The Importance of Incorporating Landscape Change for Predictions of Climate-Induced Plant Phenological Shifts
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The Importance of Incorporating Landscape Change for Predictions of Climate-Induced Plant Phenological Shifts. / Chisholm, Chelsea; Becker, Michael S.; Pollard, Wayne H.
In: Frontiers in Plant Science, Vol. 11, 759, 2020.Research output: Contribution to journal › Journal article › Research › peer-review
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TY - JOUR
T1 - The Importance of Incorporating Landscape Change for Predictions of Climate-Induced Plant Phenological Shifts
AU - Chisholm, Chelsea
AU - Becker, Michael S.
AU - Pollard, Wayne H.
PY - 2020
Y1 - 2020
N2 - Warming in the high Arctic is occurring at the fastest rate on the planet, raising concerns over how this global change driver will influence plant community composition, the timing of vegetation phenological events, and the wildlife that rely on them. In this region, as much as 50% of near-surface permafrost is composed of thermally sensitive ground ice that when melted produces substantial changes in topography and microbiome conditions. We take advantage of natural variations in permafrost melt to conduct a space-for-time study on Ellesmere Island in northern Canada. We demonstrate that phenological timing can be delayed in thermokarst areas when compared to stable ground, and that this change is a function of shifting species composition in these vegetation communities as well as delayed timing within species. These findings suggest that a warming climate could result in an overall broadening of blooming and leafing windows at the landscape level when these delayed timings are taken into consideration with the projected advance of phenological timings in ice-poor areas. We emphasize that the impacts of geomorphic processes on key phenological drivers are essential for enhancing our understanding of community response to climate warming in the high Arctic, with implications for ecosystem functioning and trophic interactions.
AB - Warming in the high Arctic is occurring at the fastest rate on the planet, raising concerns over how this global change driver will influence plant community composition, the timing of vegetation phenological events, and the wildlife that rely on them. In this region, as much as 50% of near-surface permafrost is composed of thermally sensitive ground ice that when melted produces substantial changes in topography and microbiome conditions. We take advantage of natural variations in permafrost melt to conduct a space-for-time study on Ellesmere Island in northern Canada. We demonstrate that phenological timing can be delayed in thermokarst areas when compared to stable ground, and that this change is a function of shifting species composition in these vegetation communities as well as delayed timing within species. These findings suggest that a warming climate could result in an overall broadening of blooming and leafing windows at the landscape level when these delayed timings are taken into consideration with the projected advance of phenological timings in ice-poor areas. We emphasize that the impacts of geomorphic processes on key phenological drivers are essential for enhancing our understanding of community response to climate warming in the high Arctic, with implications for ecosystem functioning and trophic interactions.
KW - leaf phenology
KW - flower phenology
KW - permafrost
KW - geomorphology
KW - ground stability
KW - Arctic
KW - plant ecology
KW - ICE-WEDGE DEGRADATION
KW - GROUND ICE
KW - TUNDRA PLANTS
KW - PERMAFROST
KW - RESPONSES
KW - PATTERNS
KW - MISMATCH
KW - GROWTH
KW - VOLUME
KW - ISLAND
U2 - 10.3389/fpls.2020.00759
DO - 10.3389/fpls.2020.00759
M3 - Journal article
C2 - 32670312
VL - 11
JO - Frontiers in Plant Science
JF - Frontiers in Plant Science
SN - 1664-462X
M1 - 759
ER -
ID: 248332459