about
Experiment, monitoring, and gradient methods used to infer climate change effects on plant communities yield consistent patternsHistorical ecology: using unconventional data sources to test for effects of global environmental change.Greater temperature sensitivity of plant phenology at colder sites: implications for convergence across northern latitudes.Different parts, different stories: climate sensitivity of growth is stronger in root collars vs. stems in tundra shrubs.Plant Biodiversity Change Across Scales During the Anthropocene.Multi-decadal changes in tundra environments and ecosystems: synthesis of the International Polar Year-Back to the Future project (IPY-BTF).Global assessment of experimental climate warming on tundra vegetation: heterogeneity over space and time.Global meta-analysis reveals no net change in local-scale plant biodiversity over time.Shrub canopies influence soil temperatures but not nutrient dynamics: An experimental test of tundra snow-shrub interactions.Expansion of canopy-forming willows over the twentieth century on Herschel Island, Yukon Territory, CanadaEstimates of local biodiversity change over time stand up to scrutiny.Trait covariance: the functional warp of plant diversity?A synthesis of methane emissions from 71 northern, temperate, and subtropical wetlands.Comment on "Precipitation drives global variation in natural selection".Uniform female-biased sex ratios in alpine willows.Shrub expansion in tundra ecosystems: dynamics, impacts and research prioritiesBioTIME: A database of biodiversity time series for the AnthropoceneBackground invertebrate herbivory on dwarf birch (Betula glandulosa-nana complex) increases with temperature and precipitation across the tundra biomeVegetation composition and shrub extent on the Yukon coast, Canada, are strongly linked to ice-wedge polygon degradationContrasting shrub species respond to early summer temperatures leading to correspondence of shrub growth patternsShrub growth and expansion in the Arctic tundra: an assessment of controlling factors using an evidence-based approachTemperature-induced recruitment pulses of Arctic dwarf shrub communitiesRecent dynamics of arctic and sub-arctic vegetationChanging climate sensitivity of black spruce (Picea mariana Mill.) in a peatland–forest landscape in Interior AlaskaTips for Effective Communication in EcologyWarming shortens flowering seasons of tundra plant communitiesPlant traits inform predictions of tundra responses to global changeVegetation monitoring using multispectral sensors - best practices and lessons learned from high latitudesSeed predation increases from the Arctic to the Equator and from high to low elevationsPublisher Correction to: Background invertebrate herbivory on dwarf birch (Betula glandulosa-nana complex) increases with temperature and precipitation across the tundra biomeShrub Line Advance in Alpine Tundra of the Kluane Region: Mechanisms of Expansion and Ecosystem ImpactsLocal snow melt and temperature—but not regional sea ice—explain variation in spring phenology in coastal Arctic tundraAuthor Correction: Warming shortens flowering seasons of tundra plant communitiesSeed predation increases from the Arctic to the Equator and from high to low elevationsComplexity revealed in the greening of the ArcticGlobal plant trait relationships extend to the climatic extremes of the tundra biomeThe geography of biodiversity change in marine and terrestrial assemblagesTRY plant trait database - enhanced coverage and open accessLandscape-scale forest loss as a catalyst of population and biodiversity change
P50
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P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Isla H Myers-Smith
@ast
Isla H Myers-Smith
@en
Isla H Myers-Smith
@es
Isla H Myers-Smith
@nl
Isla H Myers-Smith
@sl
type
label
Isla H Myers-Smith
@ast
Isla H Myers-Smith
@en
Isla H Myers-Smith
@es
Isla H Myers-Smith
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Isla H Myers-Smith
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prefLabel
Isla H Myers-Smith
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Isla H Myers-Smith
@en
Isla H Myers-Smith
@es
Isla H Myers-Smith
@nl
Isla H Myers-Smith
@sl
P1053
D-1529-2013
P106
P1153
6507057225
P31
P3829
P496
0000-0002-8417-6112