Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows

Abstract Climate change is shifting phenology globally, altering when and how species respond to environmental cues such as temperature and the timing of snowmelt. These shifts may result in phenological mismatches among interacting species, creating cascading effects on community and ecosystem dyna...

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Main Authors: J. Simone Durney, Arden Engel, Diane M. Debinski, Laura A. Burkle
Format: Article
Language:English
Published: Wiley 2022-08-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1002/ecs2.4198
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author J. Simone Durney
Arden Engel
Diane M. Debinski
Laura A. Burkle
author_facet J. Simone Durney
Arden Engel
Diane M. Debinski
Laura A. Burkle
author_sort J. Simone Durney
collection DOAJ
description Abstract Climate change is shifting phenology globally, altering when and how species respond to environmental cues such as temperature and the timing of snowmelt. These shifts may result in phenological mismatches among interacting species, creating cascading effects on community and ecosystem dynamics. Using passive warming structures and snow removal, we examined how experimentally increased temperatures, earlier spring snowmelt, and the poorly understood interaction between warming and earlier spring snowmelt affected flower onset, flowering duration, and maximum floral display of the spring‐flowering montane species, arrowleaf balsamroot (Balsamorhiza sagittata), over a 7‐year period. Additionally, potential cumulative effects of treatments were evaluated over the study duration. The combination of heating with snow removal led to earlier flower onset, extended flowering duration, and increased maximum floral display. While there was year‐to‐year variation in floral phenology, the effect of heating with snow removal on earlier onset and maximum floral display strengthened over time. This suggests that short‐term studies likely underestimate the potential for climate change to influence phenological plant traits. Overall, this research indicates that B. sagittata's flowering onset responded more strongly to snow removal than to heating, but the combination of heating with snow removal allowed plants to bloom earlier, longer, and more profusely, providing more pollinator resources in spring. If warming and early snowmelt cause similar responses in other plant species, these patterns could mitigate phenological mismatches with pollinators by providing a wider window of time for interaction and resiliency in the face of change. This example demonstrates that a detailed understanding of how spring‐flowering plants respond to specific aspects of predicted climatic scenarios will improve our understanding of the effects of climate change on native plant–pollinator interactions in montane ecosystems. Studies like this help elucidate the long‐term physiological effects of climate‐induced stressors on plant phenology in long‐lived forbs.
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spelling doaj.art-73758f786a084ffa83d9e08068eb09342022-12-22T03:07:49ZengWileyEcosphere2150-89252022-08-01138n/an/a10.1002/ecs2.4198Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadowsJ. Simone Durney0Arden Engel1Diane M. Debinski2Laura A. Burkle3Department of Ecology Montana State University Bozeman Montana USADepartment of Ecology Montana State University Bozeman Montana USADepartment of Ecology Montana State University Bozeman Montana USADepartment of Ecology Montana State University Bozeman Montana USAAbstract Climate change is shifting phenology globally, altering when and how species respond to environmental cues such as temperature and the timing of snowmelt. These shifts may result in phenological mismatches among interacting species, creating cascading effects on community and ecosystem dynamics. Using passive warming structures and snow removal, we examined how experimentally increased temperatures, earlier spring snowmelt, and the poorly understood interaction between warming and earlier spring snowmelt affected flower onset, flowering duration, and maximum floral display of the spring‐flowering montane species, arrowleaf balsamroot (Balsamorhiza sagittata), over a 7‐year period. Additionally, potential cumulative effects of treatments were evaluated over the study duration. The combination of heating with snow removal led to earlier flower onset, extended flowering duration, and increased maximum floral display. While there was year‐to‐year variation in floral phenology, the effect of heating with snow removal on earlier onset and maximum floral display strengthened over time. This suggests that short‐term studies likely underestimate the potential for climate change to influence phenological plant traits. Overall, this research indicates that B. sagittata's flowering onset responded more strongly to snow removal than to heating, but the combination of heating with snow removal allowed plants to bloom earlier, longer, and more profusely, providing more pollinator resources in spring. If warming and early snowmelt cause similar responses in other plant species, these patterns could mitigate phenological mismatches with pollinators by providing a wider window of time for interaction and resiliency in the face of change. This example demonstrates that a detailed understanding of how spring‐flowering plants respond to specific aspects of predicted climatic scenarios will improve our understanding of the effects of climate change on native plant–pollinator interactions in montane ecosystems. Studies like this help elucidate the long‐term physiological effects of climate‐induced stressors on plant phenology in long‐lived forbs.https://doi.org/10.1002/ecs2.4198arrowleaf balsamrootclimate changeflower durationflower onsetGreater Yellowstone Ecosystemmaximum floral display
spellingShingle J. Simone Durney
Arden Engel
Diane M. Debinski
Laura A. Burkle
Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
Ecosphere
arrowleaf balsamroot
climate change
flower duration
flower onset
Greater Yellowstone Ecosystem
maximum floral display
title Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
title_full Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
title_fullStr Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
title_full_unstemmed Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
title_short Earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
title_sort earlier spring snowmelt drives arrowleaf balsamroot phenology in montane meadows
topic arrowleaf balsamroot
climate change
flower duration
flower onset
Greater Yellowstone Ecosystem
maximum floral display
url https://doi.org/10.1002/ecs2.4198
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