecology, Evolution, Behavior and Systematics
Ecology
Soil Science
[SDE.BE]Environmental Sciences/Biodiversity and Ecology
coastal erosion Supplementary material for this article is available
Agricultural and Biological Sciences (miscellaneous)
coastal erosion
ARCTIC TUNDRA
Global warming
Meta-analysis
Nitrogen mineralization
Plant Science
Plant productivity
Soil respiration
Arctic-alpine ecosystems
BOREAL FOREST
CLIMATE-CHANGE
ECOSYSTEMS
FIRE
INTERIOR ALASKA
NITROGEN DEPOSITION
SEQUESTRATION
STORAGE
VULNERABILITY
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